Proto-Tocharians: From Afanasievo to the Tarim Basin through the Tian Shan

tocharians-early-eneolithic

A reader commented recently that there is little information about Indo-Europeans from Central and East Asia in this blog. Regardless of the scarce archaeological data compared to European prehistory, I think it is premature to write anything detailed about population movements of Indo-Iranians in Asia, especially now that we are awaiting the updates of Narasimhan et al (2018).

Furthermore, there was little hope that Tocharians would be different than neighbouring Andronovo-like populations (see a recent post on my predicted varied admixture of Common Tocharians), so the history of both unrelated Late PIE languages would have had to be explained by the admixture of Afanasievo-related groups with peoples of Andronovo descent and their acculturation.

However, data reported recently by Ning, Wang et al. Current Biology (2019) confirmed that peoples of mainly Afanasievo ancestry – as opposed to those of Corded Ware-related ancestry expanding with the Srubna-Andronovo horizon – spread the Tocharian branch of Proto-Indo-European from the Altai into the Tian Shan area, surviving essentially unadmixed into the Early Iron Age.

This genetic continuity of Tocharians will no doubt help us disentangle a great part the ethnolinguistic history of speakers of the Tocharian branch of Proto-Indo-European, from Pre-Proto-Tocharians of Afanasievo to Common Tocharians of the Late Bronze Age/Iron Age eastern Tian Shan.

NOTE. Tocharian’s isolation from the rest of Late PIE dialects and its early and intense language contacts have always been the key to support an early migration and physical separation of the group, hence the traditional association with Afanasievo, a late Repin/early Yamna offshoot. Even with the current incomplete archaeological and genetic picture, there is no other option left for the expansion of Tocharian.

It is not possible to use the currently available ancestry data to map the evolution of Afanasievo ancestry, lacking a proper geographical and temporal transect of Central and East Asian groups. In spite of this, Ning, Wang, et al. (2019) is a huge leap forward, discarding some archaeological models, and leaving only a few potential routes by which Tocharians may have spread southward from the Altai.

NOTE. I have updated the maps of prehistoric cultures accordingly, with colours – as always – reflecting the language/ancestry evolution of the different groups, even though the archaeological data of some groups of Xinjiang remains scarce, so their ethnolinguistic attribution – and the colours picked for them – remain tentative.

xinjiang-andronovo-xiaohe-horizon-bronze-iron-age
A rough timeline of related archaeological sites from North Eurasia. Image modified from Yang (2019).

Tocharians

The recent book Ancient China and its Eurasian Neighbors. Artifacts, Identity and Death in the Frontier, 3000–700 BCE, by Linduff, Sun, Cao, and Liu, Cambridge University Press (2017) offers an interesting summary of the introduction of metalworking into western China.

Here are some relevant excerpts (emphasis mine):

Although [the Xinjiang] route is not uniformly agreed upon (Shelach-Lavi 2009: 134–46), this western transmission has been thought to have passed through eastern Kazakhstan, especially as it is manifest in Semireiche, with Yamnaya, Afanasievo (copper) and Andronovo (tin bronze) peoples (Mei 2000: Fig. 3). From Xinjiang this knowledge has been thought to have traveled through the Gansu Corridor via the Qijia peoples (Bagley 1999) and then into territories controlled by dynastic China. The dating of this process is still a problem, as the sites and their contents in Xinjiang are consistently later than those in Gansu, suggesting that the point of contact was in Gansu and that the knowledge then spread from there westward.

1. Eneolithic Altai

tocharians-chalcolithic-eneolithic
Afanasievo expansion ca. 3300-2600 BC. See full culture and ancient DNA maps.

The Afanasievo sites, as they are identified in Mongolia, for instance, make up an Eneolithic culture analogous to that of southern Siberia (3100/2500–2000 BCE) in the Upper Yenissei Valley that is characterized by copper tools and an economy reliant on horse, sheep and cattle breeding as well as hunting. (…) The Afanasievo is best known through study of its burials, which typically include groups of round barrows (kurgans), each up to 12 m in diameter with a stone kerb and covering a central pit grave containing multiple inhumations. In their Siberian context, burial pottery types and styles have suggested contacts with the slightly earlier Kelteminar culture of the Aral and Caspian Sea area.

The Afanasievo culture monuments, located in the northern Altai and in the Minusinsk Basin (the western Sayan), have been seen as analogous evidence for cross-Eurasian exchange. These complexes contain small collections of metal, and many of the items are made of brass, although golden, silver and iron ornaments were also identified. A mere one-fourth of these objects are tools and ornaments, while the rest consist of unshaped remains and semi-manufactured objects. Its metallurgical tradition has recently been dated by Chernykh to as early as 3100 to 2700 BCE (1992),making it more compatible chronologically with the early brass-using sites in Shaanxi mentioned above. Kovalev and Erdenebaatar have excavated barrows in Bayan-Ulgii, Mongolia, that have been carbon-dated to the first half of the third millennium BCE and associated by ceramic types and styles and burial patterns with the Afanasievo (Kovalev and Erdenebaatar 2009: 357–58). These mounded kurgans were covered with stone and housed rectangular, wooden-faced tombs that included Afanasievo-type bronze awls, plates and small “leaf-shaped” knife blades (Kovalev and Erdenebaatar 2009: Figs. 6 and 7).

They also excavated sites belonging to the more recently identified Chemurchek archaeological culture, located in the foothills of the Mongolian Altai (Kovalev 2014, 2015) (Fig. 2.6). These sites are carbon-dated to the same period as the Afanasievo burials or to c. 3100/2500–1800 BCE (six barrows in Khovd aimag and four in Bayan-Ulgo aimag). In the rectangular stone kerbed Chemurchek slab burials (Ulaaanhus sum, Bayan-ul’gi aimag and so forth), bronze items included awls; and at Khovd aimag, Bulgan sum, in addition to stone sculptures, three lead and one bronze ring were excavated (Kovalev and Erdenebaatar 2009: Figs. 2 and 3; Fig. 2.6). Although we will not know if they were produced locally until much further investigation is undertaken, these discoveries do document knowledge of various uses and types of metal objects in western and south central Mongolia. The types of metal items thus far recovered are simple tools (awls) and rings (ornamental?) not unlike those associated with Andronovo archaeological cultures as well.

This is a complex circumstance where archaeological evidence is not complete, but raises very important questions about transmission of metallurgical knowledge to and from areas in present-day China. In the 1970s some Afanasievo mounds were excavated in Central Mongolia by a Soviet–Mongolian expedition led by V. V. Volkov and E. A. Novgorodova (Novgorodova 1989: 81–85). Unfortunately, these mounds did not yield metal objects, only ceramics, but they show that the Afanasievo culture with the Eneolithic metallurgical tradition of manufacturing pure copper items had already moved east at least far as central Mongolia. In 2004, Kovalev and Erdenebaatar investigated a large Afanasievo mound, Kulala ula, in the extreme northwest of Mongolia, near the Russian border (Kovalev and Erdenebaatar 2009). There they found a copper knife and awl (Fig. 2.5). There are five C14 dates on wood, coal and human bones from this mound, which belong to the period 2890–2570 BCE. This shows that the Afanasievo culture were carriers of technology and produced artifacts in the first half of the third millennium BCE and that they also moved south along the foothills of the Mongolian Altai. Afanasievo culture in Altai and the Minusinsk basin is dated by C14 to 3600–2500 BCE (Svyatko et al. 2009; Polyakov 2010). In the north of Xinjiang in the Altai district, several typical egg-shaped vessels and two censers of Afanasievo types were found. Some of these have been obtained from the stone boxes (chambers of megalithic graves of the Chemurchek culture) (Kovalev 2011). Thus, the Afanasievo tradition of pure copper metallurgy must have spread to the northern foothills of the Tienshan Mountains no later than the mid-third millennium BCE. The links with Afanasievo and local cultures adjacent to and south of the mountains into present-day China can now be assumed.

tocharians-chalcolithic-late
Afanasievo – Chemurchek evolution ca. 2600-2200 BC. See full culture and ancient DNA maps.

2. Bronze Age Altai

Kovalev and Erdenebaatar (2014a) and later Tishkin, Grushin, Kovalev and Munkhbayar (2015) in Western Mongolia conducted large-scale excavations of megalithic barrows of the Chemurchek culture (dated about 2600–1800 BCE). This peculiar culture appeared in Dzungaria and the Mongolian Altai in the second quarter of the third millennium BCE and for some time existed together with the late Afanasievo culture, as evidenced by the findings of Afanasievo ceramics in Chemurchek graves, in the stone boxes. Unfortunately, in China we do not yet know of any metal object related,without doubt, to the Chemurchek culture. Kovalev, Erdenebaatar, Tishkin and Grushin found several leaden ear rings and one ring of tin bronze in three excavated Chemurchek stone boxes (Kovalev and Erdenebaatar 2014a; Tishkin et al. 2015). Such lead rings are typical for Elunino culture,which occupied the entire West Altai after 2400–2300 BCE (Tishkin et al. 2015). This culture had developed a tradition of bronze metallurgy with various dopants, primarily tin. Thus, the tradition of bronze metallurgy as early as this time could have penetrated the Mongolian Altai far to the south. In addition, in the Hadat ovoo Chemurchek stone box, Kovalev and Erdenebaatar discovered stone vessels refurbished with the help of copper “patches,” indicating the presence there of metallurgical production (Fig. 2.7) (Kovalev and Erdenebaatar 2014a). In one of the secondary

Chemurchek graves unearthed by Kovalev and Erdenebaatar in Bayan-Ulgi (2400–2220 BCE), a bronze awl was found (Kovalev and Erdenebaatar 2009). Kovalev and Erdenebaatar also discovered a new culture in the territory of Mongolia (Map 2.3), one that begins immediately after Chemurchek – Munkh-Khairkhan culture (Kovalev and Erdenebaatar 2009, 2014b). To date, about 17 mounds of this culture have been excavated in Khovd, Zavkhan, Khovsgol, Bulgan aimag of Mongolia. This culture dates from about 1800 to 1500 BCE, that is, contemporary with the Andronovo culture. Therefore, the Andronovo culture does not extend far into the territory of Mongolia. Three knives without dedicated handles or stems and five awls have been found in the Munkh-Khairkhan culture mounds (Fig. 2.8). All these products are made of tin bronze. (…) Additionally, eight Late Bronze Age burials (c. 1400–1100 BCE) were unearthed in the Bulgan sum of Khovd aimag and belong to another previously unknown culture called Baitag. And in the Gobi Altai, a new group of “Tevsh” sites dating to the Late Bronze Age were defined in Bayankhongor and South Gobi aimags (Miyamoto and Obata 2016: 42–50). From these Tevsh and Baitag sites, we see the expansion of burial goods to include beads of semiprecious stones (carnelian), bronze beads, buttons and rings and even the famous elaborate golden hair ornaments (Tevsh uul;Bogd sum;Uverkhanagia aimag) from the Baitag barrows (Kovalev and Erdenebaatar 2009: Fig. 5; Miyamoto and Obata 2016).

2.1. Chemurchek

About the Chemurchek culture, from A re-analysis of the Qiemu’erqieke (Shamirshak) cemeteries, Xinjiang, China, by Jia and Betts JIES (2010) 38(4):

The major characteristics of Qiemu’erqieke Phase I include:

  1. Burials with two orientations of approximately 20° or 345°.
  2. Rectangular enclosures built using large stone slabs. The size of the enclosure varies from a maximum of 28 x 30 m.*to a minimum of 10.5 x 4.4 m. (Figure 8, Table 2).
  3. *The stone enclosure located near Hayinar is the largest one at approximately 30 x 40 m. based on pacing of the site during a visit by the authors in 2008.

