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dc.contributor.author Ruban D.A.
dc.date.accessioned 2024-11-09T08:38:18Z
dc.date.available 2024-11-09T08:38:18Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13528000
dc.identifier.citation Acta Geologica Hungarica, 2006, 49, 1, 57-71
dc.identifier.issn 0236-5278
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46434
dc.description.abstract The diversity of the brachiopods in the Northern Caucasus significantly fluctuated throughout the Paleozoic-Mesozoic. Weak diversifications occurred in the Middle Cambrian, Late Silurian - Early Devonian, and Late Devonian - Early Carboniferous. Since the Late Permian brachiopod assemblages became quite diverse. The maximum number of species was reached in the Rhaetian. The Permian/Triassic mass extinction and enigmatic Ladinian crisis, on the other hand, led to regional brachiopod demises. In the Jurassic - Early Cretaceous interval the diversity of brachiopods generally decreased. The strongest drops of species numbers occurred in the Toarcian and Berriasian following the Pliensbachian-Toarcian and end-Jurassic global mass extinctions, and in the Kimmeridgian due to the regional salinity crisis. It is evident that some of the regional brachiopod diversifications coincided with the development of rimmed shelves. © 2006 Akadémiai Kiadó, Budapest.
dc.subject BRACHIOPODS
dc.subject CAUCASUS
dc.subject DIVERSITY
dc.subject MASS EXTINCTIONS
dc.subject MESOZOIC
dc.subject PALEOZOIC
dc.subject REEFS
dc.title DIVERSITY CHANGES OF THE BRACHIOPODS IN THE NORTHERN CAUCASUS: A BRIEF OVERVIEW
dc.type Статья
dc.identifier.doi 10.1556/AGeol.49.2006.1.4
dc.subject.age Mesozoic
dc.subject.age Мезозойская


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