“Steppe people seem not to have penetrated South Asia”

indo-iranian-sintashta-uralic-migrations

Open access structured abstract for The first horse herders and the impact of early Bronze Age steppe expansions into Asia from Damgaard et al. Science (2018) 360(6396):eaar7711.

Abstract (emphasis mine):

The Eurasian steppes reach from the Ukraine in Europe to Mongolia and China. Over the past 5000 years, these flat grasslands were thought to be the route for the ebb and flow of migrant humans, their horses, and their languages. de Barros Damgaard et al. probed whole-genome sequences from the remains of 74 individuals found across this region. Although there is evidence for migration into Europe from the steppes, the details of human movements are complex and involve independent acquisitions of horse cultures. Furthermore, it appears that the Indo-European Hittite language derived from Anatolia, not the steppes. The steppe people seem not to have penetrated South Asia. Genetic evidence indicates an independent history involving western Eurasian admixture into ancient South Asian peoples.

INTRODUCTION
According to the commonly accepted “steppe hypothesis,” the initial spread of Indo-European (IE) languages into both Europe and Asia took place with migrations of Early Bronze Age Yamnaya pastoralists from the Pontic-Caspian steppe. This is believed to have been enabled by horse domestication, which revolutionized transport and warfare. Although in Europe there is much support for the steppe hypothesis, the impact of Early Bronze Age Western steppe pastoralists in Asia, including Anatolia and South Asia, remains less well understood, with limited archaeological evidence for their presence. Furthermore, the earliest secure evidence of horse husbandry comes from the Botai culture of Central Asia, whereas direct evidence for Yamnaya equestrianism remains elusive.

RATIONALE
We investigated the genetic impact of Early Bronze Age migrations into Asia and interpret our findings in relation to the steppe hypothesis and early spread of IE languages. We generated whole-genome shotgun sequence data (~1 to 25 X average coverage) for 74 ancient individuals from Inner Asia and Anatolia, as well as 41 high-coverage present-day genomes from 17 Central Asian ethnicities.

damgaard-south-asia
Model-based admixture proportions for selected ancient and present-day individuals, assuming K = 6, shown with their corresponding geographical locations. Ancient groups are represented by larger admixture plots, with those sequenced in the present work surrounded by black borders and others used for providing context with blue borders. Present-day South Asian groups are represented by smaller admixture plots with dark red borders.

RESULTS
We show that the population at Botai associated with the earliest evidence for horse husbandry derived from an ancient hunter-gatherer ancestry previously seen in the Upper Paleolithic Mal’ta (MA1) and was deeply diverged from the Western steppe pastoralists. They form part of a previously undescribed west-to-east cline of Holocene prehistoric steppe genetic ancestry in which Botai, Central Asians, and Baikal groups can be modeled with different amounts of Eastern hunter-gatherer (EHG) and Ancient East Asian genetic ancestry represented by Baikal_EN.

In Anatolia, Bronze Age samples, including from Hittite speaking settlements associated with the first written evidence of IE languages, show genetic continuity with preceding Anatolian Copper Age (CA) samples and have substantial Caucasian hunter-gatherer (CHG)–related ancestry but no evidence of direct steppe admixture.

In South Asia, we identified at least two distinct waves of admixture from the west, the first occurring from a source related to the Copper Age Namazga farming culture from the southern edge of the steppe, who exhibit both the Iranian and the EHG components found in many contemporary Pakistani and Indian groups from across the subcontinent. The second came from Late Bronze Age steppe sources, with a genetic impact that is more localized in the north and west.

CONCLUSION
Our findings reveal that the early spread of Yamnaya Bronze Age pastoralists had limited genetic impact in Anatolia as well as Central and South Asia. As such, the Asian story of Early Bronze Age expansions differs from that of Europe. Intriguingly, we find that direct descendants of Upper Paleolithic hunter-gatherers of Central Asia, now extinct as a separate lineage, survived well into the Bronze Age. These groups likely engaged in early horse domestication as a prey-route transition from hunting to herding, as otherwise seen for reindeer. Our findings further suggest that West Eurasian ancestry entered South Asia before and after, rather than during, the initial expansion of western steppe pastoralists, with the later event consistent with a Late Bronze Age entry of IE languages into South Asia. Finally, the lack of steppe ancestry in samples from Anatolia indicates that the spread of the earliest branch of IE languages into that region was not associated with a major population migration from the steppe.

I think the wording of the abstract is weird, but consequent with their samples and results, so probably just clickbait / citebait for Indian journalists and social networks, or maybe a new attempt to ‘show respect for the sensibilities of Indians’ related to the artificially magnified “AIT vs. OIT” controversy, that is only present in India.

However, everything is possible, since it is brought to you by the same Danish group who proposed the Yamnaya ancestral component™, the CHG = Indo-European (and simultaneously EHG in Maykop = Anatolian??), and now also the CWC/R1a = Indo-European & Volosovo = Uralic

Here is the reaction of Narasimhan: Narasimhan has deleted the Tweet, it basically questioned the sentence that steppe people did not penetrate South Asia.

Related

Sredni Stog, Proto-Corded Ware, and their “steppe admixture”

steppe-eneolithic-migrations

Once the haplogroups of the announced West Yamna and Yamna settlers in Hungary and Khvalynsk from Ekaterinovka appear, it is to be expected that there won’t be much discussion on the Y-DNA bottlenecks that affected Khvalynsk – Yamna migrations.

So let’s cut to the chase and see where Corded Ware peoples (mainly of R1a-Z645 subclades) got their so-called “steppe admixture” different from that of Yamna. Because, as you might have realized by now, Sredni Stog – and consequently Corded Ware – remains nowadays an undefined (archaeological) mess.

Rassamakin explains it quite well, in the chapter Eneolithic of the Black Sea Steppe; In Levine M., Rassamakin Yu., Kislenko A. and Tatarintseva N., 1999. Late Prehistoric Exploitation of the Eurasian Steppe. McDonald Institute Monographs, University of Cambridge.

NOTE. These are only certain relevant excerpts. The whole chapter is worth a thorough read, whatever position you hold regarding steppe expansions. In fact, he supports the Skelya cultural (macro-)group instead of Khvalynsk-Novodanilovka vs. Sredni Stog, he does not believe in significant expansions from the east (but in local movements and a ‘general evolution’ of Pontic-Caspian steppe cultures to Early Yamna), and offers e.g. the presence of copper and trade from the west (and its poor presence in the east) as an example of the importance of the North Pontic area vis-à-vis Khvalynsk/Repin. Not an interested party in supporting Gimbutas or Anthony, then, if you fear that.

Cultural groups in the North Pontic area

Telegin divided the Sredny Stog culture into three local variants – the Dnepr Culture variant, the Oskol-Donets (Aleksandriya) Culture variant, and the Lower Don (Konstantinovka) Culture variant. He elaborated a periodization based on the evolution of decorative motifs in the pottery assemblages.

At first, the internal contradictions of the Sredny Stog culture were not accorded particular prominence, despite clear intimations of problems when, for example, sites like the settlement of Konstantinovka on the Lower Don, was identified as actually belonging to another, independent culture (Kiyashko 1974). The first real blow to the integrity of the Sredny Stog culture was dealt by Telegin himself, when he removed five Novodanilovka-type sites, and accorded them the status of an independent cultural phenomenon (Telegin 1985a). Until that point, sites of this type had were customarily considered to be within the framework of the late group of Sredny Stog cemeteries, despite having been for long regarded by some as representative of an earlier, independent cultural group (Movsha & Chebotarenko 1969; Zbenovich 1973, 74-5; Gimbutas, Merpert and Danilenko passim). Indeed, it was unclear why these cemeteries had initially been assigned to the Late, rather than the Early, Sredny Stog culture. Now these sites were mechanically stripped out of the one system, but their place in the new system was not clearly defined.

rassamakin-skelya-culture
Rassamakin (1999) concept of cultural development of burial rituals in the North Pontic steppe.

Thus a paradox arose. Sites that had served to a considerable extent as the initial basis for the Sredny Stog culture, for the elaboration of its periodization and chronology, were now accepted as forming the core of an essentially different culture. Because of this, by the mid 1980s, both the Sredny Stog culture and the Eneolithic systematization as a whole were becoming rather amorphous. Essentially, the Sredny Stog culture was associated in the minds of many researchers solely with the settlement site at Dereivka, while they had only a confused and indistinct idea of the nature of early Sredny Stog sites. (…) Ultimately a situation developed where all attempts to view new evidence, new local groups, or even cultures through the prism of the Sredny Stog culture were futile, since researchers were unclear about of the essence of the culture itself, and often qualified themselves in footnotes with references to ‘preCorded Ware’ or ‘Corded Ware’ stages, or by relating their observations back directly to the specific sites of Sredny Stog II or Dereivka.

Thus, in the Middle Eneolithic, a number of independent cultures (Kvityana, Repin, Konstantinovka, and, to some degree, Dereivka, Cernavoda and Lower Mikhailovka) emerged in the region that had in the Early Eneolithic been occupied by the Skelya culture, either as lineal successors to this culture or under its influence. But the principal stimuli in this period were the Tripolye tribes, direct imports from whom reach the southern zone of the Dnepr left bank.

It is apparent that, for all their conceptual differences, if we remove Danilenko’s subdivisions, Telegin’s and Danilenko’s models are identical in terms of site periodization and sequence: first Kvityana, then Sredny Stog II, and finally Dereivka.

The North Pontic area in the Eneolithic (4000-3500 BC)

kvityana-dereivka-repin-trypolie-maykop
The Kvityana and Dereivka cultures in relation to other sites: 1) Molyukhov Bugor (settlement); 2) Dereivka (settlement); 3) Aleksandriya (settlement); 4) Minevsky Yar (settlement); 5) Khutor Repin (settlement).

Tripolye influence is seen most clearly in the development of the Lower Mikhailovka culture and a new burial rite which spread as far as the Molochnaya. Changes are apparent in kurgan architecture; that is, in the construction of stone chambers, sanctuaries comprising upright elements, and ring-shaped ditches (Rassamakin 1990; 1993; 1994; Pleshivenko & Rassamakin 1994 ). Lower Mikhailovka sites in the northwestern Black Sea coast region are known by a whole series of different designations, one of which, as I have already noted above, is ‘the Bessarabian variant of the Cernavoda I culture’ (Manzura 1993).

The formation of the Kvityana culture should be considered both in the context of the development of the Lower Mikhailovka culture, and in terms of the influence of the Sredny Stog II pottery assemblage. The first is manifested in the development of the kurgan ritual itself, with such structural elements as cromlechs, orthostats and stone cists. These are most apparent to the south, in the zone of contact with the Lower Mikhailovka culture. The second is apparent in the similarity between Kvityana pottery and Sredny Stog II pottery, notably in a number of shared compositional and technical elements, despite the fact that the shapes, techniques and style are all quite different.

As a whole, the Kvityana culture is notably conservative and archaic in appearance; this is manifest both in the preservation of a burial rite involving a supine position, and in the appearance of the pottery which, on the basis of the absence of corded or caterpillar track decoration, was until recently considered the earliest Sredny Stog ware.

(…) we still lack sufficient evidence to trace in detail the path by which the Kvityana culture spread from the Dnepr into the Dnestr-Danube region. The southern steppe route is excluded, but Kvityana sites are recorded on the Southern Bug, in the Dnestr region, and even along the forest-steppe boundary on the Prut Gudging by the numerous excavations of kurgans in this belt. This route in some respects repeats that along which the Skelya elite groups moved. Southward movement along the Southern Bug and its tributaries into the steppe zone is indicated only by isolated sites, the number of which is far smaller than in the Dnestr-Danube region, despite the intensive excavation of kurgans in this region. Evidence for Kvityana penetration into the northwestern Black Sea coast is provided by the appearance in Usatovo assemblages of typical Kvityana figural tubular bone beads, with diagnostic lateral notches on the sides (Malyukevich & Petrenko 1993).

kvityana-cucuteni-tripolye-expansions
Expansions of Kvityana and Trypillia cultures. Rassamakin (1999)

[The Dereivka] culture is currently only known only from settlement material, notably from sites in the Dnepr region (Dereivka and Molyukhov Bugor), but also from typologically distinctive pottery in the Eneolithic layer of the settlement of Aleksandriya on the Oskol. Dereivka culture pottery has also been recorded at a number of locations in the forest-steppe Dnepr region and the Seversky Donets, at Tetyanchino, Kamennye Pataki, and Minevsky Yar. The ceramic assemblage is well-defined and easily recognizable: vessels consistently display a weak profile and slightly elongated proportions, with high, straight mouths, evenly cut off at the rim, and conical bases (Fig. 3.23). The Dereivka culture occupies the southern part of the forest-steppe region and is bounded to the south by the Kvityana culture.

