European hydrotoponymy (IV): tug of war between Balto-Slavic and West Uralic

germanic-balto-slavic-expansion

In his recent paper on Late Proto-Indo-European migrations, when citing Udolph to support his model, Frederik Kortlandt failed to mention that the Old European hydrotoponymy in northern Central-East Europe evolved into Baltic and Slavic layers, and both take part in some Northern European (i.e. Germanic – Balto-Slavic) commonalities.

Proto-Slavic

From Expansion slavischer Stämme aus namenkundlicher und bodenkundlicher sicht, by Udolph, Onomastica (2016), translated into English (emphasis mine):

NOTE. An archived version is available here. The DOI references for Onomastica do not work.

(…) there is a clear center of Slavic names in the area north of the Carpathians. Among them are root words of the Slavic languages such as reka / rzeka, potok u. a. m.

Even more important than this mapping is the question of how the dispersion of ancient Slavic names happened. What is meant by ancient Slavic names? I elaborated on this in this journal years ago (Udolph, 1997):

(1)Ancient suffixes that are no longer productive today.

This clearly includes Slavic *-(j)ava as in Vir-ava, Vod-ava, Il-ava, Glin-iawa, Breg-ava, Ljut-ava, Mor-ava, Orl-java among others. It has clear links to the ancient common Indo-European language (Lupawa, Morava-March-Moravia, Orava, Widawa). They have a center north of the Carpathians.

ava-slavic

(2) Unproductive appellatives (water words), which have disappeared from the language, are certain witnesses of ancient Slavic settlements. A nice example of this is Ukr. bahno, Pol. bagno ‘swamp, bog, morass’ etc. The word has long been missing in South Slavic, although it appears in South Slavic names, but only in very specific areas (see Udolph, 1979, pp. 324-336).

(3) Names that go back to different sound shifts. [Examples:]

  • (…) the Slavic clan around Old Sorbian brna ‘feces, earth’, Bulgarian OCS brьnije ‘feces, loam’, OCS brъna ‘feces’, Slovenian brn, ‘river mud’, etc. is solved with the inclusion of onomastic materials (Udolph, 1979, p. 499-514). (…) Toponymic mapping shows important details.
  • bryn-slavic
    Karte 4. brъn < *brŭn und bryn- < *brūn- in slavischen Namen
  • (…)We also have an ablauting *krŭn-:*krūn- in front of us. Map 5 shows the distribution of both variants in Slavic names.
  • The next case is quite similar. It concerns Russ. appellative grjaz’ ‘dirt, feces, mud’, (…) for which an Old Slavic form *gręz exists. Slavic also knows the ablauting variant *grǫz.

    These maps (see Map 6, p. 222) show that a homeland of Slavic tribes can only be inferred north of the Carpathians.

    (4) Place-names formed by Slavic suffixes of Pre-Slavic nature, i.e. derived from Old European hydronyms.

    (a) The largest river in Poland, the Wisła, German Vistula, bears a clearly Pre-Slavic name, no matter how one explains it (Babik, 2001, pp. 311-315; Bijak, 2013, p. 34, Udolph, 1990 , Pp. 303-311).

    (b) With the same suffix are formed Sanok, place on the southwest of Przemyśl; Sanoka, a no longer known waters name, 1448 as fluvium Szanoka, near the place Sanoka and with a diminutive suffix -ok- a tributary of the Sanok, which is called Sanoczek (for details see Udolph, 1990, pp. 264-270; Rymut / Majtan, 1998, p. 222). The San also has a single-language name, but that does not change anything about the right etymology. The suffix variant -očь also includes Liwocz and Liwoczka, river names near Cracow; also a mountain range of the Beskydy is mentioned at Długosz as Lywocz.

    According to the opinion of the “Słownik prasłowiański” (Sławski (red.), 1974, p. 92), the suffix -ok- represents a Proto-Slavic archaism. It appears, for example, in sъvědokъ, snubokъ, vidokъ, edok, igrok, inok among others, but its antiquity also shows, among other things, that it started at archaic athematic tribes.

    east-slavic-language-expansion
    Mapping of older and younger East Slavic place-names and translation into settlement evolution.

    Slavonic Urheimat

    If we apply this to the loess distribution in western Ukraine and south-eastern Poland, it is very noticeable that the center of the Old Slavic place names lies in the area where loess dispersal is gradually “frayed out”, i.e. for example, in the area west of Kiev between Krakow in the west and Winnycja and Moldavia in the east. In short, the distribution of good soils coincides with ancient Slavic names. If that is correct, we can expect a homeland in the Pre-Carpathian region, or better, a core landscape of Slavic settlement.

    The existence of Pre-Slavic Indo-European place names and water names whose structure indicates that they originated from an Indo-European basis, but then also developed Slavic peculiarities, can now – as stated above – only be understood to mean that the language group that we call today Slavic emerged in a century-long process from an Indo-European dialectal area.

    Loess areas between Poland and Ukraine. Image from Jary et al. (2018).

    From a genetic point of view, the scarce data published to date show a clear shift of central-east populations from more Corded Ware-like groups in the EBA towards more BBC-derived ancestry in the common era, to the point where ancient DNA samples from East Germany, Poland and Lithuania evolve from clustering between Corded Ware and Sub-Neolithic peoples to clustering close to Bell Beaker-derived groups, such as West Germanic peoples, Tollense samples, etc. (see below)

    Furthermore, sampled Early Slavs show bottlenecks under “Dinaric” I2a-L621 and central-eastern E1b-V13, which – in combination with the known phylogeography of Únětice and Urnfield – is compatible with its late expansion from a central-east European Slavonic homeland, such as the Pomeranian culture, in turn likely derived from Lusatian culture groups.

    This doesn’t preclude a more immediate expansion of Common Slavic in Antiquity closer to the northern Carpathians, which is also supported by the available Early Slavic sampling, apart from samples from the Avar and Hungarian polities.

    pca-balto-slavic-iron-age
    Likely Baltic (yellow-green) and Slavic (orange) groups ca. 500 AD on, with Finnic (cyan) and Mordvinic (blue) groups roughly divided through hydrotoponymy line ca. 1000 AD Top Left: Late Iron Age cultures. Top right: PCA of groups from the Iron Age to the Middle Ages. Y-DNA haplogroups during the Germanic migrations (Bottom left) and during the Middle Ages (Bottom right). Notice a majority non-R1a lineages among sampled Early Slavs. See full maps and PCAs.

    Proto-Baltic / Proto-Slavic

    Northern European hydronymy

    From Alteuropäische Hydronymie und urslavische Gewässernamen, by Udolph, Onomastica (1997), translated into English (emphasis mine):

    NOTE. An HTML version is available at Jurgen Udolph’s personal site.

    Because of the already striking similarities as the well-known “-m-case”, the number-words for ‘1000’, ’11’ and ’12’ and so on, J. Grimm had already assumed a close relationship between Germanic and Baltic and Slavic. (…)

    In my own search, I approached this trinity from the nomenclature side. In doing so, I noticed some name groups that can speak for a certain common context:

    1.* bhelgh-, *bholgh-.

    Map 10, p. 64, shows that a root * bhelgh- occurs in the name material of a region from which later Germanic, Baltic and Slavic originated. The Balkans play no role in this.

    bholgh-germanic-balto-slavic

    2. *dhelbh-, *dholbh-, *dhl̥bh-

    The proof of the three ablauting * dhelbh, * dholbh, * dhl̥bh- within a limited area shows the close relationship that this root has with the Indo-European basis. Again it is significant in which area the names meet (…)

    dhelbh-germanic-balto-slavic

    3. An Indo-European root extension *per-s- with the meaning ‘spray, splash, dust, drop’ is detectable in several languages (…). From a Baltic-Slavic-Germanic peculiarity cannot therefore be spoken from the toponymic point of view. The picture changes, however, if one includes the derived water names.

    4. The root extension *pel-t-, *pol-t-, *pl̥-t- of a tribe widely spread in the Indo-European languages around *pel-, pol- ‘pour, flow, etc.’, whose reflexes are found Armenian through Baltic and Slavic to the Celtic area, is found in the Baltic toponymy, cf. Latv. palts, palte ‘puddle, pool’.

    trzciniec-riesenbecher-culture
    The dynamics of stylistic changes of the form of the “Trzciniec pot” in the lowland regions of Central Europe, and spreading routes of the Trzciniec package in Central Europe. A good proxy for contacts through the Northern European Plain during the Early Bronze Age. Modified from Czebreszuk (1998).

    Early Balto-Finnic

    In order to properly delimit (geographically and chonologically) the Proto-Baltic and Proto-Slavic expansions, it is necessary to understand where the late Balto-Finnic homeland was located during the Bronze Age. The following are excerpts from the comprehensive hydrotoponymic study by Pauli Rahkonen (2013):

    In any case, Finnic probably had its origin somewhere around the Gulf of Finland. Names of large and central rivers such as Vuoksi (< Finnic vuo ‘stream’) and Neva (< Finnic neva ‘marsh, river’) must be very old and might represent Proto-Finnic hydronyms. In the southern coastal area of Finland, the names Kymi and Nietoo < *Niet|oja (id. later Porvoonjoki) may also be of Finnic origin and derive from, respectively, kymi ‘stream’ (see SSA I s.v. *kymi; see however SPK s.v. Kemijärvi; Rahkonen 2013: 24) and nieto(s) ‘heap of snow’ (SSA II s.v. nietos), in hydronyms probably ‘high (snowy?) banks of a river’. Mustion|joki is clearly a Finnish name < *must|oja ‘black river’. The river name Vantaa remains somewhat obscure, although Nissilä (see SPK s.v. Vantaanjoki) has derived it from the Finnic word vana ‘water route’. In western Finland the names of large rivers, such as Aura and Eura, are supposedly of Germanic origin (Koivulehto 1987).

    In Estonia the names of many of the most important rivers might be of Finnic origin: e.g. Ema|jõgi Est. ema ‘mother’ [Tartu district] (?? cf. the Lake Piiga|ndi < Est. piiga ‘maiden’), Pärnu [Pärnu district] < Est. pärn ‘linden’, Valge|jõgi [Loksa district] < Est. valge ‘white’, Must|jõgi [Võru district] < Est. must ‘black’. It is possible that Emajogi and especially Piigandi are the result of later folk etymologizing of a name with some unknown origin. However, as a naming motif there exist in Finland numerous toponyms with the stems Finnic *emä (e.g. 3 Emäjoki), *neit(V)- ‘maiden’ (e.g. Neitijärvi, Neittävänjoki, Neittävänjärvi) and Saami stems that can be derived from Proto Saami *nejte̮ ‘id’ (GT2000; NA).

    finnic-toponyms
    The historical southern boundary of Finnic hydronyms, excluding hydronyms produced by the Karelian refugees of the 17th century.

    These seemingly very old names of relatively large rivers in southern Finland, modern Leningrad oblast and Estonia support the hypothesis that Proto-Finnic was spoken for a long time on both sides of the Gulf of Finland and it thus basically corresponds to the hypothesis of Terho Itkonen (see below). In the Novgorod, Tver or Vologda oblasts of Russia, Finnic names for large rivers cannot be found (Rahkonen 2011: 229). For this reason, it is likely that the Late Proto-Finnic homeland was the area around the Gulf of Finland.

    Beyond the southeastern boundary of the modern or historically known Finnic-speaking area, there exists a toponymic layer belonging to the supposedly non-Finnic Novgorodian Čudes (see Rahkonen 2011). In theory it is possible that Proto-Finnic and Proto-Čudian separated from each other at an early stage or it is even possible that Proto-Čudian was identical with Proto-Finnic. However, this cannot be proven, because there is not enough material available describing what Novgorodian Čudic was like exactly.

    finno-saamic-mordvin
    Yakhr-, -khra, yedr-, -dra and yer-/yar, -er(o), -or(o) names of lakes in Central and North Russia and the possible boundary of the proto-language words *jäkra/ä and *järka/ä. Rahkonen (2013)

    A summary of the data is then:

    • The Daugava River and the Gulf of Livonia formed the most stable south-western Balto-Finnic border (up until ca. 1000 AD): the Daugava shows a likely Indo-European etymology, while some of its tributaries are best explained as derived from Uralic.
    • The first layer of “Early Baltic” loans in Early Balto-Finnic are of a non-attested Baltic dialect closest to Proto-Balto-Slavic (read more about this early layer).
    • The latest samples of the Trzciniec culture (or derived Iron Age group) from its easternmost group in Turlojiškė (ca. 1000-800 BC?) show a western shift towards Bell Beaker, although they show a majority of hg. R1a-Z280; while the earliest sample from Gustorzyn (ca. 1900 BC), likely from Trzciniec/Iwno, from the westernmost area of the culture, shows a Corded Ware-like ancestry (and hg. R1a-Z280, likely S24902+) among a BA sampling from Poland clearly derived from Bell Beaker groups.

    One can therefore infer that the expansion of the Trzciniec culture – as the earliest expansion of central-west European peoples into the Baltic after the Bell Beaker period – represented either the whole disintegrating Balto-Slavic community, or at least an Early Baltic-speaking community expanding from the West Baltic area to the east.

    The similarity of Early Slavs and the Trzciniec outlier with the Czech BA cluster, formed by samples from Bohemia (ca. 2200–1700 BC), and the varied haplogroups found among Early Slavs – reminiscent of the variability of the Unetice/Urnfield sampling – may help tentatively connect the early Proto-Slavic homeland more strongly with a Proto-Lusatian community immediately to the south-west of the Iwno/Proto-Trzciniec core.

    pca-late-bronze-age-balto-slavic-finnic
    Top Left:Likely Baltic, Slavic, and Balto-Finnic-speaking territories (asynchronous), overlaid over Late Bronze Age cultures. Balto-Slavic in green: West(-East?) Baltic (B1), unattested early Baltic (B2), and Slavic (S). Late Balto-Finnic (F) in cyan. In red, Tollense and Turlojiškė sampling. Dashed black line: Balto-Slavic/West Uralic hydrotoponymy border until ca. 1000 AD. Top right: PCA of groups from the Early Bronze Age to the Late Bronze Age. Marked are Iwno/Pre-Trzciniec of Gustorzyn (see below), Late Trzciniec/Iron Age samples from Turlojiškė, and in dashed line approximate extent of Tollense cluster; Y-DNA haplogroups during the Late Bronze Age (Bottom left) and during the Early Iron Age (Bottom right). Notice a majority non-R1a lineages among sampled Early Slavs. See full maps and PCAs.

    Proto-Balto-Slavic homeland

    Disconnected western border: Germanic

    The common Balto-Slavic – Germanic community must necessarily be traced back to the West Baltic. From Udolph’s Namenkundliche Studien zum Germanenproblem, de Gruyter (1994), translated from German (emphasis mine):

    My work [Namenkundliche Studien zum Germanenproblem] has shown how strong the Germanic toponymy is related to the East, less to Slavic, much more to Baltic. It confirms the recent thesis by W.P. Schmid on the special relationship Germanic and Baltic, according to which “the formation of the typical Germanic linguistic characteristics…must have taken place in the neighborhood of Baltic“.

    If one starts from a Germanic core area whose eastern boundary is to be set on the middle Elbe between the Erzgebirge and Altmark, there are little more than 400 km. to the undoubtedly Baltic settlement area east of the Vistula. Stretching the Baltic area westwards over the Vistula (as far as the much-cited Persante), the distance is reduced to less than 300 km. Assuming further that Indo-European tribes between the developing Germanic and the Baltic groups represent the connection between the two language groups, so can one understand well the special relationship proposed by W.P. Schmid between Germanic and Baltic. In an earlier period shared Slavic evidently the same similarities (Baltic-Slavic-Germanic peculiarities).

    balto-slavic-balto-finnic-homeland
    Top: Palaeo-Germanic (G2, blue area), Proto-Balto-Slavic/Pre-Baltic (PBSL, green area) and Early Proto-Balto-Finnic (PBF, cyan area) homelands superimposed over Early Bronze Age cultures. Persante hydronym and Gustorzyn ancient DNA sample location marked. Y-DNA haplogroups during the Early Bronze Age (Bottom left) and during the Middle Bronze Age (Bottom right). Notice a mix of R1b-L151 samples from the west and the process of integration of R1a-Z645 lineages from the the north-east. See full maps and PCAs.

    Substrate and immediate eastern border: Early Balto-Finnic

    While Balto-Finnic shows a late Balto-Slavic adstrate, Balto-Slavic has a Balto-Finnic(-like) substrate, also found later in Baltic and Slavic, which implies that Balto-Slavic (and later Baltic and Slavic) replaced the language of peoples who spoke Balto-Finnic(-like) languages, influencing at the same time the language of neighbouring peoples, who still spoke Balto-Finnic (or were directly connected to the Balto-Finnic community).

    For more on this relative chronology in Balto-Slavic – Balto-Finnic contacts, see e.g. the recent posts on Kallio (2003), Olander (2019), or a summary of this substrate.

    While Rahkonen (2013) entertains Parpola’s theory of a West-Uralic-speaking Netted Ware area (ca. 1900-500 BC), due to the Uralic-like hydrotoponymy of its territory, he also supports Itkonen’s idea of the ancient presence of almost exclusively Balto-Finnic place and river names in the Eastern Baltic and the Gulf of Finland since at least the Corded Ware period, due to the lack of Indo-European layers there:

    NOTE. This idea was also recently repeated by Kallio (2015), who can’t find a non-Uralic layer of hydrotoponymy in Balto-Finnic-speaking areas.