  4. Almost life-sized anthropomorphic stone stelae erected along one side of the stone enclosures (Lin Yun 2008).
  5. Single enclosures tend to contain one or more than one burial, all or some with stone cist coffins.
  6. The cist coffin is usually constructed using five large stone slabs, four for the sides and one on top, leaving bare earth at the base (Zhang Yuzhong 2007). Sometimes the insides of the slabs have simple painted designs (Zhang Yuzhong 2005).
  7. Primary and secondary burials occur in the same grave.
  8. Some decapitated bodies (up to 20) may be associated with the main burial in one cist.
  9. Bodies are commonly placed on the back or side with the legs drawn up.
  10. Grave goods include stone and bronze arrowheads, handmade gray or brown round-bottomed ovoid jars, and small numbers of flat-bottomed jars (Fig. 7).
  11. Clay lamps appear to occur together with roundbottomed jars.
  12. Complex incised decoration on ceramics is common but some vessels are undecorated.
  13. The stone vessels are distinctive for the high quality of manufacture.
  14. Stone moulds indicate relatively sophisticated metallurgical expertise.
  15. Artefacts made from pure copper occur.
  16. Sheep knucklebones (astragali) imply a tradition (as in historical and modern times) of keeping knucklebones for ritual or other purposes. They also indicate the herding of domestic sheep as part of the subsistence economy.
tocharians-bronze-age-early
Chemurchek culture ca. 2200-1750 BC. See full culture and ancient DNA maps.

Chemurchek dating

Available evidence suggests that the date range for Qiemu’erqieke Phase I should fall from the later third into the early second millennium BC. There are several reasons to suggest that the time span is around the early second millennium BC. Lin Yun (2008) (…) maintains that the bronze artefacts found in Phase I show a greater sophistication in the level of copper alloy technology than that of the pure copper artefacts common to the Afanasievo tradition. On this basis it might be suggested that the Afanasievo could be considered to be Chalcolithic with a time span across much of the third millennium BC ( Gorsdorf et al. 2004: 86, Fig. 1). Qiemu’erqieke Phase I, however, should more properly be considered as Bronze Age.

Lin Yun also used the bronze arrowhead from burial Ml 7 to narrow down the date of Qiemu’erqieke Phase I. Two arrowheads were found in this burial, one of them leaf shaped with a single barb on the back (Fig. 7:4). A similar arrowhead, together with its casting mould, has been found at the Huoshaogou site of Siba tradition (Li Shuicheng 2005, Sun Shuyun and Han Rufen 1997), in Gansu province, northwest China, dated around 2000-1800 BC (Li Shuicheng and Shui Tao 2000) . This supports a date in the early second millennium BC for the Qiemu’erqieke arrowhead. The painted, round-bottomed jar from the Tianshanbeilu cemetery Qia Weiming, Betts and Wu Xinhua 2008: Fig. 7, bottom left) has been considered as a hybrid between the Upper Yellow River Bronze Age cultures of Siba in northwest China and the steppe tradition of Qiemu’erqieke in west Siberia (Li Shuicheng 1999). If this assumption is correct, the date of Tianshanbeilu, around 2000 BC, can be used as a reference for Qiemu’erqieke Phase I (Jia Weiming, Betts and Wu Xinhua 2008, Lin Yun 2008, Li Shuicheng 1999). Stone arrowheads found in Qiemu’erqieke Phase I also imply that the date is likely to fall within the earlier part of the Bronze Age as no such stone arrowheads have yet been found elsewhere in sites of the Bronze Age in Xinlang dated after the beginning of the second millennium BC.*
*For example Chawuhu and Xiaohe cemeteries (Xinjiang Institute of Archaeology 1999, 2003).

pottery-afanasevo-chemurchek
Pottery of Afanasevo and East European traits from the Chemurchek complex. Image modified from Kovalev (2017).

(…) Pottery “oil burners” (goblet-like ceramic vessels, possibly lamps) have been found in three traditions: Afanasievo (Gryaznov and Krizhevskaya 1986:21), Okunevo and Qiemu’erqieke. It is believed that this oil-burner found in Siberia and the Altai is a heritage from the Yamnaya and Catacomb
cultures (Sulimirski 1970: 225, 425; Shishlina 2008:46) in the Caspian steppe further to the west, but does not seem to exist in known Andronovo cultures.
The oil-burner tends to disappear after around 2300 BC during the mid-Okunevo period. It is, however, possible that the tradition continues longer in the Qiemu’erqieke sites.

The construction of the stone enclosures also reveals a close connection between Qiemu’erqieke Phase I and the mid and late Okunevo tradition (Sokolova 2007). Slab built stone enclosures emerged in both the Okunevo and Afanasievo traditions (Gryaznov and Krizhevskaya 1986:15-23, Kovalev 2008, Sokolova 2007, Anthony 2007:310, Koryakova and Epimakhov 2007). In the early Afanasievo the enclosure is circular with no cist coffin (Anthony 2007:310, Gryaznov and Krizhevskaya 1986:20), but in the early stage of the Okunevo square stone enclosures with a single cist burial are dominant. Square or rectangular stone enclosures are a marked feature of Qiemu’erqieke Phase I, suggesting temporal relationships between Qiemu’erqieke Phase I and the Okunevo. In Okunevo chronological group II, possibly with influence from the Anfanasievo, circular stone enclosures appeared in combination with rectangular enclosures within individual cemeteries, referred to by Sokolova (2007: table 2) as hybrid examples. By Okunevo chronological group III, rectangular stone slab enclosures with multi-burials emerged again. This is the dominant form in Qiemu’erqieke Phase I. Okunevo burial traditions changed again to single cist burials in the late stage around chronological group V ( Sokol ova 2007). A specific mortuary rite of decapitated burials exists in both the Qiemu’erqieke and Okunevo traditions (Sokolova 2007, Chen Kwang-tzuu and Hiebert 1995), as does the occasional occurrence of painted designs on the interior of the slabs forming the cists ( e.g., Khavrin 1997: 70, fig. 4; 77: tab. IV.5). Based on these comparisons, the date of Qiemu’erqieke Phase I may well parallel that of the Okunevo from at least chronological group II around 2400 BC (Gorsdorf et al. 2004: fig. 1).

khuh-udzuur-barrow
Khuh Udzuuriin I-1 elite barrow (ca. 2470-2190 BC). Modified from Image modified from Kovalev (2014).

In addition to the pottery making tradition, the anthropomorphic stone stelae may also have earlier antecedents. In the Okunevo assemblage there are anthropomorphic stelae that are longer, thinner and more abstract than those of Qiemu’erqieke. There is no indication of such stelae in the Afanasievo tradition (Gryaznov and Krizhevskaya 1986:15-23). However, further to the west, anthropomorphic stone stelae are associated with the Kemi-Oba and Yamnya cultures around the third millennium BC (Telegin and Mallory 1994; Figure 13). Some major characteristics of these stelae such as the icons on the front face of the stelae (Telegin and Mallory 1994:8-9) also appear on stelae found in Qiemu’erqieke Phase I. Recalling the oil burners that may have been inherited from the Yamnya culture and which are found in the Afansievo, Okunevo and Qiemu’erqieke Phase I, it migh t be possible to speculate that Qiemu’erqieke Phase I has its origins even earlier than the first half of the third millennium BC. This idea has also been suggested by Kovalev ( 1999).

Despite the affinities with the Okunevo cultural tradition, Qiemu’erqieke Phase I appears to be a discrete regional variant. The ceramic assemblage shows traits unique to this cluster of sites, while the anthropomorphic stelae are also distinctive markers of this tradition.

khuh-udzuur-stela
Khuh Udzuur anthropomorphic stone stela, oriented toward the south – south-east. Image modified from Kovalev (2014).

3. Bronze Age Xinjiang

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

It also offered a full summary of findings from prehistoric sites of Xinjiang related to the arrival of a cultural package from the Altai region, ultimately connected to Afanasievo. Relevant excerpts include the following (emphasis mine):

In Bronze Age Xinjiang, burials were diverse but also show some common features between different geographic sections. The main three mountains, including Kunlun Mountains, Tian Shan (mountains) and Altai Mountains, enclose the Tarim Basin, and the Dzungaria Basin, but leave the eastern part of the Tarim Basin and the south-eastern part of the Dzungaria Basin open (with easy access to the surroundings). The Hami Basin is located at the transitional area, connecting the two basins. Burials are mainly spread along the edge of the mountain ranges.

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

3.1. The Lop Nur region

In the Lop Nur region, the Xiaohe cemetery (2000-1450 BCE) and the Gumugou cemetery (1900-1800 BCE) had many common features shared, and so is the Keliyahe northern cemetery:

  • Cemeteries were located in sandy areas;
  • Rectangular/boat-shaped wooden coffins with monuments of wooden planks or poles;
  • Coffins had no bottoms;
  • The dead were placed lying straight on the back;
  • The dead were commonly buried in single graves.

The Gumugou cemetery contained six special sun-radiating-spokes burial pattern in addition to the normal burials, which were similar to the wooden coffin graves of the Xiaohe cemetery.

NOTE. For more on Xiaohe and Gumugou, see the recent post on Proto-Tocharians. See other papers on the Andronovo horizon for other Early to Middle Bronze Age cultural groups less clearly associated with the Xiaohe horizon, like Hazandu, Xintala, or the Chust culture.

From Shuicheng (2006):

An assemblage of early bronzes had been recovered from northwestern Xinjiang and the periphery of Dzungaria 准噶尔 Basin. It comprises a variety of utilitarian tools and weapons, and a small number of apparels. These artifacts bear the stamps of Andronovo Culture in form, artifact type and decorative pattern. The metallographic analysis on selected artifacts indicates that they comprise mainly of tin-bronzes that contain 2–10% of tin. Moreover, the chemical compositions of these artifacts are similar to that of the Andronovo Culture. Latter date (first half of the 1st millennium BC) artifacts of the assemblage include a small number of arsenic bronzes. In all, during the period between the mid-2nd and mid-1st millennium BC, copper and bronze artifacts coexisted in this region, albeit tin-bronze comprised the majority. The composition of alloy did not show significant change over time. Some colleagues pointed out that the Nulasai 奴拉赛 site at Nileke 尼勒克 County in the Yili 伊犁 River basin of Xinjiang was the pioneer in the use of “sulphuric ore–ice copper–copper”technology. It is also the only early smelting site in Euro-Asia that arsenic ore was added to deliberately produce an alloy

tocharians-bronze-age-middle
Prehistoric cultures of Xinjiang during the Middle Bronze Age. See full culture and ancient DNA maps.

3.2. The Hami Basin-the Balikun Grassland

From Yang (2019):

The Hami Basin-the Balikun Grassland area is located at the eastern part of Tian Shan. The area is divided in a northern basin and a southern basin by the east-west stretch of the Tian Shan. In the Hami Basin-the Balikun Grassland area, the main type of burials were earth-pit graves in the early Bronze Age, and burials of stone-pit with barrows became more common in the late Bronze Age. The Hami-Tianshan-Beilu cemetery is a representative of the earth-pit graves. The features of the Hami-Tianshan-Beilu cemetery (2000-1500 bce) here were:

  • Rectangular earth pit graves;
  • The dead were often in a hocker position lying on one side;
  • Commonly a single dead in one grave.
balikun-grassland
The Balikun grassland today (source).

The Hami-Wubu cemetery (earlier than 1000 bce) and the Yanbulake cemetery (1200-600 bce) are representatives of another common earth-pit graves. Common features here were:

  • Rectangular earth pits, with two storeys and/or roofed with wooden boards;
  • The dead was placed in a hocker position lying on one side;
  • Mostly a single dead in one grave.

Later there appeared more stone-pit graves in this area, and the features can be summarized as:

  • Round burial mounds, commonly constructed by stones or a mix of stones and earth;
  • Burial mounds with a sunken top or a normal (dome) top;
  • The diameter of the burial mounds varied between 3 and 25.4 m (but not necessarily limited in this scope);
  • Circular or rectangular stone kerbs;
  • Rectangular stone pits, constructed by earth, or stones, or a mix of earth and stones;
  • Rectangular stone pits contained wooden coffins (represented by the Yiwu Baiqi’er cemetery).
hami-basin-balikun-grassland-iron-age-burials
Some representatives of stone burials in the Hami Basin – the Balikun Grassland in the Iron Age (Adapted from: Xinjiang 2011, 29-41). Image modified from Yang (2019).

