The First Data on the N Isotopic Composition of the Permian and Triassic of Northeastern Russia and Their Significance for Paleotemperature Reconstructions

dc.contributor.author	Zakharov Y.
dc.contributor.author	Biakov A.
dc.contributor.author	Horacek M.
dc.contributor.author	Goryachev N.
dc.contributor.author	Vedernikov I.
dc.date.accessioned	2020-01-21T20:45:18Z
dc.date.available	2020-01-21T20:45:18Z
dc.date.issued	2019
dc.identifier.issn	1028-334X
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/157725
dc.description.abstract	© 2019, Pleiades Publishing, Ltd. Abstract: It is proposed that unstable temperature conditions in the Late Wuchiapingian and Early Changhsingian (Late Permian) changed in the Boreal Superrealm to less contrasting climatic conditions in the Late Changhsingian and Early Induan (the formation time of trap formation of the Siberian Platform), with a stable trend of increasing temperature in the Early Triassic. The problem of the absence of signs of mass extinction of marine organisms at the Permian–Triassic boundary in the Boreal Superrealm is discussed.
dc.relation.ispartofseries	Doklady Earth Sciences
dc.title	The First Data on the N Isotopic Composition of the Permian and Triassic of Northeastern Russia and Their Significance for Paleotemperature Reconstructions
dc.type	Article
dc.relation.ispartofseries-issue	1
dc.relation.ispartofseries-volume	484
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	21
dc.source.id	SCOPUS1028334X-2019-484-1-SID85063992962

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Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.