    It should be observed that the territory between the historical Finnic and Mordvin-speaking areas matches quite well with the area of the so-called Textile Ceramics [circa 1900–800 BC] (cf. Parpola 2012: 288). The culture of Textile Ceramics could function as a bridge between these two extreme points. Languages that were spoken later in this vast territory between Finland–Estonia and Mordovia seem to derive from Western Uralic (WU) as well. I have called those languages Meryan-Muroma, Eastern and Western Čudian and an unknown “x” language spoken in inland Finland, Karelia and the Lake Region of the Russian North (Rahkonen 2011; 241; 2012a: 19–27; 2013: 5– 43). This might mean that the territory of the Early Textile Ceramics reflects to some extent the area of late Western Uralic.

    The archaeologically problematic area is Estonia, Livonia and Coastal Finland – the area traditionally assumed to have been populated by the late Proto-Finns. The Textile Ceramics culture was absent there. It is very difficult to believe that the Textile Ware population in inland Finland migrated or was even the main factor bringing the Pre- or Early Proto-Finnic language to Estonia or Livonia. There are no archaeological or toponymic signs of it. Therefore, I am forced to believe that Textile Ceramics did not bring Uralic-speaking people to those regions. This makes it possible, but not absolutely proven, to assume that some type of Uralic language was spoken in the region of the Gulf of Finland already before Textile Ceramics spread to the northwest (circa 1900 BC).

    corded-ware-west-uralic
    Top Left: Corded Ware culture expansion. Top right: PCA of Corded Ware and Sub-Neolithic groups. Y-DNA haplogroups during the Corded Ware expansion (Bottom left) and during the subsequent Bell Beaker expansion (Bottom right). Notice the rapid population replacement of typical Corded Ware R1a-Z645 lineages by expanding Bell Beakers of hg. R1b-L23 in central-east Europe, while they show continuity in the described ancestral Fennoscandian West-Uralic-speaking territory. See full maps and PCAs.

    The Corded Ware population in Finland is thought to have been NW Indo-European by many scholars (e.g. Koivulehto 2006: 154–155; Carpelan & Parpola 2001: 84). At least, it is probable that the Corded Ware culture was brought to Finland by waves of migration, because the representatives of the former Late Comb Ceramics partially lived at the same time side by side with the Corded Ware population. However, it is possible that the immigrants were a population that spoke Proto-Uralic, who had adopted the Corded Ware culture from their Indo-European neighbors, possibly from the population of the Fatjanovo culture, e.g. in the Valdai region. This was suggested by Terho Itkonen (1997: 251) as well. In that case the population of the Typical and Late Comb Ceramics may have spoken some Paleo European language (see Saarikivi 2004a). In the Early Bronze Age, the Baltic Pre-Finnic language that I have suggested must have been very close to late WU and therefore no substantial linguistic differences existed between the Baltic Pre-Finns and the population of Textile Ceramics in inland Finland. I admit that this model is difficult to prove, but I have presented it primarily in order to offer new models of thinking.16 At least, there is no archaeological or linguistic reason against this idea.

    This dubitative attribution of Proto-Uralic to the expansion of Corded Ware groups in eastern Europe, which is what hydrotoponymic data suggests in combination with archaeology, has to be understood as a consequence of how striking Rahkonen finds the results of his research, despite Itkonen’s previous proposal, in the context of an overwhelming majority of Indo-Europeanists who, until very recently, simplistically associated Corded Ware with the Indo-European expansion.

    Conclusion

    Even Kortlandt accepts at this point the identification of expanding East Bell Beakers from the Carpathian Basin as those who left the Alteuropäische layer reaching up to the Baltic. However, he identified Udolph’s data solely with West Indo-European, forgetting to mention the commonly agreed upon western Proto-Balto-Slavic homeland, most likely because it contradicts two of his main tenets:

    1. that Balto-Slavic split from a hypothetical Indo-Slavonic (i.e. Satem) group expanding from the east; and
    2. that laryngeals can be reconstructed for Balto-Slavic – unlike for North-West Indo-European.
    old-european-asian-hydro-toponymy
    Indo-European hydrotoponymy in Europe and the Middle East (scarce Central Asian data). Baltic data compensated, statistical method RBF: intermediate regions devoid of Indo-European toponyms are inferred to have them; it compensates thus e.g. for the scarce Indo-European hydrotoponyms in Poland by assuming ‘soft’ continuity from West Germany to the Baltic.

    A hypothetic “Pre-Indo-Slavonic” laryngeal Indo-European layer reaching Fennoscandia and the Forest Zone with Corded Ware is fully at odds with all known data:

    • in comparative grammar, since the one feature that characterizes Graeco-Aryan is precisely its set of innovations relative to Northern Indo-European, which presupposes a longer contact (and further laryngeal loss) once Tocharian and North-West Indo-European had separated – hence probably represented by Palaeo-BalkanCatacomb-Poltavka contacts once Afanasevo and Yamna settlers from the Carpathian Basin / East Bell Beakers had become isolated;
    • in hydrotoponymy, because of the prehistoric linguistic areas that can be inferred from (1) the distribution of Old European hydrotoponymy; (2) Udolph’s work on Germanic and the likely non-Indo-European substrate in Scandinavia and land contacts with Balto-Finnic; (3) from the Northern European traits in the Northern European Plain; or (4) from the decreasing proportion of Indo-European place and river names from central Europe towards the east and north.
    • NOTE. An alternative explanation of Old European/Balto-Slavic layers, e.g. by a ‘Centum’ Temematic – even if one obviates the general academic rejection to Holzer’s proposal – couldn’t account for the absolute lack of an ancestral layer of Indo-European hydrotoponymy in North-Eastern Europe (i.e. the longest-lasting Corded Ware territory), in sharp contrast with Western Europe, South-Eastern Europe, and South Asia. All of that contradicts an Eastern Indo-European community, even without a need to recall that the oldest hydrotoponymic layers common to Fennoscandia and the Forest Zone are of Uralic nature.

    • in archaeology, because cultural expansions of the Eastern European Early Bronze Age province since the Bell Beaker period (viz. Mierzanowice, Trzciniec, Lusatian, Pomeranian, West Baltic Culture of Cairns) suggest once and again west-east movements, most (if not all) of which – based on the presence of Indo-European speakers during the common era – were likely associated with Indo-European-speaking communities replacing or displacing previous ones.
    • in palaeogenomics, because of the late and different association of Corded Ware ancestry and haplogroups among Balto-Slavic and Indo-Iranian communities, in turn corresponding to the different satemization processes found in both dialects, which may have actually been related to the Uralic substrate that is found in both (read more on Uralic influences on Balto-Slavic and on Indo-Iranian).

    On the other hand, a careful combination of Uralic and Indo-European comparative grammar, hydrotoponymic data, and population genomics fits perfectly well Itkonen’s and Rahkonen’s association of Corded Ware in Eastern Europe with Uralic languages, as well as the traditional mainstream view of Uralic before Indo-European in Fennoscandia and in the Forest Zone, as I explained in a recent post about genetic continuity in the East Baltic area.

    Population genomics is not the main reason to reject the Indo-European Corded Ware theory – or any other prehistoric ethnolinguistic identification, for that matter. It can’t be. This new field offers just the occasional confirmation of a well-founded theory or, alternatively, another nail in the coffin of fringe theories that were actually never that likely, but seemed impossible to fully dismiss on purely theoretical grounds.

    The problem with Corded Ware was that we couldn’t see how unlikely its association with Indo-European languages was until we had ancient DNA to corroborate archaeological models, because few (if any) Indo-Europeanists really cared about the linguistic prehistory of eastern and northern Europe, or about Uralic languages in general (contrary to the general trend among Uralicists to be well-versed in Indo-European studies). Now they will.

    Related

    European hydrotoponymy (III): from Old European to Palaeo-Germanic and the Nordwestblock

    nordic-bronze-age-cultures

    The study of hydrotoponymy shows a prevalent initial Old European layer in central and northern Germany, too, similar to the case in Iberia, France, Italy, and the British Isles.

    The recent paper on Late Proto-Indo-European migrations by Frederik Kortlandt relies precisely on this ancestral layer as described by Jürgen Udolph to support a Danubian expansion of North-West Indo-European with East Bell Beakers, identified as the Alteuropäische (Old European) layer that was succeeded by Germanic in the North European Plain.

    The Proto-Germanic homeland

    The following are excerpts are translated from the German original (emphasis mine) in Udolph’s Namenkundliche Studien zum Germanenproblem, de Gruyter (1994):

    udolph-namenkunde
    Buy the book at De Gruyter’s site or at Amazon.

    The following is a concise compilation of the investigation into nine points, which will be subsequently discussed: there are Brink (in the north brekk-), -by (on the Elbe), the name of the Elbe itself, germ, haugaz and blaiw, klint, malm / melm, the name of the Rhön, and the place name element -wedel.

    I want to briefly summarize the results:

    1. Brink has toponymically a clear focus in Germany between the Rhine and the Weser; in Schleswig-Holstein and Denmark it is almost completely missing, the Scandinavian place name documents show an accumulation in eastern Sweden. The English Brink names can not be associated with the Scandinavian ones. The “real” Scandinavian variant brekka, brekke, however, also appear on the Shetland and Orkney Islands and in central England.

    2. The Central Elbian –by-place names have nothing to do with the Danish and Scandinavian -by-names.

    3. The name of the Elbe has been carried from south to north and has become an appellative in Scandinavia. This clearly proves that a south-north migration has taken place.

    4. The distribution of haugaz does not support a Nordic origin of the word. K. Bischoff in his thorough investigation never asked whether the reverse path from south to north would be possible. However, in comparison with the results of the study of other toponyms, this second option will be much more likely to be accepted. On the “problem of the gap” in the distribution (between Aller and northern Holstein) see page 910.

    hlaiwaz-germanisch

    5. Completely missing is the assumption of Nordic origin in the case of hlaiwaz. A look at Map 67 shows this clearly.

    6. Even in the case of klint, Denmark and Scandinavia are only marginally involved in the distribution of names. This contradicts the thesis that the English Klint names are of Nordic origin. On the other hand, Map 68 (Klit- / Klett-) shows how Nordic place names can have an influence on the British Isles.

    klint-germanisch

    7. Even in the case of germ, melm (ablauting malm, mulm), everything speaks for a continental Germanic starting point: here are all ablaut stages in the appellative vocabulary and in the toponymy, which shows together with the name Melmer perhaps the most ancient -r-derivations, which are unknown to the Nordic area, while the Nordic names, in turn, have a distinct tendency to spread to eastern Sweden, towards the Baltic Sea.

    8. The name of the Rhön can only be interpreted with the aid of the Nord Germanic apellative hraun “boulder field, stony ground, lava field”. This does not mean that Nord Germanic peoples have given this name, but that the Common or Proto-Germanic peoples knew the appelative still. The Rhön owes its name to this language stage.

    9. The spread of the fronds names in Germany, classified by E. Schröder as “North Germanic invasion”, can be explained differently: more important than the often younger names north of the Elbe in Schleswig-Holstein (type Wedelboek) are the place names near Braunschweig, Büren (Westphalia), and in the Netherlands, in which case a south-north spread is more convincing than the assumption of a Nordic expansion.

    wedel-germanisch

    If you take the similar distribution maps 15 (wik), 31 (fenn), 36 (slk), 39 (büttel), 47 (live), 49 (quem), 50 (thing), 61 (brink) and 66 (haugaz) It can be seen from this (page 72, page 908) that there are parts of Germany which, to a lesser degree, are more heavily involved than others in Old Germanic place name formations: that applies to southern Thuringia, the Area between Werra and Fulda, the Magdeburger Börde and its western foothills to the Weser at the Porta Westfalica). On the other hand, the areas north of the Aller, Hanoverian Wendland and wide areas between the Lower Weser and the Lower Elbe (apart from the area around Osterholz-Scharmbeck as well as Kehdingen and Hadeln) are little and hardly affected.

    There is no question that the reasons for the different dispersion can not lie in the name itself, but have other causes. H. Kuhn has considered the natural conditions of the landscape with the fronds. Comparing the place name expansion outlined here with a bog map of Lower Saxony, as found in numerous publications (Map 73, page 910), solves the problems: even today’s bog distribution of Lower Saxony, diminished through cultivation and drainage (albeit still considerable), reflects the fact that the early colonization and naming of northern Germany has been shaped and, to a certain extent, controlled by settler-friendly and not-settler-friendly conditions.

    moorkarte-deutschland
    Distribution of bogs in Germany. Source: M. Sommer, Institut für Bodenlandschaftsforschung, ZALF, Müncheberg.

    On the location of the Germanic Urheimat

    According to the space briefly outlined by the present study, the Old Germanic settlement area in toponymic terms is roughly to be located between the Erzgebirge, Thüringerwald, Elbe, Aller and an open border in Westphalia, for the following reasons:

    • High proportion of old European names. This is a basic requirement, which of course is also fulfilled by other areas, but not by Schleswig-Holstein, Denmark and Scandinavia. (…)
    • Of particular importance was the discussion about relations with the north (the generally accepted ancient Germanic settlement area, section L, p. 830-917). I believe that the detailed study of the geographical names no longer allows one to assume a Scandinavian homeland of Germanic tribes. Too many arguments speak against it. It is much more likely to start with a northward migration (…).
    bell-beaker-germanic
    Bell Beaker expansion ca. 2600-2200 BC. Top Left: Tentative location of the Pre-Proto-Germanic homeland (earliest stage), in the North European Plain between the Elbe and the the Aller (open border). Top right: PCA of the Bell Beaker period, with Netherlands EBA cluster (population west of the Germanic Urheimat) in red, and Battle Axe/Baltic CWC (population east and north of the Urheimat) in cyan. Bottom left: ADMIXTURE analysis of ancient DNA samples. Bottom right: Y-DNA haplogroup map. See full maps and PCAs.

    Western border: Nordwestblock

    Recently, W. Meid has once more dealt in detail with Kuhn’s thesis. After that, the most important criteria for the approach of this thesis are the following:

    1. -p- (and other shutter sounds) are partly not shifted in North German names;
    2. the existence of a -sí-suffix;
    3. -apa in river names;
    4. the suffix -andr-;
    5. certain words u. Name strains, e.g. Veneter, Belgian.
    6. Above-average relations of the northwestern block to Italic (Latin, Osco-Umbrian).

    W. Meid agrees with Kuhn’s theses, but with limitations: “These evidences seem to indicate that the NW-space did not belong to the original settlement area of ​​the Teutons, but that the Germanization of this area or larger parts of it did not take place until relatively late, namely – as Kuhn thinks – after the Germanic sound shift or during its last phase. According to Kuhn’s own words this “space… appears as a block that has long defied Germanization”.

    Udolph continues explaining why most of these non-Germanic examples are “optic illusions”, since he can explain most of them as from Old European to Old Germanic stages, which is mostly in agreement with the known features of Old European hydrotoponymy. For example, -apa- and -andra-names as Old European; -p- as before the Germanic sound shift; -st- and -s-formations as Northern European; -ithi- also unrelated to a hypothetic “Venetic” substrate.

    I think that the point to discuss should not be the similarity with Old European or the oldest reconstructible Proto-Germanic stage (i.e. the closest to North-West Indo-European), or the appearance of these traits also in neighbouring Germanic territory, but the proportion of “more archaic” features contrasting with the proper Germanic area, and thus differences in frequency with the Germanic core territories.

    Just as Udolph can’t accept the non-Indo-European nature of most cases, one can’t simply accept his preference for a Pre-Proto-Germanic nature either, for the same reason one can’t accept the relationship of Western European “Pre-Celtic” hydrotoponymy with Celtic peoples because of some shared appellatives whose Celtic nature is not proven.

    NOTE. If there is something missing from this huge book is certainly statistical analyses with GIS, which would make this case much easier to discuss in graphical and numerical terms. Let’s hope Udolph can update the data in the near future, because he is still (fortunately) active.

    In any case, the Nordwestblock remains a likely Old European hydrotoponymic area partially shared by Germanic, which doesn’t lie at the core of the spread of Old European place names and has a potential non-Indo-European substrate shared with Northern European groups. Combined with comparative grammar and with results of population genomics supporting the spread of East Bell Beakers of Yamna descent from the Carpathian Basin, this essentially renders interpretations of Old European expansion from Northern Europe devoid of support in linguistics.

    Palaeo-Germanic expansion

    To the north, the settlement movement depends on the location and spread of settlement-deficient areas, such as the moors northeast of Wolfsburg, north of Gifhorn, south of Fallingbostel, etc. As soon as this belt has been breached, the place name frequency in the eastern Lüneburg Heath indicates where more favorable settlement conditions are to be found: the Altmark in Saxony-Anhalt, the Jeetzel lowlands and especially the Ilmenau area near Uelzen, Bevensen and Lüneburg (it is difficult not to recall the name Jastorf here).

    If one combines these findings with the dispersion of ancient Germanic place names, one will find that above all the section of the river east from Hamburg to about Lauenburg was particularly favorable for crossing. The onomastic data speaks in favour of this aspect, e.g. the following names lying north and south of this area.

    brink-germanisch

    1. Delvenau = Elbe-Lübeck Canal.

    2. Neetze north of Lüneburg (-d-/-t-change).

    3. Wipperau north of Lüneburg (-p-/-b- change).

    4. The dispersion of the -wik places (Bardowik), cf. Map 15, p. 106.

    5. The dissemination of the -r formations (Map 24, p. 191).

    6. The -ithi formations Geesthacht, Bleckede u.a. south of the Elbe, Eckede north of the stream (see Map 28, p.272).

    7. Fenn south of the Elbe in the north of Lüneburg (Map 31, p.315).

    8. The distribution of the Hor name (Harburg) and northeast of it in Holstein (Map 32, p.328).

    9. Germ, sik- with clear clusters southeast. and northeastern. from Hamburg (Map 36, p. 409).

    10. Also the -büttel names show a concentration east of Hamburg on the one hand and a second accumulation at the estuary of the Elbe (Brunsbüttel) (map 39, p.438).

