RATE OF CARBON ACCUMULATION IN SEDIMENTS IN GEOLOGIC HISTORY

dc.contributor.author	Sidorenko Sv.A.
dc.contributor.author	Tenyakov V.A.
dc.date.accessioned	2020-11-02T00:30:44Z
dc.date.available	2020-11-02T00:30:44Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31150159
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 4, 146-148
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18357
dc.description.abstract	On the basis of new data we have confirmed our previous conclusion as to the extremely high level of biological activity in the Precambrian. On the other hand, linking this new fact with our previously established fact of the clear connection of the global epochs of accumulation of high-carbon-containing deposits with the main stages in the evolution of the 'living systems' themselves, we can arrive at the essentially new conclusion that evolution itself was considerably more intensive in the Precambrian.
dc.subject	Precambrian	en
dc.title	RATE OF CARBON ACCUMULATION IN SEDIMENTS IN GEOLOGIC HISTORY
dc.type	Статья
dc.subject.age	Precambrian	en
dc.subject.age	Докембрий	ru

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