伊拉克北部库尔德斯坦地区Dhouk地区Bekhere背斜bekme组钙质纳米化石生物地层学与古气候学

Adnan Hakeem, Mohammed Ameen, Mahfoudh Abdulla, Al-Hadeedy, O. Al-Badrani
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引用次数: 0

摘要

在伊拉克北部Bajlur村附近的Dohuk市东侧Bekhere背斜南缘,对bekme组进行了详细的钙质纳米化石研究。贝克梅组由泥灰岩、有机灰岩和化石灰岩组成。这些钙质纳米化石的纳米古生物分类使我们确定了9科34个属/种。纳米生物地层分析表明,从最古老到最年轻的三个钙质纳米化石生物带分别为:(1)Quadrum sissinghii区间带;(2)三角四方区间带;(3) Tranolithus phacelosus间隔带。这些生物带表明所研究的贝克梅组剖面为坎帕尼亚中晚期,它指的是温度波动,被认为是亚热带地区可能的温暖时期。
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Calcareous nannofossils biostratigraphy and Paleoclimatology of the Bekhme Formation, Bekhere anticline, Dhouk area, Kurdistan region, Northern Iraq
A Detailed Calcareous nannofossil study conducted on the Bekhme Formation that is cropped out at the Southern limb of the Bekhere anticline, eastern ward of the Dohuk city near Bajlur village, northern Iraq. The Bekhme Formation is composed of marly limestone, Organic limestone and fossiliferous limestone. The nannopaleontological classification of these calcareous nannofossils led us to determine thirty-four genus/species belonging to nine families. The nannobiostratigraphic analysis suggested three calcareous nannofossils biozones from oldest to youngest are: (1) Quadrum sissinghii Interval Zone; (2) Quadrum trifidum Interval Zone; (3) Tranolithus phacelosus Interval Zone. These biozones suggest that the studied section from the Bekhme Formation is the Middle to Late Campanian, and it refers to temperature fluctuations which considered as possible warm time period at subtropical areas.
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