In the Hami Basin, the Bronze Age cemeteries show common burial features like earth pits and hocker position of the dead. With similar pottery styles in the Hami-Tianshan-Beilu cemetery to those in the Machang and Siba cultures (Xinjiang 2011: 17), it suggests possible cultural influence or people’s migrating from the Hexi Corridor in the east.

In the Balikun Grassland, burials in an earlier time contained mostly earth-pit graves but also a small number of stone-pit graves. The pebbles were imbedded in the floors and the walls of the graves in a rectangular shape, e.g. the Balikun-Nanwan cemetery (1600-1000 bce). In a later time, there appeared huge burial mounds with a sunken top, and with the diameters of the burial mounds varying from 3 to 25.4 m, e.g. the Balikun-Dongheigou cemetery and the Balikun-Heigouliang cemetery. The Yiwu-Bai’erqi and the Yiwu-Kuola cemeteries contained either round stone burial mounds or circular stone kerbs on the ground surface. Considering the three burial elements including burial mounds, stone pits and circular kerbs, the later period cemeteries in the Balikun Grassland were actually similar to cemeteries from the southern edge of the Altai Mountain area.

From Shuicheng (2006):

The Nanwan 南湾 cemetery site at Kuisu 奎苏 Town, Balikun 巴里坤 (1600–1100 BC) also yielded an assemblage of early bronzes. The style of its early phase artifacts is similar to that of the burials distributed in the North Tianshan Route. Some sorts of cultural connection should have existed between the two.

The dates of Yanbulake 焉不拉克 Culture (1300–700 BC) are comparatively late. Its metallurgy was a continuation of the western China tradition. Artifact types include a variety of utilitarian tools, weapons and apparels.

tocharians-bronze-age-late
Prehistoric cultures of Xinjiang during the Late Bronze Age. See full culture and ancient DNA maps.

3.3. The Turpan Basin-the middle part of Tian Shan

From Yang (2019):

Turpan Basin is located at the western part of the Hami Basin, and lies at the southern edge of the eastern Tian Shan. In the Turpan Basin-the middle part of Tian Shan area, the main representative of the Bronze Age cemeteries is the Yanghai Nr.1 cemetery. The features here were:

  • Elliptic earth pit graves, commonly covered by round logs on the top;
  • Some graves contained burial beds made of round logs or reeds;
  • The dead were mainly placed lying straight on the back;
  • Mostly a single dead in one grave.

In Iron Age, the stone burials became dominant, but the stone burials varied in different regions of the Turpan Basin-the middle part of Tian Shan area. Graves containing burial mounds, stone pit, and circular stone kerbs are represented by the Shanshan-Ertanggou cemetery, the Tuokexun-Alagou cemetery, the Urumqi-Chaiwobu cemetery and the Urumqi-Yizihu-Sayi cemetery, etc. The stone funeral construction features here are similar to those contemporary cemeteries in the Hami Basin-the Balikun Grassland area.

3.4. The southern edge of the western and middle part of Tian Shan

In the southern edge of the western and middle part of Tian Shan area, the main representatives of the late Bronze Age cemeteries are the Hejing-Chawuhu Nr.4 cemetery (around 1000-500 bce), the Hejing-Xiaoshankou cemetery, the Baicheng-cemetery, etc. The main burial features of the late Bronze Age and the early Iron Age cemeteries (see Fig.12) here were:

  • Burial mounds, constructed by stones or a mix of stones and earth;
  • Irregular circular or rectangular stone kerbs;
  • Stone pit graves in a bell-shape or a rectangular shape;
  • Stone pit graves constructed by imbedding pebbles or stone slabs in walls and floors;
  • The dead were often placed lying on their back with bent legs;
  • The dead were commonly reburied a second time with multiple burials.

From the late Bronze Age to the early Iron Age in this area, the burial traditions tended to be in a more varied way. In the stone burials with stone kerbs, there is a mixture of stone pit and earth pit graves. The burial features of the Iron Age cemeteries in this section were similar to those contemporary both in the Hami Basin-the Balikun Grassland area and in the Turpan Basin-the middle part of Tian Shan area.

From Shuicheng (2006):

The Chawuhu 察吾呼 Culture (1100–500 BC) distributes on the foothills between the middle section of the Tianshan Mountain Ranges and Tarim River. Its bronze assemblage comprises a variety of weapons, utilitarian tools and small apparels. They show no apparent temporal change in form and type through the four cultural phases. In addition, bronzes bear the Chawuhu characteristics were found in Hejing 和静, Baicheng 拜城 and Luntai 轮台 (Bügür). Yet, sites distributed along the Tarim River, such as Heshuo 和硕, Kuga 库车and Aksu 阿克苏, yielded remains of a bronze culture different from that of Chawuhu. Bronzes recovered include double-eared socketed axe, arrowheads, awls, knives, needles and bracelets. Their absolute dates have been estimated to be earlier than that of Chawuhu.

tocharians-iron-age-early
Prehistoric cultures of Xinjiang during the Early Iron Age. See full culture and ancient DNA maps

3.5. The Pamir Plateau

From Yang (2019):

A typical Bronze Age cemetery from the Pamir Plateau area is the Tashenku’ergan-Xiabandi cemetery (around 1000-500 bce). The burial features here were:

  • Mainly inhumations, but also a few cremations;
  • Burial mounds, constructed of stones;
  • Irregular circular or rectangular stone kerbs;
  • Mostly a single dead in one grave;
  • The dead was placed in a hocker position lying on one side.

The adoption of burial customs from the east supports the migration of Afanasievo-related peoples from the Tian Shan up to the Pamir Plateau, strongly influencing the findings of the Xiabandi cemetery, which has been dated from an early Bronze Age phase (ca. 1500-300 BC) to a late date up to ca. 600 BC.

While it is today unclear how far the Afanasievo admixture reached into the western Xinjiang, it seems that the Pamir Plateau remained culturally connected to neighbouring Andronovo-related cultures in pottery and metallurgical innovations, hence their language probably belonged – during most part of the Bronze and Iron Ages – to the Indo-Iranian branch, even though specific dialects might have changed with each new attested group.

In particular, it is possible that the early Andronovo groups related to the Xiaohe Horizon spoke Indo-Aryan or West Iranian dialects, while Saka-related groups replaced them – or an intermediate Tocharian-speaking group – with East Iranian dialects. A close interaction with West Iranian would justify the known ancient borrowings of Tocharian, although they could also be explained by contacts with Chust-related groups farther west. For more on this, see Ged Carling’s work on the different layers of Iranian loans.

Xinjiang BA/IA Summary

From Yang (2019):

In the early Bronze Age, there are distinct regional differences in the burial customs in and surrounding the Tarim Basin. At the southern edge of the Altai Mountains area, the burial customs included stone burial mounds, stone pit graves, circular or rectangular stone kerbs and stone human sculptures; the dead were placed lying straight on the back. In the Hami Basin-the Balikun Grassland area, the burial customs included earth pit graves; the dead were placed in a hocker position lying on one side. In the Turpan Basin-the middle part of Tian Shan area, the burial customs included earth pit graves; the dead were placed lying straight on the back. In the Lop Nur region, the burial customs included wooden coffins buried in sand; the dead were placed lying straight on the back.

But from the late Bronze Age to the early Iron Age, there was a common shift in burial customs from earth pit graves to stone burials in the Hami Basin-the Balikun Grassland area and in the Turpan Basin-the middle part of Tian Shan area. The main features of the stone burials include stone burial mounds, circular or rectangular stone kerbs, and the stone pit graves in the cemeteries. Similar stone burial customs commonly appeared at the southern edge of the western and middle part of Tian Shan area and the Pamir Plateau area in Iron Age. The burial features in most areas are in a mixture of both the earth pit graves and stone pit graves, especially in the Hami Basin-the Balikun Grassland area and the Turpan Basin-the middle part of Tian Shan area.

xinjiang-bronze-age-iron-age

From Shuicheng (2006):

Historians of metallurgy conducted metallographic analyses on a sample of 234 metal specimens recovered from 16 localities in eastern Xinjiang. They concluded that the metallurgic industry in eastern Xinjiang could be roughly partitioned into three developmental phases. The early phase is represented by the burials distributed in the North Tianshan Route. The majority of the metal assemblage was tin-bronzes; however, copper and arsenic-bronzes maintained considerable proportions. The middle phase is represented by the burials at Yanbulake. During this phase, tin-bronze still maintained the majority; the proportion of arsenic-bronze increased, and some of them were high arsenic-bronzes. The late phase is represented by the burials at Heigouliang 黑沟梁. The composition of lead increased in the bronze alloy in the expense of arsenic. In addition, this phase witnessed the appearance of high tin-bronze that composed up to 16% of tin and the appearance of brass, that is, an alloy of copper and zinc. The bronze alloy consistently contained significant amount of impurities regardless of temporal difference. Casting and forging technologies coexisted throughout the three phases. The early bronzes (2000–500 BC) of eastern Xinjiang, in general, contained arsenic; however, the composition of arsenic was usually under 8%, but a few artifacts contained more than 20% arsenic. In all, arsenic had long been used in the alloy-forming of the early bronzes in eastern Xinjiang. Consequently, arsenic-bronzes were widely found in the prehistoric archaeology of the region. The artifact types, chemical compositions and manufacture techniques of the bronze assemblage of the burials of the North Tianshan Route are similar to those of Siba Culture, indicating that eastern Xinjiang had played a significant role in the East-West interactions.

An assemblage of early bronzes had been recovered from northwestern Xinjiang and the periphery of Dzungaria 准噶尔 Basin. It comprises a variety of utilitarian tools and weapons, and a small number of apparels. These artifacts bear the stamps of Andronovo Culture in form, artifact type and decorative pattern. The metallographic analysis on selected artifacts indicates that they comprise mainly of tin-bronzes that contain 2–10% of tin. Moreover, the chemical compositions of these artifacts are similar to that of the Andronovo Culture. Latter date (first half of the 1st millennium BC) artifacts of the assemblage include a small number of arsenic-bronzes. In all, during the period between the mid-2nd and mid-1st millennium BC, copper and bronze artifacts coexisted in this region, albeit tin-bronze comprised the majority.

tocharians-iron-age-late
Prehistoric cultures of Xinjiang during the Late Iron Age. See full culture and ancient DNA maps.

Tocharians in population genomics

Prehistoric population movements between the Altai and the Tian Shan are difficult to pinpoint, not the least because of the division of these territories among three different countries and their archaeological teams, only recently (more) open to the international scholarship.

The available schematic archaeological picture, where migrations could only be roughly inferred, has been recently updated to a great extent by Ning, Wang et al. (2019), whose genetic analysis of the samples is as thorough as anyone could have asked for, with a level of detail which matches the complex genetic picture of the region by the Iron Age.

As a summary, here is what they described about the samples from Shirenzigou (ca 400-200 BC), corresponding to the Iron Age populations of the Hami Basin-the Balikun Grassland area, and closely related to the preceding Yanbulake Culture:

As shown in Figure S3, the Steppe_MLBA populations including Srubnaya, Andronovo, and Sintashta were shifted toward farming populations compared with Yamnaya groups and the Shirenzigou samples. This observation is consistent with ADMIXTURE analysis that Steppe_MLBA populations have an Anatolian and European farmer-related component that Yamnaya groups and the Shirenzigou individuals do not seem to have. The analysis consistently suggested Yamnaya-related Steppe populations were the better source in modeling the West Eurasian ancestry in Shirenzigou.

biplot-yamnaya-tocharians-shirenzigou
Biplot of f3-outgroup tests illustrating the Kostenki14 and Anatolia_N like ancestries in Shirenzigou individuals. Most Shirenzigou individuals were on a cline with Yamnaya and European hunter-gatherer groups, lacking the European farmer ancestry as compared to the Steppe_MLBA populations such as Andronovo, Srubnaya and Sintashta [S1-S5]. Horizontal and vertical bars represent ± 3 standard errors, corresponding to form of outgroup f3 tests on the x axis and y axis respectively.

