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Middle Permian U–Pb zircon ages of the “glacial” deposits of the Atkan Formation, Ayan-Yuryakh anticlinorium, Magadan province, NE Russia: Their significance for global climatic interpretations

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dc.contributor.author Davydov V.
dc.contributor.author Biakov A.
dc.contributor.author Isbell J.
dc.contributor.author Crowley J.
dc.contributor.author Schmitz M.
dc.contributor.author Vedernikov I.
dc.date.accessioned 2018-09-19T21:14:21Z
dc.date.available 2018-09-19T21:14:21Z
dc.date.issued 2016
dc.identifier.issn 1342-937X
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/143664
dc.description.abstract © 2015 International Association for Gondwana ResearchThe Atkan Formation in the Ayan-Yuryakh anticlinorium, Magadan province, northeastern Russia, is of great interest because of the occurrence of deposits of apparent “dropstones” and “ice rafted debris” that have been previously interpreted as glacial. Two high-precision U–Pb zircon ages, one for an intercalated volcanic tuff (262.5 ± 0.2 Ma) and the other for a boulder clast (269.8 ± 0.1 Ma) within a diamictite of the Atkan Formation, constrain the age of the Atkan Formation as Guadalupian (middle Permian). Sedimentologic study of the Atkan Formation casts doubt on the glacial nature of the diamictites. Deposition of rocks of the Atkan Formation temporally correlates with the Capitanian interglacial event in the southern hemisphere that recently was calibrated with high precision CA-TIMS. The previously proposed climate proxy record based upon warm-water foraminifera, which corresponds closely to global climate fluctuations, is compared with the glacial record of eastern Australia and indicates that the Capitanian was a time of globally warm climate. The sedimentology of Atkan Formation, the record of diversification of both fusulinids and rugosa corals, global sea-water temperature, and sea-level fluctuations agree well with high latitude paleoclimate records in northeastern Russia and eastern Australia. Major components of the Atkan Formation, the volcanic rocks, are syngenetic with the sedimentation process. The volcanic activity in the nearby regions during middle–late Permian was quite extensive.
dc.relation.ispartofseries Gondwana Research
dc.subject Guadalupian climate
dc.subject Guadalupian volcanism
dc.subject Middle–Late Permian glaciation
dc.subject North-East Russia
dc.subject U/Pb geochronology
dc.title Middle Permian U–Pb zircon ages of the “glacial” deposits of the Atkan Formation, Ayan-Yuryakh anticlinorium, Magadan province, NE Russia: Their significance for global climatic interpretations
dc.type Article
dc.relation.ispartofseries-volume 38
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 74
dc.source.id SCOPUS1342937X-2016-38-SID84949658506


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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