Telegin rightly noted that Dereivka and Kvityana pottery bore some resemblance to one another. Several fragments of the latter were found in the Dereivka assemblage, and provide evidence for the contemporaneous existence of the two cultures. The Molyukhov Bugor pottery assemblage stands out in terms of a prevalence of pottery with corded decoration, which only occurs in insignificant amounts at Dereivka and Aleksandriya. However, artefactual analysis has not produced any clear guidance for a chronological organization of these sites, as was postulated by Telegin.

sredni-stog-yamnaya
Rassamakin’s (1999) periodization of the North Pontic cultures

Late Phase and Final Eneolithic (3500-3000 BC)

In the Dnestr region, southward pressure from Tripolye led to the formation of, firstly, Vykhvatinsk-type sites, and then, in the steppe zone, Usatovo-type sites, which had undoubtedly absorbed some features of the Lower Mikhailovka culture. In the Prut and Middle Dnestr regions, sites of the Gordineşti (Kasperovkao) types are formed (these correspond, in the Romanian Prut region and on the Siret, to sites of the Horodiştea-Erbiceni type, and on the Lower Danube to the Cernavoda III culture: Morintz & Roman 1968; Dinu 1980; 1987). Movsha considers that sites of this type (Kasperovkao in her terminology) also occur in the Southern Bug region.

Sofievka-type sites emerge in the forest-steppes of the Middle Dnepr. A number of researchers (Zbenovich, Dergachev, and Sorokin), taking account of the change in the Tripolye culture at stage C2, propose a special division, considering sites of this period alone as ‘Late Tripolye’. In their view (with which I agree), stage Cl in culture-historical terms still corresponds to ‘Middle Tripolye’.

(…) existing evidence allows us to put forward the following scheme (Fig. 3.49:2). To the east of the Usatovo sites, from the lower reaches of the Southern Bug to the Azov region, encroaching on the Crimean steppes, the Lower Mikhailovka culture remains intact. To the north, upstream along the Dnepr and its tributaries, the Kvityana culture survives in its initial core zone. Between the Southern Bug and the Dnepr, in the contact zone between the three cultures (Tripolye, Lower Mikhailovka and Kvityana) the Dnepr-Bug group of sites emerges, displaying mixed features (Nikolova & Rassamakin 1985; Rassamakin 1988) Tripolye influence on the Dereivka culture appears to increase, as manifested in the appearance of late cultural elements (corded decoration, plastic art, bowls). The fate of the Pivikha culture is unclear. On the Lower Don, the late phase of the Konstantinovka culture (corresponding to the settlements of Konstantinovka and Razdorskoe I: Level 7) continued.

The final stage

The final stage of this period is characterized by two waves of migration, which properly speaking conclude the development of the Eneolithic.(…)

The first migration is connected with the breakdown of that system of Late Tripolye forest-steppe sites of the Prut-Dnestr and Southern Bug regions, dealt with by Movsha within the framework of the Kasperovo local group (and termed Gordineşti by others such as Dergachev, Manzura, and Petrenko). Almost all researchers into the Tripolye culture note the widespread occurrence of diagnostic elements of this group in the south, in the zone of the Usatovo sites and, in the east and southeast, towards the Dnepr and its left bank (Movsha 1984; 1990; 1993; Subbotin & Petrenko 1986; Manzura 1990a). (…)

The migrational wave that left Zhivotilovo-Volchanskoe-type burials in the steppe also linked up the forest-steppe Bug, Dnestr, and Prut regions with the Lower Don region, and, possibly with the North Caucasus, where the late stage of the Maikop culture (the Novosvobodnaya sites) continued. The identical rites of the Maikop culture and Zhivotilovo-Volchanskoe sites makes it difficult to establish the direction of migration, or which was the active side in the process. A number of researchers have given precedence to the Maikop culture. But the spread of the Tripolye assemblage unambiguously indicates the active involvement of the Tripolye tribes.

north-pontic-kvityana-dereivka
The system of the latest Eneolithic Pointic cultures and the sites of the Zhivotilovo-Volchanskoe type: 1) Volchanskoe; 2) Zhivotilovka; 3) Vishnevatoe; 4) Koisug

The second migration, at the very end of the Eneolithic, is connected with the spread of the Repin culture (in its second phase) from the Middle Don. Sinyuk defined three main directions: north, to the Upper Don; southwest, into the Dnepr region; and south, to the Lower Don and the Lower Volga. Trifonov considers this broad expansion of the Repin culture to be colonization (Trifonov 1996). The Repin culture level at Razdorskoe I (Razdorskoe I: Level 8) overlies the Konstantinovka levels (Levels 6 and 7), signalling that the Konstantinovka culture had apparently ceased to exist (Kiyashko 1994, 80). It seems that the expansion of the Repin culture is also associated with a reduction in the territorial extent of the Kvityana and Dereivka cultures. Repin burial assemblages, settlements and temporary camps appear in the Seversky Donets basin and in the Eastern Azov region (at Trekhizbenka, Kapitanovo, Aleksandriya, and Razdolnoe). The same complexes are also widely distributed towards the Dnepr (Marina 1992). The most striking western manifestation of Repin elements is seen in the upper horizon of the middle level of the Mikhailovka settlement (Lagodovska et al. 1962, 39-46).

Khvalynsk-Yamna and Sredni Stog-Corded Ware

We already know that Ukraine Eneolithic samples showed steppe ancestry and had apparently began a process of convergence coinciding with (or after) the first Khvalynsk-related migrations. It is unclear what had happened before (i.e. how much “CHG ancestry” was absorbed by Ukraine Neolithic groups in their transition to the Eneolithic before ca. 4500 BC), although in principle we can assume that all Caucasus-related admixture received by North Pontic cultures ca. 4500-4000 BC was mediated by westward movements from Khvalynsk-related peoples.

PCA-caucasus-lola-ane-chg
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. An EHG and a Caucasus ‘clouds’ have been drawn, leaving Pontic-Caspian steppe and derived groups between them.See the original file here.

Contacts with (and later absorption of) Khvalynsk-Novodanilovka-related migrants, as well as heir cultures, like those in the steppe adjacent to the Black Sea coast, and also direct contacts with Caucasus-related populations through Zhivotilovo-Volchanskoe can justify a greater contribution of CHG ancestry ca. 4000-3500 BC. Close contacts with Cucuteni-Trypillia (through Mikhailovka and maybe Kvityana, possibly with WHG and CHG admixture related to Khvalynsk-Novodanilovka) and GAC peoples to the north are the obvious source of further similarities with Yamna. Distinct similarities, that is, if we take into account the different sources and timing of such ancestral components, and Y-chromosome bottlenecks…

Therefore, after a process of convergence ca. 4500-4000 BC, and potentially more contacts with late Eneolithic North Pontic steppe cultures ca. 4000-3500 BC, Proto-Corded Ware peoples must have finally spread from the northernmost (forest-steppe) areas previously occupied by Dereivka, Pivikha, or Sofievka groups from ca. 3300 BC onwards – a date roughly coincident with the expansion of late Khvalynsk/Repin to the west developing the Early Yamna culture, with which it likely entered in contact (hence potentially a source for further admixture convergence ca. 3500-3000 BC).

Only later happened the great migration ca. 3000-2800 BC of Classical Corded Ware culture migrants, at the same time as Early Yamna migrants expanded to the west, and some groups also to the north along the Prut (possibly directly connected to the admixture found in the two Baltic LN/CWC ‘outliers’).

steppe-chalcolithic-migrations
Steppe-related migrations ca. 3100-2600 BC with tentative linguistic identification.

We didn’t know much about Sredni Stog or Corded Ware, and we still don’t. I can’t see the future, and I don’t have access to information from Reich-Jena or Copenhagen groups, and never have. But I just don’t see the need to explain Corded Ware as derived from (coeval) Early Yamna, and I haven’t since the 2015 papers. It was not the best explanation for the data that was published, and the more information we receive, the less sense this theory makes.

However, I guess we will see some groups still resorting to the good old Yamnaya ancestral component™ = Indo-European no matter what, consciously ignoring that a proportion of ancestral components (some combination of EHG:CHG:WHG in this case) means nothing without a proper explanation of their precise temporal and regional origin, and how they connect with Yamna; just like the CHG ancestry = Indo-European trend we are living right now does not make any sense.

Publishing only selected results after trying every possible combination of samples with bioinformatic tools does not help strengthen this connection, either.

Related

Steppe and Caucasus Eneolithic: the new keystones of the EHG-CHG-ANE ancestry in steppe groups

indo-uralic-ehg-chg-ane-ancestry

Some interesting excerpts from Wang et al. (2018):

An interesting observation is that steppe zone individuals directly north of the Caucasus (Eneolithic Samara and Eneolithic steppe) had initially not received any gene flow from Anatolian farmers. Instead, the ancestry profile in Eneolithic steppe individuals shows an even mixture of EHG and CHG ancestry, which argues for an effective cultural and genetic border between the contemporaneous Eneolithic populations in the North Caucasus, notably Steppe and Caucasus. Due to the temporal limitations of our dataset, we currently cannot determine whether this ancestry is stemming from an existing natural genetic gradient running from EHG far to the north to CHG/Iran in the south or whether this is the result of farmers with Iranian farmer/ CHG-related ancestry reaching the steppe zone independent of and prior to a stream of Anatolian farmer-like ancestry, where they mixed with local hunter-gatherers that carried only EHG ancestry.

PCA-caucasus-khvalynsk-sredni-stog
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. An Eastern European (blue) and a Caucasus (brown) ‘clouds’ have been drawn in dotted circles, leaving Pontic-Caspian steppe and derived groups between them.See the original file here.

Concerning the influences from the south, our oldest dates from the immediate Maykop predecessors Darkveti-Meshoko (Eneolithic Caucasus) indicate that the Caucasus genetic profile was present north of the range ~6500 BP, 4500 calBCE. This is in accordance with the Neolithization of the Caucasus, which had started in the flood plains of the great rivers in the South Caucasus in the 6th millennium BCE from where it spread to the West and Northwest Caucasus during the 5th millennium BCE9, 49. It remains unclear whether the local CHG ancestry profile (represented by Late Upper Palaeolithic/Mesolithic individuals from Kotias Klde and Satsurblia in today’s Georgia) was also present in the North Caucasus region before the Neolithic. However, if we take the Caucasus hunter-gatherer individuals from Georgia as a local baseline and the oldest Eneolithic Caucasus individuals from our transect as a proxy for the local Late Neolithic ancestry, we notice a substantial increase in Anatolian farmer-related ancestry. This in all likelihood is linked to the process of Neolithization, which also brought this type of ancestry to Europe. As a consequence, it is possible that Neolithic groups could have reached the northern flanks of the Caucasus earlier50 (Supplementary Information 1) and in contact with local hunter gatherers facilitated the exploration of the steppe environment for pastoralist economies. Hence, additional sampling from older individuals is needed to fill this temporal and spatial gap.

The newest paper of the Reich/Jena group has brought samples (probably) much nearer to the actual CHG and ANE contribution seen in Eneolithic steppe peoples than the previously available Kotias Klde, Satsurblia, Afontova Gora 3, or Mal’ta.

