Calcareous nannofossils from chalky limestone intervals of the Abderaz formation in the Kopet Dagh range, NE Iran

الموضوعات :

Somayeh Sanjary ¹ , Fatemeh Hadavi ² , Marziyeh Notghi Moghaddam ³ , Mohsen Allameh ⁴

1 - Department of Geology, Ferdowsi University of Mashhad, International Campus, Iran
2 - Department of Geology, Ferdowsi University of Mashhad, Iran
3 - Department of Geology, Payame Noor University, Tehran, Iran
4 - Department of Geology, Mashhad Branch, Islamic Azad University, Mashhad, Iran

تاريخ الإرسال : 09 السبت , ربيع الأول, 1440 تاريخ التأكيد : 09 السبت , ربيع الأول, 1440 تاريخ الإصدار : 25 الثلاثاء , ربيع الثاني, 1440

الکلمات المفتاحية: Iran, Calcareous nannofossil, Chalky limestone, Abderaz, Kopet Dagh,

ملخص المقالة :

A biostratigraphic study based on calcareous nannofossils was performed on the chalky limestone from the Abderaz Formation in the Mozduran section (Kopet Dagh basin, NE Iran). Semiquantitative estimates of total nannofossil and single species abundances showed that calcareous nannofossil assemblages are common and their preservation is good. In this study 37 species have been identified in chalky limestone beds. The following biohorizons were identified: the first occurrence (FO) of Broinsonia parca parca; the last occurrence (LO) of Marthasterites furcatus; the FO of Ceratolithoides aculeus; and the FO of Uniplanarius sissinghii. Based on nannofossil assemblages' four biozones were determined in this section which is the time equivalent of UC14 to UC15cTP of (Burnett 1998), and CC18 to CC21 of (Roth et al. 1986). According to present biozones, early Campanian to early late Campanian ages are suggested. Calcareous nannofossils allow the detailed reconstruction of paleoecological trends in the chalky limestone beds. The chalky limestone of the Abderaz Formation was deposited in a shallow-marine environment, at relatively low latitude with low primary productivity.

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