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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TÜBİTAK Academic Journals
2020
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Online Access: | https://journals.tubitak.gov.tr/earth/vol29/iss8/4 https://journals.tubitak.gov.tr/cgi/viewcontent.cgi?article=1122&context=earth |