Latest Priabonian larger benthic foraminiferal assemblages at the demise of theSoğucak Carbonate Platform (Thrace Basin and Black Sea shelf, NW Turkey):implications for the shallow marine biostratigraphy

The Eocene-Oligocene transition corresponds to a significant biotic turnover globally. In shallow marine realms, the larger benthic foraminifera (LBF) belonging to most nummulitids and all orthophragminids became extinct at or near the Eocene/Oligocene boundary, reflecting the environmental deterior...

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Bibliographic Details
Main Authors: YÜCEL, ALİ OSMAN, ÖZCAN, ERCAN, ERBİL, ÜMİTCAN
Format: Text
Language:unknown
Published: TÜBİTAK Academic Journals 2020
Subjects:
Soğucak Carbonate Platform
larger benthic foraminifera
Priabonian
SBZ 20
Thrace Basin
Black Sea shelf
Earth Sciences
Lamarck
Thrace
Planktonic foraminifera
Online Access:https://journals.tubitak.gov.tr/earth/vol29/iss8/4
https://journals.tubitak.gov.tr/cgi/viewcontent.cgi?article=1122&context=earth

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