Кольский Оленеостровский могильник, 1925-2013 = Kola Oleneostrovsky cementery, 1925-2013 / Колпаков Е. М., Мурашкин А. И., Хартанович В. И., Шумкин В. Я. ; Институт истории материальной культуры РАН, Кольская археологическая экспедиция [и др.]. - Санкт-Петербург ; Вологда : Древности Севера, 2019.

53% 9). (29.6%) - Anthropology The first two main components jointly account for about 53% of the total variation 9). The first one (29.6%) differentiates groups according to the degree of lower molar variation. The samples with relatively high frequencies of 6-cusped lower first molars are in the positive field, while those with high percentage of 4-cusped lower first and second molars are on the opposite extreme. It contrasts the Serovian and populations of the Baikal region with the Late Krotovo population of the Barablnsk forest-steppe. The series is in the positive field, close to the Krotovo (Barablnskaya forest-steppe) and Okunev (South Siberia) culture people, which agrees with the results of craniological studies. 9. 12 9'. Correlation coefficients between first two principal components and dental traits in analysis of 12 ancient series of the continental Asia and / Traits 1 / Shoveling I 1 0.52 0.25 / Carabelli's trait 0.33 -0.24 / Hypocone reduction -0.34 0.51 / 6-cusped 0.87 0.26 / 4-cusped -0.54 0.15 / 4-cusped -0.90 0.11 / Distal trigonid crest 0.12 0.69 / Deflecting wrinkle 1 0.01 -0.95 / Explained variance % / % of total variance (23.3%) 100%, - 2). 390 1.752 1.382 29.6 23.3 The second component (23.3%) differentiates series with elevated frequencies of distal trigonid crests from those displaying elevated frequencies of deflecting wrinkles. The positive pole is represented the Neo-Eneolithic population of the Altai-Sayan mountain land with the frequency of distal crest approaching 100%. The negative pole is formed the Glazkovo, and Ymiyakhtakh populations together with the series (Graph 2).