    11. Gorleben and other places in Hann. Wendland south of the river (Map 47, p.503).

    12. Werber-names southeast from Hamburg and in eastern Holstein (Map 53, p.742).

    13. The scattering of brink names (Map 61, p. 843).

    The place name distributions also make it possible to track the settlement movement north of the Elbe. It has been repeatedly emphasized that Schleswig-Holstein has little share in old Germanic toponymy. One tries to explain this fact, which reaches into the realm of the Old European hydronyms, by saying that, according to archeology, “large parts of Schleswig-Holstein in the 5th to 7th centuries were sparsely populated”.

    scandinavia-neolithic-dagger-period
    Close contacts in Fennoscandia. The distribution of Scandinavian flint daggers (A) in the east and south Baltic region and possible trends of “down the line” trade (B). Good size and quality flint zone in the south-west Baltic region is hatched (C). According to: Wojciechowski 1976; Olausson 1983, fig. 1; Madsen 1993, 126; Libera 2001; Kriiska & Tvauri 2002, 86. Image modified from Piličiauskas (2010).

    If one summarizes these synoptically (Map 74, p.914) and also takes into account the not-included -leben-names (Map 47, p.503), then it is quite clear that Denmark by no means shares these types of names. The most important points are, in my opinion:

    1. North of today’s German-Danish border, the quantity of old place names drops rapidly and even tends towards zero. West Jutland in particular is rarely involved in the dispersion.
    2. Within Jutland there is a clear orientation to the east. The connection with southern Sweden is established via Funen and Zeeland.
    3. Disputed is in my opinion, whether the spread of toponymy followed a roughly direct line Fehmarn and Lolland/Falster. This is not to be excluded, but the maps of toponymy distribution do not give a clear indication in this direction.

    The synoptic map makes it clear that both western Schleswig-Holstein and western Jutland are not to be regarded as Old Germanic settlement areas. Rather, East Jutland and the Danish islands were reached by Germanic tribes.

    pca-bronze-age-germanic
    Bronze Age groups ca. 2200-1750 BC. Top Left: Tentative location of (1) the Pre-Proto-Germanic homeland (earliest stage), in the North European Plain between the Elbe and the the Aller (open border), (2) the Pre-Proto-Germanic expansion area, coinciding with the Nordic Dagger Period, and (3) the Pre-Proto-Germanic-like Nord-West-Block. Top right: PCA of European Bronze Age groups. Bottom left: ADMIXTURE analysis of ancient DNA samples. Bottom right: Y-DNA haplogroup map. See full maps and PCAs.

    Absolute chronology and Balto-Finnic

    It is imprecise to estimate the age of settlement movements from toponymic research. I do not want to be involved in speculation, but I think that Klingberg’s estimate could have some arguments in its favor. In the approximate dating, however, it is important to include a fact that has already been briefly mentioned above and should be treated here in more detail: the fact of Germanic-Finnic relations.

    W.P. Schmid has emphatically pointed out the difficulty that arises when one considers the unfolding of Germanic too far from the Baltic Sea settlement areas. Among other things, it draws attention to the fact that a Germanic homeland that were postulated too far west could not explain how Germanic loanwords might appear in the Finnic names of Northern Russia. These will be mentioned with reference to M. Vasmer: Randale to Finn. ranta “beach”, Pel’doza and Nimpel’da to Finn. pelto, Justozero to Finn. juusto “cheese”, Tervozero to Finn. terva “tar” and Rovdina Gora to Finn. rauta “ore”.

    I think it is possible that the clear spread of Old and North Germanic toponyms, as described in the synoptic map 74 (p. 914) and in the already mentioned -ing, -lösa, -by, -sta(d) and -säter-maps (19, 46, 63-65), can offer some help: quite early the Germanic tribes reached the Swedish east coast. It is also clear that there have previously been contacts with Slavic and Finno-Ugric tribes by sea. However, intensive German-Finnic relations can, in my opinion, have come about only through close contacts on the mainland.

    Pre-Indo-European substrate

    In my investigation, I have repeatedly come up with suggestions to explain a hard-to-interpret North Germanic name from a Pre-Germanic, possibly Non-Indo-European substrate. Most of these were views of H. Kuhn, which he also used to support his so-called “Nord-West block”.

    On one point H. Kuhn may have been right with an assumption of a Pre-Germanic substrate that did not provide the basis for further development in Germanic terms: he very clearly argued that Scandinavia too was Pre-Germanic, even Pre-Indo-European A substrate that stands out above all because of the lack of Lautverschiebung : “In the Nordic countries, we have to reckon with non-Germanic, non-Indo-European prehistoric names scarcely less than in the other Germanic languages”. In light of the results of the present work that makes a relatively late Germanization of Scandinavia very likely, this sentence should not be set aside in the future, but carefully examined on the basis of the material.

    Both data, the known long-lasting Palaeo-Germanic – Finno-Samic contacts, and the underresearched presence of non-Indo-European vocabulary in Scandinavia, are likely related to the presence of a West Uralic(-like) substrate in Scandinavia and most likely also in Northern Europe, based on the disputed non-Indo-European components shared through the North European Plain (see above), and on the scarce ancient Indo-European hydrotoponymy in central-east Europe to the north of the Carpathians.

    Population genomics

    Although there is yet scarce genetic data from northern European territories, the haplogroup distribution among sampled peoples from the Germanic migration period and during the Viking expansion suggests a prevalence of R1b-U106 in the North European Plain (also found in Barbed Wire Beakers), and thus a later integration of typically Neolithic (I1) and CWC-related (R1a) subclades to the Germanic-speaking community during the expansion into Southern Scandinavia.

    This is compatible with the described development of maritime elites by Bell Beakers, representing maritime mobility and trade, and an appealing ideology, similar to the prevalence of Athens over Sparta (Corded Ware in this analogy). It is also supported by the bottlenecks under R1b-U106 to the north of Schleswig-Holstein.

    NOTE. Nevertheless, other R1b-L151 may have been part of the Germanic-speaking communities, especially during its earliest stage, and also R1b-U106 (and other R1b-L161) subclades may appear all the way from the Carpathians to Northern Europe, including the Eastern European Early Bronze Age.

    germanic-iron-age
    Common Germanic expansions ca. 500 BC on. Top Left: Early Iron Age cultures. Top right: PCA of groups from the Iron Age to the Middle Ages. Y-DNA haplogroups during the Germanic migrations (Bottom left) and during the Middle Ages (Bottom right). Notice a majority of R1b-U106 (practically absent from previous Bronze Age populations of Central Europe) among sampled Germanic tribes. See full maps and PCAs.

    Archaeology

    This sudden population bust to the south and predominance of a Southern Scandinavian maritime society in the Nordic circle seems to be also supported by inferences from archaeological data, too. For example, from the recent Human impact and population dynamics in the Neolithic and Bronze Age: Multi-proxy evidence from north-western Central Europe, by Feeser et al. The Holocene (2019):

    The second boom between c. 3000 and 2900 cal. BC relates to increases in the palynological proxy and the binned all site SCDPD curve. From an archaeological point of view, this time reflects the transition from the Funnelbeaker to the Single Grave Culture. The emergence of this new cultural phenomenon is often regarded to have been associated with a shift in subsistence practices, that is, a shift from sedentary agricultural to mobile pastoral subsistence (Hinz, 2015; Hübner, 2005; Iversen, 2013; Sangmeister, 1972).

    denmark-demography-bronze-age
    Left: Map with pollen sites. Right: Bin sensitivity plots based on summed calibrated date probability distributions (SPD) using different degrees of binning on-site level (h = 0 no binning; h = 1000 high binning) and Kernel density plots (KDE) of available radiocarbon dates from the settlement context (settlement sites). Modified from the paper to include a red arrow showing Corded Ware bust and subsequent boom with the Dagger Period..

    (…) there is palynological evidence for increased importance of cereal cultivation during the Young Neolithic in comparison to the Early Neolithic (Feeser et al., 2012). This, however, does not rule out an increased importance of pastoralism, as grazing on grasslands and extensive cereal cultivation are difficult to distinguish and to disentangle in the palynological record. Generally however, human impact on the environment and population levels, respectively, did not reach Funnelbeaker times maxima values during this boom phase at the beginning of the Younger Neolithic. The similar short-term synchronous developments in both the pollen profiles during 2800–2300 cal. BC could point to large-scale, over-regional uniform development during the Younger Neolithic in our study area (cf. also Feeser et al., 2016).

    Between c. 2400 and 2300 cal. BC, the palynological proxy and the binned all site SCDPD curve show a similar distinct decrease (Figure 6), and we define a second bust phase accordingly. The soil erosion record, however, indicates elevated values at around this time but declines, although not very well defined, to a minimum at around 2200 cal. BC. Due to the generally low number of colluvial deposits recorded for the Younger Neolithic, this is not regarded to contradict our interpretation, as low sample sizes generally minimize the chances of identifying a robust pattern. A strong increase in all the three proxies between 2200 and 2100 cal. BC defines our third boom phase.

    Bronze Age evolution

    Candidate homelands for the succeeding (Palaeo-Germanic) stages of the language are shifted also in archaeology to the south, due to the economic influence of demographically stronger Nordic Bronze Age cultural groups of northern Germany over Southern Scandinavia.

    A good description of societal changes in the Palaeo-Germanic stages is offered by the recent paper Cultural change and population dynamics during the Bronze Age: Integrating archaeological and palaeoenvironmental evidence for Schleswig-Holstein, Northern Germany, by Kneisel et al. The Holocene (2019):

    schleswig-holstein-culture-demography
    Qualitative data from material culture and demography in Schleswig-Holstein and Mecklenburg-Western Pomerania. Modified from the original to remark periods of likely demographic decrease (red square) and growth (blue square).

    At each beginning of a boom phase and each end of a bust phase, changes in the material culture could be observed.

    When the pressure on the landscape is at its lowest around 1500 BC and shortly before it rises again, the type of burial changes, hoards and bronzes increase, and monumental burial mounds are erected again. Vice versa, when the pressure on the landscape reaches its maximum value around 1250 BC, tools and hoard depositions decrease again and only the monumental burial and prestige goods are maintained. The ‘elite’ are continuing with their way of burial. The reduction in house surface area and the number of hoards takes place earlier, possibly because of material scarcity as could also be proven in Thy, northern Jutland (Bech and Rasmussen 2018).

    Again, the human impact decreases, and at its lowest point at the beginning of Period IV ca. 1100 BC, the monumental burial custom and the addition of prestige goods also end. The number of hoards and graves begins to rise again, and cooking pits appear. Exchange networks shift with the beginning of Period V, while axes increase again together with a slight decrease in the human impact curve. The appearance of certain artefacts or burial rites at the beginning of such a period of upheaval seems to suggest the role of a trigger. With this analysis, we have defined several likely indicators for social change in the less distinct phases and societal change in the strongly pronounced phases around 1500 BC and 1100 BC and the most important triggers for the Schleswig-Holstein Bronze Age.

    soegel-wohlde-nordic-bronze-age
    Distribution of burials with Valsømagle, Sögel and Wohlde blades with provenance known to parish. q = Valsømagle blades; s = Wohlde blades (small = one grave with a blade; medium = two graves with a blade); l = Sögel blades (small = one grave with a blade, medium = two graves with a blade, large = three graves with a blade). From Bergerbrant (2007).

    While population movements can’t be really understood without a proper genetic transect proving or disproving archaeological theories, it seems that the intermediate zone of the Nordic circle was subjected to at least two demographic busts and succeeding booms during the Middle and Late Bronze Age periods, which not only affected the hydrotoponymy of Schleswig-Holstein (see above), but probably served as dynamic changes in the linguistic evolution of Palaeo-Germanic-speaking communities up to the Common Germanic expansion.

    Read more on the Northern Early Bronze Age province.

    Related

    Volosovo hunter-gatherers started to disappear earlier than previously believed

    volosovo-corded-ware

    Recent paper (behind paywall) Marmot incisors and bear tooth pendants in Volosovo hunter-gatherer burials. New radiocarbon and stable isotope data from the Sakhtysh complex, Upper-Volga region, by Macānea, Nordqvist, and Kostyleva, J. Archaeol. Sci. (2019) 26:101908.

    Interesting excerpts (emphasis mine):

    The Sakhtysh micro-region is located in the Volga-Oka interfluve, along the headwaters of the Koyka River in the Ivanovo Region, central European Russia (Fig. 1). The area has evidence of human habitation from the Early Mesolithic to the Iron Age, and includes altogether 11 long-term and seasonal settlements (Sakhtysh I–II, IIa, III–IV, VII–XI, XIV) and four artefact scatters (sites V–VI, XII–XIII), in addition to which burials have been detected at five sites (I–II, IIa, VII, VIII) (Kostyleva and Utkin, 2010). The locations have been known since the 1930s and intensively studied since the 1960s under the leadership of D.A. Kraynov, M.G. Zhilin, E.L. Kostyleva, and A.V. Utkin.

    Sakhtysh II and IIa are the most extensively studied sites of the complex, with ca. 1500m2 and around 800m2 excavated, respectively. The burial grounds at both sites are considered as fully investigated.

    volosovo-sakhtysh-dates
    AMS datings from the sites Sakhtysh II and IIa. Sampled contexts are given in parentheses (burial/hoard), “crust” indicates samples of charred organic
    residues on pottery from cultural layer. For data, see Tables 1–2.

    Sakhtysh chronology

    The AMS dates do not support the previously proposed phasing of the Sakhtysh burials to early (4750–4375 BP/3600–3000 cal BCE), late (or developed; 4375–4000 BP/3000–2500 cal BCE), and final (4000–3750 BP/2500–2200 cal BCE): the early and late burials at Sakhtysh IIa do not stand out as two separate groups, and also the burials and hoards from Sakhtysh II, connected to the final phase, are temporally overlapping with these. Neither the use sequence, where the settlement and burial phases are non-overlapping and also complementary between the sites (Kostyleva and Utkin, 2010, 2014), finds support in the present material.

    The AMS datings indicate that the Volosovo people started to bury their dead at Sakhtysh IIa after 3700 cal BCE; dates earlier than this may be affected by FRE or suffer from mixed contexts and poor quality of dates. The present data questions the interpretation that the Sakhtysh IIa cemetery was used without interruptions between 4800 and 4080 BP (Kostyleva and Utkin, 2010), i.e. for a millennium between 3550 and 2600 cal BCE. The AMS dates rather suggest a use period of some centuries only around the mid-4th millennium cal BCE, tentatively 3650–3400 cal BCE. This would also be more realistic considering the number of burials at the site.

    volosovo-sakhtysh-sites
    The core area of Volosovo culture (after Kraynov, 1987) and the sites of the Sakhtysh complex (after Kostyleva and Utkin, 2010). Eurasian map base made with Natural Earth. Illustration: K. Nordqvist.

    Volosovo chronology

    The absolute dating of Volosovo culture was for a long time hampered by the small number of radiocarbon dates (see Kraynov, 1987). Today,>100 datings connected with it can be found in literature (Korolev and Shalapinin, 2010; Chernykh et al., 2011; Nikitin, 2012; Mosin et al., 2014). Unfortunately, the available dates do not form solid grounds for dating the cultural phenomenon, as many of them have quality-related issues, large measurement errors, and ambiguous cultural or physical contexts. Consequently, particular datings may be connected to different cultural phases by different scholars. Finally, a large part of the newly-published datings are obtained through direct dating of potsherds (Kovaliukh and Skripkin, 2007; Zaitseva et al., 2009), and therefore, their cogency must be faced with reservation (see Van der Plicht et al., 2016; Dolbunova et al., 2017).

    The datings connected with Volosovo cover a wide time range between ca. 5500 BP (4400 cal BCE) and ca. 3700 BP (2100 cal BCE). However, datings from secure contexts, with good quality (error ca. 50 years or below) and no probable FRE, place the beginning of Volosovo culture to the first half of the 4th millennium cal BCE, around 3700–3600 cal BCE. This is also supported by the roughly coeval terminal dates given for the preceding Lyalovo (Zaretskaya and Kostyleva, 2011) and Volga-Kama cultures (Lychagina, 2018), as well as the appearance of related neighbouring cultures, for example, in the Kama region (Nikitin, 2012; Lychagina, 2018), the southern forest steppe area (Korolev and Shalapinin, 2014), and north-western Russia and Finland (Nordqvist, 2018). Still, the dating of many of these cultural phases suffers from the same problems as of Volosovo.

    A handful of contested datings place the end of Volosovo culture to the final centuries of the 3rd millennium cal BCE, or even later (Kostyleva and Utkin, 2010; Chernykh et al., 2011; Nikitin, 2012). On the other hand, the new AMS dates indicate that Volosovo activities at Sakhtysh II and IIa ceased before or towards the early 3rd millennium cal BCE; if this reflects the general decline of Volosovo culture must be still confirmed by more dates from Sakhtysh and elsewhere. In this context, the general cultural development must be accounted for. To what extent – if at all – the Volosovo people were present after the arrival of the Corded Ware culture-related Fatyanovo-Balanovo populations? Based on the current, albeit scant and inconclusive radiocarbon data this took place from ca. 2700 cal BCE onwards (Krenke et al., 2013).

    volosovo-fatyanovo-balanovo
    Corded Ware and Comb Ware hunter-gatherer-related populations in north-eastern Europe from ca. 2600 BC. See full map.