We continued to use qpAdm to estimate the admixture proportions in the Shirenzigou samples by using different pairs of source populations, such as Yamnaya_Samara, Afanasievo, Srubnaya, Andronovo, BMAC culture (Bustan_BA and Sappali_ Tepe_BA) and Tianshan_Hun as the West Eurasian source and Han, Ulchi, Hezhen, Shamanka_EN as the East Eurasian source. In all cases, Yamnaya, Afanasievo, or Tianshan_Hun always provide the best model fit for the Shirenzigou individuals, while Srubnaya, Andronovo, Bustan_BA and Sappali_Tepe_BA only work in some cases.

p-values-shirenzigou-samples-han-chinese
Table S2. P values in modelling a two-way (P=rank 1) admixture in Shirenzigou samples using each of the four populations (Bustan_BA, Sappali_Tepe_BA, Andronovo.SG, Srubnaya) together with Han Chinese as two sources [S6], Related to Figure 2. We used the following set of outgroups populations: Dinka, Ust_Ishim, Kostenki14, Onge, Papuan, Australian, Iran_N, EHG, LBK_EN.

shirenzigou-afanasievo-yamnaya-andronovo-srubna-ulchi-han

In the PCA, ADMIXTURE, outgroup f3 statistics [see Figure S4], as well as f4 statistics (Table S3), we observed the Shirenzigou individuals were closer to the present day Tungusic and Mongolic-speaking populations in northern Asia than to the populations in central and southern China, suggesting the northern populations might contribute more to the Shirenzigou individuals. Based on this, we then modeled Shirenzigou as a three-way admixture of Yamnaya_Samara, Ulchi (or Hezhen) and Han to infer the source from the East Eurasia side that contributed to Shirenzigou. We found the Ulchi or Hezhen and Han-related ancestry had a complicated and unevenly distribution in the Shirenzigou samples. The most Shirenzigou individuals derived the majority of their East Eurasian ancestry from Ulchi or Hezhen-related populations, while the following two individuals M820 and M15-2 have more Han related than Ulchi/ Hezhen-related ancestry

It is unclear whether the Chemurchek population will show a sizeable local contribution from neighbouring groups. The fact that Okunevo shows 20% Yamnaya-related ancestry strongly supports the nature of neighbouring stone-grave-building peoples of the Altai and the northern Tian Shan as mostly Afanasievo-like, and the apparent lack of contributions of Srubna/Andronovo-like ancestry in the early Hami-Balikun stone burial builders also speaks for radical population replacement events reaching the areas south of Tian Shan, at least initially.

While ancestry cannot settle linguistic questions, it seems that nomads of the Gansu and Qinghai grasslands retained an ancestry close to Andronovo, whereas nomads of the Hami Basin-Balikun grasslands and related populations of Xinjiang remained closely related to Afanasievo. This doesn’t preclude that the ancestors of the Yuezhi became acculturated under the influence of peoples from eastern Xinjiang, but all data combined suggest an isolation of both populations – relative to other groups and to each other – and it is therefore more likely that they spoke Indo-Iranian-related languages rather than a language of the Tocharian branch.

Haplogroups

In an interesting twist of events, despite the initially reported hg. R1b and Q, Tocharians from Shirenzigou actually show a haplogroup diversity comparable to that attested in other late Iron Age populations: a similar diversity is seen, for example, among Germanic, Baltic, and Balto-Finnic peoples of the Baltic region; among East Germanic or Scythians of the north Pontic region; or among Mediterranean peoples sampled to date. Iron Age peoples show thus a complex sociopolitical setting that overcame the previous patrilineal homogeneity of Bronze Age expansions.

tocharians-pca
PCA and ADMIXTURE for Shirenzigou Samples. Modified from the original to include in black squares samples related to Yamnaya. Modified from the paper to include labels of modern populations and a dotted lines with the cline formed by Shirenzigou, from (Yamnaya-like) Afanasievo to Central and East Asian-like populations. In red circles, samples with best fit for Andronovo-like ancestry. In green circles, samples with Han-related admixture.

M15-2 (with Han-related ancestry) is of the rare haplogroup Q1a-M120, while the samples with highest Steppe_MLBA-related ancestry are of hg. R1b-PH155, which points to their recent origin among Yuezhi, or to Hun-related populations showing an admixture related to the proto-historic nomads of the Gansu and Qinghai grasslands.

The expansion of Chemurchek-related peoples was probably associated more with hg. Q1a (dubious if it’s a Pre-ISOGG 2017 nomenclature, hence possibly Q1b), a haplogroup that might be found in Khvalynsk as a “significant minority” according to Anthony (2019), and it might also be attested in sampled individuals from Afanasievo in its late phase. This might be, therefore, a case similar to the early expansion of Indo-Europeans with R1b-V1636 lineages through the Volga – North Caucasus region, and of the later expansion with I2a-L699 lineages into the Balkans.

Haplogroup Q1a2-M25 is found in individual X3, whose Steppe ancestry is likely a combination of Afanasievo plus Andronovo-like ancestry heavily admixed with Hezhen/Ulchi-like populations, in line with the expected recent contacts with the neighbouring Xiongnu, Yuezhi, and other population movements affecting eastern Xinjiang.

Sample M4, which packs the most Afanasievo-like ancestry, is of hg. R1a-Z645, which – like sample M8R1 of hg. O – is most likely related to haplogroup resurgence events of local populations, which left the predominant Afanasievo-like admixture brought by builders of stone burials essentially intact, evidenced by the almost 100% of R1a found in the Xiaohe cemetery – and in most of the early Andronovo horizon – and among expanding Kangju and Wusun, as well as by the prevalence of hg. O among sampled East Asian populations.

A question that will only be answered with more samples is how and when the prevalent R1b-L23 and Q1b lineages among Afanasievo-related peoples began to be replaced to reach the high variability seen in Shirenzigou. Given the pastoralist nature of peoples around Tian Shan, the succeeding expansions of Proto-Tocharians, and the late isolation of different Common Tocharian groups, it is more than likely that this variability represents a late and local phenomenon within Xinjiang itself.

tocharians-antiquity
Peoples of Xinjiang during Antiquity. See full culture and ancient DNA maps.

Conclusion

Tocharians are one of the main pillars that confirm the Late Proto-Indo-European homeland of the R1b-rich populations of the Don-Volga region. There is already:

Just like the East Bell Beaker expansion from Yamnaya Hungary has confirmed that Corded Ware peoples did not partake in spreading Indo-European languages (spreading Uralic languages instead), data on the expansion of Tocharian speakers from Afanasievo to the Tian Shan was always there; population genomics is merely helping to connect the dots.

In summary, genetic research is supporting the expected linguistic expansions of the Neolithic and Bronze Age step by step, slowly but surely.

Related

Common Slavs from the Lower Danube, expanding with haplogroup E1b-V13?

late-iron-age-eastern-europe

Florin Curta has published online his draft for Eastern Europe in the Middle Ages (500-1300), Brill’s Companions to European History, Vol. 10 (2019), apparently due to appear in June.

Some interesting excerpts, relevant for the latest papers (emphasis mine):

The Archaeology of the Early Slavs

(…) One of the most egregious problems with the current model of the Slavic migration is that it is not at all clear where it started. There is in fact no agreement as to the exact location of the primitive homeland of the Slavs, if there ever was one. The idea of tracing the origin of the Slavs to the Zarubyntsi culture dated between the 3rd century BC and the first century AD is that a gap of about 200 years separates it from the Kiev culture (dated between the 3rd and the 4th century AD), which is also attributed to the Slavs. Furthermore, another century separates the Kiev culture from the earliest assemblages attributed to the Prague culture. It remains unclear as to where the (prehistoric) Slavs went after the first century, and whence they could return, two centuries later, to the same region from which their ancestors had left. The obvious cultural discontinuity in the region of the presumed homeland raises serious doubts about any attempts to write the history of the Slavic migration on such a basis. There is simply no evidence of the material remains of the Zarubyntsi, Kiev, or even Prague culture in the southern and southwestern direction of the presumed migration of the Slavs towards the Danube frontier of the Roman Empire.

Moreover, the material culture revealed by excavations of 6th- to 7th-century settlements and, occasionally, cremation cemeteries in northwestern Russia, Belarus, Poland, Moravia, and Bohemia is radically different from that in the lands north of the Danube river, which according to the early Byzantine sources were inhabited at that time by Sclavenes: no settlement layout with a central, open area; no wheel-made pottery or pottery thrown on a tournette; no clay rolls inside clay ovens; few, if any clay pans; no early Byzantine coins, buckles, or remains of amphorae; no fibulae with bent stem, and few, if any bow fibulae. Conversely, those regions have produced elements of material culture that have no parallels in the lands north of the river Danube: oval, trough-like settlement features (which are believed to be remains of above-ground, log-houses); exclusively handmade pottery of specific forms; very large settlements, with over 300 houses; fortified sites that functioned as religious or communal centers; and burials under barrows. With no written sources to inform about the names and identities of the populations living in the 6th and 7th centuries in East Central and Eastern Europe, those contrasting material culture profiles could hardly be interpreted as ethnic commonality. In other words, there is no serious basis for attributing to the Sclavenes (or, at least, to those whom early Byzantine authors called so) any of the many sites excavated in Russia, Belarus, Poland, Moravia, and Bohemia.

slavic-expansion-prague-korchak
Common Slavic expanding with Prague-Korchak from the east…or was it from the west?

Migrations

There is of course evidence of migrations in the 6th and 7th centuries, but not in the directions assumed by historians. For example, there are clear signs of settlement discontinuity in northern Germany and in northwestern Poland. German archaeologists believe that the bearers of the Prague culture who reached northern Germany came from the south (from Bohemia and Moravia), and not from the east (from neighboring Poland or the lands farther to the east). At any rate, no archaeological assemblage attributed to the Slavs either in northern Germany or in northern Poland may be dated earlier than ca. 700. In Poland, settlement discontinuity was postulated, to make room for the new, Prague culture introduced gradually from the southeast (from neighboring Ukraine). However, there is increasing evidence of 6th-century settlements in Lower Silesia (western Poland and the lands along the Middle Oder) that have nothing to do with the Prague culture. Nor is it clear how and when did the Prague culture spread over the entire territory of Poland. No site of any of the three archaeological cultures in Eastern Europe that have been attributed to the Slavs (Kolochin, Pen’kivka, and Prague/Korchak) has so far been dated earlier than the sites in the Lower Danube region where the 6th century sources located the Sclavenes. Neither the Kolochin, nor the Pen’kivka cultures expanded westwards into East Central or Southeastern Europe; on the contrary, they were themselves superseded in the late 7th or 8th century by other archaeological cultures originating in eastern Ukraine. Meanwhile, there is an increasing body of archaeological evidence pointing to very strong cultural influences from the Lower and Middle Danube to the Middle Dnieper region during the 7th century—the opposite of the alleged direction of Slavic migration.

When did the Slavs appear in those regions of East Central and Eastern Europe where they are mentioned in later sources? A resistant stereotype of the current scholarship on the early Slavs is that “Slavs are Slavonic-speakers; Slavonic-speakers are Slavs.”* If so, when did people in East Central and Eastern Europe become “Slavonic speakers”? There is in fact no evidence that the Sclavenes mentioned by the 6th-century authors spoke Slavic (or what linguists now call Common Slavic). Nor can the moment be established (with any precision), at which Slavic was adopted or introduced in any given region of East Central and Eastern Europe.** To explain the spread of Slavic across those regions, some have recently proposed the model of a koiné, others that of a lingua franca. The latter was most likely used within the Avar polity during the last century of its existence (ca. 700 to ca. 800).

*Ziółkowski, “When did the Slavs originate?” p. 211. On the basis of the meaning of the Old Church Slavonic word ięzyk (“language,” but also “people” or “nation”), Darden, “Who were the Sclaveni?” p. 138 argues that the meaning of the name the Slavs gave to themselves was closely associated with the language they spoke.

