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dc.contributor.author | Biakov A. | |
dc.date.accessioned | 2020-01-21T20:32:53Z | |
dc.date.available | 2020-01-21T20:32:53Z | |
dc.date.issued | 2019 | |
dc.identifier.issn | 0031-0301 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/157395 | |
dc.description.abstract | © 2019, Pleiades Publishing, Ltd. Abstract: The change in marine bivalve communities at the Carboniferous–Permian transition of Northeast Asia has been analyzed for the first time. A significant increase in the taxonomic diversity of the group occurs near the Carboniferous–Permian boundary, most likely, due to the invasion of a number of thermophilic elements from the more southerly basins into the Omolon Basin, associated with a short-term global warming episode. The position of the Carboniferous–Permian boundary in Northeast Asia is considered. A conclusion is made that this boundary in the Kolyma–Omolon–Chukchi region is most likely located within the Verchojania mirandus–Prothyris elongatus complex Zone. | |
dc.relation.ispartofseries | Paleontological Journal | |
dc.subject | bivalves | |
dc.subject | Carboniferous–Permian boundary | |
dc.subject | Northeast Asia | |
dc.subject | Okhotsk massif | |
dc.subject | Omolon massif | |
dc.subject | taxonomic diversity | |
dc.subject | Verkhoyansk region | |
dc.title | Bivalves of Northeast Asia at the Carboniferous–Permian Transition | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 3 | |
dc.relation.ispartofseries-volume | 53 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 241 | |
dc.source.id | SCOPUS00310301-2019-53-3-SID85067416676 |