    Comments

    One of the interesting genetic papers in the near future will be the one that finally includes samples from Corded Ware groups in the forest zone (i.e. Fatyanovo-Balanovo and Abashevo), which will most likely confirm that they are the origin of the known genetic profile of Central and East Uralic-speaking peoples, seeing how West Uralic peoples show genetic continuity in the East Baltic area, coinciding with the Battle Axe culture.

    Uralicists have come a long way from the 1990s, when the picture of Uralic before Balto-Slavic in the Baltic was already evident, and Uralians were identified with Comb Ware peoples. The linguistic data and relative chronology are still valid, despite the now outdated interpretations of absolute archaeological chronology, as happens with interpretations of Krahe or Villar about Old European.

    As an example, here are some relevant excerpts from Languages in the Prehistoric Baltic Sea Region, by Kallio (2003):

    NOTE. Kallio’s contribution appeared in the book Languages in Prehistoric Europe (2003), which I hold nostalgically close in my Indo-European library (now almost impossible to read fully). It is still one of my preferred books (from those made up of mostly unconnected chunks on European linguistic prehistory), because it contains Oettinger’s essential update of North-West Indo-European common vocabulary, which led us indirectly to our Modern Indo-European project from 2005 on.

    In any case, the Uralic arrival in the region east of the Baltic Sea preceded the Indo-European one (…).

    This theory that the ancestors of Finno-Saamic speakers arrived in the Baltic Sea region earlier than those of Balto-Slavic speakers is still rejected by some scholars (e.g. Napolskikh 1993: 41-44), who claim, for instance, that Finno-Saamic speakers would not have known salmons before they met Balts because the Finno-Saamic word for ‘salmon’ (i.e. *losi) is a borrowing from Baltic. Similarly, one could claim that English speakers would not have known salmons before they met Frenchmen because English salmon is a borrowing from French. In other words, Worter und Sachen are not necessarily borrowed hand in hand. Otherwise, it would not be so easy to explain how many Finnish names of body parts are borrowings from Baltic (e.g. hammas ‘tooth’, kaula ‘neck’, reisi ‘thigh’) and from Germanic (e.g. hartia ‘shoulder’, lantio ‘loin’, maha ‘stomach’).

    A more probative argument is the fact that Balto-Slavic features in Finno-Saamic are mostly lexical ones (i.e. typical superstrate features), where Finno-Saamic features in Balto-Slavic are mostly non-lexical ones (i.e. typical substrate features). Note that there are more Balto-Slavic features in Finnic than in Saamic and more Finno-Saamic features in Baltic than in Slavic. This fact could be explained by presuming that Pre-Saamic was spoken north of the Corded Ware area and Pre-Slavic was spoken south of the Typical Pit-Comb Ware area, whereas Pre-Finnic and Pre-Baltic alone were spoken in the area, where both the Typical Pit-Comb Ware culture (ca. 4000-3600 BC) and the Corded Ware culture (ca. 3200-2300 BC) were situated. This area was most probably bilingual, until Finnic and Baltic won in the north and in the south, respectively.

    As is well-known, the idea of Uralic substrate features in Balto-Slavic is not new (cf. e.g. Pokorny 1936/1968: 181-185). As recent studies (e.g. Bednarczuk 1997) have shown, their density is the most remarkable in the four Balto-Slavic languages spoken in the earlier Pit-Comb Ware area (i.e. Latvian, Lithuanian, Belorussian, Russian). On the other hand, occasional Uralisms in the other Balto-Slavic languages spoken west of the Vistula and south of the Pripyat may rather be considered adstrate features spread from the northeast.

    comb-ware-uralic
    Our beliefs from the 2000s. A hypothetic Uralic Comb Ware distribution before the arrival of a hypothetic North-West Indo-European-speaking Corded Ware. “Generalized distribution of the Pit-Comb Ware cultural complex (Mallory & Adams 1997: 430, Carpelan 1999: 257) and the most probable homelands of Saamic, Finnic, Mordvin, Mari, and Permic.”

    The idea of Indo-European superstrate features in Finnic is not new either (cf. e.g. Posti 1953). As Jorma Koivulehto (1983) has recently shown, the earliest Indo-European loanword stratum in the westernmost Uralic branches alone can be considered Northwest Indo-European and connected with the Corded Ware culture (ca. 3200-2300 BC). Since this layer, there have been continuous contacts between Baltic and Finnic. According to Koivulehto (1990), the following stratum can be called Proto-Balt(o-Slav)ic and dated to the Late Neolithic period (ca. 2300-1500 BC). Note that this Proto-Balt(o-Slav)ic dating agrees with the established ones (cf. e.g. Shevelov 1964: 613-614, Kortlandt 1982: 181), when we remember the fact that archaeologists have also moved their datings back by centuries during the last decades.

    Finally, there is also a Baltic loanword stratum which was not borrowed from the ancestral stage of Latvian, Lithuanian and/or Old Prussian but from some extinct Baltic language or dialect (Nieminen 1957). However, as these words still go back to the early Proto-Finnic stage, they can hardly be dated later than Bronze-Age ( ca. 1500-500 BC). Therefore, we may conclude that they were probably borrowed from a Baltic superstrate, which arrived in the Finnish Gulf area during the Corded Ware period and survived there until the Bronze Age, when it was no longer identical with other Baltic dialects. In any case, as later Baltic loanword strata concern southern Finnic languages alone, we may presume that this ‘North Baltic’superstrate had become extinct.

    The traditional association of Uralic with Volosovo hunter-gatherers doesn’t make sense, since they neither miraculously survived for thousands of years nor mixed for hundreds of years with Corded Ware peoples, so we can now more confidently reject the recent assumption by Carpelan & Parpola that their language was adopted by incoming Fatyanovo, Balanovo and Abashevo groups, to develop into the known Uralic languages (more here). This includes one of the many models of the the Copenhagen group, who simplistically follow “Steppe ancestry” for Indo-Europeannes.

    If one combines the known relative linguistic chronology with the North-West Indo-European hydrotoponymy layer, now more clearly identified as Old Europeans expanding with East Bell Beakers and derived Early Bronze Age groups, I think there is little space left for maneuvering out of the overwhelming evidence for a Uralic homeland in the forest-steppes, linked to the spread of late Sredni Stog/Corded Ware ancestry into north-eastern Europe and beyond the Urals.

    Related

    European hydrotoponymy (II): Basques and Iberians after Lusitanians and “Ligurians”

    bronze-age-languages-western-europe

    The first layer in hydrotoponymy of Iberia is clearly Indo-European, in territories that were occupied by Indo-Europeans when Romans arrived, but also in most of those occupied by non-Indo-Europeans.

    Among Indo-European peoples, the traditional paradigm – carried around in Wikipedia-like texts until our days – has been to classify their languages as “Pre-Celtic” despite the non-Celtic phonetics (especially the initial -p-), because the same toponyms appear in areas occupied by Celts (e.g. Parisii, Pictones, Pelendones, Palantia); or – even worse – just as “Celtic”, because of the famous -briga and related components. This was evidently not tenable at the end of the 20th century, and it is simply anachronistic today.

    NOTE. Since Indo-Europeans and non-Indo-Europeans of Western Europe show strong Y-chromosome bottlenecks under R1b-P312 lineages, maps below show the evolution of cultural groups side by side with ADMIXTURE of ancient DNA samples instead. The map series on prehistorical migrations contains also Y-DNA and mtDNA maps.

    Most excerpts below (emphasis mine) are translated from Spanish (see the original text here):

    iberia-bell-beakers-steppe
    Top Left: Arrival of Indo-European-speaking East Bell Beakers and likely disruption of the Basque-Iberian community (ca 2500 BC on). Top Right: corresponding (unsupervised) ADMIXTURE map of ancient DNA samples. Arrival of Central European ancestry (“Steppe ancestry”, roughly represented by the blue color), with other components still prevalent, roughly including Anatolia Neolithic (brown), WHG (red), and sporadically Northern African (violet). Notice the high proportion of Central European ancestry in central and north-western Iberia. See full maps including Y-DNA and mtDNA. Bottom: PCA of Bell Beaker and contemporaneous samples.

    Palaeo-Indo-Europeans

    While the non-Celtic Indo-European nature of Lusitanian is certain, the nature of the “Pre-Celtic” language spoken by peoples such as Cantabri, Astures, Pellendones, Carpetani and Vettones is still being discussed, due to the scarcity of material to work with.

    Galaico-Lusitanian

    From Hacia una definición del lusitano, by Vallejo (2013):

    It is certain that the delimitation of the geographical area set by Tovar is still valid, basically determined by the known direct documents, that is, the traditionally accepted inscriptions (the classic ones of Lamas de Moledo, Arroyo de la Luz and Cabeço das Fráguas), in addition to the new ones from Arroyo and the recent one from Arronches, see Fig. 1), to which some others could be added: the new bilingual inscription from Viseu necessarily compels us to consider it as indigenous, because it contains terms that belong to the core of the language and not only onomastics (I refer to the nexus igo and the nicknames deibabor and deibobor). By virtue of this new incorporation, we can also consider other texts as indigenous, although they do not include a common lexicon (see Fig. 1, inscriptions 7 to 22), in the expectation that many Lusitanian scribes were consciously mixing two linguistic registers (code switching), one to refer to the deities (for which they frequently used indigenous inflection) and another for anthroponyms (always with Latin inflection).

    iberia-early-bronze-age
    Left: Early Bronze Age cultures in Iberia (in red, likely Indo-European groups; in green, likely non-Indo-European groups). Right: Unsupervised ADMIXTURE of ancient DNA samples. See full maps including Y-DNA and mtDNA.

    Firstly, it is striking that this geographical profile drawn by the texts correspond almost exactly to the distribution of large series of anthroponyms and theonyms.* Among the abundant names of people we can highlight those with a large number of repetitions whose appearance is circumscribed to our region of study (see Fig. 2). Some of them are truly frequent and lack parallels on the outside, such as the stem Tanc / Tang- (of Tanginus) with no less than 130 attestations, or Tonc- / Tong- (of Tongius or Tongetamus) with 70. Others show also sufficiently representative figures as Camalus and Maelo (with 46 repetitions each), Celtius (with 29), Caturo or Sunua (with 23), Camira (with 22), Doquirus (with 20), Louesius (with 18), Al(l)ucquius (with 17) or Malge(i)nus (with 16). According to these quantities, it appears that these are not casual occurrences of names, taking into account that chance tends to be reduced to a minimum in the study of the Iberian Peninsula, since we can easily handle the entire peninsular corpus. In turn, Reue, Bandue, Nauiae and Crougiae are the theonyms that best represent the Lusitanian-Galician area, coinciding fundamentally (Figure 3) with the picture that anthroponymy and texts had drawn, although with less examples.

    lusitanian-inscriptions-toponymy-anthroponymy-teonymy
    Top left: Lusitanian (long and short) inscriptions; top right: Map of the distribution of statue-menhirs and south-western stelae, by Rodríguez-Corral (2014) [(1) stelae in Beira Alta and Tras-os-Montes (Portugal), and Orense (Galicia, Spain); (2) both in the same territory: northwestern statue-menhirs and southwestern stelae; (3) hybridization of both into the same material form (stela/stela-menhir from Pedra Alta)]; bottom left: Lusitanian teonymy; bottom right: Lusitanian anthroponymy.

    * The other subdivision of the onomastics, toponymy, presents difficulty in the elaboration of series, by the few repetitions of segments, once the universal element -briga has been eliminated.

    It is not only these groups of names and roots that help us define a large northwestern area, but, as I have had occasion to mention in other places, some onomastic data that share a similar distribution can also be added: the desinence -oi (with an assimilation in -oe / -ui) of theonymic dative singular, the ending -bo of dative plural, the presence of the noun-forming suffix -aiko-, in addition to other phonetic features such as the passage of e> ei in anthroponymy, the reduction ug> uo the step of w> b.

    iberia-north-west-dna
    Genetic isolation in modern north-western Iberia (northern Portugal / southern Galicia) is greater than in other Iberian regions, forming different ancestral clusters splitting before others (including Basques). Image from Bycroft et al. (2018). See explanatory video by Carracedo.

    Astur-Cantabrian

    From The concept of Onomastic Landscape: the case of the Astures, by Vallejo (2013):

    (…) First of all, it seems that there is an independent onomastic area, which can be defined by a series of names and suffixes that are repeated there exclusively or predominantly. This area does not seem to correspond with what we know of the Lusitanian-Galician onomastics nor of the more coastal Asturian; it also differs from the Celtiberian area, with which it does not have features in common. In this way, and always in the conjectural terrain, we could find ourselves before an Indo-European non-Celtic language different from the Lusitanian language.

    A peculiarity that will have to be investigated is the presence of an excessively wide border corridor, where the names of the southern Astures (Augustales) do not predominate, but neither those of the northern Astures (Transmontanos). Similarly, we will have to see the scope of the hypothesis that there might have been a language perhaps differentiated from that spoken in the Lusitanian, Galician or Celtiberian zones; the lower documentary richness of the Asturian zone of Transmontana makes it more difficult to guarantee that it is not the same linguistic area as the one we isolate among Asturian cities.

    In any case, de Hoz, even taking into account the difficulty of an affirmation of this type, pointed out ambiguously that we could find ourselves in front of different languages. On the other hand, the absence of texts directly transmitted by this people leaves us without a definitive confirmation the argument that it is a linguistically differentiated region, but it does not invalidate it at all. These drawbacks require the suspension of the exact characterization of our area, awaiting advances in the field of epigraphy and methodology.

    astur-cantabrian-toponymy

    Non-Indo-Europeans

    The following are mainly excerpts from Villar (2007, 2014):

    villar-vascos
    Lenguas, genes y culturas en la Prehistoria de Europa y Asia suroccidental (2007). Buy the ebook online (or the printed version, if available).

    Basques

    Anthroponymy

    The information provided by place-names and hydronyms on the one hand and anthroponyms on the other is of undoubted historical value in both cases, but of different specific significance. Anthroponyms reflect the present situation at the moment when living people were using them. It is an aspect very sensitive to social changes of all kinds, reaching its highest level of instability when there is language change.

    (…) the Pre-Roman anthroponymic inventory of the Basque Country and Navarre indicates that prior to the arrival of Romans the language spoken was Indo-European (reflected in the names used) in the territories of Caristii, Varduli and Autrigones, while in Vasconic territory (especially in the current Navarre) most of the speakers chose Iberian names. In the territories of the current Basque Country, only a negligible statistical proportion chose Basque names, whereas in Navarre it was a minority of the population. That’s how things were towards the 3rd century BC.

    Hydro-Toponymy

    Cities and rivers are not subject to the ephemeral life cycle of humans. Rivers have very long cycles that go far beyond the life time not only of individuals, but also of languages ​​and cultures. Cities are also generally very stable, although social circumstances occasionally cause one to be abandoned or destroyed, while new ones are created from time to time. That means that the names of rivers and cities are not subject to fashions or frequent change. Nor does a language change imply a renewal of the previous hydronymy and toponymy.

    Speakers of the new languages ​​incorporated into a territory learn from the natives the hydronymic and toponymic system, producing what we call the “toponymic transmission”. (…) it requires a prolonged contact between the native population and the new occupants, which can only occur when the indigenous population is not annihilated quickly and radically.

    iberia-middle-bronze-age
    Top Left: Middle Bronze Age cultures in Iberia (in red, likely Indo-European groups; in green, likely non-Indo-European groups). Top Right: Unsupervised ADMIXTURE of ancient DNA samples. See full maps including Y-DNA and mtDNA. Bottom: Bottom: PCA of Bronze Age groups.

    The ancient onomastic data of the Basque Country and Navarre can be summarized as follows:

    • Ancient hydronymy, the longest lasting onomastic component, is not Basque, but Indo-European in its entirety.
    • The old toponymy, which follows it in durability, is also Indo-European in its entirety, except Poampaelo (now Pamplona) and Oiarso (now Oyarzun).
    • And in anthroponymy, which reflects the language used at the time when those names were in use, is also massively Indo-European, although there are between 10-15% anthroponyms of Vasconic etymology.

    (…) the existing data show that, while in Roman times in Hispania there were only a couple of place-names in the Pyrenean border and a dozen anthroponyms of Vasconic etymology, in Aquitaine there was an abundant antroponymy of that etymology.

    iberia-late-bronze-age
    Left: Late Bronze Age cultures in Iberia (in red, likely Indo-European groups; in green, likely non-Indo-European groups). Right: Unsupervised ADMIXTURE of ancient DNA samples. See full maps including Y-DNA and mtDNA.

    This set of facts is most compatible with a hypothesis that postulated a late infiltration of this type of population from Aquitaine, which at the time of the Roman conquest had only reached to establish a bridgehead, consisting of a small population center in Navarre and Alto Aragón and nothing else, except some isolated individuals in the current provinces of Álava, Vizcaya and Guipúzcoa. The almost complete absence of old place-names of Vasconic etymology would be explained in this way: Vasconic speakers, recently arrived and still in small numbers, would not have had the possibility of altering in depth the toponymic heritage prior to their arrival, which was Indo-European.

    The idea of ​​a late Vasconization of a part of those territories, in the High Middle Ages or late Antiquity, is not new. Already in the 1920s M. Gómez Moreno said about the modern Basque provinces, with the district of Estella in Navarra, that “personal nomenclature allows comparisons of definitive value, probative that there lived people of the Cantabrian-Asturian race [who for Gómez Moreno were Indo-European], without the slightest trace of perceptible Basqueness”. For him, the first Indo-European people to penetrate the peninsula would have been Ligurian, which evolved into Cantabrians, Asturians, Venetians, Lusitanians, Tormogi, Vacaeans, Autrigones, Caristii and Varduli.

    iberia-early-iron-age
    Top Left: Pre-Roman cultures in Iberia (in red/brown, Indo-European groups; in pink, Greek; in yellow, Phoenician; in green, likely non-Indo-European groups; Tartessian is disputed). Top Right: Unsupervised ADMIXTURE of ancient DNA samples. See full maps including Y-DNA and mtDNA. Bottom: PCA of Iron Age groups.