**Uncertainty in this respect dominates even in recent studies of contacts between Slavic and Romance languages (particularly Romanian), even though such contacts are presumed to have been established quite early (Paliga, “When could be dated ‘the earliest Slavic borrowings’?”; Boček, Studie). Recent studies of the linguistic interactions between speakers of Germanic and speakers of Slavic languages suggest that the adoption of place names of Slavic origin was directly linked to the social context of language contact between the 9th and the 13th centuries (Klír, “Sociální kontext”).

Avars

During the 6th century, the area between the Danube and the Tisza in what is today Hungary, was only sparsely inhabited, and probably a “no man’s land” between the Lombard and Gepid territories. It is only after ca. 600 that this area was densely inhabited, as indicated by a number of new cemeteries that came into being along the Tisza and north of present-day Kecskemét. There can therefore be no doubt about the migration of the Avars into the Carpathian Basin, even though it was probably not a single event and did not involve only one group of population, or even a cohesive ethnic group.

The number of graves with weapons and of burials with horses is particularly large in cemeteries excavated in southwestern Slovakia and in neighboring, eastern Austria. This was a region of special status on the border of the qaganate, perhaps a “militarized frontier.” From that region, the Avar mores and fashions spread farther to the west and to the north, into those areas of East Central Europe in which, for reasons that are still not clear, Avar symbols of social rank were particularly popular, as demonstrated by numerous finds of belt fittings. Emulating the success of the Avar elites sometimes involved borrowing other elements of social representation, such as the preferential deposition of weapons and ornamented belts. For example, in the early 8th century, a few males were buried in Carinthia (southern Austria) with richly decorated belts imitating those in fashion in the land of the Avars, but also with Frankish weapons and spurs. Much like in the Avar-age cemeteries in Slovakia and Hungary, the graves of those socially prominent men are often surrounded by many burials without any grave goods whatsoever.

early-avar-khaganate
Territory of the early Avar Qaganate and the location of the investigated sites in the Carpathian Basin in Csáky et al. (2019).

Carantanians

Carantania was a northern neighbor of the Lombard duchy of Friuli, which was inhabited by Slavs. According to Paul the Deacon, who was writing in the late 780s, those Slavs called their country Carantanum, by means of a corruption of the name of ancient Carnuntum (a former Roman legionary camp on the Danube, between Vienna and Bratislava). Carantanians were regarded as Slavs by the author of a report known as the Conversion of the Bavarians and Carantanians, and written in ca. 870 in order to defend the position of the archbishop of Salzburg against the claims of Methodius, the bishop of Pannonia.94 According to this text, a duke named Boruth was ruling over Carantania when he was attacked by Avars in ca. 740. He called for the military assistance of his Bavarian neighbors. The Bavarian duke Odilo (737–748) obliged, defeated the Avars, but in the process also subdued the Carantanians to his authority. Once Bavarian overlordship was established in Carantania, Odilo took with him as hostages Boruth’s son Cacatius and his nephew Chietmar (Hotimir). Both were baptized in Bavaria. During the 743 war between Odilo and Charles Martel’s two sons, Carloman and Pepin (the Mayors of the Palace in Austrasia and Neustria, respectively), Carantanian troops fought on the Bavarian side. The Bavarian domination cleared the field for missions of conversion to Christianity sent by Virgil, the new bishop of Salzburg (746–784). Many missionaries were of Bavarian origin, but some were Irish monks.

Moravians

Several Late Avar cemeteries dated to the last quarter of the 8th century are known from the lands north of the middle course of the river Danube, in what is today southern Slovakia and the valley of the Lower Morava [see image below]. By contrast, only two cemeteries have so far been found in Moravia (the eastern part of the present-day Czech Republic), along the middle and upper course of the Morava and along its tributary, the Dyje. In both Dolní Dunajovice and Hevlín, the latest graves may be dated by means of strap ends and belt mounts with human figures to the very end of the Late Avar period. (…)

The archaeological evidence pertaining to burial assemblages dated to the early 9th century is completely different. Shortly before or after 800, all traces of cremation—with or without barrows—disappear from the valley of the Morava river and southwestern Slovakia, two regions in which cremation had been the preferred burial rite during the previous centuries. This dramatic cultural change has often been interpreted as a direct influence of both Avar and Frankish burial rites, but it coincides in time with the adoption of Christianity by local elites. In spite of conversion, however, the representation of status through furnished burial continued well into the 9th century. Unlike Avar-age sites in Hungary and the surrounding regions, many men were buried in 9th-century Moravia together with their spurs, in addition to such weapons as battle axes, “winged” lance heads, or swords with high-quality steel blades of Frankish production.

morvaian-sites
Relevant Moravian sites mentioned in Curta’s new book.

When the Magyars inflicted a crushing defeat on the Bavarians at Bratislava (July 4, 907), the fate of Moravia was sealed as well. Moravia and the Moravians disappear from the radar of the written sources, and historians and archaeologists alike believe that the polity collapsed as a result of the Magyar raids.

Magyars

(…) although there can be no doubt about the relations between Uelgi and the sites in Hungary attributed to the first generations of Magyars, those relations indicate a migration directly from the Trans-Ural lands, and not gradually, with several other stops in the forest-steppe and steppe zones of Eastern Europe. In the lands west of the Ural Mountains, the Magyars are now associated with the Kushnarenkovo (6th to 8th century) and Karaiakupovo (8th to 10th century) cultures, and with such burial sites as Sterlitamak (near Ufa, Bashkortostan) and Bol’shie Tigany (near Chistopol, Tatarstan).* However, the same problem with chronology makes it difficult to draw the model of a migration from the lands along the Middle Volga. Many parallels for the so typically Magyar sabretache plates found in Hungary are from that region. They have traditionally been dated to the 9th century, but more recent studies point to the coincidence in time between specimens found in Eastern Europe and those from Hungary.

* Ivanov, Drevnie ugry-mad’iary; Ivanov and Ivanova, “Uralo-sibirskie istoki”; Boldog et al., “From the ancient homelands,” p. 3; Ivanov, “Similarities.” Ivanov, “Similarities,” p. 562 points out that the migration out of the lands along of the Middle Volga is implied by the disappearance of both cultures (Kushnarenkovo and Karaiakupovo) in the mid-9th century. For the Kushnarenkovo culture, see Kazakov, “Kushnarenkovskie pamiatniki.” For the Karaiakupovo culture, see Mogil’nikov, “K probleme.”

Given that the Magyars are first mentioned in relation to events taking place in the Lower Danube area in the 830s, the Magyar sojourn in Etelköz must have been no longer than 60 years or so—a generation. (…)

arrival-of-hungarians-feszty-slavs
A detail of the Arrival of the Hungarians, Árpád Feszty’s and his assistants’ vast (1800 m2) cyclorama, painted to celebrate the 1000th anniversary of the Magyar conquest of Hungary, now displayed at the Ópusztaszer National Heritage Park in Hungary. This specific detail is probably based on the account on The Annals of Fulda, which narrates under the year 894 that the Hungarians crossed the Danube into Pannonia where they “killed men and old women outright and carried off the young women alone with them like cattle to satisfy their lusts and reduced the whole” province “to desert”.

It has become obvious by now that one’s impression of the Magyars as “Easterners” and “steppe-like” was (and still is) primarily based on grave finds, while the settlement material is considerably more aligned with what is otherwise known from other contemporary settlement sites in Central and Southeastern Europe. The dominant feature on the 10th- and 11th-century settlements in Hungary is the sunken-floored building of rectangular plan, with a stone oven in a corner. Similarly, the pottery resulting from the excavation of settlement sites is very similar to that known from many other such sites in Eastern Europe. Moreover, while clear changes taking place in burial customs between ca. 900 and ca. 1100 are visible in the archaeological record from cemeteries, there are no substantial differences between 10th- and the 11th-century settlements in Hungary. (…)

As a matter of fact, the increasing quantity of paleobotanical and zooarchaeological data from 10th-century settlements strongly suggests that the economy of the first generations of Magyars in Hungary was anything but nomadic. To call those Magyars “half-nomad” is not only wrong, but also misleading, as it implies that they were half-way toward civilization, with social changes taking place that must have had material culture correlates otherwise visible in the burial customs.

Comments

The origin of “Slavs” (i.e. that of “Slavonic” as a language, whatever the ancestral Proto-Slavic ethnic make-up was) is almost as complicated as the origin of Albanians, Basques, Balts, or Finns. Their entry into history is very recent, with few reliable sources available until well into the Middle Ages. If you add our ignorance of their origin with the desire of every single researcher or amateur out there to connect them to the own region (or, still worse, to all the regions where they were historically attested), we are bound to find contradictory data and a constantly biased selection of information.

Furthermore, it is extremely complicated to connect any recent population to its ancestral (linguistic) one through haplogroups prevalent today, and just absurd to connect them through ancestral components. This, which was already suspected for many populations, has been confirmed recently for Basques in Olalde et al. (2019) and will be confirmed soon for Finns with a study of the Proto-Fennic populations in the Gulf of Finland.

NOTE. Yes, the “my parents look like Corded Ware in this PCA” had no sense. Ever. Why adult people would constantly engage in that kind of false 5,000-year-old connections instead of learning history – or their own family history – escapes all comprehension. But if something is certain about human nature, is that we will still see nativism and ancestry/haplogroup fetishism for any modern region or modern haplogroups and their historically attested ethnolinguistic groups.

balto-slavic-pca
Genetic structure of modern Balto-Slavic populations within a European context according to the three genetic systems. Image from Kushniarevich et al. (2015)

As you can see from my maps and writings, I prefer neat and simple concepts: in linguistics, in archaeology, and in population movements. Hence my aversion to this kind of infinite proto-historical accounts (and interpretations of them) necessary to ascertain the origins of recent peoples (Slavs in this case), and my usual preference for:

  • Clear dialectal classifications, whether or not they can be as clear cut as I describe them. The only thing that sets Slavic apart from other recent languages is its connection with Baltic, luckily for both. Even though this connection is disputed by some linguists, and the question is always far from being resolved, a homeland of Proto-Balto-Slavic would almost necessarily need to be set to the north of the Carpathian Mountains in the Bronze Age (or at least close to them).
  • NOTE. A dismissal of a connection with Baltic would leave Slavic a still more complicated orphan, and its dialectal classification within Late PIE more dubious. Its union with Balto-Slavic locates it close to Germanic, and thus as a Bronze Age North-West Indo-European dialect close to northern Germany. So bear with me in accepting this connection, or enter the linguistic hell of arguing for Indo-Slavonic of R1a-Z93 mixed with Temematic….

  • A priori “pots = people” assumption, which may lead to important errors, but fewer than the usual “pots != people” of modern archaeologists. The traditional identification of the Common Slavic expansion with the Prague-Korchak culture – however undefined this culture may be – has clear advantages: it may be connected (although admittedly with many archaeological holes) with western cultures expanding east during the Bronze Age, and then west again after the Iron Age, and thus potentially also with Baltic.
  • A simplistic “haplogroup expansion = ethnolinguistic expansion”, which is quite useful for prehistoric migrations, but enters into evident contradictions as we approach the Iron Age. Common Slavs may be speculatively (for all we know) associated with an expansion of recent R1a-M458 lineages – among other haplogroups – from the east, and possibly Balto-Slavic as an earlier expansion of older subclades from the west, as I proposed in A Clash of Chiefs.
r1a-m458-underhill-2015
Modern distribution of R1a-M458, after Underhill et al. (2015).

NOTE. The connection of most R1a-Z280 lineages is more obviously done with ancient Finno-Ugric peoples, as it is clear now (see here and here).

Slavs appeared first in the Danube?

No matter what my personal preference is, one can’t ignore the growing evidence, and it seems that Florin Curta‘s long-lasting view of a Danubian origin of expansion for Common Slavic, including its condition as a lingua franca of late Avars, won’t be easy to reject any time soon:

1) Theories concerning Chernyakhov as a Slavic homeland will apparently need to be fully rejected, due to the Germanic-like ancestry that will be reported in the study by Järve et al. (2019).

