Trypillia and Greece Neolithic outliers: the smoking gun of Proto-Anatolian migrations?

neolithic-migrations-khvalynsk-novodanilovka-anatolian

(Continued from the post Corded Ware culture origins: The Final Frontier).

Looking at the PCA of Wang et al. (2018), I realized that Sredni Stog / Corded Ware peoples seem to lie somewhere between:

  • the eastern steppe (i.e. Khvalynsk-Yamna); and
  • Lower Danube and Balkan cultures affected by Anatolian- and steppe-related (i.e. Khvalynsk-Novodanilovka) migrations.

This multiethnic interaction of the western steppe fits therefore the complex archaeological description of events in the North Pontic, Lower Danube, and Dnieper-Dniester regions. Here are some interesting samples related to those long-lasting contacts:

1. I3719 (mtDNA H1, Y-DNA I2a2a) Ukraine Neolithic sample from Dereivka ca. 4949–4799 BC, described in Mathieson et al. (2018) as of “entirely northwestern-Anatolian-Neolithic-related ancestry”.

2. ANI163 from Varna I ca. 4711–4550 BC (mtDNA H7a1), and I2181 from Balkans Chalcolithic (Smyadovo, in Bulgaria) ca. 4500 BC (mtDNA HV15, Y-DNA R) show the first steppe ancestry in regions known to be affected by the expansion of Suvorovo chiefs.

3. The Yamna Bulgaria outlier (Y-DNA I2a2a1b1b), 3012-2900 calBCE, shows apparently an admixture with cultures of that region (but 1,500 years later).

PCA-trypillia-greece-neolithic-outlier-anatolian
Image modified from Wang et al. (2018). Samples projected in PCA of 84 modern-day West Eurasian populations (open symbols). Previously known clusters have been marked and referenced. Marked and labelled are the Balkan samples referenced in this text An EHG and a Caucasus ‘clouds’ have been drawn, leaving Pontic-Caspian steppe and derived groups between them. See the original file here.

Trypillia and Corded Ware

4. There is one ‘Trypillia outlier’ among five samples from the Verteba cave in Wang et al. (2018): I1927 (Y-DNA G2a2b2a1a1b1a1a1, mtDNA H1b), ca. 3619-2936 BC, a sample published previously in Nikitin et al. (2017) and Mathieson et al. (2017). We were very quick to dismiss Trypillia (three samples of haplogroup G2a, one sample E) and GAC as a source of Corded Ware admixture, but archaeology clearly shows important population movements at the end of the fourth millennium between late Trypillia groups, GAC, and post-Sredni Stog populations, and genetics is showing that in both cultures, too.

I am not a fan of the ‘lack of samples’ argument, but (similar to Old Hittite samples related to all Anatolian speakers) one site is not enough to describe a culture that spanned millennia and many different early and late groups. One among five Trypillian samples (from a single site), showing a late date (ca. 3228 BC) compared to the other samples (ca. 3700 BC), and quite close to the only three Ukraine Eneolithic samples we have may mean much more than what we may a priori think, i.e. some simplistic unidirectional punctual ‘intrusion’ of steppe ancestry, and instead hint at the known close contacts of late Trypillian groups and North Pontic cultures, including also the Caucasus.

NOTE. The big difference in PCA among GAC-like Hungary LCA – EBA samples (see above two star symbols close to Ukraine Neolithic outlier in the PCA, in contrast with the other three at the bottom) may also be significant, although we don’t have any data about their culture, sites, or the relationship between them.

trypillia-verteba-cave
Location of Verteba Cave in relation to different stages and neighbouring groups of the Cucuteni-Trypillia culture. Image from the paper A Subterranean Sanctuary of the Cucuteni-Trypillia Culture in Western Ukraine, by Kadrow and Pokutta (2016).

Greece Neolithic outlier: Proto-Anatolians?

5. Especially interesting is I6423, one of the Greece Neolithic samples referred to in Wang et al. (2018), which is obviously an outlier among the three used in the paper. It does not seem to correspond to any of the ancient DNA samples published to date; it is not in Hofmanova et al. (2016), in Lazaridis et al. (2017), or in Mathieson et al. (2018).

Since the Neolithic in Greece could mean any period from ca. 6500 BC to ca. 3200 BC, I guess we are talking here about some migration related to the expansion of Khvalynsk-Novodanilovka chieftains after ca. 4500 BC, because it appears on the PCA precisely on the same spot as Varna and Smyadovo outliers, and its ADMIXTURE shows similar components

admixture-ukraine-eneolithic-greece-neolithic
Image modified from Wang et al. (2018). “ADMIXTURE results of relevant prehistoric individuals mentioned in the text (filled symbols)”. ‘Outlier’ samples referred to in this post have been marked in red. See the original file here.