    Aquitaine

    If, as we said above, Basque speakers began to enter the Iberian Peninsula from the other side of the Pyrenees only from the Roman-Republican era, to intensify their presence in the following centuries we must assume that they were to the north of the Pyrenees already before those dates. And, indeed, the existence of this abundant Vasconic antroponymy shows that in the first centuries of our era – while Vasconic speakers in the Peninsula were very few in number, their population in Aquitaine was abundant.

    In a provisional manner we can advance that [Aquitaine’s] hydronyms are also known in other places of Europe and easily compatible with Indo-European etymologies (Argantia, Aturis, Tarnes, Sigmanos); and among the place names there are also many that are compatible with non-Gallic Indo-European etymologies, or not necessarily Gallic (Curianum, Aquitania, Burdigala, Cadurci, Auscii, Eluii, Rutani, Cala- (gorris), Latusates, Cossion, Sicor, Oscidates, Vesuna, etc.).

    In addition to those place names that we classify as generically Indo-European, there are not a few Celts (Lugdunum, Mediolanum, Noviomagos, Segodunon, Bituriges, Petrucorii, Pinpedunni), several Latins (Aquae Augustae, Convenae, ad Sextum, Augusta), and even some Celto-Latin hybrids (Augustonemeton, Augustoriton). On the other hand, there are hardly any names, neither serial nor not serial, that have a reasonable possibility of being explained by Vasconic etymology (Anderedon could be one of them).

    Consequently, the onomastic question of Aquitaine is not compatible with the possibility that Vasconic is the “primordial element” there, either. On the contrary, it is compatible with the hypothesis that they arrived also late in Aquitaine, when hydro-toponymy was already established. They had to Vasconize all or part of the previous population, that turned to use to a large extent the Vasconic anthroponymy. But the previous toponymy remained and the Vasconization process was probably soon interrupted by Celticization first, and Romanization later.

    aquitanian-tribes-vascones
    Aquitani and neighbouring tribes around the Pyrenees, as described by the Romans (ca. 1st c. BC). The Basque language likely expanded south and west of the Pyrenees into Indo-European-speaking territories during the Roman period. The term ‘Vascones’ only became applied to Basque-speaking tribes in medieval times. Map modified from image by Sémhur at Wikipedia.

    A prediction in genetics

    This is how Francisco Villar and co-authors from the University of Salamanca saw what would happen with the genetic studies of modern Basques in 2007, based on the similarity with neighbouring Iberians and French, and the late intrusion of the language in its current territory:

    Unfortunately, linguistics does not have the means to establish the moment of that arrival in terms of absolute chronology. In any case, this hypothesis is not incompatible with some peculiarities in the frequency of certain genes of the Basque-speaking population. Indeed, today we tend to attribute these peculiarities to the joint action of genetic drift and isolation; to which perhaps we could add a bottleneck in the Vasconic founding population that would one day settle in Aquitaine.

    villar-indoeuropeos
    Indoeuropeos, iberos, vascos y sus parientes (2014). Buy the ebook online (Or printed version, if available).

    Also Villar, in 2014:

    In the hypothesis that I propose, future speakers of Basque would have settled initially in Aquitaine, where there would have been an inevitable genetic diffusion with pre-existing [first stage] populations. On the other hand, Basque speakers from Aquitaine would have started to arrive to the Basque Country and Navarre only from Roman times (only a couple of Vasconic toponyms, at least one of them of recent creation; scarce anthroponyms of Vasconic etymology). The part of those populations that mixed with the pre-existing Palaeo-Indo-Europeans (Indo-European names of rivers; general Indo-European toponymy) saw how the uniqueness of their haplogroups, if there was any, was diluted, making it difficult to distinguish from the general [Indo-European] background; being a minority, it could had been even lost as a result of adverse genetic drift.

    Olalde et al. (2019) confirmed this hypothesis that modern Basques are quite similar to investigated Iron Age Indo-Europeans from Iberia (such as Celtiberians sampled from the Basque Country):

    For the Iron Age, we document a consistent trend of increased ancestry related to Northern and Central European populations with respect to the preceding Bronze Age. The increase was 10 to 19% (95% confidence intervals given here and in the percentages that follow) in 15 individuals along the Mediterranean coast where non-Indo-European Iberian languages were spoken; 11 to 31% in two individuals at the Tartessian site of La Angorrilla in the southwest with uncertain language attribution; and 28 to 43% in three individuals at La Hoya in the north where Indo-European Celtiberian languages were likely spoken. This trend documents gene flow into Iberia during the Late Bronze Age or Early Iron Age, possibly associated with the introduction of the Urnfield tradition.

    Modern Basques show therefore, paradoxically, an ancestry similar to recent Iron Age Indo-European invaders (quite likely the ancestors of Celtiberians), which confirms the hypothesis of bottlenecks/founder effects followed by a very recent isolation of its population:

    (…) the genetic profile of present-day Basques who speak the only non-Indo-European language in Western Europe [] overlap genetically with Iron Age populations showing substantial levels of Steppe ancestry.

    iberia-roman-period
    Left: Roman period in Iberia. Right: Unsupervised ADMIXTURE of ancient DNA samples. See full maps including Y-DNA and mtDNA. Notice increase of steppe ancestry in the north, associated with the (Late Bronze Age / Early Iron Age) arrival of Central Europeans.

    Iberians

    Regarding the Iberian language, the circumstances of analysis are less favorable. However, we can observe in the ancient toponymy of typically Iberian areas (the Spanish Levant and Catalonia) a considerable proportion of toponymy of Indo-European etymology, often identical to that which F. Villar (2000) has called “Southern-Iberian-Pyrenean”. In fact, its presence in the Levant is nothing else but a continuation from Catalonia to the South along the Mediterranean coast. Here are some examples: Caluba, Sorobis, Uduba, Lesuros, Urce / Urci, Turbula, Arsi / Arse, Asterum, Cartalias, Castellona, ​​Lassira, Lucentum, Saguntum, Trete, Calpe, Lacetani, Onusa, Palantia, Saetabis, Saetabicula, Sarna , Segestica, Sicana, Turia, Turicae, Turis.

    Compatible with the Indo-European etymology can also be Blanda, Sebelacum, Sucro, Tader, Sigarra, Mastia, Contestania, Liria, Lauro, Indibilis, Herna, Edeta, Dertosa, Cesetania, Cossetani, Celeret, Bernaba, Biscargis, (…)

    Finally, in other place names there are Indo-European components in hybrid toponymic syntagms, such as:

    1. orc- / urc-: Orceiabar, Urcarailur, Urceatin, Urcebas, Urcecere, Urcescer, Urceticer.
    2. Il-: Iltukoite, Iluro (3), Ilurci, Ilorci, Ilurcis, Ilucia, Iliturgi, Ilarcurris, Iluberitani, etc.

    il-iberian

    Examples like these show that in Catalonia and the Spanish Levant the Iberian language is not the deepest identifiable substrate language, but that it took root there when there was previously an Indo-European language that had created a considerable network of toponyms and hydronyms that we can recognize, and over which Iberians settled as a superstrate. The pre-existence of an Indo-European language in the historically Iberian area is further corroborated by the fact that its ancient hydronyms are all Indo-European, with the exception of a single river that has a name that is supposed to be Iberian: the Iberus (Ebro), of which obviously the country and its inhabitants took their name. No doubt ib- was an appellation for river, so that in the language that created that hydronym the Iber should have simply been “the river”. But we will see in the body of this work that ib- is in various places outside the Iberian Peninsula as an appellation for «river», which will force us to rethink its supposed Iberian affiliation. In fact, the Iberus had another name, Elaisos, whose etymology is compatible with Indo-European. As we know with certainty that after Iberians no other Indo-European peoples came to their territory before the Romans, the Indo-European creators of that hydronymy have had to be there before the Iberians. And its antiquity must be considerable because, as we have already said, the vast majority of its hydronyms (Alebus, Caluba, Lesuros, Palantia, Saetabis, Sigarra, Sucro, Tader, Turia and Uduba, Elaisos) belong to that anonymous Indo-European language that didn’t leave written texts or had historical continuity.

    inscriptions-celtiberians-iberians-hispania
    Inscriptions in Iberia ca. 2nd–1st c. BC. Purple squares show Celtiberian inscriptions, blue circles show Iberian inscriptions. Image modified from Hesperia – Banco de datos de lenguas paleohispánicas.

    Villar (2014):

    Not always that a language is settled in a territory is it able to eradicate the existing ones definitively. Even a political system as unitary and unifying as the Roman was not able to eradicate the Basque language. And nowadays in Latin America, despite the crushing cultural dominance of Spanish, despite the means for the schooling of a modern society, in spite of the media, a multitude of pre-Columbian languages ​​are spoken that coexist with the language of culture, the only one that is written in those countries. In those situations, which can be prolonged for quite a lot of time, there are individuals who only speak the language newly imposed, others who speak only the language that has resisted disappearing, and others who speak both, in a broad framework of bilingualism. My proposal is that something similar to that must have happened in the Iberian territory when the Romans arrived: A language of culture, Iberian, diversified into more or less distant local dialects, coexisted with several previous languages, equally differentiated from the dialectal point of view. This explains the irruption in the Iberian texts of non-Iberian anthroponyms and, above all, the existence there of a Palaeo-Indo-European hydro-toponymy that had remained in use not only because it was transmitted to Iberian speakers, but also because its native users were still present.

    Related

    European hydrotoponymy (I): Old European substrate and its relative chronology

    old-european-hydronymy-toponymy

    These first two posts on Old European hydro-toponymy contain excerpts mainly from Indoeuropeos, iberos, vascos y sus parientes, by Francisco Villar, Universidad de Salmanca (2014), but also from materials of Lenguas, genes y culturas en la Prehistoria de Europa y Asia suroccidental, by Villar et al. Universidad de Salamanca (2007). I can’t recommend both books hardly enough for anyone interested in the history of Pre-Roman peoples in Iberia and Western Europe.

    NOTE. Both books also contain detailed information on hydrotoponymy of other regions, like Northern Europe, the Aegean and the Middle East, with some information about Asia, apart from (outdated) genetic data, but their main aim is obviously the Prehistory of Iberia and neighbouring regions like France, Italy, or Northern Africa.

    Here are only some excerpts (emphasis mine), translated from Spanish (see the original texts here), accompanied by images from both books.

    villar-indoeuropeos
    Indoeuropeos, iberos, vascos y sus parientes (2014). Buy the ebook online (Or printed version, if available).

    Alteuropäisch and Krahe

    The investigation of “Old European” or Alteuropäisch, popularized by Krahe, began precisely with the study of some toponyms and personal names spread all over Europe, previously considered “Ligurian” (by H. d’Arbois de Jubainville and C. Jullian) or “Illyrian” (by J. Pokorny), with which those linguistic groups – in turn badly known – were given an excessive extension, based only on some lexical coincidences.

    This is a comment made by the author about Krahe‘s data and his opinions, frequently used against his compiled data, which I find paradoxically applicable to Villar’s data and his tentative assignment of the relative linguistic chronology to an absolute one – including the expansion of a “Mesolithic” Indo-European vs. a “Neolithic” Basque / Iberian vs. a Bronze Age Celtic – when it is now clear that the sequence of events was much later than that:

    It is very widespread today a derogatory and globally disqualifying attitude to everything that sounds like Alteuropäisch and Krahe, sometimes without the necessary discrimination between different hypotheses, or even between data and hypothesis. It is not fair that the version of H. Krahe and that of W. P. Schmid be disqualified in a single simplistic judgment as if they were the same thing. But it is a major mistake to reduce the value of the hydro-toponymic data of Europe by the mere fact that Krahe attributed an implausible historical explanation to them. The data are real and still need an adequate explanation within a real historical framework, despite the unfeasibility of Krahe’s explanation.

    With that we reach a point that I want to highlight. Among those who are allergic to anything that involves deviating one iota of the Indo-European paradigm as a single event, an attitude gaining momentum considers that hydro-toponymy was introduced in the different regions of Europe and Southeast Asia by the same Indo-European languages ​​that appear historically occupying their territory. H. Krahe had argued strongly against this possibility, so now I will save myself a deeper refutation and I will limit myself to pointing out some difficulties that position is forced to face.

    salo-salano
    Sala, Sala, Sala, Sala, Sala, Sala, Sala, Sala, Sala, Sala, Sala, Salaca/Salis, Salaceni,
    Salacia, Salacia, Salaeni, Salam, Salandona, Salangi, Salangi , Salaniana, Sãlantas,
    Salapa, Salapeni, Salaphitanum, Salapia / Salpia / Salapina palus / Salpe, Salar, Salara, Salarama,
    Salarbima, Salariga, Salars, Salas, Salat, Salauris, Salcitani, Sale, Sale, Sale, Sale
    stagnum, Salecon, Saleia, Salentina, Salentini, Salernum, Salerni, Sales, Sali, Salia, Salia,
    Salica, Salica, Salice, Salii, Salija, Salinẽlis, Salìnis, Salìnis, Salìnis, Salìnis, Salinsae, Salionca,
    Salius, Salō, Salō, Saloca, Salodurum, Salona, Salonae, Salonenica, Salonia, Saloniana,
    Salonime, Salonium, Salontia, Saluca, Salum, Salum, Salunatasi, Saluntum / Salluntum,
    Salùpis, Sãlupis, Salur, Salurnis, Selepitani, Sõlis.

    The defenders of that alternative have to assume that the process of dialectalization, that before the migrations from the Urheimat was separating into the different Indo-European branches, affected each of them in the phonetic aspect in the general naming vocabulary, but left them unaltered in its phonetic predialectal state with regards to hydro-toponymy, as well as a good part of the naming lexicon related to the concepts of “river, water” and the different qualities of water currents. For example, according to those sharing that opinion, the Hispanic Palantia of the area of Vaccei would be in fact Celtic, but in that name the loss of the initial /p/ that characterizes Celtic would not have been applicable. Similarly, the hydro-toponymy in Germania is largely exempt from the Lautverschiebung, in Greece the loss of initial /s/, etc. These names not only fail to suffer the dialectal innovations corresponding to their zones, but sometimes they present innovations different from the features of the dialect involved. For example the word *mori “sea, standing water” is sometimes found in the hydro-toponymy of Gaul in the form *mari instead of *mori proper of Celtic (Marantium, Marisanga, Marsus), which in the framework of the paradigm has to be inevitably interpreted as a non-Celtic innovation.

    wako-wogo
    Potential geographic relationship between a priori unrelated graphic-phonetic variants.

    Names of this nature that appear in areas where a pre-Roman historical Indo-European language never existed remain unexplained, such as in North Africa, Arabia Felix or the Caucasus: Lake Pallantias in Libya; the Salat River in Mauritania Tingitana; Auso in Mauritania Caesariensis; the Alonta River in Georgia; the Abas River in Caucasian Albania; Salma and Salapeni in Arabia Felix; etc. Of course, for these cases it is always possible to deny any relationship of kinship between these forms and their European cognates, and attribute everything to the chance of random homophonies. Thus, once again, the annoying comparative data are sacrificed in the sacred altar of the paradigm, despite the fact that they are so numerous and consistent that if there were no blind faith in the current dogma, they would be sufficient to articulate a new paradigm over them.

    The choice of each Indo-Europeanist between the non-Indo-European and the Indo-European interpretation to explain the prehistoric toponymy of Europe is not motivated by the fact that they manage partial sets of hydronyms that are more propitious alternatively for the one or the other option. On the contrary, frequently the same batch of materials is claimed by both trends as its own. An extreme example is that of Th. Vennemann, who considers simply as non-Indo-European (specifically Paleo-Basque) exactly the same material that H. Krahe used to support his Indo-European interpretation. Thus, the structure and linguistic characteristics of the studied material have little role in the choice of one or the other path, which is rather conditioned by convictions and adhesion to a varied range of personal beliefs, traditional dogmas and scientific paradigms.

    villar-vascos
    Lenguas, genes y culturas en la Prehistoria de Europa y Asia suroccidental (2007). Buy the ebook online (or the printed version, if available).

    The linguistic column

    The sequence of languages ​​that were successively spoken in any territory constitutes what by analogy [with the “geological column”] we could call its “ethno-linguistic column”.

    Next I offer the list of the languages ​​detected in the compositional (and to a lesser extent derivational) toponymic syntagms in which the appellatives ub-, up-, ab-, ap-, ur-, il-, igi, tuk, -ip – analyzed in this work – are involved.

    From the interaction of the different strata in words and hybrid syntagms we can, therefore, establish the linguistic column in the Iberian Peninsula and its neighboring territories (Western Europe and Northern Africa) with the following sequence:

    1. A first stratum of very old chronology, which in a previous publication I have proposed to call Palaeo-Indo-European [“arqueo-indoeuropeo”]. The toponymic elements belonging to this stratum dealt with throughout this text are abundant: kerso-, turso-, alawo-, lako-, mido-, silo-, tibo-, etc.

