Arid
DOI10.1016/j.jafrearsci.2018.06.015
Morphologic change and evolution of Acarinina sibaiyaensis and its descendants during the earliest Eocene CIE/PETM interval in southern Egypt
Ouda, Khaled Abdel-Kader
通讯作者Ouda, Khaled Abdel-Kader
来源期刊JOURNAL OF AFRICAN EARTH SCIENCES
ISSN1464-343X
EISSN1879-1956
出版年2018
卷号147页码:78-125
英文摘要

Acarinina sibaiyaensis is a very distinctive and short-lived planktonic foraminiferal taxon that is restricted to the temporally short Carbon Isotope Excursion (CIE) interval characteristic of the Paleocene-Eocene Thermal Maximum (PETM) event. It is confined to the planktonic foraminiferal Zone El which in southern Egypt corresponds to the Dababiya Quarry Member (DQM). This member yields a complete record of the biotic changes induced by the intense warming during the basal Eocene.


Although this distinctive taxon is widely distributed throughout the tropic to the temperate regions, its morphologic changes and phylogenetic relations during the CIE/PETM interval have not yet been documented. The present study discusses and documents the morphologic changes which affected the short-lived Ac. sibaiyaensis probably caused by the extreme warming during the very brief (175-200 ka) CIE/PETM interval in southern Egypt. These morphologic variations are particularly well developed in the middle phosphatic phase (Beds 2 and 3 of the DQM), in which the CIE curve shows its maximum negative shift. The origin, morphology, wall texture, coiling direction and their changes during ontogeny and evolution of Ac. sibaiyaensis during the CIE-PETM interval at Qreiya, Gebel Abu Had, northeast Qena (southern Nile Valley) and Darb Gaga (southeast of Kharga Oasis, southern Western Desert) are described, interpreted and illustrated. During the PETM, numerous intraspecific varieties of Ac. sibaiyaensis are recorded. Several evolutionary lineages are delineated; some of them stay within the morphologic range of Ac. sibaiyaensis, whereas others lead to other excursion taxa i.e. Acarinina africana and Morozovella allisonensis. In addition, forms transitional to taxa which appear in younger horizons than the PETM (younger than Zone El) are recorded, described and illustrated.


英文关键词Acarinina sibaiyaensis Ac. africana Morozovella allisonensis Paleocene eocene thermal maximum Darb gaga Qreiya Southern Egypt
类型Article
语种英语
国家Egypt
收录类别SCI-E
WOS记录号WOS:000447096300008
WOS关键词UPPER NILE VALLEY ; PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHY ; CARBON-ISOTOPE STRATIGRAPHY ; PALEOCENE THERMAL MAXIMUM ; GEBEL-ABU-HAD ; GLOBIGERINA-PACHYDERMA ; DABABIYA SECTION ; WESTERN DESERT ; ORGANIC-CARBON ; KHARGA OASIS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/210419
作者单位Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt
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GB/T 7714
Ouda, Khaled Abdel-Kader. Morphologic change and evolution of Acarinina sibaiyaensis and its descendants during the earliest Eocene CIE/PETM interval in southern Egypt[J],2018,147:78-125.
APA Ouda, Khaled Abdel-Kader.(2018).Morphologic change and evolution of Acarinina sibaiyaensis and its descendants during the earliest Eocene CIE/PETM interval in southern Egypt.JOURNAL OF AFRICAN EARTH SCIENCES,147,78-125.
MLA Ouda, Khaled Abdel-Kader."Morphologic change and evolution of Acarinina sibaiyaensis and its descendants during the earliest Eocene CIE/PETM interval in southern Egypt".JOURNAL OF AFRICAN EARTH SCIENCES 147(2018):78-125.
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