Calcareous nannofossil stratigraphy of the Upper Cretaceous–lower Paleocene sequence from the Dokan section, Sulaimani, Kurdistan- Iraq

Soran O. A. Kharajiany1, Sherwood W. Wise, Jr.2 , Basim A. Al-Qayim 1

1 Department of Plastic Art, College of Fine Art, University of Sulaimani, Kurdistan Region, Iraq
Florida State University, Tallahassee, Florida, USA

Original: 22 Feburary 2018, Revised: 6 May 2018, Accepted: 11 June 2018, Published online: 20 June 2018


The boundary of the Cretaceous/Tertiary in the Kurdistan region of Iraq is still under debate. Most previous studies consider the Danian sediments to be absent. This paper examines the
boundary in the Dokan area northwest of the Sulaimani city of Kurdistan in northern Iraq. This research analyzes calcareous nannofossil assemblages and the biostratigraphy of the
boundary. The sequence in the study section is characterized by alternations of olive green to greenish gray sandstone, siltstone, shale and marlstone of the Tanjero Formation of the late
Campanian- Maastrichtian and the overlying Kolosh Formation of the early Paleocene. The upper part of the section includes thick sandstone beds and a reworked bioclastic
conglomerate bed in addition to a dark- grey, silty calcareous shale. The study shows that deposition across the boundary is continuous. The boundary is biostratigraphically delineated
by the last occurrence of Maastrichtian taxon and the first occurrences of Biantholithus sparsus, Cruciplacolithus spp. and Coccolithus pelagicus of biozone NP1, which indicate no
hiatus. This succession highlights the occurrence of the early Danian sequence at the bottom of the Kolosh Formation.

Key Words: Dokan, K/T boundary, early Danian, NP1, Biantholithus sparsus, Tanjero, Kolosh, Sulaimani, Kurdistan/Iraq.


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