It is impossible to say without direct access to the samples, but it is very likely that we will soon be able to break down different gross contributions from groups similar to these Steppe/Caucasus Neolithic ancestral groups into the diverse Eneolithic cultures of the Pontic-Caspian steppe, and thus trace more precisely each of these cultures to their genetic (and thus ethnolinguistic) heirs.

qpgraph-eneolithic-steppe
Admixture Graph modelling of the population history of the Caucasus region. We started with a skeleton tree without admixture including Mbuti, Loschbour and MA1. We grafted onto this EHG, CHG, Globular_Amphora, Eneolithic_steppe, Maykop, and Yamnaya_Caucasus, adding them consecutively to all possible edges in the tree and retaining only graph solutions that provided no differences of |Z|>3 between fitted and estimated statistics. The worst match is |Z|=2.824 for this graph. We note that the maximum discrepancy is f4(MA1, Maykop; EHG, Eneolithic_steppe) = -3.369 if we do not add the 4% EHG ancestry to Maykop. Drifts along edges are multiplied by 1000 and dashed lines represent admixture.”

Some more representative samples from Eneolithic steppe, steppe-forest and forest zone cultures of Eastern Europe will probably help with the fine-scale structure of different Chalcolithic groups, especially the homeland of early Corded Ware groups.

These new samples seem another good reason (like the Botai and R1b-M73) to rethink the role of (what I assumed were) different westward Mesolithic Eurasian waves of expansion influencing the formation of an Indo-Uralic and Indo-European community in Eastern Europe, and return to the simpler idea of local contributions from North Caucasus and steppe peoples absorbed by expanding EHG-like groups.

Related:

The new Scicomm’s warhorse is “CHG ancestry = PIE” and the Iranian homeland

invasion-from-the-steppe-yamnaya

Funny reports are popping up due to a recent article in New Scientist (behind paywall), World’s most-spoken languages may have arisen in ancient Iran, which echoes the controversial interpretations of Wang et al. (2018).

I have been waiting to read the printed edition, but that of May 26th doesn’t have the article in it, so it may be a web-only text.

Nevertheless, here are some excerpts about the PIE homeland from a news aggregator that caught my attention (emphasis mine):

The two proposed locations are divided by the Caucasus mountains, which are found between the Black and Caspian Seas. In today’s geography, the mountains cover parts of Russia, Georgia, Azerbaijan, and Armenia.

To find out whether the ancient language came from north or south of these mountains, a team from the Max Planck Institute for the Science of Human History looked at the bones of 45 ancient humans from the Caucasus region, and analyzed their DNA. These people lived in the area between 3,200 and 6,500 years ago.

Interestingly, from looking at their genes, the researchers determined that these ancient people seemed to be moving predominantly in one direction – they were heading north. This suggests that, contrary to what was previously believed, the first Indo-European language might actually have arisen south of the Caucasus mountains, only spreading to other parts of Europe and Asia as people migrated north from this region. The findings are currently available on BioRxiv.

We know that the Proto-Indo-European language appeared somewhere between 5,500 and 9,000 years ago, and the study suggests it only spread to Europe about 6,500 years ago. Therefore, this lost language could have originated south of the Caucasus.

What’s more, the ancient people analyzed had similar genetic signatures to prehistoric farmers who once lived in western Iran. Therefore, the ancient version of many of our languages may have first evolved in ancient Iran, before spreading with the people who first spoke it, and their ancestors, as they radiated north of the Caucasus mountains to the Eurasian steppe.

However, there are still many who favor the conflicting theory – that the Proto-Indo-European language arose in the Eurasian steppe. But this would only take the language back about 4,800 years – when people moved from the Eurasian steppe into Europe – and specialists think the language is significantly older. The idea that it first sprung up in Iran about 6,500 years ago follows this assumption.

It seems that – now that the Danish workgroup (responsible for the “steppe ancestry = Indo-European” and “Corded Ware expanded from Yamna“) is backing down, and both it and the Reich/Jena group are accepting that Yamna represents the expansion of Late Indo-European into Afanasevo, Bell Beaker, and Sintashta – anything before Yamna in the steppe is just another “conflicting theory” among equals…

So forget the “steppe ancestry = PIE”, and welcome the newly fashionable “CHG ancestry = PIE“, and of course the Iranian homeland.

This is how I imagine genetic labs writing anthropological interpretations and conclusions of their papers, against every single reasonable restraint (and the well-established models of linguists and archaeologists) and then publicizing them:

mr-bean-middle-finger

Related:

Haplogroup J spread in the Mediterranean due to Phoenician and Greek colonizations

iron_age_europe_mediterranean

Open access A finely resolved phylogeny of Y chromosome Hg J illuminates the processes of Phoenician and Greek colonizations in the Mediterranean, by Finocchio et al. Scientific Reports (2018) Nº 7465.

Abstract (emphasis mine):

In order to improve the phylogeography of the male-specific genetic traces of Greek and Phoenician colonizations on the Northern coasts of the Mediterranean, we performed a geographically structured sampling of seven subclades of haplogroup J in Turkey, Greece and Italy. We resequenced 4.4 Mb of Y-chromosome in 58 subjects, obtaining 1079 high quality variants. We did not find a preferential coalescence of Turkish samples to ancestral nodes, contradicting the simplistic idea of a dispersal and radiation of Hg J as a whole from the Middle East. Upon calibration with an ancient Hg J chromosome, we confirmed that signs of Holocenic Hg J radiations are subtle and date mainly to the Bronze Age. We pinpointed seven variants which could potentially unveil star clusters of sequences, indicative of local expansions. By directly genotyping these variants in Hg J carriers and complementing with published resequenced chromosomes (893 subjects), we provide strong temporal and distributional evidence for markers of the Greek settlement of Magna Graecia (J2a-L397) and Phoenician migrations (rs760148062). Our work generated a minimal but robust list of evolutionarily stable markers to elucidate the demographic dynamics and spatial domains of male-mediated movements across and around the Mediterranean, in the last 6,000 years.

greek-phoenician
J2-L397. The star indicates the centroid of derived alleles. The solid square indicates the centroid of ancestral alleles, with its 95% C.I. (ellipse). In the insets: distributions of the pairwise sampling distances (in Km) for the carriers of the ancestral (black) and derived (white) allele, with solid and dashed lines indicating the respective averages. At right: median joining network of 7-STR haplotypes and SNPs in the same groups, with sectors coloured according to sampling location. Haplotype structure is detailed for some nodes, in the order YCA2a-YCA2b-DYS19-DYS390-DYS391-DYS392-DYS393 (in italics).

Interesting excerpts:

Two features of our tree are at odds with the simplistic idea of a dispersal of Hg J as a whole from the Middle East towards Greece and Italy and an accompanying radiation26. First, there is little evidence of sudden diversification between 15 and 5 kya, a period of likely population increase and pressure for range expansion, due to the Agricultural revolution in the Fertile Crescent. Second, within each subclade, lineages currently sampled in Turkey do not show up as preferentially ancestral. Both findings are replicated and reinforced by examining the previous landmark studies. Our Turkish samples do not coalesce preferentially to ancestral nodes when mapped onto these studies’ trees.

Additional relevant information on the entire Hg J comes from the discontinuous distribution of J2b-M12. The northern fringe of our sample is enriched in the J2b-M241 subclade, which reappears in the gulf of Bengal38,45, with low frequencies in the intervening Iraq46 and Iran47. No J2b-M12 carriers were found among 35 modern Lebanese, as contrasted to one of two ancient specimens from the same region35.

In summary, a first conclusion of our sequencing effort and merge with available data is that the phylogeography of Hg J is complex and hardly explained by the presence of a single population harbouring the major lineages at the onset of agriculture and spreading westward. A unifying explanation for all the above inconsistencies could be a centre of initial radiation outside the area here sampled more densely, i.e. the Caucasus and regions North of it, from which different Hg J subclades may have later reached mainland Italy, Greece and Turkey, possibly following different routes and times. Evidence in this direction comes from the distribution of J2a-M41045,48 and the early-49 or mid-Holocene50 southward spread of J1.

greek-colonization
Supplemental Figure 7. Maps of sampling locations for the carriers of the derived allele (white triangle point down) at the indicated SNP vs carriers of the ancestral allele (black triangle point-up), conditioned on identical genotype at the same most terminal marker. Coastlines were drawn with the R packages18 “map” and “mapproj” v. 3.1.3 (https://cran.r-project.org/web/packages/mapproj/index.html), and additional features added with default functions. The star triangle indicates the centroid of derived alleles. The solid square indicates the centroid of ancestral alleles, with its 95% C.I. (ellipse). In the insets: distributions of the pairwise sampling distances (in Km) for the carriers of the ancestral (black) and derived (white) allele, with solid and dashed lines indicating the respective averages. At right: median joining network of 7-STR haplotypes and SNPs in the same groups, with sectors coloured according to sampling location. Haplotype structure is detailed for some nodes, in the order YCA2a-YCA2b-DYS19-DYS390-DYS391-DYS392-DYS393 (in italics).

The lineage defined by rs779180992, belonging to J2b-M205, and dated at 4–4.5 kya, has a radically different distribution, with derived alleles in Continental Italy, Greece and Northern Turkey, and two instances in a Palestinian and a Jew. The interpretation of the spread of this lineage is not straightforward. Tentative hypotheses are linked to Southward movements that occurred in the Balkan Peninsula from the Bronze Age29,53, through the Roman occupation and later54.

The slightly older (5.6–6.3 kya) branch 98 lineage displays a similar trend of a Eastward positioning of derived alleles, with the notable difference of being present in Sardinia, Crete, Cyprus and Northern Egypt. This feature and the low frequency of the parental J2a-M92 lineage in the Balkans27 calls for an explanation different from the above.

Finally, we explored the distribution of J2a-L397 and three derived lineages within it. J2a-L397 is tightly associated with a typical DYS445 6-repeat allele. This has been hypothesized as a marker of the Greek colonizations in the Mediterranean55, based on its presence in Greek Anatolia and Provence (France), a region with attested Iron Age Greek contribution. All of our chromosomes in this clade were characterized also by DYS391(9), confirming their Anatolian Greek signature. We resolved the J2a-L397 clade to an unprecedented precision, with three internal markers which allow a finer discrimination than STRs. The ages of the three lineages (2.0–3.0 kya) are compatible with the beginning of the Greek colonial period, in the 8th century BCE. The three subclades have different distributions (Fig. 2B), with two (branches 57, 59) found both East and West to Greece, and one only in Italy (branch 58). As to Mediterranean Islands, J2a-L397 was found in Cyprus56 and Crete43. Its presence as one of the three branches 57–59 will represent an important test. In Italy all three variants were found mainly along the Western coast (18/25), which hosted the preferred Greek trade cities. The finding of all three differentiated lineages in Locri excludes a local founder effect of a single genealogy. Interestingly, an important Greek colony was established in this location, with continuity of human settlement until modern times. The sample composed of the same subjects displayed genetic affinities with Eastern Greece and the Aegean also at autosomal markers57. In summary, the distributions of branches 57–59 mirror the variety of the cities of origin and geographic ranges during the phases of the colonization process58.

So, there you have it, another proof that haplogroup J and CHG-related ancestry in the Mediterranean was mainly driven by different (and late) expansions of historic peoples.

Related:

Consequences of Damgaard et al. 2018 (II): The late Khvalynsk migration waves with R1b-L23 lineages

chalcolithic_early-asia

This post should probably read “Consequences of Narasimhan et al. (2018),” too, since there seems to be enough data and materials published by the Copenhagen group in Nature and Science to make a proper interpretation of the data that will appear in their corrected tables.

The finding of late Khvalynsk/early Yamna migrations, identified with early LPIE migrants almost exclusively of R1b-L23 subclades is probably one of the most interesting findings in the recent papers regarding the Indo-European question.

Although there are still few samples to derive fully-fledged theories, they begin to depict a clearer idea of waves that shaped the expansion of Late Proto-Indo-European migrants in Eurasia during the 4th millennium BC, i.e. well before the expansion of North-West Indo-European, Palaeo-Balkan, and Indo-Iranian languages.

Late Khvalynsk expansions and archaic Late PIE

Like Anatolian, Tocharian has been described as having a more archaic nature than the rest of Late PIE. However, Pre-Tocharian belongs to the Late PIE trunk, clearly distinguishable phonetically and morphologically from Anatolian.

It is especially remarkable that – even though it expanded into Asia – it has more in common with North-West Indo-European, hence its classification (together with NWIE) as part of a Northern group, unrelated to Graeco-Aryan.

