Stratigraphic organisation, spatial distribution, palaeoenvironmental reconstruction, and demise of Lower Cretaceous (Barremian-lower Aptian) carbonate platforms of the Western Pontides (Black Sea region, Turkey)


Masse J., Tuysuz O. , FENERCI-MASSE M., Ozer S., Sari B.

CRETACEOUS RESEARCH, cilt.30, ss.1170-1180, 2009 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 30 Konu: 5
  • Basım Tarihi: 2009
  • Doi Numarası: 10.1016/j.cretres.2009.05.004
  • Dergi Adı: CRETACEOUS RESEARCH
  • Sayfa Sayıları: ss.1170-1180

Özet

Barremian-Lower Aptian platform carbonates ("Urgonian limestones") of the northern margin of the Istanbul zone extend from Zonguldak to the Kurucasile area along the Black Sea coast. New stratigraphic data on the "Inpiri" Formation of the Inpiri-Kurucasile area are based on the identification of calcareous algae, foraminifera, and rudists. They show that this lithostratigraphic unit is stratigraphically and lithologically equivalent to the Okusmedere Formation from Zonguldak. Some of the biostratigraphic markers are reported for the first time in Anatolia. Foraminifera are represented by several forms with a significant biostratigraphic potential used to distinguish the Barremian from the lower Aptian. Lower Aptian beds also yield relatively advanced caprinid rudists.