So, this may be the smoking gun of Proto-Anatolian (or maybe early Common Anatolian) expansion with steppe migrants up to the border of Western Anatolia, and we may be able to get rid of those unfounded doubts about Anatolian origins once and for all…

NOTE. Also interesting seems another Greece Neolithic sample, I6420, in ADMIXTURE, although its position in the PCA (near Minoans and Mycenaeans) does not necessarily point to potential steppe influence, but rather to the extra ‘eastern (Caucasus/Iran-related) ancestry’ contribution found in Minoans and in Mycenaeans (and Anatolia Chalcolithic) compared to previous samples of the region. The third Greece Nelithic sample, I5427 (mtDNA K1a24), from Diros, Alepotrypa Cave, is dated 6005-5879 BC (mean 5892 BC), and appeared first in Mathieson et al. (2018).

greece-neolithic
Modified from Wang et al. (2018) (Greece_Neolithic in red). Supplementary Table 6. P values of rank=1 in modelling the two-way admixture in the Caucasus cluster. Right populations: Mbuti.DG, Ust_Ishim.DG, Kostenki14, MA1, Han.DG, Papuan.DG, Onge.DG, Villabruna, Vestonice16, ElMiron, Ethiopia_4500BP.SG, Karitiana.DG, Natufian, Iran_Ganj_Dareh_Neolithic. Source 2 populations in bold print are used as examples in modelling the Caucasus cluster groups (See Supplementary Table 7).
greece-neolithic-caucasus
Modified from Wang et al. (2018) (Greece_Neolithic in red). Supplementary Table 10. P values of rank=2 and ancestry proportions in modelling a three-way admixture in the Caucasus cluster testing additional contribution from Iran_ChL. Here, we used an extended set of outgroup populations populations to constrain standard errors: Right populations: Mbuti.DG, Ust_Ishim.DG, Kostenki14, MA1, Han.DG, Papuan.DG, Onge.DG, Villabruna, Vestonice16, ElMiron, Ethiopia_4500BP.SG, Karitiana.DG, Natufian, Iran_Ganj_Dareh_Neolithic, EHG, WHG, Levant_N.

If this Greece Neolithic sample is not related to Yamna migrations – and its use for statistical analysis of Caucasus samples from Wang et al. (2018) suggests that it is not – , it may have important consequences:

If it is located near the Western Anatolian coast – especially near Troy – there won’t be much to add about the potential site of entry of Common Anatolian languages into Anatolia… I have read some comments about how ‘impossible’ it was for steppe migrants and their language to ‘invade’ the more advanced cultures of Anatolia from the west, but it seems as ‘impossible’ as it was for Barbarians to invade the Roman Empire and impose their language as elites in certain regions. (And yes, we have at least one important weak political period among Middle Eastern cultures in the early 3rd millennium BC, similar to the period of the Fall of the Western Roman Empire).

indo-european-anatolian-uralic-migrations
Most likely Proto-Anatolian expansion in the North Pontic and Balkan area with Khvalynsk-Novodanilovka chieftains, including ADMIXTURE data from Wang et al. (2018).

If it is located somewhere more ‘central’ in the Greek Peninsula, then it could also be used to support the Anatolian nature of the controversial Pre-Greek (‘Pelasgian’) substrate. While we know that Greek (at least since Mycenaean) shows a strong Pre-Greek cultural and linguistic heritage (also reflected in its genetic continuity), the nature of that language is usually believed to be non-Indo-European, and Anatolian contacts are rather few and coincident with the Mycenaean period. I don’t think this sample can tell much about the Pre-Greek language, though, because – if it is really Neolithic, and comparing it with later Minoan and Mycenaean samples – it seems a clear outlier.

suvorovo-novodanilovka-expansion-europe
Heyd (2016): The Southeast European distribution of graves of the Suvorovo-Novodanilovka group and such unequipped ones mentioned in the text which can be attributed by burial custom and stratigraphic position in the barrow, plus zoomorphic and abstract animal head sceptres as well as specific maceheads with knobs as from Decea Maresului (mid-5th millennium until around 4000 BC). The site in the south-west Balkans is Suvodol-Šuplevec, Northern Macedonia (FYROM).