The linguistic supplement by Kroonen et al. accepts that peoples from the Afanasevo culture (ca. 3000-2500 BC) are the most likely ancestors of Tocharians.

NOTE. For those equating the Tarim Mummies (of R1a-Z93 lineages) with Tocharians, you have this assertion from the linguistic supplement, which I support:

An intermediate stage has been sought in the oldest so-called Tarim Mummies, which date to ca. 1800 BCE (Mallory and Mair 2000; Wáng 1999). However, also the language(s) spoken by the people(s) who buried the Tarim Mummies remain unknown, and any connection between them and the Afanasievo culture on the one hand or the historical speakers of Tocharian on the other has yet to be demonstrated (cf. also Mallory 2015; Peyrot 2017).

New samples of late Khvalynsk origin

These are are the recent samples that could, with more or less certainty, correspond to migration waves from late Khvalynsk (or early Yamna), from oldest to most recent:

  • The Namazga III samples from the Late Eneolithic period (in Turkmenistan), dated ca. 3360-3000 BC (one of haplogroup J), potentially showing the first wave of EHG-related steppe ancestry into South Asia. Not related to Indo-Iranian migrations.

NOTE. A proper evaluation with further samples from Narasimhan et al. (2018) is necessary, though, before we can assert a late Khvalynsk origin of this ancestry.

  • Afanasevo samples, dated ca. 3081-2450 BC, with all samples dated before ca. 2700 BC uniformly of R1b-Z2103 subclades, sharing a common genetic cluster with Yamna, showing together the most likely genomic picture of late Khvalynsk peoples.

NOTE 1. Anthony (2007) put this expansion from Repin ca. 3300-3000 BC, while his most recent review (2015) of his own work put its completion ca. 3000-2800. While the migration into Afanasevo may have lasted some time, the wave of migrants (based on the most recent radiocarbon dates) must be set at least before ca. 3100 BC from Khvalynsk.

NOTE 2. I proposed that we could find R1b-L51 in Afanasevo, presupposing the development of R1b-L51 and R1b-Z2103 lineages with separating clans, and thus with dialectal divisions. While finding this is still possible within Khvalynsk regions, it seems we will have a division of these lineages already ca. 4250-4000 BC, which would require a closer follow-up of the different inner late Khvalynsk groups and their samples. For the moment, we don’t have a clear connection through lineages between North-West Indo-European groups and Tocharian.

tocharian-early-copper-age
Early Copper Age migrations in Asia ca. 3300-2800, according to Anthony (2015).
  • Subsequent and similar migration waves are probably to be suggested from the new sample of Karagash, beyond the Urals (attributed to the Yamna culture, hence maintaining cultural contacts after the migration waves), of R1b-Z2103 subclade, ca. 3018-2887 BC, potentially connected then to the event that caused the expansion of Yamna migrants westward into the Carpathians at the same time. Not related to Indo-Iranian migrations.
  • The isolated Darra-e Kur sample, without cultural adscription, ca. 2655 BC, of R1b-L151 lineage. Not related to Indo-Iranian migrations.
  • The Hajji Firuz samples: I4243 dated ca. 2326 BC, female, with a clear inflow of steppe ancestry; and I2327 (probably to be dated to the late 3rd millennium BC or after that), of R1b-Z2103 lineage. Not related to Indo-Iranian migrations.

NOTE. A new radiocarbon dating of I2327 is expected, to correct the currently available date of 5900-5000 BC. Since it clusters nearer to Chalcolithic samples from the site than I4243 (from the same archaeological site), it is possible that both are part of similar groups receiving admixture around this period, or maybe I2327 is from a later period, coinciding with the Iron Age sample F38 from Iran (Broushaki et al. 2016), with which it closely clusters. Also, the finding of EHG-related ancestry in Maykop samples dated ca. 3700-3000 BC (maybe with R1b-L23 subclades) offers another potential source of migrants for this Iranian group.

NOTE. Samples from Narasimhan et al. (2018) still need to be published in corrected tables, which may change the actual subclades shown here.

These late Khvalynsk / early Yamna migration waves into Asia are quite early compared to the Indo-Iranian migrations, whose ancestors can only be first identified with Volga-Ural groups of Yamna/Poltavka (ca. 3000-2400 BC), with its fully formed language expanding only with MLBA waves ca. 2300-1200 BC, after mixing with incoming Abashevo migrants.

While the authors apparently forget to reference the previous linguistic theories whereby Tocharian is more archaic than the rest of Late PIE dialects, they refer to the ca. 1,000-year gap between Pre-Tocharian and Proto-Indo-Iranian migrations, and thus their obvious difference:

The fact that Tocharian is so different from the Indo-Iranian languages can only be explained by assuming an extensive period of linguistic separation.

Potential linguistic substrates in the Middle East

A few words about relevant substrate language proposals.

Euphratic language

What Gordon Whittaker proposes is a North-West Indo-European-related substratum in Sumerian language and texts ca. 3500 BC, which may explain some non-Sumerian, non-Semitic word forms. It is just one of many theories concerning this substratum.

eneolithic_steppe
Diachronic map of Eneolithic migrations ca. 4000-3100 BC

This is a summary of his findings from his latest writing on the subject (a chapter of a book on Indo-European phonetics, from the series Copenhagen Studies in Indo-European):

In Sumerian and Akkadian vocabulary, the cuneiform writing system, and the names of deities and places in Southern Mesopotamia a body of lexical material has been preserved that strongly suggests influence emanating from a superstrate of Indo-European origin. his Indo-European language, which has been given the name Euphratic, is, at present, attested only indirectly through the filters of Sumerian and Akkadian. The attestations consist of words and names recorded from the mid-4th millennium BC (Late Uruk period) onwards in texts and lexical lists. In addition, basic signs that originally had a recognizable pictorial structure in proto-cuneiform preserve (at least from the early 3rd millennium on) a number of phonetic values with no known motivation in Sumerian lexemes related semantically to the items depicted. This suggests that such values are relics from the original logographic values for the items depicted and, thus, that they were inherited from a language intimately associated with the development of writing in Mesopotamia. Since specialists working on proto-cuneiform, most notably Robert K. Englund of the Cuneiform Digital Library Initiative, see little or no evidence for the presence of Sumerian in the corpus of archaic tablets, the proposed Indo-European language provides a potential solution to this problem. It has been argued that this language, Euphratic, had a profound influence on Sumerian, not unlike that exerted by Sumerian and Akkadian on each other, and that the writing system was the primary vehicle of this influence. he phonological sketch drawn up here is an attempt to chart the salient characteristics of this influence, by comparing reconstructed Indo-European lexemes with similarly patterned ones in Sumerian (and, to a lesser extent, in Akkadian).

His original model, based on phonetic values in basic proto-cuneiform signs, is quite imaginative and a very interesting read, if you have the time. His Academia.edu account hosts most of his papers on the subject.

We could speculate about the potential expansion of this substrate language with the commercial contacts between Uruk and Maykop (as I did), now probably more strongly supported because of the EHG found in Maykop samples.

NOTE. We could also put it in relation with the Anatolian language of Mari, but this would require a new reassessment of its North-West Indo-European nature.

Nevertheless, this theory is far from being mainstream, anywhere. At least today.

NOTE. The proposal remains still hypothetic, because of the flaws in the Indo-European parallels – similar to Koch’s proposal of Indo-European in Tartessian inscriptions. A comprehensive critic approach to the theory is found in Sylvie Vanséveren’s A “new” ancient Indo-European language? On assumed linguistic contacts between Sumerian and Indo-European “Euphratic”, in JIES (2008) 36:3&4.

Gutian language

References to Gutian are popping up related to the Hajji Firuz samples of the mid-3rd millennium.

The hypothesis was put forward by Henning (1978) in purely archaeological terms.

This is the relevant excerpt from the book:

(…) Comparativists have asserted that, in spite of its late appearance, Tokharian is a relatively archaic form of Indo-European.3 This claim implies that the speakers of this group separated from their Indo-European brethren at a comparatively early date. They should accordingly have set out on their migrations rather early, and should have appeared within the Babylonian sphere of influence also rather early. Earlier, at any rate, than the Indo-Iranians, who spoke a highly developed (therefore probably later) form of Indo-European. Moreover, as some of the Indo-Iranians after their division into Iranians and Indo-Aryans4 appeared in Mesopotamia about 1500 B.C., we should expect the Proto-Tokharians about 2000 B.C. or even earlier.

If, armed with these assumptions as our working hypothesis, we look through the pages of history, we find one nation – one nation only – that perfectly fulfills all three conditions, which, therefore, entitles us to recognize it as the “Proto-Tokharians”. Tis name was Guti; the intial is also spelled with q (a voiceless back velar or pharyngeal), but the spelling with g is the original one. The closing -i is part of the name, for the Akkadian case-endings are added to it, nom. Gutium etc. Guti (or Gutium, as some scholars prefer) was valid for the nation, considered as an entity, but also for the territory it occupied.
(…).

The text goes on to follow the invasion of Babylonia by the Guti, and further eastward expansions supposedly connected with these, to form the attested Tocharians.

The referenced text by Thorkild Jakobsen offers the interesting linguistic data:

Among the Gutian rulers is one Elulumesh, whose name is evidently Akkadian Elulum slightly “Gutianized” by the Gutian case(?) ending -eš.40 This Gutian ruler Elulum is obviously the same man whom we find participating in the scramble for power after the death of Shar-kali-sharrii; his name appears there in Sumerian form without mimation as Elulu.

The Gutian dynasty, from ca. 22nd c. BC appears as follows:

gutian-rulers

I don’t think we could derive a potential relation to any specific Indo-European branch from this simple suffix repeated in Gutian rulers, though.

The hypothesis of the Tocharian-like nature of the Guti (apart from the obvious error of considering them as the ancestors of Tocharians) remains not contrasted in new works since. It was cited e.g. by Gamkrelidze and Ivanov (1995) to advance their Armenian homeland, and by Mallory and Adams in their Encyclopedia (1997).

It lies therefore in the obscurity of undeveloped archaeological-linguistic hypotheses, and its connection with the attested R1b-Z2103 samples from Iran is not (yet) warranted.

Related:

Consequences of Damgaard et al. 2018 (I): EHG ancestry in Maykop samples, and the potential Anatolian expansion routes

neolithic_steppe-anatolian-migrations

This is part I of two posts on the most recent data concerning the earliest known Indo-European migrations.

Anatolian in Armi

I am reading in forums about “Kroonen’s proposal” of Anatolian in the 3rd millennium. That is false. The Copenhagen group (in particular the authors of the linguistic supplement, Kroonen, Barjamovic, and Peyrot) are merely referencing Archi (2011. “In Search of Armi”. Journal of Cuneiform Studies 63: 5–34) in turn using transcriptions from Bonechi (1990. “Aleppo in età arcaica; a proposito di un’opera recente”. Studi Epigrafici e Linguistici sul Vicino Oriente Antico 7: 15–37.), who asserted the potential Anatolian origin of the terms. This is what Archi had to say about this:

Most of these personal names belong to a name-giving tradition different from that of Ebla; Arra-ti/tulu(m) is attested also at Dulu, a neighbouring city-state (Bonechi 1990b: 22–25).28 We must, therefore, deduce that Armi belonged to a marginal, partially Semitized linguistic area different from the ethno-linguistic region dominated by Ebla. Typical are masculine personal names ending in -a-du: A-la/li-wa-du/da, A-li/lu-wa-du, Ba-mi-a-du, La-wadu, Mi-mi-a-du, Mu-lu-wa-du. This reminds one of the suffix -(a)nda, -(a)ndu, very productive in the Anatolian branch of Indo-European (Laroche 1966: 329). Elements such as ali-, alali-, lawadu-, memi-, mula/i- are attested in Anatolian personal names of the Old Assyrian period (Laroche 1966: 26–27, 106, 118, 120).

First_Eblaite_Empire
Ebla’ first kingdom at its height c. 2340 BC. Hipothetical location of Armi depicted. The first Eblaite kingdom extended from Urshu in the north,1 to Damascus area in the south.2 And from Phoenicia and the coastal mountains in the west,3 4 to Tuttul,5 and Haddu in the east.6 The eastern kingdom of Nagar controlled most of the Khabur basin from the river junction with the Euphrates to the northwestern part at Nabada.7 Page 101. From Wikipedia.

