The Origin of Biogenic Horizons in the Pleistocene Strata of Denisova Cave: Mineralogical and Geochemical Markers Help to Reconstruct the Sources of Matter

Author:

Sokol E. V.1,Nekipelova A. V.1,Kozlikin M. B.2,Shunkov M. V.2,Kokh S. N.1,Tikhova V. D.3,Filippova K. A.4,Danilenko I. V.1,Khvorov P. V.4

Affiliation:

1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences

2. Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences

3. Vorozhtsov Novosibirsk Institute of Organic Chemistry, Siberian Branch, Russian Academy of Sciences

4. South Urals Federal Research Center of Mineralogy and Geoecology

Publisher

Institute of Archaeology and Ethnography SB RAS

Reference18 articles.

1. Berna F., Matthews A., Weiner S. 2004 Solubilities of bone mineral from archaeological sites: The recrystallization window. Journal of Archeological Science, vol. 31 (7): 867–882.

2. Birkeland P.W. 1999 Soils and Geomorphology. New York: Oxford Univ. Press.

3. Bohn H.L., Myer R.A., O’Connor G.A. 2002 Soil Chemistry. Oxford: John Wiley & Sons.

4. Fadeeva V.P., Tikhova V.D., Nikulicheva O.N. 2008 Elementniy analiz organicheskikh soyedineniy s ispolzovaniyem avtomaticheskikh CHNS-analizatorov. Zhurnal analiticheskoy khimii, vol. 63 (11): 1197–1210.

5. Forest Insects as Food: Humans Bite Back. 2010 B. Durst, D.V. Johnson, R.N. Leslie, K. Shono (eds.). Bangkok: Food and Agriculture Organization of the United Nations, RAP publication.

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