    They always function as determinant toponyms of a place-name in any other language. It never uses the name “city” (or “river”) in hybrid syntagms. Their place names (determinants) are combined with names of the following languages:

       a) Iberian in Iberia or Southern France: kiŕś-iltiŕ, tuŕś-iltiŕ, alaun-iltiŕte, lakunm ∙ -iltiŕte.

       b) The language of the igi in southern Iberia and perhaps Northern Africa: Cantigi, Saltigi, Sagigi, Sicingi.

       c) The southern language of the postponed -il: Mid-ili, Sil-ili, Tib-ili.

       d) The language of the postponed -ip: Lac-ipo, Ost-ipo, Vent-ipo.

       e) Celtic in Gaul: kerso-ialos > Cersolius > Cerseuil; Ibili-duros > Ibliodurus.

    karo-karanto
    Cariensi, Carantium, Carandonis, Carae, Caraca / Caracca, Carrinensis, Cariaca, Carneus, Carula, Carlae, Carieco, Cariocieco, Caricillum, Carona, Carnona, Caranta, Carantonus / Carantana, Caronte, Carantomum / Carantomium, Carronenses / Garronenses, Cares / Carus, Caranusca, Carona, Caro vicus, Carninia, Carus, Carnutes, Carnonis castrum, Carenses, Caralis / Carallis, Carni, Carnicum, Caraceni, Careia, Carici, Carant / Carrant, Carnonacae, Carontō, Cariolum, Caritani, Carinum, Carantani, Carnuntum, Cariniana Vallis, Cariones, Careotae, Caroia, Caria, Careum, Carnae, Caran, Carnasium, Carnus, Carneates, Carnium, Carenus, Karlasuwa, Carnias, Karahna, Karna, Cariuntis, Kariuna, Careotis, Karu, Caralitis, Carus, Carnasso, Cares, Carene, Caranum, Caria, Carina, Carura, Caralis, Coralis, Carana, Carnalis, Carinum, Carnus, Carium, Carnium, Carnus Carnuntus / Carnusii, Chariuntas, Carandra, Carna, Carana, Carine, Cariatae, Caralae, Carura, Carei, Carura, Caricum, Caranis, Caralia, Carustum, Carystus, Carastasei.

    This first Palaeo-Indo-European layer also corresponds to:

    Several Palaeo-Indo-European varieties that have ab-, ap-, ub-, up- as a name for «river». To them belong also numerous place names (balsa-, siko-, wol-, etc.) that act as first members composed in both monoglotic and hybrid syntagmas.

    Palaeo-Indo-European varieties in which ur- is the name “river”.

    ab-hydronyms

    2. The second stratum in decreasing order of antiquity is formed by the language of the place name igi “city”, although its presence is only verified with certainty in Iberia (especially in the south) and Northern Africa:

       a) It sets the igi name in compounds with Palaeo-Indo-European toponyms as in Salt-, Ast-, Olont-, Cant-, Aur- (Hispania) and Sagigi, Sicingi (Northern Africa).

       b) It works as the first place-name of the compound when the second is il: Igilium, Igilgili, Singili.

    3. The third stratum is the language of the name il “city”:

       a) It puts the nickname il as determined in hybrid syntagms with Palaeo-Indo-European determinants: Mid-ili, Sil-ili, Tib-ili.

       b) It puts the nickname il as determined in hybrid syntagms with determinant toponyms igi: Igilium, Igilgili, Singili.

       c) It puts the place names (determinants) in front of the name (determined) of the language -ip (Il-ipa, Il-ipula and Il-ipla).

    il-toponyms

    4. Fourth is the language of the name ip- “city”, which puts the name (determined) in syntagms with:

       a) Palaeo-Indo-European toponym (determinant): Lac-ipo, Ost-ipo, Vent-ipo.

       b) Toponym (determinant) il: Ilipa.

       c) Second generation hybrid toponym of Palaeo-Indo-European + il: Balsilippa.

       d) In the Balsilippa and Sicilippa conglomerates, the three strata appear in the expected sequence: Palaeo-Indo-European + il + ip.

    ip-toponyms

    5. In the fifth place of the sequence is the language of the tuk-:

       a) It puts the name tuk- in compounds in which the place-name is a Palaeo-Indo-European element: Acatucci (see Aduatuci in Germania).

       b) It puts the name tuk- “height, top” in compounds in which the place-name is an ip- fossilized as place-names: Iptuci, etc.

       c) On at least one occasion an ip-fossilized syntagm acts as a toponym opposite a Celtic name: Itucodon (<Iptuco-dunum).

    NOTE. Even though Villar talks about this stratum -tuk in Germania (Aduatukus) and the British Isles (Itucodon), only one case is found in each territory.

    tuk-variants

    6. The last place is occupied by Celtic:

       a) In Itucodon it puts the name (dunum) in front of a complex toponym of two previous strata, ip- + tuk-; and in Iliodurus it gives the name duro- in front of an equally complex Ibliodurus (<Ibili + duro).

       b) In bilbiliz it puts the casual morpheme in a fossilized bi-member toponym of a previous stratum, one of whose components is il-: Bilbil-iz.

    linguistica-cronologia-hispania
    [First column modified to include relative instead of absolute chronology]

    A hard change of paradigm

    More effort did it cost me to accept that ub- is a dialectal variant of a known Indo-European word for “water, river”, of which previously knew three others: ap-, ab-, up-. The obviousness of the phonetic correlation ap- / ab- // up- / ub- together with the semantic link with rivers, which can be verified above all outside of Spain, but is also present in our Peninsula, forced my resistance little by little. And with it fell the first trench of the dogma, unshakable until that moment, that everything in the Peninsula in the south was to be non-Indo-European.

    ub-ob-hydronyms

    Along with this serial component, many other isolated place names were revealed as very likely of Indo-European etymology, both in the “Iberian” East and in the “Tartessian” South. So the ubiquity of Indo-European throughout the Peninsula began to impose itself to me painfully. I say painfully because I lacked a paradigm in which to fit the new perspective that was making its way into my mind, which was therefore suspended in nothing, without any theoretical support, leaving me with a feeling that I was losing my footing. And for a time I was reluctant to accept the profound implications that all of this had entailed.

    All il languages, in any of their locations, exhibit a compositional behavior in hybrid toponymic syntagms that place them all in an intermediate position between the clearly [first/second layer] strata, with place-names for their human settlements semantically derived from water realities (ur), and those clearly attributable to the [fifth layer] with appellations derived from settlements in heights (briga, dunum). But in that intermediate segment of the column there are three strata: 1) il, 2) ip-, 3) tuk-. In Andalusia there is an additional one: the igi stratum, of opaque semantics, which immediately precedes the il stratum.

    or-ur-hydronyms
    Hydronyms in -or-, -ur-.

    To postulate that any of the toponymic strata of our column imply a new linguistic stratum, certain additional requirements will be necessary. One of them is that, in addition to the name in question, the languages ​​involved should share other features that could not have been lent, such as the very precise order of elements in the compounds Toponym + Name coexisting with Name + Adjective. Or the sharing of additional lexical elements that are not usually subject to loans, such as the semantically basic adjectives beri «new» and bels «black».

    Unfortunately, the toponymic method, like the Comparative Method itself, does not have the capacity to establish precise absolute chronologies. (…)

    Linguistic chronology

    old-european-hydro-toponymy
    Old European hydrotoponymy. Baltic data compensated. Statistical method Kriging.

    In Europe (Hispania, South of France, Germania, British Isles, Baltic) the oldest stratum that can be identified is an indeterminable number of palaeo-varieties of the Indo-European macro-family, which do not have a direct local relationship with historical Indo-European languages, to the extent that we can verify. In fact, we have seen that stratigraphic signs lead us to consider the main Indo-European pre-Roman language of Hispania, the Celtic language, as a stratum after the il language, which in turn is later than the peninsular Indo-European palaeo-varieties.

    In North Africa there is also a Palaeo-Indo-European stratum present. But there is also a very old non-Indo-European stratum whose identity I can not define through the material used. Nor has it been possible for me to establish relative antiquity of one and the other on African soil.

    Another of the languages ​​involved, which has il- as an appellation for “city” in the Southwest of Hispania and North Africa, could have some kind of kinship relationship with Basque on the one hand and the Iberian language on the other, but the same indirect form that I have just pointed out for the Indo-European palaeo-varieties with respect to the historical Indo-European languages. Or in other words: the language(s) of the place-names referred to in this work would be palaeo-varieties of a linguistic family to which two known historical languages, Iberian and Basque, may have belonged, although we can’t establish a relation of direct affiliation neither between those two historical languages ​​among themselves, nor between any of them and the palaeo-varieties of the prehistoric toponymy.

    linguistica-cronologia-africa
    [First column modified to include relative instead of absolute chronology]

    In general, Celtic does not have in its historical territories the onomastic behavior of an ancestral language, but that of an intrusive language, whose presence there is not only more recent than other Indo-European varieties, but also after that of various non-Indo-European strata, which are themselves ranked between the oldest detected (Palaeo-Indo-European) and the last of Pre-Romans, which is Celtic itself. If we only detected two strata, the Indo-European and the Celtic ones, we could discuss if it is possible that both are one and the same, so that what we define as “Celtic” is nothing other than the modern in situ evolution of Palaeo-Indo-European. But examples like those of kiŕśiltiŕ, kerso-ialos, Cirsa or Itucodon, among many others analyzed throughout this book, make it unlikely. And, in addition, the mediation of several strata in the column between the Palaeo-Indo-European language of Cirsa, as well as the greater antiquity of the ip- and tuk- languages ​​in Spanish, Gallic and British territory, defines the latter as a new and more recent layer than the aforementioned, which burst into its historical sites during the Iron Age.

    Because Archaeology continues to deny the existence of population movements of a size worthy of consideration in the Iron Age, it is necessary to accept that the Indo-European Problem remains intact. It is understandable that before this aporia, many minds who are uncomfortable living with doubts, prefer to adopt a creed (the traditional, the Neolithic or the continuist) and expose it as a certainty to their students in the classrooms or their colleagues in conferences and publications. It’s not my case. For me, with Voltaire, “le doute est désagréable, mais la certitude est ridicule”. Or with Manzoni: “E men male l’agitarsi nel dubbio, che riposar nell’errore”.

    Continue reading on European hydrotoponymy (II): Basques, Iberians, and Etruscans after Old Europeans.

    Related

    Villabruna cluster in Late Epigravettian Sicily supports South Italian corridor for R1b-V88

    epipalaeolithic-whg-expansion

    New preprint Late Upper Palaeolithic hunter-gatherers in the Central Mediterranean: new archaeological and genetic data from the Late Epigravettian burial Oriente C (Favignana, Sicily), by Catalano et al. bioRxiv (2019).

    Interesting excerpts (emphasis mine):

    Grotta d’Oriente is a small coastal cave located on the island of Favignana, the largest (~20 km2) of a group of small islands forming the Egadi Archipelago, ~5 km from the NW coast of Sicily.

    The Oriente C funeral pit opens in the lower portion of layer 7, specifically sublayer 7D. Two radiocarbon dates on charcoal from the sublayers 7D (12149±65 uncal. BP) and 7E, 12132±80 uncal. BP are consistent with the associated Late Epigravettian lithic assemblages (Lo Vetro and Martini, 2012; Martini et al., 2012b) and refer the burial to a period between about 14200-13800 cal. BP, when Favignana was connected to the main island (Agnesi et al., 1993; Antonioli et al., 2002; Mannino et al. 2014).

    sicily-grotta-oriente
    A-B) Geographic location of Grotta d’Oriente.

    The anatomical features of Oriente C are close to those of Late Upper Palaeolithic populations of the Mediterranean and show strong affinity with other Palaeolithic individuals of Sicily. As suggested by Henke (1989) and Fabbri (1995) the hunter-gatherer populations were morphologically rather uniform.

    Genetic analysis

    We confirmed the originally reported mitochondrial haplogroup assignment of U2’3’4’7’8’9. This haplogroup is present in both pre- and post-LGM populations, but is rare by the Mesolithic, when U5 dominates (Posth et al.2016).

    Lipson et al. (2018) (their supplementary Figure S5.1) and Villalba-Mouco et al. (2019) (their Figure 2A) showed that European Late Palaeolithic and Mesolithic hunter-gatherers fall along two main axes of genetic variation. Multidimensional scaling (MDS) of f3-statistics shows that these axes form a “V” shape (Fig. 3). (…)

    Focusing further on Oriente C, we find that it shares most drift with individuals from Northern Italy, Switzerland and Luxembourg, and less with individuals from Iberia, Scandinavia, and East and Southeast Europe (Fig. 4A-B). Shared drift decreases significantly with distance (Fig. 4C) and with time (Fig. 4D) although in a linear model of drift with distance and time as a covariate, only distance (p=1.3×10-6) and not time (p=0.11) is significant. Consistent with the overall E-W cline in hunter-gatherer ancestry, genetic distance to Oriente C increases more rapidly with longitude than latitude, although this may also be affected by geographic features. For example, Oriente C shares significantly more drift with the 8,000 year-old 1,400 km distant individual from Loschbour in Luxembourg (Lazaridis et al.,2014), than with the 9,000 year old individual from Vela Spila in Croatia (Mathieson et al.,2018) only 700 km away as shown by the D-statistic (Patterson et al.,2012) D (Mbuti, Oriente C, Vela Spila, Villabruna); Z=3.42. Oriente C’s heterozygosity was slightly lower than Villabruna (14% lower at 1240k transversion sites), but this difference is not significant (bootstrap P=0.12).

    oriente-c-villabruna-f3-statistics
    Multidimensional scaling of outgroup f3-statistics for Late 531 Upper Palaeolithic and Mesolithic hunter-gatherers.

    Discussion and Conclusion

    The robust record of radiocarbon dates proves that they reached Sicily not before 15-14 ka cal. BP, several millennia after the LGM peak. In our opinion, in fact, the hypothesis about an early colonization of Sicily by Aurignacians (Laplace, 1964; Chilardi et al., 1996) must be rejected, on the basis of a recent reinterpretation of the techno-typological features of the lithic industries from Riparo di Fontana Nuova (Martini et al., 2007; Lo Vetro and Martini, 2012; on this topic see also Di Maida et al., 2019).

    These analyses have implications for understanding the origin and diffusion of the hunter-gatherers that inhabited Europe during the Late Upper Palaeolithic and Mesolithic. Our findings indicate that Oriente C shows a strong genetic relationship with Western European Late Upper Palaeolithic and Mesolithic hunter-gatherers, suggesting that the “Western hunter-gatherers” was a homogeneous population widely distributed in the Central Mediterranean, presumably as a consequence of continuous gene flow among different groups, or a range expansion following the LGM.

    shared-drift-whg-villabruna-oriente-c
    The same statistic as in A plotted with geographic position

    The South Italian corridor

    Once again, a hypothesis based on phylogeography – apart from scarce archaeological and palaeolinguistic data (“Semitic”-like topo-hydronymy and substrates in Europe) – seems to be confirmed step by step. Since the finding of the Villabruna individual of hg. R1b-L754 (likely R1b-V88, like south-eastern European lineages expanded with WHG ancestry), it was quite likely to find out that southern Europe was the origin of the expansion of R1b-V88 into Africa.

    The most likely explanation for the presence of “archaic” R1b-V88 subclades among modern Sardinians was, therefore, that they represented a remnant from a Late Upper Palaeolithic/Early Mesolithic population that had not been replaced in subsequent migrations, and thus that the migration of these lineages into Northern Africa and the Green Sahara happened during a period when Italy was connected by a shallower Mediterranean (and more land connections) to Northern Africa.

    late-epigravettian
    Likely Late Epigravettian/Mesolithic expansion of R1b-V88 into Northern Africa. See full map.

    Nevertheless, the arguments for a quite recent expansion of R1b-V88 through the Mediterranean and into Africa keep being repeated, probably based on ancestry from the few ancient (and many modern) populations that have been investigated to date, a simplistic approach prone to important errors that overarch whole migration models.

    For example, in the recent paper by Marcus et al. (2019) the presence of these lineages among ancient Sardinians (from the late 4th millennium BC on) is interpreted as an expansion of R1b-V88 with the Cardial Neolithic based on their ancestry, disregarding the millennia-long gap between these samples and the presence of this haplogroup in Palaeolithic/Mesolithic Northern Iberia and Northern Italy, and the comparatively much earlier splits in the phylogenetic tree and dispersal among African populations.

    Afroasiatic and Nostratic

    I was asked recently if I really believed that we could reconstruct Proto-Nostratic and connect it with any ancestral population. My answer is simple: until the Chalcolithic – when the whole picture of Indo-Europeans, Uralians, Egyptians or Semites becomes quite clear – we have just very few (linguistic, archaeological, genetic) dots which we would like to connect, and we do so the best we can. The earlier the population and proto-language, the more difficult this task becomes.

    NOTE. 1) I tentatively connected hg. R with Nostratic in a previous text – when it appeared that R1a expanded from around Lake Baikal, hence Eurasiatic; R1b from the south with AME-WHG ancestry, hence Afroasiatic; and R2 with Dravidian.

    2) After that, I though it was more likely to be connected to AME ancestry and the Middle East, because of the apparent expansion of WHG from south-eastern Europe, and the potential association of Afroasiatic and (Elamo-?)Dravidian to Middle Eastern populations.

    3) However, after finding more and more R1b samples expanding through northern Eurasia, spreading through the (then wider) steppe regions; and R1a essentially surviving among other groups in eastern Europe for thousands of years without being associated to significant migrations (like, say, hg. C after the Palaeolithic), it didn’t seem like this division was accurate, hence my most recent version.

