
Originally Posted by
Kale
A 'psuedo-steppe' ancestry would not share drift with actual steppe populations to the exclusions of their formative components. I.E. (no pun intended), if we model South Asians with Steppe_MBA as an input, and Steppe_EBA as an outgroup (to which shared drift is measured against), if the 'psuedo-steppe' idea were correct, we would expect that if South Asians accept Steppe_MBA as an input, their Steppe_EBA affinity would be overfit. We don't see this happening.
It is true that there does appear to be a presence of West_Siberia_N throughout Central Asia (even in the Indus_periphery samples, which have ~30% what looks like AASI), so who knows how far that stretched, and the Central Asian neolithic samples do appear more related to CHG than just simply Iran_N + West_Siberia_N, so there might be something going on there. So sure, one could say there is a pseudo-steppe thing going on in Central/South Asia, but actual steppe input is still required.
Here's a rough trace-backwards using f-3 outgroup nmonte...
Columns: Barcin_N, Iran_N, Levant_N, Kotias, MA1, Anzick, Iron_Gates_HG, Ukraine_Mesolithic, Yamnaya_Samara, Ust_Ishim
Swat = 74% Indus periphery, 19% Uzbekistan_LBA, 7% BMAC (added Ami and Australian as columns to accurately gauge ENA levels)
Indus periphery = 70% something similar to central Asian neolithic, 30% something East-Eurasian
Uzbekistan_LBA = 70% Steppe_MBA, 30% Central Asian BA
BMAC = like earlier Central Asian BA populations
Neolithic Tajik+Turkmen and early Central Asian bronze age populations = Iran_LN + Hajji_Firuz + West_Siberia_N + CHG