Planktonic foraminifera biozones and isotope stratigraphy of the Cenomanian-Turonian boundary in the western part of the Kopet-Dagh Basin, NE Iran

Author:

Ezampanah Yadolah,Sadeghi Abbas,Scopelliti Giovanna,Adabi Mohammad Hossein,Jamali Amir Mohammad

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference97 articles.

1. Petrographic and geochemical evidence for original aragonite mineralogy of Upper Jurassic carbonates (Mozduran Formation), Sarakhs area, Iran;Adabi;Sediment. Geol.,1991

2. Geology of Kopet-Dagh;Afshar-Harb,1994

3. Palynology and palynofacies of Aitamir Formation at zavin section (Khorasan razavi);Allameh;Sci. Q. J. Geosci.,2015

4. Variations in the global carbon cycle during the cretaceous related to climate, volcanism, and changes in atmospheric CO2. The carbon cycle and atmospheric CO: natural variations archean to present;Arthur,1985

5. Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian–Turonian boundary;Arthur;Nature,1988

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