If it is, however, related to later Yamna migrations after ca. 3000 BC (and, like the ‘Ukraine Eneolithic’ sample that is likely from Catacomb, it is classified as Neolithic just because it cannot be attributed to precise Helladic periods), then we may be in front of the first obvious Yamna migrants in Greece. If that is the case (which I doubt), the sample wouldn’t be so informative for PIE dialectal expansions, because by now it is evident that we will find steppe ancestry and R1b-Z2103 subclades accompanying Yamna migrants in the southern Balkans, and probably well into Mycenaean Greece.

NOTE. Whatever the case, I am sure that for those fond of absurd autochthonous continuity theories, as well as for anti-steppe conspirationists, this sample will be just another good way of arguing for anything, ranging from a rejection of the Middle PIE – Late PIE division, to a support for some mythic ancient autochtonous Proto-Graeco-Anatolian group, or maybe some ancient Graeco–Indo-Slavonic split, or whatever new dialectal stage one can invent to support the own genealogical fantasies…

So, if it actually is a Neolithic sample, let’s hope that it shows a clear R1b-M269 (xL23 or early L23) subclade distinct from those (likely Z2103) expanded later with Late PIE-speaking Yamna (and probably to be found among Mycenaeans), so that there can be no more place for ethnic fantasies.

EDIT (28 JUL 2018): Added information on Greece Neolithic and Trypillia samples

Related

Corded Ware culture origins: The Final Frontier

corded-ware-yamna-bell-beaker

As you can imagine from my latest posts (on kurgan origins and on Sredni Stog), I am right now in the middle of a revision of the Corded Ware culture for my Indo-European demic diffusion model, to see if I can add something new to the draft. And, as you can see, even with ancient DNA on the table, the precise origin of the Corded Ware migrants – in spite of the imaginative efforts of the Copenhagen group to control the narrative – are still unknown.

Corded Ware origins

The main objects of study in Corded Ware origins are necessarily the region where the oldest Corded Ware vessels appeared, Lesser Poland, as well as the adjacent (traditionally considered Proto-Corded Ware regions) Volhynia, Podolia, and upper Dniester river basin. These are some relevant points, continuing where I left the Eneolithic steppe developments (following Szmyt 1999, Rassamakin 1999, Kadrow 2008, Furholt 2014):

gac-trypillia-yamna-usatovo
Kadrow (2008). Cultural interactions around Carpathians at the beginnings of the 3rd millennium BC: 1 – Globular Amphora culture; 2 – Sofievka group of Trypillia culture; 3 – Funnel Beaker culture; 4 – Baden culture; 5 – Kostolac culture; 6 – Coţofeni culture; 7 – Cernavoda II culture; 8 – Yamnaya culture and Usatovo group of Trypillia culture (apud Kadrow, 2001).
  • More frequent contacts were seen ca. 3500-3000 BC, with an interaction showing multidirectional migrations of larger human groups in the centuries around 3000 BC, involving a significant part of the population of central-east Europe.
  • The easternmost area of the Funnel Beaker culture had become more Baden-like with the expansion of the Baden culture in its western area ca. 3300-2900 BC (with findings up to 2600 BC), and these younger groups with Baden features moved increasingly into the western part of Volhynia.
  • The influence of the neighbouring Trypillian culture is seen in the eastern parts of Volhynia, from ca. 3000 BC, either from a younger phase CII (cf. Troyaniv, Koshilivtsy, Brînzeni, Zhvaniets, or Vychvatintsy) or later groups (cf. Gorodsk, Kasperivtsy, Sofievka, Horodiştea-Folteşti, Usatovo).
  • In the forest-steppe zone, herding and hunting activities intensified, while agricultural traditions were preserved, as shown by the Sofievka, Kasperivtsy, and Gorodsk groups. From the end of the 4th millennium BC mobile parts of the late Trypillian populations moved to the steppe zone, absorbing more and more steppe elements; among others, cord ornamentation (in Vykhvatintsy, Troyaniv, and Gorodsk groups), pottery forms (Vykhvatintsy, which served as prototype for the Thuringian Apmphorae, dispersed along the Dniester river, too), flat burials with bodies in contracted position on the left or right side (Vykhvatintsy, reminding of Polgár culture different male-female position, and later Corded Ware burials, and also Lower Mikhailovka, under a mound without stone constructions). At the end of the Trypillia culture, its agricultural system collapsed completely.
gac-trypillia-usatovo-corded-ware
Globular Amphorae culture „exodus” to the Danube Delta: a – Globular Amphorae culture; b – GAC (1), Gorodsk (2), Vykhvatintsy (3) and Usatovo (4) groups of Trypillia culture; c – Coţofeni culture; d – northern border of the late phase of Baden culture;red arrows – direction of Globular Amphora culture expansion; blue arrow – direction of „reflux” of Globular Amphora culture (apud Włodarczak, 2008, with changes).
  • Slash and burn techniques of agriculture – especially those practiced by Trypillian and Funnel Beaker populations – must have intensified effects of natural growth of humidity (ca. 3400-2400), increasing fluvial activities in west Ukrainian river valleys, and increasing deforestation processes, which favoured pastoralism and nomadisation of the settlement system, and a consequent change of the social structure
  • At the same time, Yamna communities expanded along the lower and central Danube to the west, while the populations of the late phase of the Baden culture took the opposite direction and reached as far as Kiev in the north-east, contributing to the culture of the Sofievka group.
  • Globular Amphora communities migrated from the north-west, from eastern Poland, towards the Danube Delta and as far as the Dnieper in the east, destroying the primary structures of the communities in the supposed cradle territories of the Corded Ware culture. These communities found refuge and conditions for further development in south-eastern margin zone of the Funnel Beaker culture territories, penetrating at first the upper parts of the loess uplands like typical Funnel Beaker sites, but on the margins of their range, and also on areas avoided by Funnel Beaker settlement agglomerations. They brought with them the so-called Thuringian amphora up to Lesser Poland, borrowed from the late Trypillian Usatovo group. This resulted in the Złota culture, which eventually gave rise to the A-Amphorae.
funnelbeaker-trypillia-corded-ware
Map of territorial ranges of Funnel Beaker Culture (and its settlement concentrations in Lesser Poland), local Tripolyan groups and Corded Ware Culture settlements (■) at the turn of the 4th/3rd millennia BC.