This was used by Archi to speculatively locate the state of Armi, in or near Ebla territory, which could correspond with the region of modern north-western Syria:

The onomastic tradition of Armi, so different from that of Ebla and her allies (§ 5), obliges us to locate this city on the edges of the Semitized area and, thus, necessarily north of the line running through Hassuwan – Ursaum – Irritum – Harran. If Armi were to be found at Banat-Bazi, it would have represented an anomaly within an otherwise homogenous linguistic scenario.34

Taken as a whole, the available information suggests that Armi was a regional state, which enjoyed a privileged relationship with Ebla: the exchange of goods between the two cities was comparable only to that between Ebla and Mari. No other state sent so many people to Ebla, especially merchants, lú-kar. It is only a hypothesis that Armi was the go-between for Ebla and for the areas where silver and copper were extracted.

This proposal is similar to the one used to support Indo-Aryan terminology in Mittanni (ca. 16th-14th c. BC), so the scarce material should not pose a problem to those previously arguing about the ‘oldest’ nature of Indo-Aryan.

NOTE. On the other hand, the theory connecting ‘mariannu‘, a term dated to 1761 BC (referenced also in the linguistic supplement), and put in relation with PIIr. *arya, seems too hypothetical for the moment, although there is a clear expansion of Aryan-related terms in the Middle East that could support one or more relevant eastern migration waves of Indo-Aryans from Asia.

Potential routes of Anatolian migration

Once we have accepted that Anatolian is not Late PIE – and that only needed a study of Anatolian archaisms, not the terminology from Armi – , we can move on to explore the potential routes of expansion.

On the Balkan route

A current sketch of the dots connecting Khvalynsk with Anatolia is as follows.

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.

First, we have the early expansion of Suvorovo chieftains spreading from ca. 4400-4000 BC in the lower Danube region, related to Novodanilovka chiefs of the North Pontic region, and both in turn related to Khvalynsk horse riders (read a a recent detailed post on this question).

Then we have Cernavoda I (ca. 3850-3550 BC), a culture potentially derived from the earlier expansion of Suvorovo chiefs, as shown in cultural similarities with preceding cultures and Yamna, and also in the contacts with the North Pontic steppe cultures (read a a recent detailed post on this question).

We also have proof of genetic inflow from the steppe into populations of cultures near those suggested to be heirs of those dominated by Suvorovo chiefs, from the 5th millennium BC (in Varna I ca. 4630 BC, and Smyadovo ca. 4500 BC, see image below).

If these neighbouring Balkan peoples of ca. 4500 BC are taken as proxies for Proto-Anatolians, then it becomes quite clear why Old Hittite samples dated 3,000 years after this migration event of elite chiefs could show no or almost no ancestry from Europe (for this question, read my revision of Lazaridis’ preprint).

NOTE. A full account of the crisis in the lower Danube, as well as the Suvorovo-Novodanilovka intrusion, is available in Anthony (2007).

mathieson-2018-balkan-expansion
Modified image, including PCA and supervised ADMIXTURE data from Mathieson et al. (2018). Blue arrow represents incoming ancestry from Suvorovo chiefs, red line represents distance from the majority of the neighbouring Balkan population in this period studied to date. Northwestern-Anatolian Neolithic (grey), Yamnaya from Samara (yellow), EHG (pink) and WHG (green).

The southern Balkans and Anatolia

The later connection of Cernavoda II-III and related cultures (and potentially Ezero) with Troy, on the other hand, is still blurry. But, even if a massive migration of Common Anatolian is found to happen from the Balkans into Anatolia in the late 4th / beginning of the 3rd millennium, the people responsible for this expansion could show a minimal trace of European ancestry.

A new paper has appeared recently (in Russian), Dubene and Troy: Gold and Prosperity in the Third Millennium Cal. BCE in Eurasia. Stratum Plus, 2 (2018), by L. Nikolova, showing commercial contacts between Troy and cultures from Bulgaria:

Earlier third millennium cal BCE is the period of development of interconnected Early Bronze Age societies in Eurasia, which economic and social structures expressed variants of pre-state political structures, named in the specialized literature tribes and chiefdoms. In this work new arguments will be added to the chiefdom model of third millennium cal BC societies of Yunatsite culture in the Central Balkans from the perspectives of the interrelations between Dubene (south central Bulgaria) and Troy (northwest Turkey) wealth expression.

Possible explanations of the similarity in the wealth expression between Troy and Yunatsite chiefdoms is the direct interaction between the political elite. However, the golden and silver objects in the third millennium cal BCE in the Eastern Mediterranean are most of all an expression of economic wealth. This is the biggest difference between the early state and chiefdoms in the third millennium cal BCE in Eurasia and Africa. The literacy and the wealth expression in the early states was politically centralized, while the absence of literacy and wider distribution of the wealth expression in the chiefdoms of the eastern Mediterranean are indicators, that wider distribution of wealth and the existed stable subsistence layers prevented the formation of states and the need to regulate the political systems through literacy.

The only way to link Common Anatolians to their Proto-Anatolian (linguistic) ancestors would therefore be to study preceding cultures and their expansions, until a proper connecting route is found, as I said recently.

These late commercial contacts in the south-eastern Balkans (Nikolova also offers a simplified presentation of data, in English) are yet another proof of how Common Anatolian languages may have further expanded into Anatolia.

NOTE. One should also take into account the distribution of modern R1b-M269* and L23* subclades (i.e. those not belonging to the most common subclades expanding with Yamna), which seem to peak around the Balkans. While those may just belong to founder effects of populations preceding Suvorovo or related to Yamna migrants, the Balkans is a region known to have retained Y-DNA haplogroup diversity, in contrast with other European regions.

On a purely linguistic aspect, there are strong Hattic and Hurrian influences on Anatolian languages, representing a unique layer that clearly differentiates them from LPIE languages, pointing also to different substrates behind each attested Common Anatolian branch or individual language:

  • Phonetic changes, like the appearance of /f/ and /v/.
  • Split ergativity: Hurrian is ergative, Hattic probably too.
  • Increasing use of enclitic pronoun and particle chains after first stressed word: in Hattic after verb, in Hurrian after nominal forms.
  • Almost obligatory use of clause initial and enclitic connectors: e.g. semantic and syntactic identity of Hattic pala/bala and Hittite nu.

NOTE. For a superficial discussion of this, see e.g. An Indo-European Linguistic Area and its Characteristics: Ancient Anatolia. Areal Diffusion as a Challenge to the Comparative Method?, by Calvert Watkins. You can also search for any of the mentioned shared isoglosses between Middle Eastern languages and Anatolian if you want more details.

On the Caucasus route

It seems that the Danish group is now taking a stance in favour of a Maykop route (from the linguistic supplement):

The period of Proto-Anatolian linguistic unity can now be placed in the 4th millennium BCE and may have been contemporaneous with e.g. the Maykop culture (3700–3000 BCE), which influenced the formation and apparent westward migration of the Yamnaya and maintained commercial and cultural contact with the Anatolian highlands (Kristiansen et al. 2018).

In fact, they have data to support this:

The EHG ancestry detected in individuals associated with both Yamnaya (3000–2400 BCE) and the Maykop culture (3700–3000 BCE) (in prep.) is absent from our Anatolian specimens, suggesting that neither archaeological horizon constitutes a suitable candidate for a “homeland” or “stepping stone” for the origin or spread of Anatolian Indo- European speakers to Anatolia. However, with the archaeological and genetic data presented here, we cannot reject a continuous small-scale influx of mixed groups from the direction of the Caucasus during the Chalcolithic period of the 4th millennium BCE.

While it is difficult to speak about the consequences of this find without having access to this paper in preparation or its samples, we already knew that Maykop had obvious cultural contacts with the steppe.

It will not be surprising to find not only EHG, but also R1b-L23 subclades there. In my opinion, though, the most likely source of EHG ancestry in Maykop (given the different culture shown in other steppe groups) is exogamy.

The question will still remain: was this a Proto-Anatolian-speaking group?

eneolithic_steppe
Diachronic map of Eneolithic migrations ca. 4000-3100 BC

My opinion in this regard – again, without access to the study – is that you would still need to propose:

  • A break-up of Anatolian ca. 4500 BC represented by some early group migrating into the Northern Caucasus area.
  • For this group – who were closely related linguistically and culturally to early Khvalynsk – to remain isolated in or around the Northern Caucasus, i.e. somehow ‘hidden’ from the evolving LPIE speakers in late Khvalynsk/early Yamna peoples.
  • Then, they would need to have migrated from Maykop to Anatolian territory only after ca. 3700 BC – while having close commercial contacts with Khvalynsk and the North Pontic cultures in the period 3700-3000 BC -, in some migration wave that has not showed up in the archaeological records to date.
  • Then appear as Old Hittites without showing EHG ancestry (even though they show it in the period 3700-3000 BC), near the region of the Armi state, where Anatolian was supposedly spoken already in the mid-3rd millennium.

Not a very convincing picture, right now, but indeed possible.

Also, we have R1b-Z2103 lineages and clear steppe ancestry in the region probably ca. 2500 BC with Hajji Firuz, which is most likely the product of the late Khvalynsk migration waves that we are seeing in the recent papers.

These migrations are then related to early LPIE-speaking migrants spreading after ca. 3300 BC – that also caused the formation of early Yamna and the expansion of Tocharian-related migrants – , which leaves almost no space for an Anatolian expansion, unless one supports that the former drove the latter.

NOTE. In any case, if the Caucasus route turned out to be the actual Anatolian route, I guess this would be a way as good as any other to finally kill their Indo-European – Corded Ware theory, for obvious reasons.

On the North Iranian homeland

A few thoughts for those equating CHG ancestry in IE speakers (and especially now in Old Hittites) with an origin in North Iran, due to a recent comment by David Reich:

In the paper it is clearly stated that there is no Neolithic Iranian ancestry in the Old Hittite samples.

Ancestry is not people, and it is certainly not language. The addition of CHG ancestry to the Eneolithic steppe need not mean a population or linguistic replacement. Although it could have been. But this has to be demonstrated with solid anthropological models.

NOTE. On the other hand, if you find people who considered (at least until de Barros Damgaard et al. 2018) steppe (ancestry/PCA) = Indo-European, then you should probably confront them about why CHG in Hittites and the arrival of CHG in steppe groups is now not to be considered the same, i.e why CHG / Iran_N ≠ PIE.

Since there has been no serious North Iranian homeland proposal made for a while, it is difficult to delineate a modern sketch, and I won’t spend the time with that unless there is some real anthropological model and genetic proof of it. I guess the Armenian homeland hypothesis proposed by Gamkrelidze and Ivanov (1995) would do, but since it relies on outdated data (some of which appears also in Gimbutas’ writings), it would need a full revision.

NOTE. Their theory of glottalic consonants (or ejectives) relied on the ‘archaism’ of Hittite, Germanic, and Armenian. As you can see (unless you live in the mid-20th century) this is not very reasonable, since Hittite is attested quite late and after heavy admixture with Middle Eastern peoples, and Germanic and Armenian are some of the latest attested (and more admixed, phonetically changed) languages.

This would be a proper answer, indeed, for those who would accept this homeland due to the reconstruction of ‘ejectives’ for these languages. Evidently, there is no need to posit a homeland near Armenia to propose a glottalic theory. Kortlandt is a proponent of a late and small expansion of Late PIE from the steppe, and still proposes a reconstruction of ejectives for PIE. But, this was the main reason of Gamkrelidze and Ivanov to propose that homeland, and in that sense it is obviously flawed.

Those claiming a relationship of the North Iranian homeland with such EHG ancestry in Maykop, or with the hypothetic Proto-Euphratic or Gutian, are obviously not understanding the implications of finding steppe ancestry coupled with (likely) early Late PIE migrants in the region in the mid-4th millennium.

Related:

No large-scale steppe migration into Anatolia; early Yamna migrations and MLBA brought LPIE dialects in Asia

eurasian-hittite-samples

Another, simultaneous paper with the Eurasian samples from Nature, The first horse herders and the impact of early Bronze Age steppe expansions into Asia, by de Barros Damgaard et al., Science (2018).