EDIT (3 MAY 2019). From their poster Shift in the genetic landscape of the western Eurasian Steppe not due to Scythian dominance, but rather at the transition to the Chernyakhov culture (Ostrogoths) (download PDF):

(…) the transition from the Scythian to the Chernyakhov culture (~2,100–1,700 cal BP) does mark a shift in the Ponto-Caspian genetic landscape. Our results agree well with the Ostrogothic origins of the Chernyakhov culture and support the hypothesis that Scythian dominance was cultural rather than achieved through population replacement.

scythians-chernyakhov-ostrogoths-jarve
PCA of novel and published ancient samples from Scythian/Sarmatian and related groups on the background of modern samples presented as population medians. Δ – ref. 1, ○ – ref. 2, □ – ref. 3, ◊ – this study. Embedded are the locations of some of the samples. Notice the wide cluster formed by the three samples, from Hungarian Scythians in the west to steppe-like peoples in the east.

2) Therefore, unless Przeworsk shows the traditionally described mixture of populations in terms of ancestry and/or haplogroups, it will also be a sign of East Germanic peoples expanding south (and potentially displacing the ancestors of Slavs in either direction, east or south).

It would seem we are stuck in a Danubian vs. Kievan homeland for Common Slavs, then:

3) About the homeland in the Kiev culture, two early Avar females from Szólád have been commented to cluster “among Modern Slavic populations” based on some data in Amorim et al. (2018).

Rather than supporting an origin of Slavs in common with modern Russians, Poles, and Ukranians as observed in the PCA, though, the admixture of AV1 and AV2 (ca. AD 540-640) paradoxically supports an admixture of Modern Slavs of Eastern Europe in common with early Avar peoples (an Altaic-speaking population) and other steppe groups with an origin in East Asia… So this admixture would actually support a western origin of the Common Slavs with which East Asian Avars may have admixed, and whose descendants are necessarily sampled at later times.

pca-medieval-avar-longobards
Procrustes transformed PCA of medieval ancient samples against POPRES imputed SNP dataset. AV1 and Av2 samples have been circled in red. Color coding of medieval samples is same as in Figs 1 and 2. Two letter and three codes for POPRES samples: AL=Albania, AT=Austria, BA=Bosnia-Herzegovina, BE=Belgium, BG=Bulgaria, CH=Switzerland, CY=Cyprus, CZ=Czech Republic, DE=Germany, DK=Denmark, ES=Spain, FI=Finland, FR=France, GB=United Kingdom, GR, Greece, HR=Croatia, HU=Hungary, IE=Ireland, IT=Italy, KS=Kosovo, LV=Latvia, MK=Macedonia, NO=Norway, NL=Netherlands, PL=Poland, PT=Portugal, RO=Romania, SM=Serbia and Montenegro, RU=Russia, Sct=Scotland, SE=Sweden, SI=Slovenia, SK=Slovakia, TR=Turkey, UA=Ukraine.

4) Favouring Curta’s Danubian origin (or even an origin near Bohemia) at the moment are thus:

  • The “western” cluster of Early Slavs from Brandýsek, Bohemia (ca. AD 600-900).
  • Two likely Slavic individuals from Usedom, in Mecklenburg-Vorpommern (AD 1200) show hg. R1a-M458 and E1b-M215 (Freder 2010).
  • An early West Slav individual from Hrádek nad Nisou in Northern Bohemia (ca. AD 1330) also shows E1b-M215 (Vanek et al. 2015).
  • One sample from Székkutas-Kápolnadülő (SzK/239) among middle or late Avars (ca. AD 650-710), a supposed Slavonic-speaking polity, of hg. E1b-V13.
  • Two samples from Karosc (K1/13, and K2/6) among Hungarian conquerors (ca. AD 895-950), likely both of hg. E1b-V13, probably connected to the alliance with Moravian elites.
  • Possibly a West Slavic sample from Poland in the High Middle Ages (see below).

A later Hungarian sample (II/53) from the Royal Basilica, where King Béla was interred, of hg. E1b1, supports the importance of this haplogroup among elite conquerors, although its original relation to the other buried individuals is unknown.

NOTE. You can see all ancient samples of haplogroup E to date on this Map of ancient E samples, with care to identify the proper subclades related to south-eastern Europe. About the ancestral origin of the haplogroup in Europe, you may read Potential extra Iberomaurusian-related gene flow into European farmers, by Chad Rohlfsen.

Even assuming that the R1a sample reported from the late Avar period is of a subclade typically associated with Slavs (I know, circular reasoning here), which is not warranted, we would have already 6 E1b1b vs. 1-2 R1a-M458 in populations that can be actually assumed to represent early Slavonic speakers (unlike many earlier cultures potentially associated with them), clearly earlier than other Slavic-speaking populations that will be sampled in eastern Europe. It is more and more likely that Early Slavs are going to strengthen Curta’s view, and this may somehow complicate the link of Proto-Slavic with eastern European BA cultures like Trzciniec or Lusatian.

NOTE. I am still expecting a clear expansion associated with Prague-Korchak, though, including a connection with bottlenecks based on R1a-M458 in the Middle Ages, whether the expansion is eventually shown to be from the west (i.e. Bohemia -> Prague -> Korchak), or from the east (i.e. Kiev -> Korchack -> Prague), and whether or not this cultural community was later replaced by other ‘true’ Slavonic-speaking cultures through acculturation or population movements.

slavic-origins
Common theories on Slavic origins.. After “The Early Slavs. Culture and Society in Early Medieval Europe” by P. M. Barford, Cornell University Press (2001). Image by Hxseek at Wikipedia.

5) Back to Przeworsk and the “north of the Carpathians” homeland (i.e. between the Upper Oder and the Upper Dniester), but compatible with Curta’s view: Even if Common Slavic is eventually evidenced to be driven by small migrations north and south of the Danube during the Roman Iron Age, before turning into a mostly “R1a-rich” migration or acculturation to the north in Bohemia and then east (which is what this early E1b-V13 connection suggests), this does not dismiss the traditional idea that Late Bronze Age – Iron Age central-eastern Europe was the Proto-Slavic homeland, i.e. likely the Pomeranian culture disturbed by the East Germanic migrations first (in Przeworsk), and the migrations of steppe nomads later (around the Danube).

Even without taking into account the connection with Baltic, the relevance of haplogroup E1b-V13 among Early Slavs may well be a sign of an ancestral population from the northern or eastern Carpathian region, supported by the finding of this haplogroup among the westernmost Scythians. The expansion of some modern E1b-CTS1273 lineages may link Slavic ancestrally with the Lusatian culture, which is an eastern (very specific) Urnfield culture group, stemming from central-east Europe.

An important paper in this respect is the upcoming Zenczak et al., where another hg. E1b1 will be added to the list above: such a sample is expected from Poland (from Kowalewko, Maslomecz, Legowo or Niemcza), either from the Roman Iron Age or Early Middle Ages, close to an early population of likely Scandinavian origin (eight I1 samples), apart from other varied haplogroups, with little relevance of R1a. Whether this E-V13 sample is an Iron Age one (justifying the bottleneck under E-V13 to the south) or, maybe more likely, a late one from the Middle Ages (maybe supporting a connection of the Gothic/Slavic E1b bottleneck with southern Chernyakhov or further west along the Danube) is unclear.

The finding of south-eastern European ancestry and lineages in both, Early Slavs and East Germanic tribes* suggests therefore a Slavonic homeland near (or within) the Przeworsk culture, close to the Albanoid one, as proposed based on topohydronymy. This may point to a complex process of acculturation of different eastern European populations which formed alliances, as was common during the Iron Age and later periods, and which cannot be interpreted as a clear picture of their languages’ original homeland and ancestral peoples (in the case of East Germanic tribes, apparently originally expanding from Scandinavia under strong I1 bottlenecks).

* Iberian samples of the Visigothic period in Spain show up to 25% E1b-V13 samples, with a mixture of haplogroups including local and foreign lineages, as well as some more E1b-V13 samples later during the Muslim period. Out of the two E1b samples from Longobards in Amorim et al. (2018), only SZ18 from Szólád (ca. AD 412-604) is within E1b-V13, in a very specific early branch (SNP M35.2), further locating the expansion of hg. E1b-V13 near the Danube. Samples of haplogroup J (maybe J2a) or G2a among Germanic tribes (and possibly in Poland’s Roman Iron Age / Early Middle Ages) are impossible to compare with early Hungarian ones without precise subclades.

east-slavic-expansion
East Slavic expansion in topo-hydronymy. Image from (Udolph 1997, 2016).

I already interpreted the earlier Slavic samples we had as a sign of a Carpathian origin and very recent bottlenecks under R1a lineages among Modern Slavs:

The finding of haplogroup E1b1b-M215 in two independent early West Slavic individuals further supports that the current distribution of R1a1a1b1a-Z282 lineages in Slavic populations is the product of recent bottlenecks. The lack of a precise subclade within the E1b1b-M215 tree precludes a proper interpretation of a potential origin, but they are probably under European E1b1b1a1b1-L618 subclade E1b1b1a1b1a-V13 (formed ca. 6100 BC, TMRCA ca. 2800 BC), possibly under the mutation CTS1273 (formed ca. 2600 BC, TMRCA ca. 2000 BC), in common with other ancient populations around the Carpathians (see below §viii.11. Thracians and Albanians). This gross geographic origin would support the studies of the Common Slavic homeland based on toponymy (Figure 66), which place it roughly between the Upper Oder and the Upper Dniester, north of the Carpathians (Udolph 1997, 2016).

EDIT (8 APR 2019): Another interesting data is the haplogroup distribution among Modern Slavs and neighbouring peoples (see Wikipedia). For example, the bottleneck seen in Modern Albanians, under Z5017 subclade, also points to an origin of the expansion of E1b-V13 subclades among multiethnic groups around the Lower Danube coinciding with the Roman Iron Age, given the estimates for the arrival of Proto-Albanian close to the Latin and Greek linguistic frontier.

Remarkable is also its distribution among Rusyns, East Slavs from the Carpathians not associated with the Kievan Rus’, isolated thus quite soon from East Slavic expansions to the east. They were reported to show ca. 35% hg. E1b-V13 globally in FTDNA, with a frequency similar to or higher than R1a, in common with South Slavic peoples*, reflecting thus a situation similar to the source of East Slavs before further R1a-based bottlenecks (and/or acculturation events) to the east:

* Although probably due in part to founder effects and biased familial sampling, this should be assumed to be common to all FTDNA sampling, anyway.

rusyns-map
Map showing the full geographic extent of the Rusyn people in Central Europe, prior to World War I (Carpatho Rusyn Society).

Repeating what should be already evident: in complex organizations and/or demographically dense populations (more common since the Iron Age), we can’t expect language change to happen in the same way as during the known Neolithic or Chalcolithic population replacements, be it in Finland, Hungary, Iberia, or Poland. For example, no matter whether Romans (2nd c. BC) brought some R1b-U152 and other Mediterranean lineages to Iberia; Germanic peoples entering Hispania (AD 5th c.) were of typically Germanic lineages or not; Muslims who spoke mainly Berber (AD 8th c.) and were mainly of hg. E1b-M81 (and J?) brought North African ancestry; etc. the language or languages of Iberia changed (or not) with the political landscape: neither with radical population replacements (or full population continuity), nor with the dominant haplogroups’ ancestral language.

Y-chromosome haplogroups are, in those cases, useful for ascertaining a more recent origin of the population. Like the finding of certain R1a-Z645, I2a-L621 & N-L392 lineages among Hungarians shows a recent origin near the Trans-Urals forest-steppes, or the finding of I1, R1b-U106 & E1b-V13 among Visigoths shows a recent origin near the Danube, the finding of Early Slavs (ca. AD 6th-7th c.) originally with small elite groups of hg. R1a-M458 & E1b-V13 from the Lower/Middle Danube – if strengthened with more Early Slavic samples, with Slavonic partially expanding as a lingua franca in some regions – is not necessarily representative of the Proto-Slavic community, just as it is clearly not representative of the later expansion of Slavic dialects. It would be representative, though, of the same processes of acculturation repeated all over Eurasia at least since the Iron Age, where no genetic continuity can be found with ancestral languages.