In the end, we are left with this information about the oldest CWC (Furholt 2014):

  • The earliest radiocarbon-dated groups associated with the Corded Ware culture come from new single graves from Jutland in Denmark and Northern Germany, ca. 2900 BC. This Early Single Grave culture is associated with the appearance of individual graves (some time after the decline of the megalithic constructions), composed of a small round barrow and a new gender-differentiated burial practice emphasising male individuals orientated west-east (with regional exceptions), combined with the internment with new local battle-axe types (A-Axe). However, there is no single type of burial or burial custom in Corded Ware:
    • In southern Sweden the prevailing orientation is north-east – south-west, and south-north, contrary to the supposed rule male individuals are regularly deposited on their left and females on their right side.
    • In the Danish Isles and north-eastern Germany, the Final Neolithic / Single Grave Period is characterized by a majority of megalithic graves, with only some single graves from typical barrows. In south Germany, west-east and collective burials prevail, while in Switzerland no graves are found.
    • In Kujawia (south-eastern Poland), Hesse (Germany), or the Baltic, west-east orientation and gender differentiation cannot be proven statistically.
corded-ware-regions-main
Furholt (2014). Map of the Corded Ware regions of central Europe. The dark shading indicates those regions where Corded Ware burial rituals are present regularly
  • The oldest Corded Ware vessels (the A-Amphorae, which define the A-Horizon of the CWC) come probably from the Złota (or a related) group in Lesser Poland, where a mixed archaeological culture connecting Funnel Beaker, Baden, Globular Amphorae and Corded Ware appears ca. 2900-2600 BC. No cultural (typological) break is seen between earlier Globular Amphorae and the first Corded Ware Amphorae, but rather a continuum of traits and characteristics among the recovered vessels. This strengthens the connection of Corded Ware with Globular Amphorae peoples. The A-horizon expanded thus probably from Lesser Poland ca. 2800-2600, as seen in local contexts.
  • And of course we have a third way of defining Corded Ware individuals, which is the presence of herding, and thus a transition from hunter-gatherers to agropastoralists. This is how some Baltic Late Neolithic individuals with no archaeological data have been classified as members of the Corded Ware culture: Even though no cultural remains were extracted with the two ‘outlier’ individuals, their haplogroup and ancestry point to a direct origin in or around the steppe and forest-steppe region (yes, that risks circular reasoning).
globular-amphorae-corded-ware-zlota-amphorae
Correspondence analysis of amphorae from the Złota-graveyards reveals that there is no typological break between Globular Amphorae and Corded Ware Amphorae, including ‘Strichbündelamphorae’ (after Furholt 2008)

Corded Ware peoples in genetics

So, no clear origin of Corded Ware migrants, a lot of data pointing to intense migrations and interaction among GAC, Trypillia and the western steppe population (remember Kristiansen’s ‘long-lasting GAC-CWC connection’, now ignored to favour their Yamnaya admixture™ concept), and also three ways of defining Corded Ware culture…

Maybe genetics can help:

Ukraine Neolithic cultures – mainly from Dereivka – show haplogroups R1b-V88, R1a1, and R1b-L754 (xP297, xM269), which is similar to the haplogroup distribution found in Ukraine Mesolithic, but apparently with an expanding group marked by haplogroup I2a2a1b1 (possibly I2a2a1b1b).