A lot of interesting data, I will try to analyse its main implications, if only superficially, in sections.

Anatolian samples

Anatolia_EBA from Ovaören, and Anatolia_MLBA (this including Assyrian and Old Hittite samples), all from Kalehöyük, show almost no change in Y-DNA lineages (three samples J2a, one G2a), and therefore an origin of these people in common with CHG and Iranian Neolithic populations is likely. No EHG ancestry is found. And PCA cluster is just somehow closer to Europe, but not to EHG populations.

NOTE. Hittite is attested only in the late first half of the 2nd millennium, although the authors cite (in the linguistic supplement) potential evidence from the palatial archives of the ancient city of Ebla in Syria to argue that Indo-European languages may have been already spoken in the region in the late 3rd millennium BCE.

Regarding the Assyrian samples (one J2a) from Ovaören:

Layer V of GT-137 was the richest in terms of architectural finds and dates to the Early Bronze Age II. In this layer, 2 different structures and a well were uncovered. The well was filled with stones, pottery, and human skeletons (Figs. S2 and S3). In total, skeletons belonging to 22 individuals, including adults, young adults, and children, must belong to the disturbed Early Bronze Age II graves adjacent to the well (103). Pottery and stones found below the skeletons demonstrate that the water well was consciously filled and closed. The fill consists of dumped stones, sherds and skeletons, and the closing stones demonstrate that the water well was consciously filled and cancelled.

Regarding the site most likely associated with the emergence of Old Hittite (two samples J2a1, one G2a2b1), this is what we know:

The Middle Bronze Age at Kaman-Kalehöyük represented by stratum IIIc yields material remains (seals and ceramics) contemporary with the international trade system managed by expatriate Assyrian merchants evidenced at the nearby site of Kültepe/Kanesh. It is therefore also referred to as belonging to the “Assyrian Colony Period” (98). The stratum has revealed three burned architectural units, and it has been suggested that the seemingly site-wide conflagration might be connected to a destruction event linked with the emergence of the Old Hittite state (99). (…) Omura (100) suggests that the rooms could belong to a public building, and that it might even be a small trade center based on the types of artifacts recovered. Omura (100) has concluded that the evidence from the first complex indicates a battle between 2 groups took place at the site. It is possible that a group died inside the buildings, mostly perishing in the fire, while another group died in the courtyard.

NOTE. For more on the Old Hittite period, you can read this for example.

Regarding PCA:

The PCA (Fig. 2B) indicates that all the Anatolian genome sequences from the Early Bronze Age ( -2200 BCE) and Late Bronze Age (-1600 BCE) cluster with a previously sequenced Copper Age ( -3900- 3700 BCE) individual from Northwestern Anatolia and lie between Anatolian Neolithic (Anatolia_ N) samples and CHG samples but not between Anatolia_N and EHG samples.

(…) we are not able to reject a two-population qpAdm model in which these groups derive -60% of their ancestry from Anatolian farmers and -40% from CHG-related ancestry (p-value = 0.5). This signal is not driven by Neolithic Iranian ancestry.

pca-ancient-modern-eurasians
Principal Component Analysis estimated with ancient and modern Eurasians.

NOTE. Anatolian Iron Age samples, from the Hellenistic period, which was obviously greatly influenced by different, later Indo-European migrations, does show a change in PCA.

Regarding CHG ancestry:

Ancient DNA findings suggest extensive population contact between the Caucasus and the steppe during the Copper Age (-5000-3000 BCE) (1, 2, 42). Particularly, the first identified presence of Caucasian genomic ancestry in steppe populations is through the Khvalynsk burials (2, 47) and that of steppe ancestry in the Caucasus is through Armenian Copper Age individuals (42). These admixture processes likely gave rise to the ancestry that later became typical of the Yamnaya pastoralists (7), whose IE language may have evolved under the influence of a Caucasian language, possibly ‘from the Maykop culture (50, 55). This scenario is consistent with both the “Copper Age steppe” (4) and the “Caucasian” models for the origin of the Proto-Anatolian language (56).

The CHG specific ancestry and the absence of EHG-related ancestry in Bronze Age Anatolia would be in accordance with intense cultural interactions between populations in the Caucasus and Anatolia observed during the late 5th millennium BCE that seem to come to an end in the first half of the 4th millennium BCE with the village-based egalitarian Kura-Araxes society (59, 60), thus preceding the emergence and dispersal of Proto-Anatolian.

Our results indicate that the early spread of IE languages into Anatolia was not associated with any large-scale steppe-related migration, as previously suggested (61). Additionally, and in agreement with the later historical record of the region (62), we find no correlation between genetic ancestry and exclusive ethnic or political identities among the populations of Bronze Age Central Anatolia, as has previously been hypothesized ( 63).

The Anatolian question

There is no steppe ancestry or R1b-M269 lineages near early historic Hittites. Yet.

Nevertheless, we already know about potentially similar cases:

So there seems to be thus no theoretical problem in accepting:

  • That neither steppe ancestry nor R1b-M269 subclades, already diminished in Bulgaria in the mid-5th millennium, did reach Anatolia, but only those Common Anatolian-speaking Aegean groups over whose ancestors Proto-Anatolians (marked by incoming EHG ancestry) would have previously dominated in the Balkans.
  • That steppe ancestry and R1b-M269 subclades did in fact arrive in the Aegean, but EHG was further diluted among the CHG-related population by the time of the historic Anatolian-speaking peoples in central Anatolia. Or, the most likely option, that their trace have not been yet found. Probably the western Luwian peoples, near Troy, were genetically closer to Common Anatolians.

Both of these scenarios are interesting, in that they show potential links between Pre-Greek peoples of Hellas (related to Anatolians) and the Pelasgian substrate of early Greek dialects, since they show a similar recent CHG-related wave from the East.

What we can assert right now is that Proto-Anatolian must have separated quite early for this kind of data to show up. This should mean an end to the Late PIE origin of Anatolian, if there was some lost soul from the mid-20th century still rooting for this.

As I said in my review of Lazaridis’ latest preprint, we will have to wait for the appropriate potential routes of expansion of Proto-Anatolian to be investigated. As he answered, the lack of EHG poses a problem for steppe expansion into Anatolia, but there is still no better alternative model proposed.

Eurasian-CHG-ancestry
Model-based clustering analysis of present-day and ancient individuals assuming K = 6 ancestral components. The main ancestry components at K = 6 correlate well with CHG (turquoise), a major component of Iran_N, Namazga_CA and South Asian dines; EHG (pale blue), a component of the steppe dine and present in South Asia; East Asia (yellow ochre), the other component of the steppe d ine also in Tibeto-Burman South Asian populations; South Indian (pink), a core component of South Asian populations; Anatolian_N (purple), an important component of Anatolian Bronze Age and Steppe_MLBA; Onge (dark pink) forms its own component.

This is what the authors have to say:

Our findings are thus consistent with historical models of cultural hybridity and “Middle Ground” in a multi-cultural and multi-lingual but genetically homogeneous Bronze Age Anatolia (68, 69). Current linguistic estimations converge on dating the Proto-Anatolian split from residual PIE to the late 5th or early 4th millennia BCE (58, 70) and place the breakup of Anatolian IE inside Turkey prior to the mid-3rd millennium (53, 71,72).

We cannot at this point reject a scenario in which the introduction of the Anatolian IE languages into Anatolia was coupled with the CHG-derived admixture prior to 3700 BCE, but note that this is contrary to the standard view that PIE arose in the steppe north of the Caucasus (4) and that CHG ancestry is also associated with several non-IE-speaking groups, historical and current. Indeed, our data are also consistent with the first speakers of Anatolian IE coming to the region by way of commercial contacts and small-scale movement during the Bronze Age. Among comparative linguists, a Balkan route for the introduction of Anatolian IE is generally considered more likely than a passage through the Caucasus, due, for example, to greater Anatolian IE presence and language diversity in the west (73). Further discussion of these options is given in the archaeological and linguistic supplementary discussions (48, 49).

If you are asking yourselves why the Danish school (of Allentoft, Kristiansen, and Kroonen, co-authors of this paper) was not so fast to explain the findings the same way the proposed their infamous Indo-European – steppe ancestry association (i.e. ancestry = language, ergo CHG = PIE in this case), and resorted to mainstream anthropological models instead to explain the incongruence, I can think of two main reasons:

The possibility of having an early PIE around the Caucasus, potentially closely related not only to Uralic to the north, but also to Caucasian languages, Sumerian, Afroasiatic, Elamo-Dravidian, etc. could be a good reason for those excited with these few samples to begin dealing with macro-language proposals, such as Eurasiatic and Nostratic. If demonstrated to be true, a Northern Iranian origin of Middle PIE would also help relieve a little bit the pressure that some are feeling about the potentially male-driven Indo-European continuity (even if not “autochthonous”) associated with the expansion of R1b-L23 subclades.

On the other hand, I am a firm supporter of solid anthropological models of migration, and of “late and small” language expansions, usually accompanied by demic diffusion, which has been demonstrated to be linked with haplogroup expansion and reduction in variability.

Therefore, for the moment, even if it is weak – as weak as it always was (but still stronger than Gimbutas’ Maykop route) – the Balkan route seems like the best fit for all the data combined.

In fact, we already have steppe ancestry moving into the Lower Danube and Bulgaria in the mid-5th millennium. Let’s not forget that.

Yamna expansion to the East

Interesting data from an early East Yamna offshoot at Karagash, ca. 3018-2887 BC, of R1b-Z2106 lineage, which shows some ancestry, lineage, and cultural continuity in Sholpan, ca. 2620-2468 BC, in Kazakhstan.

This sample might be part of another descendant group from the migration waves that reached Afanasevo, and can thus be related to other early Asian R1b-L23 samples found in Narasimhan et al. (2018).

On the formation of Yamna and its CHG contribution, from the supplementary material:

  1. An admixture event, where Yamnaya is formed from a CHG population related to KK1 [=Kotias, dated ca. 7800 BC] and an ANE population related to Sidelkino and Botai. We inferred 54% of the Yamnaya ancestry to come from CHG and the remaining 46% to come from ANE.
  2. A split event, where the CHG component of Yamnaya splits from KK1. The model inferred this time at 27 kya (though we note the larger models in Sections S2.12.4 and S2.12.5 inferred a more recent split time [see below graphic]).
  3. A split event, where the ANE component of Yamnaya splits from Sidelkino. This was inferred at about about 11 kya.
  4. A split event, where the ANE component of Yamnaya splits from Botai. We inferred this to occur 17 kya. Note that this is above the Sidelkino split time, so our model infers Yamnaya to be more closely related to the EHG Sidelkino, as expected.
  5. An ancestral split event between the CHG and ANE ancestral populations. This was inferred to occur around 40 kya.
yamnaya-chg-ancestry
A 10-leaf model based on combining the models in Fig. S16 and Fig. S19 and re-estimating the model parameters.

On the expansion of domestication

CHG is not found in Botai, no gene flow from Yamna is found in its samples, and they are more related to East Asians, while Yamna is related to West Eurasians:

The lack of evidence of admixture between Botai horse herders and western steppe pastoralists is consistent with these latter migrating through the central steppe but not settling until they reached the Altai to the east (4). More significantly, this lack of admixture suggests that horses were domesticated by hunter-gatherers not previously familiar with farming, as were the cases for dogs (38) and reindeer (39). Domestication of the horse thus may best parallel that of the reindeer, a food animal that can be milked and ridden, which has been proposed to be domesticated by hunters via the “prey path” (40); indeed anthropologists note similarities in cosmological beliefs between hunters and reindeer herders (41). In contrast, most animal domestications were achieved by settled agriculturalists (5).

NOTE. I am not sure, but they seem to hint that there were separate events of horse domestication and horse-riding technique by the Botai and Yamna populations due to their lack of genetic contribution from the latter to the former. I guess they did not take into account farming spreading to the steppe without genetic contribution beyond the Dnieper… In fact, the superiority in horse-riding shown by the expanding Yamna peoples – as they state – should also serve to suggest from where the original technique expanded.

