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Along the forest trajectory as well there is evidence of either an early Indie presence or undifferentiated Proto-Indo-Iranian or Proto-Indo-Aryan. A… - Johanna Nichols
" "Along the forest trajectory as well there is evidence of either an early Indie presence or undifferentiated Proto-Indo-Iranian or Proto-Indo-Aryan. Among the Indo-Iranian loans into early Finno-Ugric are some so phonologically archaic that they could well be Proto-Indo-Iranian... Iranian, but not Indo-Aryan, regularly reflects PIE s as h, so this Finno-Ugric form looks more Indie than Iranian. Abaev also cites some less well attested forms that could be specifically Indie... These borrowings would have taken place somewhere in the vicinity of the southern Ural Mountains. They were received from a steppe language and incorporated into Finno-Ugric as it began its spread along the forest trajectory. This linguistic evidence for an Indie or Proto-Indo-Iranian wave preceding Iranian on the steppe is weak but legitimate. In partial confirmation of it, Kuz’mina identifies the Andronovo culture of eastern Kazakhstan in the mid-second millennium BC as Indo-Aryan..... There is also evidence for Indo-Aryan along the steppe trajectory in the form of a set of Crimean place names which Trubač identifies as Indo-Aryan. This evidence is even weaker—place names in general have poor diagnostic value since they lack denotational meaning—but carefully researched and again legitimate. If Trubačv is right there is evidence for an Indie advance to the western steppe. Taken together, the Finno-Ugric and Crimean evidence are consistent with the assumption of a short-lived Indie or Indo-Aryan presence at the frontier of the Iranian spread on the steppe, in addition to the well-known Indie frontier in northeastern Mesopotamia and India.
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About Johanna Nichols
Johanna Nichols (born 1945, Iowa City, Iowa) is a linguist and professor emerita in the Department of Slavic Languages and Literatures at the University of California, Berkeley. She earned her PhD in Linguistics at the University of California, Berkeley, in 1973 with a dissertation entitled, "The Balto-Slavic predicate instrumental: a problem in diachronic syntax."
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Additional quotes by Johanna Nichols
There are several linguistically plausible possibilities for the origin of Pre-PIE. It could have spread eastward from the Black Sea steppe (as proposed by Mallory 1989 and by Anthony 1991, 1995), so that the locus formed only after this spread but still very early in the history of disintegrating PIE. This large eastward spread would be a departure from the general westward trajectory of spreads in central Eurasia, occasioned by the epoch-making domestication of the horse and development of wheeled transport. Pre-PIE could have been a central Asian language long before its rapid spread; if so it had a large range before its expansion, and the dispersal began with the development of the locus in a pre-existent range. It could have come into the spread zone from the east as Mongolian, Turkic, and probably Indo-Iranian did.
The archaeological sources on which this summary is based... most often describe the westward cultures as derived from, or extensions from, the eastern ones. Mallory (1989) and Anthony (1991, 1995) interpret the directionality of cultural derivation as west to east. It is the east-to-west directionality of cultural derivation that would be consistent with the east-to-west linguistic trajectory, since spread of a whole culture is likely to involve language spread (and vice versa). A predominantly east-to-west directionality of cultural derivation and descent for the Eneolithic steppe would be a strong indication that the spread zone with its westward trajectories had taken shape. This is a purely archaeological question, but it is important to dating the rise of the linguistic spread zone.
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The Iranian family, which was next to sweep across the steppe and deserts, finds its region of greatest diversity in the central Asian mountains, and its ancestral Indo-Iranian family finds its own greatest diversity in the mountain region from central Asia to northern India (i.e. Bactria- Sogdiana and parts just south).
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