The first thing that stands out about Ukraine Eneolithic samples is that only two of them can be said to be really Ukraine Eneolithic (i.e. from “Sredni Stog”-related groups):

  • I5876 (Y-DNA R1a-Z93(Y3+), mtDNA U5a2a), from Alexandria, 4045-3974 calBCE (5215±20BP, PSUAMS-2832)
  • I4110 (mtDN AJ2b1), from Dereivka, 3634-3377 calBCE (4725±25 BP, UCIAMS-186349), J2b1

The other two samples are quite late, and in fact one of them is clearly too late (maybe from the Catacomb culture):

  • I5882 (mtDNA U5a2a), from Dereivka, 3264-2929 calBCE (4420±20BP, PSUAMS-2826)
  • I3499 (Y-DNA R1b-Z2103, mtDNA T2e), from Dereivka, 2890-2696 calBCE (4195±20BP, PSUAMS-2828)

Corded Ware samples from Mittnik et al. (2018) offer very wide radiocarbon dates, so it is unclear which of them may be the oldest one. Most of them cluster closely to the older Ukraine Eneolithic sample I5876, but also to later steppe_MLBA samples i.e. Sintashta, Potapovka, and especially Srubna and Andronovo). This points to a genetic continuity from Pre-Corded Ware to Classic and late Corded Ware peoples. Therefore, much like Khvalynsk-Yamna and apparently many other Neolithic cultures, these peoples did not really admix; at least not with the male population.

pca-mittnik-late-neolithic
File modified by me from Mittnik et al. (2018) to include the approximate position of the most common ancestral components, and an identification of potential outliers. Zoomed-in version of the European Late Neolithic and Bronze Age samples. “Principal components analysis of 1012 present-day West Eurasians (grey points, modern Baltic populations in dark grey) with 294 projected published ancient and 38 ancient North European samples introduced in this study (marked with a red outline).

Lucky for us, even though the culture remains undefined, haplogroup R1a-Z645 seems like a unifying trait, as I said long ago, so we only have to wait for more samples to trace their origin. Nevertheless, it is clear that Corded Ware may not have been as genetically homogeneous as Khvalynsk, Yamna and Yamna-related cultures, further supporting its archaeological complexity:

  • Jagodno1 and Jagodno2 (Silesia), dated ca. 2800 BC, show haplogroup G? and I/J? – compatible with an origin of CWC in common with Trypillia (which shows 3 samples of haplogroup G2a2b2a, and one E) and Ukraine Neolithic (showing the expansion of I2a2a1b1 subclades).
  • I7272, from Brandýsek (Czech Republic), dated ca. 2900-2200 BC shows haplogroup I2a2a2 (compatible with an origin in Ukraine Neolithic peoples – this haplogroup is also found in Yamna Kalmykia and in the Yamna Bulgaria outlier, i.e. late western samples from the Early Yamna culture).

NOTE. This precise subclade is only present to date in Chalcolithic samples from Iberia, which points (possibly like the Esperstedt family) to local Central European haplogroups integrated in a mixed Proto-Corded Ware population. The upper subclade I2a2a is found in Neolithic samples from Iberia, the British Isles, Hungary (Koros EN, ALPc), and also south-east European Mesolithic and Neolithic samples.

  • RISE1, from Oblaczkowo (Greater Poland), ca. 2865-2578 BC, shows haplogroup R1b1.
  • The Esperstedt family samples have been analysed as R1a-M417 (xZ645), although the supposed ‘xZ645’ has not been confirmed – not even in the risky new Y-calls from Wang et al. (2018) supplementary materials.
corded-ware-regions-network
Network analysis based on the quantitative occurrence of Corded Ware pottery forms, pottery ornamentation styles, tools,
weapons and ornaments as stated in Table 1, based on the catalogues given in Table 2, line thickness representing similarity

Maybe this heterogeneity is a problem of better defining the culture, but from what we can see the oldest CWC regions and the unifying ‘Corded Ware province’ – formed after ca. 2700 BC by Jutland and Northern Germany, the Netherlands, Saale, Bohemia, Austria and the Upper Danube regions – are for the moment not the most genetically homogeneous groups.

Homogeneity comes later – which we may tentatively identify with the expansion of the A-horizon from the northern Dnieper-Dniester and Lesser Poland area – , as seen around the Baltic (like the Battle Axe culture) with R1a-Z283 subclades, and around Sintashta (i.e. probably Abashevo – Balanovo) with R1a-Z93 subclades, which is compatible with the late spread of different Z645 groups (and potentially a unifying language) .

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Consequences of O&M 2018 (II): The unsolved nature of Suvorovo-Novodanilovka chiefs, and the route of Proto-Anatolian expansion

neolithic_steppe-suvorovo

This is part of a series of posts analyzing the findings of the recent Nature papers Olalde et al.(2018) and Mathieson et al.(2018) (abbreviated O&M 2018).

I already expressed my predictions for 2018. One of the most interesting questions among them is the identification of the early Anatolian offshoot, and this is – I believe – where Genomics has the most to say in Indo-European migrations.

Linguistics and Archaeology had already a mainstream account from Late PIE/Yamna onwards, and it has been proven right in Genomic investigation. There is, however, no consensus on Indo-Hittite.

Suvorovo-Novodanilovka

Apart from the Anatolian homeland hypothesis and its westward migration (as referenced e.g. by Lazaridis et al. 2017), the other possibility including the most likely steppe homeland is that Proto-Anatolian spread through the Balkans, and must have separated from Khvalynsk and travelled first westward through the North Pontic region, and then southward to Ezero.

EDIT (10 MAR 2018): The Anatolian westward route within the steppe homeland model refers to the possibility that Proto-Anatolian spread south through the Caucasus, and then westward through Anatolia, as suggested e.g. originally by Marija Gimbutas for Maykop, as a link in the Caucasus.

We all know that this Khvalynsk -> Novodanilovka-Suvorovo -> Cernavoda -> Ezero -> Troy migration model proposed by Anthony shows no conspicuous chain in Archaeology, but obvious contacts (including Genomics) are seen among some of these neighbouring cultures in different times.

We know that remains of Suvorovo-Novodanilovka culture of chiefs emerged around 4400-4200 BC among ordinary local Sredni Stog settlements:

  • the Novodanilovka rich burials in the steppes, near the Dnieper,
  • and the Suvorovo group in the Danube delta, roughly coinciding with the massive abandonment of old tell settlements in the area.

One of the strongest cultural connections between Khvalynsk and Suvorovo Novodanilovka chiefs is the similar polished stone mace-heads shaped like horse heads found in both cultures, a typical steppe prestige object going back to the east Pontic-Caspian steppe beginning ca. 5000-4800 BC.

Its finding in the Danube valley may have signalled the expansion of horse riding, which is compatible with the finding of ancient domesticated horses in the region. Horses were not important in Old European cultures, and it seems that they weren’t in Sredni Stog or Kvitjana either.

sredni-stog-suvorovo-novodanilovka-cernavoda
Steppe and Danubian sites at the time: of the Suvorovo-Novodanilovka intrusion, about 4200-3900 BC. David W. Anthony (2007).

NOTE. Telegin, the main source of knowledge in Ukraine prehistoric cultures for Anthony, was eventually convinced that Surovovo-Novodanilovka was a separate culture. However, for Anthony (using Telegin’s first impressions), it may have been a wealthy elite among Sredni Stog peoples. Anthony considers Sredni Stog to have been also influenced by Khvalynsk, and thus potentially related to the Suvorovo-Novodanilovka chiefs.

Nevertheless, he obviously cannot link North Pontic Eneolithic cultures to Khvalynsk nor to horse riding – whilst he clearly assumes horse riding for Novodanilovka-Suvorovo chiefs – , and he does not link North Pontic cultures to later expansions of Late Proto-Indo-Europeans from late Khvalynsk and Yamna, either.

The question here for Anthony (as with further Proto-Anatolian expansions described in his 2007 book), in my opinion, was to offer a plausible string of connections between Khvalynsk and Anatolia, and the simplest connection one can make among steppe cultures is a general, broad community between North Pontic and North Caspian cultures. That way, the knot tying Khvalynsk to the Danube seems stronger, whatever the origin of Suvorovo-Novodanilovka chiefs.

If, however, a direct genetic connection is made between Suvorovo-Novodanilovka chiefs and Khvalynsk – as in its association with R1b-M269 and R1b-L23 lineages – , there will be little need to include Sredni Stog or any other intermediate culture in the equation.

We have already seen a movement of steppe ancestry into mainland Greece, and I would not be surprised if a parallel movement could be seen from Ezero to Troy (or a neighbouring North-West Anatolian region), so that the final migration of Common Anatolian had in fact been triggered by the massive steppe migrations during the Chalcolithic.

NOTE. Whereas we are certain to find R1b-L23 subclades in the direct Balkan migrations from Yamna, the link of steppe->Anatolia migrations may be a little trickier: even if we find out that the Suvorovo-Novodanilovka expansion was associated with an expansion and reduction of haplogroup variability (to haplogroups R1b-M269 and R1b-L23), we don’t know yet if the ca. 1,500 years passed (and the different cultural and population changes occurred) between Proto-Anatolian and Common Anatolian migrations may have impacted the main haplogroup composition of both communities.

O&M 2018

A probably unsurprising – because of its previously known admixture and PCA – , but nevertheless disappointing finding came from the Y-SNP call of the haplogroup R1 found in Varna (R1b-V88, given first by Genetiker), leaving us with no new haplogroup data standing out for this period.

This sample’s lack of obvious genetic links with the steppe and early date didn’t deter me from believing it could show subclade M269, and thus a sign of incoming Suvorovo chiefs in the region. After all, R1b-P297 subclades seemed to have almost disappeared from the Balkans by that time, and we know that assessments based only on ancestral components and PCA clusters are not infallible – we are seeing that in many, many samples already.

suvorovo-scepters
1—39 — sceptre bearers of the type Giurgiuleşti and Suvorovo; 40—60 — Gumelniţa-Varna-Bolgrad-Aldeni cultural sphere; 61 — Fălciu; 62 — Cainari; 63 — Giurgiuleşti; 64 — Suvorovo; 65 — Casimcea; 66 — Kjulevča; 67 — Reka Devnja; 68 — Drama; 69 — Gonova Mogila; 70 — Reževo. Țerna S., Govedarica B. (2016)

NOTE. In fact, the first time I checked Mathieson et al. (2018) supplementary tables I thought that the ‘Ukraine_Eneolithic’ sample of R1b-L23 subclade was ‘it’: the first clear proof in ancient samples of incoming Suvorovo chiefs from Khvalynsk I was looking for…Until I realized its date, and that it was more likely a Late Yamna (or Catacomb) sample.

Steppe ancestry is found in the Varna and Smyadovo outliers, though, and these samples cluster closely to Ukraine Eneolithic samples (which are among Khvalynsk, Ukraine Neolithic, and Anatolia Neolithic clusters), so some population movement must have happened around or before that time in the region, and it is obvious that it happened from east to west.

It remains to be seen, therefore:

a) If the incoming Suvorovo-Novodanilovka chiefs (most likely originally from Khvalynsk) dominating over North Pontic and Danube regions show – as I bet – R1b-M269, and possibly also early R1b-L23* subclades,

b) Or else they still show mixed lineages, reflecting an older admixed population of the Pontic-Caspian steppe – as the early Khvalynsk and Ukraine Eneolithic samples we have now.

NOTE. Even though my preferred model of migration is through the Balkans – due to the many east-west migrations seen from the steppe into Europe – , there is no general consensus here because of the lack of solid anthropological models, and there are cultural links found also between the steppe and Anatolia through the Caucasus, so the question remains open.

Related:

The significance of the Tollense Valley in Bronze Age North-East Germany

bronze-age-tollense-battle

An early Bronze Age causeway in the Tollense Valley, Mecklenburg-Western Pomerania – The starting point of a violent conflict 3300 years ago?, by Jantzen et al. (BERICHT RGK 95, 2014).

Excerpt (emphasis mine):

The causeway in the Tollense Valley, built of timber, stones, turf and sand, and documented over a length of more than 100 m, represents a unique finding from northern Germany. For the first time, part of a Bronze Age network of land routes could be made visible in the southern Baltic area.

Together with the other evidence, the archaeological remains suggest the construction of elaborate trackways and, in some cases, even bridges in the Bronze Age. The Tollense Valley causeway can probably be attributed to the wish or the necessity to be able to cross the Tollense Valley regardless of weather and seasonally differing water level conditions. Its location, situated at a narrow section of the Tollense Valley, offered a prime position for the construction of a permanent crossing of the floodplain on the eastern bank. It is quite possible that a bridge was also part of this.

The complex causeway construction that was likely used and maintained for centuries suggests a significance of the crossing beyond just local. In this context, finds from the valley relating to Bronze Age metal crafts are of interest: along with the scrap metal hoard mentioned above found in the immediate area of the crossing, attention is drawn to a hoard from Golchen comprising an unusual accumulation of tools, as well as to two tin rings found in the same archaeological layer as the Bronze Age skeletal remains. These finds could indicate that metal crafts were of particular significance in the Tollense Valley and its surrounding areas. The middle section of the Tollense Valley that is the focus of attention here could have derived special significance from its role as a crossroads.

