dc.contributor.author |
Naugolnykh S. |
|
dc.date.accessioned |
2018-09-19T22:04:42Z |
|
dc.date.available |
2018-09-19T22:04:42Z |
|
dc.date.issued |
2016 |
|
dc.identifier.issn |
0031-0301 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/144666 |
|
dc.description.abstract |
© 2016, Pleiades Publishing, Ltd.Three paleosol profiles (FPS-profiles) are described from the Djadokhta Formation (Upper Cretaceous, Campanian), outcropping in the Bain-Dzak section (southern Gobi aimag, Mongolia). The new data allow the climate at the time of the formation of the Late Cretaceous FPS-profiles to be interpreted as semiarid with seasonal precipitation. The isolated fossil roots of higher plants preserved in situ in the FPS-1 profile of the Bain-Dzak section are described as a new species, Radicites gobiensis Naugolnykh, sp. nov. |
|
dc.relation.ispartofseries |
Paleontological Journal |
|
dc.subject |
Cretaceous |
|
dc.subject |
fossil soils |
|
dc.subject |
FPS-profiles |
|
dc.subject |
Gobi Desert |
|
dc.subject |
Mongolia |
|
dc.subject |
new taxa |
|
dc.subject |
paleosols |
|
dc.subject |
Radicites |
|
dc.subject |
roots |
|
dc.title |
Upper Cretaceous paleosols of the Bain-Dzak section, southern Mongolia |
|
dc.type |
Article |
|
dc.relation.ispartofseries-issue |
12 |
|
dc.relation.ispartofseries-volume |
50 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.relation.startpage |
1451 |
|
dc.source.id |
SCOPUS00310301-2016-50-12-SID85012157930 |
|