Indo-Iranian migrations

On the expansion of Yamna, and the different expansion of Steppe MLBA (with Indo-Iranian speakers) into Asia, further supporting Narasimhan et al. (2018), they have this to say:

However, direct influence of Yamnaya or related cultures of that period is not visible in the archaeological record, except perhaps for a single burial mound in Sarazm in present-day Tajikistan of contested age (44, 45). Additionally, linguistic reconstruction of proto-culture coupled with the archaeological chronology evidences a Late (-2300-1200 BCE) rather than Early Bronze Age (-3000-2500 BCE) arrival of the Indo-Iranian languages into South Asia (16, 45, 46). Thus, debate persists as to how and when Western Eurasian genetic signatures and IE languages reached South Asia.

Samples from the Namazga region (current Turkmenistan) from the Iron Age show an obvious influence from steppe MLBA (ca. 2300-1200 BC), and not steppe EBA (i.e. Yamna), population, in contrast with samples from the Chalcolithic (ca. 3300 BC), which don’t show this influence. This helps distinguish prior contacts with Iran Neolithic from the actual steppe population that expanded Indo-Iranian into Asia.

Very interesting therefore the Namazga CA sample (ca. 855 BC), of R1a-Z93 subclade, showing the sign of immigrant Indo-Aryans in the region. For more on this we will need an evaluation in common with the corrected data from Narasimhan et al. (2018), and all, including de Barros (Nature 2018), in combination with statistical methods to ascertain differences between early Indo-Aryans and Iranians.

namazga-expansion-south-asia
A summary of the four qpAdm models fitted for South Asian populations. For each modern South Asian population. we fit different models with qpAdm to explain their ancestry composition using ancient groups and present the f irst model that we could not reject in the following priority order: 1. Namazga_CA + Onge, 2. Namazga_CA + Onge + Late Bronze Age Steppe, 3. Namazga_CA + Onge + Xiongnu_lA (East Asian proxy). and 4. Turkmenistan_lA + Xiongnu_lA. Xiongnu_lA were used here to represent East Asian ancestry. We observe that while South Asian Dravidian speakers can be modeled as a mixture of Onge and Namazga_CA. an additional source related to Late Bronze Age steppe groups is required for IE speakers. In Tibeto-Burman and Austro-Asiatic speakers. an East Asian rather than a Steppe_MLBA source is required.

Siberian peoples and N1c lineages

We have already seen how the paper on Eurasian steppe samples tries to assign Uralic to Neolithic peoples east of the Urals. The association with Okunevo is unlikely, since most are of haplogroup Q1a2, but they seem to suggest (combining both papers) that they accompanied N lineages from Siberian hunter-gatherers (present e.g. in Botai or Shamanka II, during the Early Neolithic), and formed part of (or suffered from) different demic diffusion waves:

These serial changes in the Baikal populations are reflected in Y-chromosome lineages (Fig. SA; figs. S24 to S27, and tables S13 and SI4). MAI carries the R haplogroup, whereas the majority of Baikal_EN males belong to N lineages, which were widely distributed across Northern Eurasia (29), and the Baikal_LNBA males all carry Q haplogroups, as do most of the Okunevo_EMBA as well as some present-day Central Asians and Siberians.

NOTE. Also interesting to see no R1a in Baikal hunter-gatherers after ca. 3500 BC, and a prevalence of N lineages as supported in a previous paper on the Kitoi culture, which some had questioned in the past.

In fact, the only N1c1 sample comes from Ust’Ida Late Neolithic, 180km to the north of Lake Baikal, apparently before the expansion of Q1a2a lineages during the EBA period. While this sample may be related to those expanded later in Finno-Ugric territory (although it may only be related to those expanded much later with Yakuts), other samples are not clearly from those found widely distributed among North-East Europeans only after the Iron Age, or – as in the case of Shamanka II (N1c2), they are clearly not of the same haplogroup.

eurasian-n-subclades
Geographical location of ancient samples belonging to major clade N of the Y-chromosome.

Wrap-up

It is great to see the paper and the supplementary material deal with Y-DNA haplogroups and their relevance for migrations with such detail. Especially because this paper comes from the same Copenhagen-based research group that originally associated ancestry with language, creating thus today’s mess based on steppe ancestry.

Regarding Y-DNA data, once again almost 100% of samples from late Khvalynsk/Yamna and derived cultures (like Afanasevo and Bell Beaker) are R1b-L23, no single R1a-M417 lineage found, and few expected by now, if any, within Late Proto-Indo-European territory.

While they claim to take Y-DNA into account to assess migrations – as they do for example with Asian cultures – , their previous model of a Yamna “R1a-R1b community” remains oddly unchanged, and they even insist on it in the supplementary materials, as they do in their parallel Nature paper.

They have also expressly mitigated the use of ancestral components to assess populations, citing the ancestral and modern association of CHG ancestry with different ethnolinguistic groups in the Middle East, to dismiss any rushed conclusions on the origin of Anatolian, and consequently of Middle PIE. And they did so evidently because it did not fit the anthropological data that is mainstream today (supporting a Balkan route), which is the right thing to do.

However, they have apparently not stopped to reconsider the links of CWC and steppe ancestry to ancestral and modern Uralic peoples – although they expressly mention the strong connection with modern Karelians in the supplementary material.

Also, after Narasimhan et al. (2018), there is a clear genetic continuity with East Yamna (in ancestry as in R1b-L23 subclades), so their interpretations about Indo-Iranian in this paper and especially de Barros (Nature 2018) – regarding the Abashevo -> Sintashta/Srunba/Andronovo connection – come, again, too late.

Related:

Haplogroup R1b-L51 in Khvalynsk samples from the Samara region dated ca. 4250-4000 BC

A commenter in a previous post left a reference to an oral communication by Aleksander Khokhlov – shared in a Russian forum on genetics – , from the XIV Conference on Samaran Archaeology, 27-28th January 2018 (still publicized in the Samaran Archaeological Society).

NOTE. You may know Khokhlov as a palaeoanthropologist, part of the Samara Valley project, like David W. Anthony. See the project referenced here, or their recently published book.

Here is my translation of the reported summary (emphasis mine):

Khokhlov, A.A. Preliminary results of anthropological and genetic studies of materials of the Volga-Ural region of the Neolithic-Early Bronze Age by an international group of scientists.

In his report, A. A. Khokhlov introduced the scientific circle to the still unpublished data of the new Eneolithic burial ground Yekaterinovskiy Cape, which combines both the Mariupol and Khvalynsk features, and is dated to the fourth quarter of the V millennium BC. All samples analyzed had a Uraloid anthropological type, the chromosome of all samples belonged to haplogroup R1b1a2 (R-P312/S116), and to haplogroup R1b1a1a2a1a1c2b2b1a2. mtDNA to haplogroups U2, U4, U5. In the Khvalynsk burial grounds (first half of the IV millennium BC), the anthropological material differs in a greater variety. In addition to the Uraloid substratum, European wide-faced and southern European variants are recorded. To the samples are added haplogroup R1a1, O1a1, I2a2 to mtDNA T2a1b, H2a1.

yekaterinovka-cape
Yekaterinovskiy burial of male, 20-25 years old, dated ca. 4400-4200 BC. Via Pikabu.

So, first of all:

  • This is a reported summary of an oral communication, and it was written in a forum by a user. Unlike many out there, though, this one uses his real name, apparently assisted to the conference, and is himself a Russian of self-reported haplogroup R1a1a, so probably no interest in reporting this if it’s not true. Errors contained may have been made by him, and may not have been found in the original communication, since he says he wrote it by hand.
  • Something is obviously off with the haplogroup nomenclature. There has recently been mixing of standards, with some papers reporting R1b1a2-M269 (which is supposed to be now ISOGG V88), and most using R1b1a1a2-M269. What I had never seen is both standards used at the same time, as in this report, so I guess it’s another error of transcription.
  • It is doubtful that we would be talking about that recent referenced subclade of U106, but it can’t be a surprise to finally find L51 subclades alongside Z2103 in Proto-Indo-European territory. Also, the summary must obviously refer to Q1a1, not O1a1, and probably to the first half of the V (and not IV) millennium BC.

NOTE. Since Khokhlov, like Anthony, is an anthropologist, and this is an archaeological conference, we could suppose – if the report is truthful to what he said or what could be read in the summary – that this is the best he can do to report genetic material that was not assessed by him, but by a specialized lab, because it is not his field. I think the relevant data is nevertheless useful until we have the official publication.

Archaeological remains studied come from a site near Yekaterinovka. You can read more about it in The Ekaterinovsky cape – A new Eneolithic burial ground in the forest-steppe volga region (2013).

From this report of archaeological works, we know there were 60 Early Eneolithic burials excavated in 2013, dating to the period between S’yezzhe and Khvalynsk. 15 more burials were excavated in 2017, and there are to date already around 93 reported burials, with ongoing excavations.

Assuming that what the report conveys is more or less correct in the basics, let’s derive some simple conclusions from the data:

  • The presence of some samples uniformly of R1b-L23 subclades that early will mean an end to the question of when this haplogroup dominated over the Khvalynsk population, and probably also when it appeared (rather early during this culture’s formation), since it would mean R1b-L23 subclades were widespread already by the end of the 5th millenium.
  • I can only guess that CHG ancestry will be found in these samples, based indirectly on what is reported in anthropological terms, and what appears later in Yamna and Afanasevo samples. This will contradict some recent comments suggesting an admixture driven by males from the south, and especially a Maykop -> Khvalynsk migration as a source of this component, placing the admixture at earlier times, and/or driven by exogamy. Therefore we can reject the formation of Middle PIE outside of Khvalynsk, and also the expansion of Proto-Anatolian from Maykop (unless Maykop itself is proposed as a steppe offshoot).
  • The presence of L51 lineages in certain clans side by side with others formed mainly by Z2103 in such a small region supports (as I proposed) the existence of early diverging LPIE communities – and therefore also the early splitting of a Northern and a Southern (i.e. Graeco-Aryan) dialect, each associated with certain regional groups – already by this time, which may help with the identification of later migrants that ended in Afanasevo (and thus confirm the dialectal origin of Pre-Tocharian). It goes without saying that all those ideas of R1b-L51 stemming from North Pontic cultures, the Balkans, Central or Western Europe – unrelated to Khvalynsk or Yamna – should be rejected.
  • Khvalynsk was probably dominated by R1b-L23 subclades already ca. 4250-4000 BC, which – combined with earlier, more diverse Eneolithic samples from the region (dated ca. 5000-4500 BC) – would support an expansion of these subclades just before this time, in the mid-5th millennium BC, as I proposed based on ancient samples and TMRCAs of modern haplogroups. It is now more likely then that I was right in linking the expansion of R1b-M269 and early R1b-L23 lineages as chiefs with the spread of horse riding from early Khvalynsk, and thus associated also with the split and migration of the Proto-Anatolian community, probably with expanding Suvorovo-Novodanilovka chiefs.
  • These findings should finally put an end to the idea of a shared “R1a-R1b Proto-Indo-European community”, by rejecting its existence already during the early Khvalynsk period, and therefore also rejecting the idea of a North Pontic Indo-Slavonic proto-language as impossible, since it would need a split 2,000 years before the known Late PIE expansions associated with Yamna, and 3,000 years before the formation of the early Indo-Iranian community in Sintashta-Andronovo.

NOTE. While the presence of R1b-P312 and R1b-U106 subclades that early does not seem likely based on their estimated formation dates (in turn based on modern descendants), this is not the first time that such estimations have been proven wrong with ancient samples (viz. the “late” Z93 subclade from Eneolithic Ukraine sample I6561). Also, we already have one sample labelled U106 supposedly expanding with Indo-Iranians, and a sample of an early L51 subclade in Central Asia potentially linked to Afanasevo migrants in the infamous tables of Narasimhan et al. (2018), which help support its early presence in the North Caspian area. Some of these younger subclades seem (based on TMRCAs and forming dates of modern haplogroups) more like a wrong ‘excessive-subclade-reporting fest’, probably due to the use of a certain software for inferences of Y-SNP calls from scarce material, but who knows.

