The study
The Genetic Origin of the Indo-Europeans had already reached the conclusion that individuals from Unakozovskaya (Darkveti-Meshoko culture) were not a good genetic source for Remontnoye (of the CLV cline), and they were not in that cline.
“What was the proximal source for the southern ancestry of the intermediate populations of the CLV cline (The CLV cline people with Lower Volga ancestry contributed four fifths of the ancestry of the Yamnaya ) ? Aknashen makes a poor choice, as it is both geographically remote from the steppe and earlier by two millennia (5985-5836 BCE) than Remontnoye. Neither is Maikop a good
proximal source; it is geographically closer, but postdates (3932-2934 BCE) Remontnoye. Settlements at Meshoko and Svobodnoe, dated 4466-3810 BCE,42 provide a temporally, geographically, and archaeologically plausible source, as they exhibit exchanges of exotic stone, copper, and stone mace heads with Volga Cline sites, setting the context for the expansion of Aknashen-like ancestry northward and Berezhnovka-like ancestry southward. These settlements are temporally earlier than Maikop and later than two individuals from Eneolithic Unakozovskaya (ref.5 4607-4450 BCE, and this study) in the North Caucasus; however, unlike Aknashen and Maikop, the Unakozovskaya population is not a good genetic source for Remontnoye, as the model BPgroup+Unakozovskaya fails (p<0.001) by overestimating (Z=3.8) shared genetic drift with the CHG. The Unakozovskaya was not exactly the same genetically as the Maikop who succeeded them (p=2e-11) but were genetically similar (Fig. 1) and can be modeled as 95.3±6.3% Maikop and 4.7±6.3% CHG (p=0.46). “
From
Supplementary Material of The Genetic Origin of the Indo-Europeans
“
The Unakozovskaya Pre-Maikop individuals from the North Caucasus predate the Maikop. These include three relatives published in ref. 8 of which the higher quality I2056 is used here, together with individual I1717. The Unakozovskaya population is not a clade with Maikop (p=2e-11), because it shares much more genetic drift with CHG, as evidenced by the statistic f4(Maikop, Unakozovskaya; CHG, OldAfrica) which has a Z-score of -6.0. However, it can be modeled as a mixture of Maikop and CHG (p=0.46) with predominantly Maikop-related ancestry (95.36.4%) and conversely Maikop can be modeled as 105.47.1% Unakozovskaya with a negative CHG contribution. Thus, Unakozovskaya (the precursors of Maikop) were similar if not quite like them. The Aknashen+BPgroup model does not fit Unakzovskaya (p=6e-9) as it underestimates CHG shared drift as well (Z=-4.8). Therefore, Unakozovskaya was not quite on the Aknashen-BPgroup (Caucasus-Lower Volga) cline but occupied a position similar to the later Maikop, offset by higher CHG affinity.”
Nalchik belongs also to the Darkveti-Meshoko culture, like the individuals from Unakozovskaya, but Nalchik has a greater steppe component that the individuals from Unakozovskaya, and cluster near Progress 2 individuals (of the CLV cline) in the PCA in this new study.
Does Nalchik change anything? Maybe not, the study about Nalchik, for example, did not detect recent gene flow between Unakozovskaya or Nalchik and Khvalynsk samples, through IBD analysis.
Like the study about Nalchik says “
Genetic infiltration of the Caucasus population into the steppe in the first half of the fifth millennium BC was, most likely, not the first and, more importantly, was not the only one. Judging by the combination of the steppe (EHG) and the Caucasus (CHG) components in some Khvalynsk individuals, the latter component could reach the steppe with the groups of the Caucasus Paleolithic and Mesolithic populations much earlier.”