Paleocene-Eocene transition at Naqb Assiut, Kharga Oasis, Western Desert, Egypt: Stratigraphical and paleoenvironmental inferences
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- 作者：Moustafa ; Hassan El-Dawy<sup>asup><sup> ; sup><sup>mostafa.hassan1@science.miniauniv.edu.eg" class="auth_mail" title="E-mail the corresponding authorsup> ; Nageh Abdelrahman Obaidalla<sup>bsup><sup> ; sup><sup>obaidala@yahoo.co.uk" class="auth_mail" title="E-mail the corresponding authorsup> ; Kamel Hussien Mahfouz<sup>csup><sup> ; sup><sup>kamel_h79@yahoo.com" class="auth_mail" title="E-mail the corresponding authorsup> ; Samar Adel Abdel Wahed<sup>asup><sup> ; sup><sup>samar_adel2425@yahoo.com" class="auth_mail" title="E-mail the corresponding authorsup>
- 关键词：Benthonic and planktonic foraminifera ; P/E boundary ; Midway-type fauna ; Velasco-type fauna ; Paleobathymetry ; Biostratigraphy ; Paleoenvironment
- 刊名：Journal of African Earth Sciences
- 出版年：2016
- 出版时间：May 2016
- 年：2016
- 卷：117
- 期：Complete
- 页码：207-222
- 全文大小：7116 K
文摘
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The lithostratigraphy of the P–E transition at Naqb Assiut, Western Desert, Egypt is studied.
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The biostratigraphy of this transition is carried out and four planktonic foraminiferal zones are defined.
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The P/E boundary is documented and discussed.
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The benthonic foraminiferal fauna during this interval are analysed and discussed.
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The Paleobathymetrical and paleoenvironmental changes across the P/E boundary are explained.