Proto-Uralic Homeland (VII): Kinship & Numerals


This post is part of a draft on palaeolinguistics and the Proto-Uralic homeland. See below for the color code of protoforms.

12. Kinship Terminology

12.1. Immediate Family

PU? (Saa.?, Fi.?, Md.?, Ma.?, Kh.?, Ms.?, Hu.?, Smy.?) *äććä?/*eć(ć)ä/*ić(ć)ä/*äjćä ‘father’ (UEW Nº 35). PSmy. was was borrowed into Yukaghir ečē ‘father’. Samoyedic form borrowed into Yukaghir ečē ‘father’ (Aikio 2014: 57)

NOTE. Pre-PSmy. *äjćä? could reflect an earlier Pre-PIIr. *eićo- or PIIr. *aića- ‘to control, to own’. An underlying Pre-PFi., Pre-PSaa. (based on PSaa. *e̮ćē from Skolt and Kildin Saami) and PMa. *ićä could reflect PIIr. īćá- ‘master, lord’, from Read the rest “Proto-Uralic Homeland (VII): Kinship & Numerals”

Tug of war between Balto-Slavic and West Uralic (II)


It is firmly established since (at least) the 1980s that Balto-Slavic, Baltic and Slavic show a strong Uralic substrate, even though many details are still the subject of ongoing controversies. Here is how the Baltic linguistic area was described in Thomason’s Language Contact (2001):

Overall, the Baltic area has the same characteristics as the Balkan area: areal linguistic features are distributed differentially among the languages, and the features themselves vary in details of their structure. As for the sources of the Baltic features, some can be traced to Uralic and some to Indo-European, especially Germanic. The Indo-European languages most

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R1a-Z93-rich Classical CWC-like Fatyanovo replaced Volosovo


Open access Genetic ancestry changes in Stone to Bronze Age transition in the East European plain, by Saag et al. bioRxiv (2020).

Interesting excerpts (emphasis mine):

Y-DNA chromosome haplogroup

(…) the Bronze Age Fatyanovo Culture individuals [] maternal (subclades of mtDNA hg U5, U4, U2e, H, T, W, J, K, I and N1a) and paternal (chrY hg R1a-M417) lineages were ones characteristic of CWC individuals elsewhere in Europe. Interestingly, in all individuals for which the chrY hg could be determined with more depth (n=6), it was R1a2-Z93, a lineage now spread in Central and South Asia, rather than the

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