Related

R1a-Z280 and R1a-Z93 shared by ancient Finno-Ugric populations; N1c-Tat expanded with Micro-Altaic

Two important papers have appeared regarding the supposed link of Uralians with haplogroup N.

Avars of haplogroup N1c-Tat

Preprint Genetic insights into the social organisation of the Avar period elite in the 7th century AD Carpathian Basin, by Csáky et al. bioRxiv (2019).

Interesting excerpts (emphasis mine):

After 568 AD the Avars settled in the Carpathian Basin and founded the Avar Qaganate that was an important power in Central Europe until the 9th century. Part of the Avar society was probably of Asian origin, however the localisation of their homeland is hampered by the scarcity of historical and archaeological data.

Here, we study mitogenome and Y chromosomal STR variability of twenty-six individuals, a number of them representing a well-characterised elite group buried at the centre of the Carpathian Basin more than a century after the Avar conquest.

The Y-STR analyses of 17 males give evidence on a surprisingly homogeneous Y chromosomal composition. Y chromosomal STR profiles of 14 males could be assigned to haplogroup N-Tat (also N1a1-M46). N-Tat haplotype I was found in four males from Kunpeszér with identical alleles on at least nine loci. The full Y-STR haplotype I, reconstructed from AC17 with 17 detected STRs, is rare in our days. Only nine matches were found among haplotypes in YHRD database, such as samples from the Ural Region, Northern Europe (Estonia, Finland), and Western Alaska (Yupiks). We performed Median Joining (MJ) network analysis using N-Tat haplotypes with ten shared STR loci (Fig. 3, Table S9). All modern N-Tat samples included in the network had derived allele of L708 as well. Haplotype I (Cluster 1 in Fig. 3) is shared by eight populations on the MJ network among the 24 identical haplotypes. Cluster 1 represents the founding lineage, as it is described in Siberian populations, because this haplotype is shared by the most populations and it is more diverse than Cluster 2.

Nine males share N-Tat haplotype II (on a minimum of eight detected alleles), all of them buried in the Danube-Tisza Interfluve. We found 30 direct matches of this N-Tat haplotype II in the YHRD database, using the complete 17 STR Y-filer profile of AC1, AC12, AC14, AC15, AC19 samples. Most hits came from Mongolia (seven Buryats and one Khalkh) and from Russia (six Yakuts), but identical haplotypes also occur in China (five in Xinjiang and four in Inner Mongolia provinces). On the MJ network, this haplotype II is represented by Cluster 2 and is composed of 45 samples (including 32 Buryats) from six populations (Fig. 3).

y-str-haplogroup-n-mongolian-ugrians
Median Joining network of 162 N-Tat Y-STR haplotypes Allelic information of ten Y-STR loci were used for the network. Only those Avar samples were included, which had results for these ten Y-STR loci. The founder haplotype I (Cluster 1) is shared by eight populations including three Mongolian, three Székely, three northern Mansi, two southern Mansi, two Hungarian, eight Khanty, one Finn and two Avar (AC17, AC26) chromosomes. Haplotype II (Cluster 2) includes 45 haplotypes from six populations studied: 32 Buryats, two Mongolians, one Székely, one Uzbek, one Uzbek Madjar, two northern Mansi and six Avars (AC1, AC12, AC14, AC15, AC19 and KSZ 37). Haplotype III (indicated by a red arrow) is AC8. Information on the modern reference samples is seen in Table S9.

A third N-Tat lineage (type III) was represented only once in the Avar dataset (AC8), and has no direct modern parallels from the YHRD database. This haplotype on the MJ network (see red arrow in Fig. 3) seems to be a descendent from other haplotype cluster that is shared by three populations (two Buryat from Mongolia, three Khanty and one Northern Mansi samples). This haplotype cluster also differs one molecular step (locus DYS393) from haplotype II. We classified the Avar samples to downstream subgroup N-F4205 within the N-Tat haplogroup, based on the results of ours and Ilumäe et al.18 and constructed a second network (Fig. S4). The N-F4205 network results support the assumption that the N-Tat Avar samples belong to N-F4205 subgroup (see SI chapter 1d for more details).

Based on our calculation, the age of accumulated STR variance (TMRCA) within N-Tat lineage for all samples is 7.0 kya (95% CI: 4.9 – 9.2 kya), considering the core haplotype (Cluster 1) to be the founding lineage. Y haplogroup N-Tat was not detected by large scale Eurasian ancient DNA studies but it occurs in late Bronze Age Inner Mongolia and late medieval Yakuts, among them N-Tat has still the highest frequency.

Two males (AC4 and AC7) from the Transtisza group belong to two different haplotypes of Y-haplogroup Q1. Both Q1a-F1096 and Q1b-M346 haplotypes have neither direct nor one step neighbour matches in the worldwide YHRD database. A network of the Q1b-M346 haplotype shows that this male had a probable Altaian or South Siberian paternal genetic origin.

EDIT (5 APR 2019): The paper offers an interesting late sample before the arrival of Hungarian conquerors, although we don’t know which precise lineage the sample belongs to:

One sample in our dataset (HC9) comes from this population, and both his mtDNA (T1a1b) and Y chromosome (R1a) support Eastern European connections. (…) Furthermore, we excluded sample HC9 from population-genetic statistical analyses because it belongs to a later period (end of 7th – early 9th centuries)

Apparently, then, results are consistent with what was already known from studies of modern populations:

According to Ilumäe et al. study, the frequency peak of N-F4205 (N3a5-F4205) chromosomes is close to the Transbaikal region of Southern Siberia and Mongolia, and we conclude that most Avar N-Tat chromosomes probably originated from a common source population of people living in this area, completely in line with the results of Ilumäe et al.

haplogroup_n1
Geographic-Distribution Map of hg N3 from Ilumäe et al.

Finno-Ugrians share haplogroup R1a-Z280

Another paper, behind paywall, Genetic history of Bashkirian Mari and Southern Mansi ethnic groups in the Ural region, by Dudás et al. Molecular Genetics and Genomics (2019).

Interesting excerpts (emphasis mine):

Y‑chromosome diversity

The most frequent haplogroups of the Bashkirian Maris were N1b-P43 (42%), R1a-Z280 (16%), R1a-Z93 (16%), N1c-Tat (13%), and J2-M172 (7%). Furthermore, subgroup R1b-M343 accounted for 4% and I2a-P37 covered 2% of the lineages. None of the Mari N1c Y chromosomes belonged to the N1c subgroups investigated (L1034, VL29, Z1936).

In the case of the Southern Mansi males, the most frequent haplogroups were N1b-P43 (33%), N1c-L1034 (28%) and R1a-Z280 (19%). The frequencies of the remaining haplogroups were as follows: R1a-M458 (6%), I1-L22 (3%), I2a-P37 (3%), and R1b-P312 (3%). The haplotype and haplogroup diversities of the Bashkirian Mari group were 0.9929 and 0.7657, whereas these values for the Southern Mansi were 0.9984 and 0.7873, respectively. The results show that, in both populations, haplotypes are much more diverse than haplogroups.

bashkir-mari-southern-mansi
Haplogroup frequencies of the Bashkirian Mari and the Southern Mansi ethnic groups in Ural region

Genetic structure

(..) the studied Bashkirian Mari and Southern Mansi population groups formed a compact cluster along with two Khanty, Northern Mansi, Mari, and Estonian populations based on close Fst-genetic distances (< 0.05), with nonsignificant p values (p > 0.05) except for the Estonian population. All of these populations belong to the Finno-Ugric language family. Interestingly, the other Mansi population studied by Pimenoff et al. (2008) (pop # 38) was located a great distance from the Southern Mansi group (0.268). In addition, the Bashkir population (pop # 6) did not show a close genetic affinity to the Bashkirian Mari group (0.194), even though it is the host population. However, the Russian population from the Eastern European region of Russia (pop # 49) showed a genetic distance of 0.055 with the Southern Mansi group. All Hungarian speaking populations (pops 13, 22, 23, 24, 50, and 51) showed close genetic affinities to each other and to the neighbouring populations, but not to the two studied populations.

y-dna-hungarians-ugric-mansi
Multidimensional scaling (MDS) plot constructed on Fstgenetic distances of Y haplogroup frequencies of 63 populations compared. The haplogroup frequency data used for population comparison together with references are seen in Online Resource 2 (ESM_2). Pairwise Fst-genetic distances and p values between 63 populations were calculated as shown in Online Resource 3 (ESM_3) Fig. 4 Multidimensional scaling (MDS) plot constructed on Rstgenetic distances of 10 STR-based Y haplotype frequencies of 21 populations compared. Image modified to include labels of modern populations.

Phylogenetic analysis

Median-joining networks were constructed for:

N-P43 (earlier N1b):

(…) TMRCA estimates for this haplogroup were made for all P43 samples (n = 157) 8.7 kya (95% CI 6.7–10.8 kya), for the N-P43 Asian.

N1c-Tat:

(…) 75% of Buryats belonged to Haplotype 2, indicating that the Buryats studied by us is a young and isolated population (Bíró et al. 2015). Bashkirian Mari samples derive from Haplotype 2 via Haplotype 3 (see dark purple circles on the top of Fig. 6a). Haplotype 3 contained six males (2 Buryat, 1 Northern Mansi, and 3 Khanty samples from Pimenoff et al. 2008). The biggest Bashkirian Mari haplotype node (3 Mari samples) was positioned three mutational steps away from Haplotype 1 and the remaining Mari samples can be derived from this haplotype. Southern Mansi haplotypes were scattered within the network except for two, which formed a smaller haplotype node with two Northern Mansi and two Khanty samples from Pimenoff et al. (2008).

n1c-n-tat-uralic-ugric
Median-Joining Networks (MJ) of 153 N-Tat (a) and 26 N-L1034 (b) haplotypes constructed. The circle sizes are proportional to the haplotype frequencies. The smallest area is equivalent to one individual. For N-Tat network, we used data from Southern Mansi (n = 11), Bashkirian Mari (n = 6) samples with Hungarian (n = 12), Hungarian speaking Székely (n = 6), Northern Mansi (n = 14), Mongolian (n = 16), Buryat (n = 44), Finnish (n = 13), Uzbek Madjar (n = 2), Uzbek (n = 3), Khanty (n = 4) populations studied earlier by us (Fehér et al. 2015; Bíró et al. 2015) and Khanty (n = 18) and Mansi (n = 4) studied by Pimenoff et al. (2008)

R1a-Z280 haplotypes, shared by Maris, Mansis, and Hungarians, hence ancient Finno-Ugrians:

The founder R1a-Z280 haplotype was shared by four samples from four populations (1 Bashkirian Mari; 1 Southern Mansi; 1 Hungarian speaking Székely; and 1 Hungarian), as presented in Fig. 7 (Haplotype 1). Haplotype 2 included five males (3 Bashkirian Mari and 2 Hungarian), as it can be seen in Fig. 7. Haplotype 4 included two shared haplotypes (1 Bashkirian Mari and one Hungarian speaking Csángó). The remaining two Bashkirian Mari haplotypes differ from the founder haplotype (Haplotype 1) by two mutational steps via Hungarian or Hungarian and Bashkirian Mari shared haplotypes. Beside Haplotype 1, the remaining Southern Mansi haplotypes were shared with Hungarians (Haplotype 5 or turquoise blue and red-coloured circles above Haplotype 7) or with Hungarians and Hungarian speaking Székely group (Haplotypes 3, 5, and 6). Haplotype 7 included ten Hungarian speakers (Hungarian, Székely, and Csángó). One Hungarian and one Uzbek Khwarezm shared haplotype can be found in Fig. 7 as well (red and white-coloured circle). All the other haplotypes were scattered in the network. The age of accumulated STR variation within R1a-Z280 lineage for 93 samples is estimated to be 9.4 kya (95% CI 6.5–12.4 kya) considering Haplotype 1 (Fig. 7) to be the founder.