EDIT (2 MAY 2018): A commenter in the forum cast doubts on the actual dates of the site, citing the reservoir effect in Khvalynsk which may show earlier radiocarbon dates than the actual ones. Since this is an international team well versed in archaeological remains of this region, and there have been already many samples and remains assessed before and after these dates, it is not very likely that they did not take such problems of radiocarbon dating into account when reporting the findings…

The publication of this and more data in a book is supposedly due for the summer, so let’s wait for the officially reported haplogroups, and for the corrected tables in Narasimhan et al. (2018), to draw the necessary detailed conclusions.

This post was emailed to subscribers of this blog on the 1st of May immediately after publication, with our Newsletter. If you want to keep up to date with the latest interesting information instantly (few mails will be submitted a month, if any), subscribe now.

EDIT (May 2017) The answer I received from the group to my questions regarding these samples can be read here.

Related:

Proto-Indo-European homeland south of the Caucasus?

User Camulogène Rix at Anthrogenica posted an interesting excerpt of Reich’s new book in a thread on ancient DNA studies in the news (emphasis mine):

Ancient DNA available from this time in Anatolia shows no evidence of steppe ancestry similar to that in the Yamnaya (although the evidence here is circumstantial as no ancient DNA from the Hittites themselves has yet been published). This suggests to me that the most likely location of the population that first spoke an Indo-European language was south of the Caucasus Mountains, perhaps in present-day Iran or Armenia, because ancient DNA from people who lived there matches what we would expect for a source population both for the Yamnaya and for ancient Anatolians. If this scenario is right the population sent one branch up into the steppe-mixing with steppe hunter-gatherers in a one-to-one ratio to become the Yamnaya as described earlier- and another to Anatolia to found the ancestors of people there who spoke languages such as Hittite.

The thread has since logically become a trolling hell, and it seems not to be working right for hours now.

Reich’s proposal based on ancestral components to explain the formation of a people and language is a continuation of their emphasis on ancestry to explain cultures and languages. It seems quite interesting to see this happen again, given their current trend to surreptitiously modify their previous ‘Yamnaya ancestry’ concept and Yamnaya millennia-long R1a-R1b community (that supposedly explains a Yamna -> Corded Ware -> Bell Beaker migration) to a more general ‘steppe people’ sharing a ‘steppe ancestry’ who spoke a ‘steppe language’.

steppe-ancestry
Interesting arrows of dispersal of steppe ancestry, from Yamna -> Corded Ware -> Bell Beaker, from David Reich’s new book (yes, from 2018, number one bestseller in Amazon.com).

This new idea based on ancestral components suffers thus from the same essential methodological problems, which equate it – yet again – to pure speculation:

  1. It is a conclusion based on the genomic analysis of few individuals from distant regions and different periods, and – maybe more disturbingly – on the lack of steppe ancestry in the few samples at hand.
  2. Wait, what? Steppe ancestry? So they are trying to derive potential genetic connections among specific prehistoric cultures with a poorly depicted genetic sketch, based on previous flawed concepts (instead of on anthropological disciplines), which seems a rather long stretch for any scientist, whether they are content with seeing themselves as barbaric scientific conquerors of academic disciplines or not. In other words, statistics is also science (in fact, the main one to assert anything in almost any scientific field), and you cannot overcome essential errors (design, sampling, hypothesis testing) merely by using a priori correct statistical methods. Results obtained this way constitute a statistical fallacy.

  3. Even if the sampling and hypothesis testing were fine, to derive anthropological models from genomic investigation is completely wrong. Ancestral component ≠ population.
  4. To include not only potential migrations, but also languages spoken by these potential migrants? It’s sad that we have a need to repeat it, but if ancestral component ≠ population, how could ancestral component = language?

The Proto-Indo-European-speaking community

This is what we know about the formation of a Proto-Indo-European community (i.e. a community speaking a reconstructible Proto-Indo-European language) in the Pontic-Caspian steppe, which is based on linguistic reconstruction and guesstimates, tracing archaeological cultures backwards from cultures known to have spoken ancient (proto-)languages, and helping both disciplines with anthropological models (for which ancient genomics is only helping select certain details) of migration or – rarely – cultural diffusion:

NOTE. The following dates are obviously simplified. Read here a more detailed linguistic assessment based on phonology.

neolithic_steppe-anatolian-migrations
Most likely Pre-Proto-Anatolian migration with Suvorovo-Novodanilovka chiefs in the North Pontic steppe and the Balkans.
  • ca. 5000 BC. Early Proto-Indo-European (or Indo-Uralic) spoken probably during the formation and development of a loose Early Khvalynsk – Sredni Stog I cultural-historical community over the Pontic-Caspian steppe region, whose indigenous population probably had mainly Caucasus hunter-gatherer ancestry.
  • ca. 4500 BC. Khvalynsk probably speaking Middle Proto-Indo-European expands, most likely including Suvorovo-Novodanilovka chiefs into the North Pontic steppe, and probably expanding R1b-M269 lineages for the first time.
  • ca. 4000 BC. Separated communities develop, including North Pontic cultures probably gradually dominated by R1a-Z645 (potentially speaking Proto-Uralic); and Khvalynsk (and Repin) cultures probably dominated by R1b-L23 lineages, most likely developing a Late Proto-Indo-European already separated from Proto-Anatolian.
  • ca. 3500 BC. A Proto-Corded Ware population dominated by R1a-Z645 expands to the north, and slightly later an early Yamna community develops from Late Khvalynsk and Repin, expanding to the west of the Don River, and to the east into Afanasevo. This is most likely the period of reduction of variability and expansion of subclades of R1a-Z645 and R1b-L23 that we expect to see with more samples.
  • ca. 3000 BC. Expansion of Corded Ware migrants in northern Europe, and Yamna migrants along the Danube and into the Balkans, with further reduction and expansion of certain subclades.
  • ca. 2500 BC. Expansion of Bell Beaker migrants dominated by R1b-L51 subclades in Europe, and late Corded Ware migrants in east Yamna expanding R1a-Z93 subclades.

All these events are compatible with language reconstruction in mainstream European schools since at least the 1980s, supported by traditional archaeological research of the past 20 years, and is being confirmed with Genomics.

For those willingly lost in a myriad of new dreams boosted by the shallow comment contained in David Reich’s paragraph on CHG ancestry, even he does not doubt that the origin of Late Proto-Indo-European lies in Yamna, to the north of the Caucasus, based on Anthony’s (2007) account:

yamnaya-migrations-reich
Both images from the book, posted by Twitter user Jasper at https://twitter.com/jaspergregory.

NOTE: By the way, David Anthony, one of the main sources of information for Reich’s group, never considered Corded Ware to have received Yamna migrants, and althought he changed his model due to the conclusions of the 2015 papers, he has recently changed his model again to adapt it to the inconsistencies found in phylogeography.

CHG ancestry and PIE homeland south of the Caucasus

As for the potential origins of CHG ancestry in early Proto-Indo-European speakers, I already stated clearly my opinion quite recently. They may be attributed to:

Just to be clear, an expansion of Proto-Anatolian to the south, through the Caucasus, cannot be discarded today. It will remain a possibility until Maykop and more Balkan Chalcolithic and Anatolian-speaking samples are published.

However, an original Early Proto-Indo-European community south of the Caucasus seems to me highly unlikely, based on anthropological data, which should drive any conclusion. From what I could read, here are the rather simplistic arguments used:

  • Gimbutas and Maykop: Maykop was thought to be (in Gimbutas’ times) a rather late archaeological culture, directly connected to a Transcaucasian Copper Age culture ca. 2400-2300 BC. It has been demonstrated in recent years that this culture is substantially older, and even then language guesstimates for a Late PIE / Proto-Anatolian would not fit a migration to the north. While our ignorance may certainly be used to derive far-fetched conclusions about potential migrations from and to it, using Gimbutas (or any archaeological theory until the 1990s) today does not make any sense. Still less if we think that she favoured a steppe homeland.

NOTE. It seems that the Reich Lab may have already access to Maykop samples, so this suggested Proto-Indo-European – Maykop connection may have some real foundation. Regardless, we already know that intense contacts happened, so there will be no surprise (unless Y-DNA shows some sort of direct continuity from one to the other).

  • Gamkrelidze & Ivanov: they argued for an Armenian homeland (and are thus at the origin of yet another autochthonous continuity theory), but they did so to support their glottalic theory, i.e. merely to support what they saw as favouring their linguistic model (with Armenian being the most archaic dialect). The glottalic theory is supported today – as far as I know – mainly by Kortlandt, Jagodziński, or (Nostraticist) Bomhard, but even they most likely would not need to argue for an Armenian homeland. In fact, their support of a Graeco-Aryan group (also supported by Gamkrelidze & Ivanov) would be against this, at least in archaeological terms.
  • Colin Renfrew and the Anatolian homeland: This conceptual umbrella of language spreading with farming everywhere has changed so much and so many times in the past 20 years, with so many glottochronological and archaeological estimates circulating, that you can support anything by now using them. Mostly used today for abstract models of long-lasting language contacts, cultural diffusion, and constellation analogies. Anyway, he strives to keep up-to-date information to revise the model, that much is certain:
  • Glottochronology, phylogenetic trees, Swadesh list analysis, statistical estimates, psychics, pyramid power, and healing crystals: no, please, no.
Science Magazine
“A first line of evidence comes from linguistic analysis based on quantitative lexical data, which returned a tree compatible with the Anatolian hypothesis

In principle, unlike many other recent autochthonous continuity theories, I doubt there can be much racial-based opposition anywhere in the world to an origin of Proto-Indo-European in the Middle East, where the oldest civilizations appeared – apart, obviously, from modern Northeast and Northwest Caucasian, Kartvelian, or Semitic speakers, who may in turn have to revisit their autochthonous continuity theories radically…

Nevertheless, it is obvious that prehistoric (and many historic) migrations are signalled by the reduction in variability and expansion of certain Y-DNA haplogroups, and not just by ancestral components. That is generally accepted, although the reasons for this almost universal phenomenon are not always clear.

In fact, Proto-Anatolian and Common Anatolian speakers need not share any ancestral component, PCA cluster, or any other statistical parameter related to steppe populations, not even the same Y-DNA haplogroups, given that approximately three thousand years might have passed between their split from an Indo-Hittite community and the first attested Anatolian-speaking communities…We must carefully follow their tracks from Anatolia ca. 1500 BC to the steppe ca. 4500 BC, otherwise we risk creating another mess like the Corded Ware one.

In my opinion, the substantial contribution of EHG ancestry and R1a-M417 lineages to the Pontic-Caspian steppe (probably ca. 6500 BC) from Central or East Eurasia is the most recent sizeable genomic event in the region, and thus the best candidate for the community that expanded a language ancestral to Proto-Indo-European – whether you call it Pre-Proto-Indo-European, Pre-Indo-Uralic, or Eurasiatic, depending on your preferences.

An early (and substantial) contribution of CHG ancestry in Khvalynsk relative to North Pontic cultures, if it is found with new samples, may actually be a further proof of the Caucasian substrate of Proto-Indo-European proposed by Kortlandt (or Bomhard) as contributing to the differentiation of Middle PIE from Uralic. Genomics could thus help support, again, traditional disciplines in accepting or rejecting academic controversial theories.

Conclusion

In the case of an Early PIE (or Indo-Uralic) homeland, genomic data is scarce. But all traditional anthropological disciplines point to the Pontic-Caspian steppe, so we should stick to it, regardless of the informal suggestion written by a renown geneticist in one paragraph of a book conceived as an introduction to the field.

It seems we are not learning much from the hundreds of peer-reviewed, statistically (superficially, at least) sound genetic papers whose anthropological conclusions have been proven wrong by now. A lot of people should be spending their time learning about the complex, endless methods at hand in this kind of research – not just bioinformatics – , instead of fruitlessly speculating about wild unsubstantiated proposals.

As a final note, I would like to remind some in the discussion, who seem to dismiss the identification of CHG with Proto-Indo-European by supporting a “R1a-R1b” community for PIE, of their previous commitment to ancestral components in identifying peoples and languages, and thus their support to Reich’s (and his group’s) fundamental premises.

You cannot have it both ways. At least David Reich is being consistent.

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