    But, in essence, it’s all about connecting the dots, and we have very few of them…

    eurasiatic-phylum-ultraconserved-words
    Phylogenetic tree from Pagel et al. (2013), partially in agreement with Kortlandt’s view on Eurasiatic. “Consensus phylogenetic tree of Eurasiatic superfamily (A) superimposed on Eurasia and (B) rooted tree with estimated dates of origin of families and of superfamily. (A) Unrooted consensus tree with branch lengths (solid lines) shown to scale and illustrating the correspondence between the tree and the contemporary north-south and east-west geographical positions of these language families. Abbreviations: P (proto) followed by initials of language family: PD, proto-Dravidian; PK, proto-Kartvelian; PU, proto-Uralic; PIE, proto–Indo-European; PA, proto-Altaic; PCK, proto–Chukchi-Kamchatkan; PIY, proto–Inuit-Yupik. The dotted line to PIY extends the inferred branch length into the area in which Inuit-Yupik languages are currently spoken: it is not a measure of divergence. The cross-hatched line to PK indicates that branch has been shortened (compare with B). The branch to proto-Dravidian ends in an area that Dravidian populations are thought to have occupied before the arrival of Indo-Europeans (see main text). (B) Consensus tree rooted using proto-Dravidian as the outgroup. The age at the root is 14.45 ± 1.75 kya (95% CI = 11.72–18.38 kya) or a slightly older 15.61 ± 2.29 kya (95% CI = 11.72–20.40 kya) if the tree is rooted with proto-Kartvelian. The age assumes midpoint rooting along the branch leading to proto-Dravidian (rooting closer to PD would produce an older root, and vice versa), and takes into account uncertainty around proto–Indo-European date of 8,700 ± 544 (SD) y following ref. 35 and the PCK date of 692 ± 67 (SD) y ago.”

    In linguistics, I trust traditional linguists who tend to trust other more experimental linguists (like Hyllested or Kortlandt) who consider that – in their experience – an Indo-Uralic and a Eurasiatic phylum can be reconstructed. Similarly, linguists like Kortlandt are apparently (partially) supportive of attempts like that of Allan Bomhard with Nostratic – although almost everyone is critic of the Muscovite school‘s attachment to the Brugmannian reconstruction, stuck in pre-laryngeal Proto-Indo-Anatolian and similar archaisms.

    I mostly use Nostratic as a way to give a simplistic ethnolinguistic label to the genetically related prehistoric peoples whose languages we will probably never know. I think it’s becoming clear that the strongest connection right now with the expansion of potential Eurasiatic dialects is offered by ANE-related populations (hence Y-chromosome bottlenecks under hg. R, Q, probably also N), however complicated the reconstruction of that hypothetic community (and its dialectalization) may be.

    Therefore, the multiple expansions of lineages more or less closely associated to ANE-related peoples – like R1b-V88 in the case of Afrasian, or R2 in the case of Dravidians – are the easiest to link to the traditionally described Nostratic dialects and their highly hypothetic relationship.

    green-sahara-neolithic
    Reconstruction of North African vegetation during past green Sahara periods. Estimated and reconstructed MAP for the Holocene GSP (6–10 kyr BP) projected onto a cross-section along the eastern Sahara (left panel) and map view of reconstructed MAP, vegetation and physiographic elements [7,8,11,45] (right panel). Image from Larrasoaña et al. (2013).

    What should be clear to anyone is that the attempt of many modern Afroasiatic speakers to connect their language to their own (or their own community’s main) haplogroups, frequently E and/or J, is flawed for many reasons; it was simplistic in the 2000s, but it is absurd after the advent of ancient DNA investigation and more recent investigation on SNP mutation rates. R1b-V88 should have been on the table of discussions about the expansion of Afroasiatic communities through the Green Sahara long ago, whether one supports a Nostratic phylum or not.

    The fact that the role of R1b bottlenecks and expansions in the spread of Afroasiatic is usually not even discussed despite their likely connection with the most recent population expansions through the Green Sahara fitting a reasonable time frame for Proto-Afroasiatic reconstruction, a reasonable geographical homeland, and a compatible dialectal division – unlike many other proposed (E or J) subclades – reveals (once again) a lot about the reasons behind amateur interest in genetics.

    Just like seeing the fixation in (and immobility of) recent writings about the role of I1, I2, or (more recently) R1a in the Proto-Indo-European expansion, R1b with Vasconic, or N1c with Proto-Uralic.

    NOTE. That evident interest notwithstanding, it is undeniable that we have a much better understanding of the expansions of R1b subclades than other haplogroups, probably due in great part to the easier recovery of ancient DNA from Eurasia (and Europe in particular), for many different – sociopolitical, geographical, technological – reasons. It is quite possible that a more thorough temporal transect of ancient DNA from the Middle East and Africa might radically change our understanding of population movements, especially those related to the Afroasiatic expansion. I am referring in this post to interpretations based on the data we currently have, despite that potential R1b-based bias.

    Related

    Sea Peoples behind Philistines were Aegeans, including R1b-M269 lineages

    New open access paper Ancient DNA sheds light on the genetic origins of early Iron Age Philistines, by Feldman et al. Science Advances (2019) 5(7):eaax0061.

    Interesting excerpts (modified for clarity, emphasis mine):

    Here, we report genome-wide data from human remains excavated at the ancient seaport of Ashkelon, forming a genetic time series encompassing the Bronze to Iron Age transition. We find that all three Ashkelon populations derive most of their ancestry from the local Levantine gene pool. The early Iron Age population was distinct in its high genetic affinity to European-derived populations and in the high variation of that affinity, suggesting that a gene flow from a European-related gene pool entered Ashkelon either at the end of the Bronze Age or at the beginning of the Iron Age. Of the available contemporaneous populations, we model the southern European gene pool as the best proxy for this incoming gene flow. Last, we observe that the excess European affinity of the early Iron Age individuals does not persist in the later Iron Age population, suggesting that it had a limited genetic impact on the long-term population structure of the people in Ashkelon.

    philistines-pca
    Ancient genomes (marked with color-filled symbols) projected onto the principal components inferred from present-day west Eurasians (gray circles). The newly reported Ashkelon populations are annotated in the upper corner.

    Genetic discontinuity between the Bronze Age and the early Iron Age people of Ashkelon

    In comparison to ASH_LBA, the four ASH_IA1 individuals from the following Iron Age I period are, on average, shifted along PC1 toward the European cline and are more spread out along PC1, overlapping with ASH_LBA on one extreme and with the Greek Late Bronze Age “S_Greece_LBA” on the other. Similarly, genetic clustering assigns ASH_IA1 with an average of 14% contribution from a cluster maximized in the Mesolithic European hunter-gatherers labeled “WHG” (shown in blue in Fig. 2B) (15, 22, 26). This component is inferred only in small proportions in earlier Bronze Age Levantine populations (2 to 9%).

    In agreement with the PCA and ADMIXTURE results, only European hunter-gatherers (including WHG) and populations sharing a history of genetic admixture with European hunter-gatherers (e.g., as European Neolithic and post-Neolithic populations) produced significantly positive f4-statistics (Z ≥ 3), suggesting that, compared to ASH_LBA, ASH_IA1 has additional European-related ancestry.

    We find that the PC1 coordinates positively correlate with the proportion of WHG ancestry modeled in the Ashkelon individuals, suggesting that WHG reasonably tag a European-related ancestral component within the ASH_IA1 individuals.

    philistines-admixture
    We plot the ancestral proportions of the Ashkelon individuals inferred by qpAdm using Iran_ChL, Levant_ChL, and WHG as sources ±1 SEs. P values are annotated under each model. In cases when the three-way model failed (χ2P < 0.05), we plot the fitting two-way model. The WHG ancestry is necessary only in ASH_IA1.

    The best supported one (χ2P = 0.675) infers that ASH_IA1 derives around 43% of ancestry from the Greek Bronze Age “Crete_Odigitria_BA” (43.1 ± 19.2%) and the rest from the ASH_LBA population.

    (…) only the models including “Sardinian,” “Crete_Odigitria_BA,” or “Iberia_BA” as the candidate population provided a good fit (χ2P = 0.715, 49.3 ± 8.5%; χ2P = 0.972, 38.0 ± 22.0%; and χ2P = 0.964, 25.8 ± 9.3%, respectively). We note that, because of geographical and temporal sampling gaps, populations that potentially contributed the “European-related” admixture in ASH_IA1 could be missing from the dataset.

    The transient impact of the “European-related” gene flow on the Ashkelon gene pool

    The ASH_IA2 individuals are intermediate along PC1 between the ASH_LBA ones and the earlier Bronze Age Levantines (Jordan_EBA/Lebanon_MBA) in the west Eurasian PCA (Fig. 2A). Notably, despite being chronologically closer to ASH_IA1, the ASH_IA2 individuals position closer, on average, to the earlier Bronze Age individuals.

    philistines-y-dna
    See more information on Y-DNA SNP calls, including ASH067 as R1b-M269 (xL151).

    The transient excess of European-related genetic affinity in ASH_IA1 can be explained by two scenarios. The early Iron Age European-related genetic component could have been diluted by either the local Ashkelon population to the undetectable level at the time of the later Iron Age individuals or by a gene flow from a population outside of Ashkelon introduced during the final stages of the early Iron Age or the beginning of the later Iron Age.

    By modeling ASH_IA2 as a mixture of ASH_IA1 and earlier Bronze Age Levantines/Late Period Egyptian, we infer a range of 7 to 38% of contribution from ASH_IA1, although no contribution cannot be rejected because of the limited resolution to differentiate between Bronze Age and early Iron Age ancestries in this model.

    Hg. R1b-M269 and the Aegean

    I already predicted this relationship of Philistines and Aegeans (Greeks in particular) months ago, based on linguistics, archaeology, and phylogeography, although it was (and still is) yet unclear if these paternal lineages might have come from other nearby populations which might be descended from Common Anatolians instead, given the known intense contacts between Helladic and West Anatolian groups.

    luwian-civilization-sea-peoples
    The alternative view: The Sea Peoples can be traced back to the Aegean, so they could also have consisted of Luwian petty kingdoms, who had formed an alliance and attacked Hatti from the south.

    The deduction process for the Greek connection was quite simple:

    Palaeo-Balkan populations

    We know that R1b-Z2103 expanded with Yamna, including West Yamna settlers: they appear in Vučedol, which means they formed part of the earliest expansion waves of Yamna settlers into the Carpathian Basin, and they also appear scattered among Bell Beakers (apart from dominating East Yamna and Afanasevo), which suggests that they were possibly one of the most successful lineages during the late Repin/early Yamna expansion.

    The “Steppe ancestry” associated with I2a-L699 samples among Balkan BA peoples may have also been associated with recent Bronze Age expansions, and this haplogroup’s presence among modern Balkan peoples may also suggest that it expanded with Palaeo-Balkan languages. Nevertheless, we don’t know which specific lineages and “Steppe ancestry” they represent, sadly.

    These samples may well be related to remnants of previous Balkan populations like Cernavodă or Ezero, because there has been no peer-reviewed attempt at distinguishing Khvalynsk-/Novodanilovka- from Sredni Stog- from Yamnaya-related populations (see here), and some groups that are associated with this ancestry, like Corded Ware, are known to be culturally distinct from Yamna.

    In any case, Proto-Greeks from the southern Balkans (say, Sitagroi IV and related groups) are probably going to show, based on Palaeo-Balkan substrate and Pre-Greek substrate and on the available Mycenaean samples, a process of decreasing proportion of R1b-Z2103 lineages relative to local ones, and a relatively similar cline of Yamna:EEF ancestry from northern to southern areas, at least in the periods closest to the Yamna expansion.

    NOTE. The finding of “archaic” R1b-L389 (R1b-V1636) and R1a-M198 subclades among modern Greeks and the likely Neolithic origin of these paternal lineages around the Caucasus suggest that their presence in Greece may be from any of the more recent migrations that have happened between Anatolia and the Balkans, especially during the Common Era, rather than Indo-Anatolian migrations; probably very very recently.

    -chalcolithic-late-balkans
    Bronze Age cultures in the Balkans and the Aegean. See full map including ancient samples with Y-DNA, mtDNA, and ADMIXTURE.

    Minoans and haplogroup J

    In the Aegean, it is already evident that the population changed language partly through cultural diffusion, probably through elite domination of Proto-Greek speakers. Whether that happened before the invasion into the Greek Peninsula or after it is unclear, as we discussed recently, because we only have one reported Y-chromosome haplogroup among Mycenaeans, and it is J (probably continuing earlier lineages).

    Now we have more samples from the so-called Emporion 2 cluster in Olalde et al. (2019), which shows Mycenaean-like eastern Mediterranean ancestry and 3 (out of 3) samples of haplogroup J, which – given the origin of the colony in Phocea – may be interpreted as the prevalence of West Anatolian-like ancestry and lineages in the eastern part of the Aegean (and possibly thus south Peloponnese), in line with the modern situation.

    NOTE. It does not seem likely that those R or R1b-L23 samples from the Emporion 1 cluster are R1b-Z2103, based on their West European-like ancestry, although they still may be, because – as we know – ancestry (unlike haplogroup) changes too easily to interpret it as an ancestral ethnolinguistic marker.

    anatolia-greek-aegean
    PCA of ancient samples related to the Aegean, with Minoans, Mycenaeans (including the Emporion 2 cluster in the background) Anatolia N-Ch.-BA and Levantine BA-LBA populations, including Tel Shadud samples. See more PCAs of ancient Eurasian populations.

    Greeks and haplogroup R1b-M269

    Therefore, while the presence of R1b-Z2103 among ancient Balkan peoples connected to the Yamna expansion is clear, one might ask if R1b-Z2103 really spread up to the Peloponnese by the time of the Mycenaean Civilization. That has only one indirect answer, and it’s most likely yes.

    We already had some R1b-Z2103 among Thracians and around the Armenoid homeland, which offers another clue at the migration of these lineages from the Balkans. The distribution of different “archaic” R1b-Z2103 subclades among modern Balkan populations and around the Aegean offered more support to this conclusion.

    But now we have two interesting ancient populations that bear witness to the likely intrusion of R1b-M269 with Proto-Greeks:

    An Ancient Greek of hg. R1b

    A single ancient sample supports the increase in R1b-Z2103 among Greeks during the “Dorian” invasions that triggered the Dark Ages and the phenomenon of the Aegean Sea Peoples. It comes from a Greek lab study, showing R1b1b (i.e. R1b-P297 in the old nomenclature) as the only Y-chromosome haplogroup obtained from the sampling of the Gulf of Amurakia ca. 470-30 BC, i.e. before the Roman foundation of Nikopolis, hence from people likely from Anaktorion in Ancient Acarnania, of Corinthian origin.

    ancient-greeks-y-dna-mtdna

    Even with the few data available – and with the caution necessary for this kind of studies from non-established labs, which may be subject to many different kinds of errors – one could argue that the western Greek areas, which received different waves of migrants from the north and shows a higher distribution of R1b-Z2103 in modern times, was probably more heavily admixed with R1b-Z2103 than southern and eastern areas, which were always dominated by Greek-speaking populations more heavily admixed with locals.

    The Dorian invasion and the Greek Dark Ages may thus account for a renewed influx of R1b-Z2103 lineages accompanying the dialects that would eventually help form the Hellenic Koiné. In a sense, it is only natural that demographically stronger populations around the Bronze Age Aegean would suffer a limited (male) population replacement with the succeeding invasions, starting with a higher genetic impact in the north-west and diminishing as they progressed to the south and the east, coupled with stepped admixture events with local populations.

    This would be therefore the late equivalent of what happened at the end of the 3rd millennium BC, with Mycenaeans and their genetic continuity with Minoans.

    pre-greek-ssos
    Distribution of Pre-Greek place-names ending in -ssos/-ssa or -sos/-sa. See original images and more on the south/east cline distribution of Pre-Greek place-names here.

    Sea peoples of hg. R1b-M269

    Thanks to Wang et al. (2018) supplementary materials we knew that one of the two Levantine LBA II samples from Tel Shadud (final 13th–early 11th c. BC) published in van den Brink (2017) was of hg. R1b-M269 – in fact, the one interpreted as a Canaanite official residing at this site and emulating selected funerary aspects of Egyptian mortuary culture.

    Both analyzed samples, this elite individual and a commoner of hg. J buried nearby, were genetically similar and indistinguishable from local populations, though:

    Principal Components Analysis of L112 and L126 was carried out within the framework described in Lazaridis et al. (2016). This analysis showed that the two individuals cluster genetically, with similar estimated proportions of ancestry from diverse West Eurasian ancestral sources. These results are consistent with the hypothesis that they derive from the same population, or alternatively that they derive from two quite closely related populations.

    We know that ancestry changes easily within a few generations, so there was not much information to go on, except for the fact that – being R1b-M269 – this individual could trace his paternal ancestor at some point to Proto-Indo-Europeans.

    One might think that, because many haplogroups in this spreadsheet were wrong, this is also wrong; nevertheless, many haplogroups are correctly identified by Yleaf, and finding R1b-M269 in the Levant after the expansion of Sea Peoples could not be that surprising, because they were most likely related to populations of the Aegean Sea. Any other related hg. R1b (R1b-M73, R1b-V88, even R1b-V1636) wouldn’t fit as well as R1b-M269.

    sea-peoples-egypt-rameses-iii

    However, the early expansion of Proto-Indo-Aryans into the Middle East, as well as the later expansion of Armenians from the Balkans through Anatolia and of West Iranians from the east may have all potentially been related to this sample. But still, the previous linguistic and archaeological theories concerning the Philistines and the expansion of Sea Peoples in the Levant made this sample a likely (originally) Greek “Dorian” lineage, rather than the other (increasingly speculative) alternatives.

    In any case, it was obvious to anyone – that is, to anyone with a minimum knowledge of how population genomics works – that just the two samples from van den Brink (2017) couldn’t be used to get to any conclusions about the ancestral origin of these individuals (or their differences) beyond Levantine peoples, because their ancestry was essentially (i.e. statistically) the same as the other few available ancient samples from nearby regions and similar periods.

