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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 |