QUASISTATIONARY MODEL OF THE GEOCHEMICAL CYCLE AND EVOLUTION OF THE BIOSPHERE AT THE PRECAMBRIAN-PHANEROZOIC BOUNDARY

dc.contributor.author	Sochava A.V.
dc.date.accessioned	2020-11-09T07:50:38Z
dc.date.available	2020-11-09T07:50:38Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=38602418
dc.identifier.citation	Известия Российской академии наук. Серия геологическая, 1992, , 6, 41-56
dc.identifier.issn	0321-1703
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18775
dc.description.abstract	The Vendian period, which preceded the Phanerozoic, was characterised not only by prominent evolutionary events, but also by an unusual composition of the sulphur, carbon and strontium in the sediments. From the point of view of the proposed model this indicates a significant drop in the content of O2 in the atmosphere and the hydrosphere. This change in the characteristics of the external environment promoted the first appearance of specialised respiratory organs in multi-celled animals. The increase in the content of O2 in the atmosphere following the Vendian-Cambrian boundary served as a precondition for the appearance of exoskeletons in animals and their rapid taxonomic radiation.
dc.subject	Precambrian	en
dc.title	QUASISTATIONARY MODEL OF THE GEOCHEMICAL CYCLE AND EVOLUTION OF THE BIOSPHERE AT THE PRECAMBRIAN-PHANEROZOIC BOUNDARY
dc.type	Статья
dc.subject.age	Precambrian	en
dc.subject.age	Докембрий	ru

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