    If anything, the PCA suggested an origin of the R1b sample closer to Aegean populations relative to the J individual (see PCA above), and this should have been supported also by amateur models, without any possible confirmation (as with the ASH_IA2 cluster in this paper). However, if you have followed online discussions of Tel Shadud R1b-M269 sample since it was mentioned first on Eupedia months ago – including another wave of misguided speculation based on the ancestry of both individuals triggered by a discussion on this blog -, you have once more proof of how misleading ancestry analyses can be in the wrong hands.

    NOTE. This is the Nth proof (and that only in 2019) of how it’s best to just avoid amateur analyses and interpretations altogether, as I did in the recent publication of the books. All those who didn’t take into account whatever was commented about the ancestry of these samples haven’t lost a single bit of relevant information on Levantine peoples, and have had more time for useful reads, compared to those dedicated to endless void speculation, once again gone awfully wrong, as does everything related to cocky ancient DNA crackpottery 😉

    bronze-age-late-aegean
    Late Bronze Age population movements in the Eastern Mediterranean and the Middle East. See full map including ancient DNA samples with Y-DNA, mtDNA, and ADMIXTURE.

    Admittedly, though, even accepting the evident Mediterranean origin of this lineage, one could have argued that this sample may have been of R1b-L151 subclade, if one were inclined to support the theory that Italic peoples were behind Sea Peoples expanding east – and consequently that the ancestors of Etruscans had migrated eastward into the Aegean (e.g. into Lemnos), so that it could be asserted that Tyrsenian might have been a remnant language of an ancient population of northern Italy.

    Philistines

    Fortunately, some of the samples recovered in Feldman et al. (2019) that could be analyzed (those of the cluster ASH_IA1) offer a very specific time frame where European ancestry appeared (ca. 1250 BC) before it subsequently became fully diluted (as seen in cluster ASH_IA2) among the prevalent Levantine ancestry of the area.

    Also fortunately, this precise cluster shows another R1b-M269 sample, likely R1b-Z2103 (because it is probably xL151), and this sample together with others from the same cluster prove that the ancestry related to the original southern European incomers was:

    1. Recent, related thus to LBA population movements, as expected; and
    2. More closely related to coeval Aegeans, including Mycenaeans with Steppe-related ancestry.

    NOTE. I say “fortunately” because, as you can imagine if you have dealt with amateurish discussions long enough, without this cluster with evident Aegean ancestry and the R1b-M269 (Z2103) sample precisely associated to it, some would enter again in endless comment loops created by ancestry magicians, showing how Aegean peoples were not behind Sea Peoples, or not behind Philistines, or not behind the R1b-M269 among Philistines, depending on their specific agendas.

    aegean-sea-peoples
    Map of the Sea People invasions in the Aegean Sea and Eastern Mediterranean at the end of the Late Bronze Age (blue arrows).. Some of the major cities impacted by the raids are denoted with historical dates. Inland invasions are represented by purple arrows. From Kaniewski et al. (2011). Some of the major cities impacted by the raids are denoted with historical dates. Inland invasions are represented by purple arrows.

    The results of the paper don’t solve the question of the exact origin of all Sea Peoples (not even that of Philistines), but it is quite clear that most of those forming this seafaring confederation must have come from sites around the Aegean Sea. This supports thus the traditional origin attributed to them, including a hint at the likely expansion of Eastern Mediterranean ancestry and lineages into the Italian Peninsula precisely from the Aegean, as some oral communications have already disclosed.

    As an indirect conclusion from the findings in this paper, then, we can now more confidently support that Tyrsenian speakers most likely expanded into the Appenines and the Alps originally from a Tyrsenian-speaking LBA population from Lemnos, due to the social unrest in the whole Aegean region, and might have become heavily admixed with local Italic peoples quite quickly, as it happened with Philistines, resulting in yet another case of language expansion through (the simplistically called) elite domination.

    Conclusion

    Even more interesting than these specific findings, this paper confirms yet another hypothesis based on phylogeography, and proves once again two important starting points for ancient DNA interpretation that I have discussed extensively in this blog:

    • The rare R1b-M269 Y-chromosome lineage of Tel Shadud offered ipso facto the most relevant clue about the ancestral geographical origin of this Canaanite elite male’s paternal family, most likely from the north-west based on ancient phylogeography, which indirectly – in combination with linguistics and archaeology – supported the ancestral ethnolinguistic identification of Philistines with the Aegean and thus with (a population closest to) Ancient Greeks.
    • Ancestry analyses are often fully unreliable when assessing population movements, especially when few samples from incomplete temporal-geographical transects are assessed in isolation, because – unlike paternal (and maternal) haplogroups – ancestry might change fully within a few generations, depending on the particular anthropological setting. Their investigation is thus bound by many limitations – of design, statistical, and anthropological (i.e. archaeological and linguistic) – which are quite often not taken into account.

    These cornerstones of ancient DNA interpretation have been already demonstrated to be valid not only for Levantine populations, as in this case, but also for Balkan peoples, for Bell Beakers, for steppe populations (like Khvalynsk, Sredni Stog, Yamna, Corded Ware), for Basques, for Balto-Slavs, for Ugrians and Samoyeds, and for many other prehistoric peoples.

    I rest my case.

    Related

    Bronze Age cultures in the Tarim Basin and the elusive Proto-Tocharians

    andronovo-xiaohe-horizon

    Master’s thesis Shifting Memories: Burial Practices and Cultural Interaction in Bronze Age China: A study of the Xiaohe-Gumugou cemeteries in the Tarim Basin, by Yunyun Yang, Uppsala University, Department of Archaeology and Ancient History (2019).

    Summary excerpts, mainly from the conclusions (emphasis mine):

    Both the Xiaohe and the Gumugou groups are suggested as possibly originating from southern Siberia or Central Asia and being related to Afanasievo and Andronovo people (Han 1986, 1994; Li et al. 2010, 2015). But a latest research suggest that the Xiaohe males are genetic distinct from the Afanasievo males, considering the paternal lineages (Hollard et al. 2018). From genetic evidence, it is suggested that southern Siberia and Central Asia were dominated by Europeans during the Bronze Age. Southern Siberia was predominant by Europeans since the Bronze Age as a result of eastward migration of Kurgan people (Keyser et al. 2009). Central Asia started to have an eastern Eurasian maternal lineage that coexisted with the previous western maternal lineage from around 700 BCE (Lalueza-Fox et al. 2004). Based on the research mentioned above, we can conclude as that the Xiaohe and the Gumugou people possibly came from the southern Siberia or Central Asia.

    Origin of the Xiaohe horizon

    There are two hypotheses about the origins of the Xiaohe horizon. The “steppe hypothesis” assumes that the early settlers (Gumugou people) of the Tarim Basin came from the Afanasievo culture in the Minusinsk Basin-Altai Mountains regions (Kuz’mina et al. 2008; Mallory et al. 2008). The “oasis hypothesis” argues that the early settlers were related to the spreading of the oasis-based agricultural groups from the Bactria and Margiana parts of the southern Central Asia area (Chen et al. 1995). Both hypotheses mainly relied on the use of some materials such as animal cattle, sheep/goats, camel hair, and plant wheat, whose origins were bound to western traditions. But these proofs cannot provide enough support to claim that the Xiaohe horizon cultures were from Afanasievo or BMAC cultures, except for telling there were possible cultural connections or interactions among them. What’s more, there were no horses or potteries in the Xiaohe horizon.

    It is worth noting that Ephedra plant is commonly thought as a strong candidate of the Soma or Haoma sacred drink for the ancient Indians or Iranians. Soma is the name recorded in the Vedic Brahmanism religious literature Rigveda, Haoma in the Zoroastrianism Avesta, and indicates as a ritual drink from plant juice. The reason to address Ephedra plant to Soma-Haoma drink is mainly because of its ephedrine, which works on muscle strength, low blood pressure, (and asthma) to make people get rid of tiredness (Houben 2013). Furthermore, it is thought that Ephedra with anti-fatigue function gives gods or the dead immortality, longevity, and resurrection (Mahdihassan 1987). From a mobile consideration of Vedic Aryans perspective, it is thought Vedic Aryans made use of Ephedra, cannabis and poppy to produce Soma drink in Margiana, only Ephedra in Bactria and in Indian mountains area, but other substitutes in Indian plains (Shah 2014). From the Ephedra perspective, it is agreeable that the Xiaohe-Gumugou people were related to the Indo-Aryan peoples (Mallory et al. 1997; Wang 2017).

    gumugou-xiaohe
    The distribution map of the sites in the Xiaohe cultural horizon.

    Burial customs

    Both the Xiaohe and the Gumugou groups maintained similar burial customs, but we can distinguish a developing process from the slight diverse ways of the Gumugou cemetery to the highly consistent and advanced technology in making coffins of the Xiaohe cemetery. In terms of the dressing, the dead wore a felt cap, a pair of leather boots, a bracelet twined on the right wrist, and was wrapped in a big felt mantle. The dead in the Xiaohe cemetery also wore a loin-cloth. Commonly, both cemeteries contained burials goods of Ephedra twigs, grains of wheat and millet, grass-made baskets, animal ears (such as calf ears), and livestock. Wooden coffins in the two cemeteries were constructed in a similar way, by assembling two side-planks, two end-boards, a lid consisting of a few short straight boards, and covered with livestock hide (mainly cattle hide in the Xiaohe cemetery and sheep/goats hide in the Gumugou cemetery).

    Considering the similar and continuous burial behaviours in the two cemeteries, it can be assumed that both the Xiaohe and the Gumugou societies were stable and consistent. The Xiaohe cemetery had both the special clay-lid wooden coffins and the normal coffins in its early phase (burial layers 4th-5th), then turned to be stable and consistent with the normal coffins (burial layers 1st-3rd), and have developed better construction of the boat-shape coffins. The Gumugou cemetery contained two main burial patterns, type I; the sun-radiating-spokes burials and type II; the normal burials, which coexisted during the same time. Burials of type II were similar but not limited to strict rules. Burials in both the Xiaohe and the Gumugou cemetery were fairly heterogeneous, and the clay-lid wooden coffins in the Xiaohe cemetery and the sun-radiating-spokes burials in the Gumugou cemetery only took up in a small percentage of each cemetery. These special burial types could indicate special roles of the dead in their related societies. Either the dead had high social positions or possibly they actually had a different ancestry origin. It is argued here that the latter is something that is quite possible, considering the mixed populations in the two cemeteries.

    The sun-radiating-spokes burials share some features with a similar type of grave, constructed of circular stone kerbs of the stone-pit graves. The sun-radiating-spokes burials might represent an adaption to the local desert environment, which had better access to wood rather than stones. Circular stone kerbs with stone-pit in centre were widely seen in Bronze Age Afanasievo and Andronovo burials, and also in the late Bronze Age and early Iron Age burials along the Tian Shan. The present study suggests a high possibility that the six males buried in the sun-radiating-spokes graves came from the contemporary parallel Andronovo horizon, and kept some of their own ancestry memories in an adapted way.

    xinjiang-afanasievo-andronovo-bmac-tian-shan
    An assumption of the spreading/expansion routes stone burial construct.

    Societies

    Although the Xiaohe and Gumugou societies were stable and consistent, it does not mean that the societies were isolated, and we can see strong indications of them being open to the outside. With time, the Xiaohe population were getting even more diverse origins, as newcomers kept joining the group from outside. However, the burial behaviours in the Xiaohe cemetery did not change as a consequence if these additions. This suggests that the newcomers inherited the local burial customs, and strongly indicates that they became part of the community and adopted the new social identity, possibly through marriage. As a result, the diverse populations can well explain the coexistence of different cultural elements in the burials, e.g. cattle, sheep/goats, camel hair (from Central Asia), grains of wheat (from the west) and millet (from the east), etc.

    The Xiaohe and the Gumugou societies were similar, but the Xiaohe society developed to a more advanced level both in economy and in social structure. First, the oasis-based economic system of the Xiaohe and the Gumugou had similar husbandry, but later this was developed to different extent. Both societies mainly relied on livestock, and while the Xiaohe people favoured cattle, the Gumugou people favoured sheep/goats. The two societies also developed agriculture, which can be seen from the grains of wheat and millet. It has been shown that grains of wheat are bread wheat. The Xiaohe people also cooked porridge with millet and milk, and had dairy products.

    From these evidences, we can assume that the Xiaohe people have developed a stronger economic level. Secondly, the Xiaohe society had more distinguished gender roles, resulting in different social roles for men and women in terms of work and religions. The female and male dead were buried in a distinguished way with loin-cloths and wooden monuments. Sexual identity on a social level refers to how people consider and expect different genders to act and behave under the social and cultural framework. In the Xiaohe society, men carried out hunting tasks (creatures like vultures, badgers, lizards, snakes); women were associated to the rebirth of lives. To synthesize, a possible relation between the Xiaohe and the Gumugou societies is that they represent two parallel groups who shared similar economic systems because of the similar environment, or that there is a chronological difference where the Gumugou people may have existed earlier. The absolute dating information from the two cemeteries is insufficient to rule out the second situation.

    tarim-basin-regions
    The area division of the Tarim Basin and its surroundings (The division is made based on the mountain ranges including Altai Mountains, Tian Shan, and Kunlun Mountains, and also the distribution of ancient cemeteries in the whole Xinjiang generally.)

    Surroundings

    To place the Xiaohe horizon in the larger context of the Bronze Age burials in its surroundings, the hypothesis presented in this study is that the Xiaohe-Gumugou people might possibly represent a parallel to the Andronovo groups, with an eastward migration, that developed their own societies and ethnicities in the Tarim Basin with some ancestral memories still preserved. Considering the location and the geographical features of Xinjiang, the Altai Mountains and the Tian Shan left open access from the Eurasian Steppe to the Dzungarian Basin. The Hami Basin-the Balikun Grassland was the first intersection area to combine the possible western and eastern cultural influences. To pass by the Turpan Basin and enter into the Tarim Basin, there were two possible routes, one northern route along the southern edge of Tian Shan, and one southern route along the northern edge of Kunlun Mountains.

    In the early Bronze Age, the burials in Xinjiang had some clear typical geographic features that distinguish them from their surroundings. But from the late Bronze Age to the early Iron Age, the tradition with circular kerbs of stones with stone-pits burials expanded along the southern edge of the Tian Shan, which was a major shift of burial practice that possibly could be linked to the expansion of the Andronovo horizon or a general nomadic expansion.

    Although there were no horses or wagons found in the Xiaohe burials, the wooden horse-hoof objects were an indication of horses, which did not exist in their daily lives anymore, but possibly were related to some settlers’ ancestral memories of their nomadic origins. However, it was more important for them to assimilate to the common social identities of their new group. After people died, it was preferred to be buried in the communal cemetery. Even if the dead bodies were lost, wooden substitutes will be used in graves to represent the dead, since they believed in afterlife and thought that the end of the death is rebirth.

    Comments

    While the results of Li et al. (2010, 2015) of Xiaohe mummies regarding Y-chromosome haplogroups – showing mostly R1a(xZ93) – and radiocarbon dates of the samples are yet to be confirmed, Proto-Tocharians are known to have had contacts with Samoyeds, early Indo-Iranians (in turn in contact with the BMAC language), then into Common Tocharian with ancient Iranians, and then Indo-Aryan and Iranian languages again (for more on this, see Ged Carling‘s publications).

    The connection of the Tocharian branch with Afanasevo is essentially indisputable today, like that of Late Proto-Indo-European with late Repin/early Yamna, even more so than it was just 10 years ago, thanks to the most recent genetic investigation. The common genetic stock of Yamna and Afanasevo – as well as that of East Bell Beakers and Palaeo-Balkan peoples – fits perfectly earlier predictions based on the linguistic estimates of the separation and evolution of the diverse language communities, and the tentative attribution to Eurasian steppe-related cultures.

    early-bronze-age-tocharian-chemurchek
    Tentative identification of language groups among Early Bronze Age cultures. Pre-/Proto-Tocharian is traditionally associated with Chemurchek. See full image.

    The trail leading from Afanasevo to Common Tocharians, on the other hand, seems to be more tricky, not unlike many other Indo-European-speaking groups from Europe and Asia, whose precise evolution until their historical attestation is often unclear. Nevertheless, the eventual presence of diverse haplogroups among historical Tocharians – whether they coincide with ancient DNA recovered from BMAC, South India, Andronovo, or Bronze Age Tian Shan populations – will only be relevant to understand the genetic evolution of the speakers of Tocharian during its different stages.

    If the genetic trail backwards from known Tocharians to (earlier) unknown Common Tocharians, and forwards from known Pre-Tocharians to (later) unknown Proto-Tocharians leads unequivocally to these populations from the Xiaohe cultural horizon, this paper shows one of the mechanisms through which peoples of the Andronovo cultural horizon (or, more precisely, male lines derived from it) may have become integrated into a Tocharian-speaking population, not dissimilar to what happened in the steppes between Uralic-speaking Abashevo and Pre-Proto-Indo-Iranian-speaking Catacomb-Poltavka to form the Proto-Indo-Iranian-speaking Sintashta-Potapovka-Filatovka culture.

    As we have discussed in this blog many times over, to solve this ethnolinguistic identification of prehistoric cultures one needs to investigate ancient DNA in combination with linguistic guesstimates and the Indo-European homeland problem from a wide anthropological perspective. People not understanding this simple concept are bound to end up in some comical Tocharo-Indo-Iranian grouping related to Corded Ware ancestry from Andronovo, similar to the Celto-Ibero-Basques of elevated CEU BA ancestry and hg. R1b-P312 to the south of the Pyrenees during the Iron Age from Olalde et al. (2019), and to the Balto-Finno-Slavs of hg. R1a-Z283 and elevated “Steppe ancestry” in the BA-IA East Baltic from Saag et al. (2019)

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