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 |
|