r1a-z280-ugrians
Median-Joining Networks (MJ) of 93 R1a-Z280 haplotypes constructed. The circle sizes are proportional to the haplotype frequencies. The smallest area is equivalent to one individual. We used haplotype data from Bashkirian Mari (n = 7), Southern Mansi (n = 7), Hungarian (n = 52), Hungarian speaking Székely (n = 11), Hungarian speaking Csángó (n = 10), Uzbek Ferghana (n = 2), Uzbek Tashkent (n = 1), Uzbek Khwarezm (n = 1) and Northern Mansi (n = 2) populations

R1a-Z93 as isolated lineages among Permic and Ugric populations:

Figure 8 depicts an MJ network of R1a-Z93* samples using 106 haplotypes from the 14 populations (Fig. 8). All of the Bashkirian Mari samples (7 haplotypes) formed a very isolated branch and differed from the one Hungarian haplotype (Fig. 8, see Haplotype 1) by seven mutational steps as well from two Uzbek Tashkent samples (see Haplotype 3). Another Hungarian sample shared two haplotypes of Uzbek Khwarezm samples in Haplotype 4. This haplotype can be derived from Haplotype 3 (Uzbek Tashkent). Haplotype 2 included one Hungarian and one Khakassian male. The remaining three Hungarian haplotypes are outliers in the network and are not shared by any sample. The other population samples included in the network either form independent clusters such as Altaians, Khakassians, Khanties, and Uzbek Madjars or were scattered in the network. The age of accumulated STR variation (TMRCA) within R1a-Z93* lineage for 106 samples is estimated as 11.6 kya (95% CI 9.3–14.0 kya) considering an Armenian haplotype (Fig. 8, “A”) to be the founder and the median haplotype.

r1a-z93-ugrians
Median-Joining Networks (MJ) of 106 R1a-Z93 haplotypes constructed. The circle sizes are proportional to the haplotype frequencies. The smallest area is equivalent to one individual. We used the next haplotype data: 7 Bashkirian Mari, 6 Khanty, 4 Uzbek Madjar, 5 Uzbek Ferghana, 9 Uzbek Tashkent, 7 Uzbek Khwarezm, 2 Mongolian, 2 Buryat, 6 Hungarian samples tested by us for this study or published earlier (Bíró et al. 2015) and populations (3 Armenian; 3 Afghan Tajik;
16 Altaian; 24 Khakassian; 12 Kyrgyz) from Underhill et al. (2015)

Comments

The results of modern populations for N (especially N1c) subclades show really wide clusters and ancient TMRCA, consistent with their known ancient and wide distribution in northern and eastern Eurasian groups, and thus with infiltration of different lineages with eastern nomads (and northern Arctic populations) coupled with later bottlenecks, as well as acculturation of groups.

EDIT (2 APR): Interesting is the specific subclade to which ancient Mongolic-speaking Avars belong (information from Yfull) N1c-F4205 (TMRCA ca. 500 BC), subclade of N1c-Y6058 (formed ca. 2800 BC, TMRCA ca. 2800 BC). This branch also gives the “European” branch N1c-CTS10760 (formed ca. 2800 BC, TMRCA ca. 2100 BC), and is subclade of a branch of N1c-L392 (formed ca. 4400 BC, TMRCA ca. 2800 BC). A northern expansion of N1c-L392 is probably represented by its branch N1c-Z1936 (formed ca. 2800, TMRCA ca. 2100 BC), the most likely candidate to appear in the Kola Peninsula in the Bronze Age as the Palaeo-Laplandic population (see here). Read more about potential routes of expansion of haplogroup N.

On the other hand, R1a-Z280 lineages form a tight cluster connecting Permic with Ugric groups, with R1a-Z93 showing early isolation (probably) between Cis-Urals and Trans-Urals regions. While both Corded Ware lineages in Finno-Ugrians are most likely related to the Abashevo expansion through Seima-Turbino and the Andronovo-like Horizon (and potentially later Eurasian expansions), a plausible hypothesis would be that Finno-Ugrians are related to an expansion of R1a-Z283 haplogroups (we already knew about the Finno-Permic connection), while the ancient connection between Permians and Hungarians with R1a-Z93 would correspond to this haplogroup’s potentially tighter link with an early Samoyedic split.

I don’t think that an explosive expansion of eastern Corded Ware groups of R1a-Z645 lineages will show a clear-cut division of haplogroups among Eastern Uralic groups, though, and culturally I doubt we will have such a clear image, either (similar to how the explosive expansion of Bell Beakers cannot be easily divided by regional/language group into R1b-L151 subclades before the known bottlenecks). Relevant in this regard are the known Z93 samples from the Árpád dynasty.

Nevertheless, this data may represent a slightly more recent wave of R1a-Z280 lineages linked to the expansion of Ugric into the Trans-Uralian region, after their split from Finno-Permic, still in close contact with Indo-Iranians in Poltavka and Sintashta-Potapovka, evident from the early and late Indo-Iranian borrowings, during a common period when Samoyedic had already separated.

Such a “Z283 over Z93” layer in the Trans-Urals (and Cis-Urals?) forest-steppes would be similar to the apparent replacement of Z284 by Z282 in the Eastern Baltic during the Bronze Age (possibly with the second or Estonian Battle Axe wave or, much more likely during later population movements). Such an early R1a-Z93 split could potentially be supported also by the separation into bottlenecks under “Northern” (R1a-Z283) Finno-Ugric-speaking Abashevo-related groups and “Southern” (R1a-Z93) acculturated Indo-Iranian-speaking Abashevo migrants developing Sintashta-Potapovka admixing with Poltavka R1b-Z2103 herders.

r1a-z282-z280-z2125-distribution
Modified image, from Underhill et al. (2015). Spatial frequency distributions of Z282 (green) and Z93 (blue) affiliated haplogroups.. Notice the potential Finno-Ugric-associated distribution of Z282 (especially R1a-M558, a Z280 subclade), the expansion of R1a-Z2123 subclades with Central Asian forest-steppe groups.

Conclusion

Let’s review some of the most common myths about Hungarians (and Finno-Ugrians in general) repeated ad nauseam, side by side with my assertions:

❌ N (especially N1c-Tat) in ancient and modern samples represent the True Uralic™ N1c peoples including Magyar tribes? Nope.

✅ Ancient N (especially N1c-Tat) lineages among Uralic populations expanded relatively recently, and differently in different regions (including eastern steppe nomads and northern arctic populations) not associated with a particular language or language group? Yep (read the series on Corded Ware = Uralic expansion).

❌ Modern Hungarian R1a-Z280 lineages represent the majority of the native population, poor Slavic ‘peasants’ from the Carpathian Basin, forcibly acculturated by a minority of bad bad Hungarian hordes? Nope.

✅ Modern Hungarian R1a-Z280 subclades represent Ugric lineages in common with ancient R1a-Z645 Finno-Ugric populations from north-eastern Europe and the Trans-Urals? Yep (see Avars and Ugrians).

❌ Modern Hungarian R1a-Z93 lineages represent acculturated Iranian/Turkic peoples from the steppes? Not likely.

✅ Modern Hungarian R1a-Z93 lineages represent a remnant of the expansion of Corded Ware to the east, potentially more clearly associated with Samoyedic? Much more likely.

finno-ugric-haplogroup-n
Map of archaeological cultures in north-eastern Europe ca. 8th-3rd centuries BC. [The Mid-Volga Akozino group not depicted] Shaded area represents the Ananino cultural-historical society. Fading purple arrows represent likely stepped movements of subclades of haplogroup N for centuries (e.g. Siberian → Ananino → Akozino → Fennoscandia [N-VL29]; Circum-Arctic → forest-steppe [N1, N2]; etc.). Blue arrows represent eventual expansions of Uralic peoples to the north. Modified image from Vasilyev (2002).

Sooo, the theory of a “diluted” Y-DNA in Modern Hungarians from originally fully N-dominated conquerors subjugating native R1a-Z280 Slavs from the Carpathian Basin is not backed up by genetic studies? The ethnic Iranian-Turkic R1a-Z93 federation in the steppes that ended up speaking Magyar is not real?? Who would’ve thunk.

Another true story whose rejection in genetics could not be predicted, like, not at all.

Totally unexpected, too, the drift of “R1a=IE” fans with the newest genetic findings towards a Molgen-like “Yamna/R1b = Vasconic-Caucasian”, “N1c = Uralic-Altaic”, and “R1a = the origin of the white world in Mother Russia”. So much for the supposed interest in “Steppe ancestry” and fancy statistics.

Related

How an empire of steppe nomads coped with environmental stress

uyghur-empire

Recent paper (behind paywall), Environmental Stress and Steppe Nomads: Rethinking the History of the Uyghur Empire (744–840) with Paleoclimate Data, by Di Cosmo et al. JINH (2018) XLVIII(4):439-463.

Abstract (emphasis mine):

Newly available paleoclimate data and a re-evaluation of the historical and archaeological evidence regarding the Uyghur Empire (744–840)—one of several nomadic empires to emerge on the Inner Asian steppe—suggests that the assumption of a direct causal link between drought and the stability of nomadic societies is not always justified. The fact that a severe drought lasting nearly seven decades did not cause the Uyghur Empire to collapse, to wage war, or to disintegrate gives rise to speculations about which of its characteristics enabled it to withstand unfavorable climatic conditions and environmental change. More broadly, it raises questions about the complex suite of strategies and responses that may have been available to steppe societies in the face of environmental stress.

Interesting excerpts:

The heart of the matter is whether the apparent capacity to withstand adverse climatic conditions was due to a set of cultural and/or political choices, unrelated to climate, or to a modification of their nomadic ways toward a greater reliance on agriculture and trade. In support of the first alternative, the Uyghur Empire’s initial military rise and expansion (c. 744 to 780) may have been aided by conditions of high moisture that would have made the grasslands especially productive. The alliance with China, the conversion to Manichaeism, and the growing incorporation of Sogdian elites in their empire that took place during this period may have aided the Uyghurs, serendipitously, to withstand the climatic crisis. In the long run, however, some areas of society most likely suffered adverse effects, which might explain the internal splits and the final defeat at the hands of the Kirgiz. These developments owe as much to the sedentary habits of the Uyghur elites and their ineffective leadership as to the erosion of the pastoral resources that constituted the main support of a nomadic army.

uyghur-climate
The findings are based on scPDSI reconstructions at 0.5-degree grid derived from tree
ring records across Asia.

The evidence from tree-ring data points to environmental conditions that alter the historical narrative of the rise and fall of the Uyghur Empire. Although several studies have focused on how climatic extremes affected agricultural societies, the fate of complex nomadic societies did not necessarily follow the same path. Steppe empires, at least from the first Türk Empire (established in the sixth century C.E.), and possibly earlier, were based on expansive geographical networks, diversified economies, and a degree of co-dependency with merchant classes. Even though these elements varied greatly between empires, they probably reacted to climatic variability in ways radically different from the ways in which agricultural and urban polities did. Once we account for socio-economic complexity, the case of the Uyghur Empire belies the general assumption that nomadic peoples are more vulnerable to climatic stress. The severe and protracted drought did not trigger migration, pillaging, or conquest. Sudden shocks, however, could have had a devastating effect on an economy already weakened.

The catastrophic event of the winter of 839/40, which appears to be a dzud (a weather condition of extreme cold and heavy snowfall that causes high animal mortality) was likely the coup de grâce to an already compromised pastoral production. Contemporary studies of the dzud emphasize that the degree of calamity of the winter disaster is closely related to the drought conditions that preceded it. Thus, the collapse of the Uyghur Empire, generally understood as a rapidly evolving political crisis compounded by a catastrophic weather event, is also connected to multidecadal climatic change, dependency mechanisms, and geopolitical constraints.

I found it interesting mainly because of the potential application of this kind of studies to other previous steppe societies.

Discovered via news on Sapiens.org, posted by Spencer Wells.

Related: