THE PATTERN OF δ13CORG VERSUS HI/OI RELATION IN RECENT SEDIMENTS AS AN INDICATOR OF GEOCHEMICAL REGIME IN MARINE BASINS: COMPARISON OF THE BLACK SEA, KARA SEA, AND CARIACO TRENCH

dc.contributor.author	Galimov E.M.
dc.date.accessioned	2022-03-30T02:31:48Z
dc.date.available	2022-03-30T02:31:48Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13462445
dc.identifier.citation	Chemical Geology, 2004, 204, 3-4, 287-301
dc.identifier.issn	0009-2541
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36712
dc.description.abstract	An approach is suggested to evaluate the geochemical regime of marine basins. By comparative study of the carbon isotopic composition of organic matter and its hydrogen index to oxygen index ratio in recent sediments a significant role of chemosynthetic bioproduction in the Black Sea, and extensive oxidative diagenesis of the organic matter in the Kara Sea have been demonstrated. The relative role of chemosynthetic production in the Cariaco Trench seems to be different compared to that in the Black Sea.
dc.title	THE PATTERN OF δ13CORG VERSUS HI/OI RELATION IN RECENT SEDIMENTS AS AN INDICATOR OF GEOCHEMICAL REGIME IN MARINE BASINS: COMPARISON OF THE BLACK SEA, KARA SEA, AND CARIACO TRENCH
dc.type	Статья

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