The documented pathway, which may have been the starting point of the violent conflict described above, not only contributes to the understanding of the entire findings and the reconstruction of the events in the early 13th century BCE in the Tollense Valley; its context also sheds new light on the cross-regional infrastructure of North-East Germany in the (Early) Bronze Age. Unfortunately, there currently is little further information to integrate it into the broader network of supraregional communication and traffic routes.

The region around the famous barrow of Seddin in Brandenburg is a further example for the significance of river systems for regional power and the exchange of goods. Similarly, the River Tollense could have played a role in the flow of commodities; the causeway at the Kessin 12 site offers a possible connection of the south-north water transportation route via the Tollense River to the Baltic Sea with an east-west land route linking the River Oder estuary region and the Mecklenburg Lake District.

The Lake District was of great importance from the Early Bronze Age; here independent bronze production was established early on. Diversity analyses indicate a shift of regions of innovation during the transition from the 3rd to the 2nd millennium BCE, as the southern Baltic Sea region and the region east of the river Oder clearly also became more important. Early Bronze Age imports from south-east Europe highlight the significance of the region west of the Oder estuary. The Tollense Valley likely played a role in connecting these areas. Therefore, the violent events in the Tollense Valley could also be seen as a result of its strategic significance for the power structure of North-East Germany and the regions on the southern Baltic coast during the Early Bronze Age.

tollensee-valley
Model of the Tollense Valley with the position of pathway (R. Scholz, using a digital model of the valley made by ArcTron [©]).

See also:

Luwians: the missing link with the Aegean Bronze Age, including Troy and the Sea Peoples

luwians-sea-peoples

A very interesting monograph on the Luwian Civilization, and its potential connection with Wilusa (Troy) from the end of the third millennium and throughout the Bronze Age: The Luwian Civilization – The Missing Link in the Aegean Bronze Age, by Eberhard Zangger (also available in German: Die luwische Kultur – Das fehlende Element in der Ägäischen Bronzezeit).

Abstract:

Aegean prehistory suffered from a bias when the field was conceived 100 years ago and subsequent research has never questioned the fundamental paradigms of the discipline. As a consequence, only one third of the Aegean coasts have thus far been attributed to ancient civilizations. This leaves tremendous opportunities for current and future generations of archaeologists – on the somewhat neglected eastern side of the Aegean. Practically all contemporary sources indicate that Late Bronze Age petty states used to form military alliances. The Assuwa league, mentioned in Hittite texts from around 1400 BCE, is a good example, but so are the mercenary forces mustered by Muwatalli and the various accounts of united tribes from the Aegean (aka “Sea Peoples”) and even – in later recollections of past events – Homer’s catalogues of ships and Trojan contingents. “The Luwian Civilization” argues that such a coalition of the petty states in western Asia Minor may have succeeded in bringing down the Hittite hegemony over central Asia Minor.

Excerpt (from the Introduction):

Possibly due to its vast extent and complicated topography, for thousands of years the majority of western Asia Minor was politically fragmented into many petty kingdoms and principalities. This certainly weakened the region in its economic and political significance, but it also delayed the recognition of a more or less consistent Luwian culture.

From a linguistics point of view, however, the Luwian culture is relatively well known. From about 2000 BCE Luwian personal names and loanwords appear in Assyrian documents retrieved from the trading town Kültepe (also Kaniš or Neša). Assyrian merchants who lived in Asia Minor at the time described the indigenous population as nuwa’um, corresponding to “Luwians.” At about the same time, early Hittite settlements arose a little further north at the upper Kızılırmak River. In documents from the Hittite capital Hattuša written in Akkadian cuneiform, western Asia Minor is originally called Luwiya. Hittite laws and other documents also contain references to translations into “Luwian language.” Accordingly, Luwian was spoken in various dialects throughout southern and western Anatolia. The language belongs to the Anatolian branch of Indo-European languages. It was recorded in Akkadian cuneiform on the one hand, but also in its own hieroglyphic script, one that was used over a timespan of at least 1400 years (2000–600 BCE). Luwian hieroglyphic ranks, therefore, as the first script in which an Indo-European language is transcribed. The people using this script and speaking a Luwian language lived during the Bronze and Early Iron Age in Asia Minor and northern Syria.

luwian-language
The region where Luwian was spoken at the end of the Bronze Age was much larger than the one where
Hittite was spoken.

Highly recommended for anyone interested in assessing where and when samples with steppe admixture and Y-DNA haplogroup R1b-M269 might appear next in Anatolian samples – and how to interpret them correctly.

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