Eighteen planktic and eleven benthic foraminiferal species were recorded from the dark grey to black shale facies of the Matulla Formation in Abu Zeneima area, West-Central Sinai, Egypt. The faunal assemblage is dominated by cosmopolitan whiteinellids, marginotruncanids, Dicarinellids, Contusotruncanids and Heterohelicids. The planktic species with high taxonomic diversity were used to zone the Coniacian and Santonian stages, as well as define the Coniacian/ Santonian boundary, while benthic foraminifera is of minor contribution in age assignment. The stratigraphic analysis of the relations and ranges of these fauna led to the recognition of five biozones; Dicarinella primitiva or Huberella huberi or Marginotruncana sinuosa for the Coniacian, while Dicarinella concavata and Dicarinella asymetrica for the Santonian. Also, the Coniacian/Santonian boundary was delineated, considering the appearance of Dicarinella concavata and disappearance of Huberella huberi, as well as the increase of Marginotruncanids (M. renzi, M. sigali, M. marginata, M. pseudolinneiana….etc.). Furthermore, the black shales found in the middle part of the Matulla Formation were attributed to the Coniacian-Santonian Oceanic Anoxic Event (OAE3). The occurrence of black shales with planktic foraminifera during the Coniacian–Santonian interval in several countries belonging to five continents, was the main impetus to render this event a global event.
| Published in | American Journal of BioScience (Volume 12, Issue 1) |
| DOI | 10.11648/j.ajbio.20241201.14 |
| Page(s) | 22-34 |
| Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2024. Published by Science Publishing Group |
Foraminifera, Coniacian, Santonian, OAE3, Egypt
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APA Style
Ismail, A. A. (2024). A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3). American Journal of BioScience, 12(1), 22-34. https://doi.org/10.11648/j.ajbio.20241201.14
ACS Style
Ismail, A. A. A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3). Am. J. BioScience 2024, 12(1), 22-34. doi: 10.11648/j.ajbio.20241201.14
AMA Style
Ismail AA. A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3). Am J BioScience. 2024;12(1):22-34. doi: 10.11648/j.ajbio.20241201.14
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Download@article{10.11648/j.ajbio.20241201.14,
author = {Ahmed Aly Ismail},
title = {A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3)},
journal = {American Journal of BioScience},
volume = {12},
number = {1},
pages = {22-34},
doi = {10.11648/j.ajbio.20241201.14},
url = {https://doi.org/10.11648/j.ajbio.20241201.14},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajbio.20241201.14},
abstract = {Eighteen planktic and eleven benthic foraminiferal species were recorded from the dark grey to black shale facies of the Matulla Formation in Abu Zeneima area, West-Central Sinai, Egypt. The faunal assemblage is dominated by cosmopolitan whiteinellids, marginotruncanids, Dicarinellids, Contusotruncanids and Heterohelicids. The planktic species with high taxonomic diversity were used to zone the Coniacian and Santonian stages, as well as define the Coniacian/ Santonian boundary, while benthic foraminifera is of minor contribution in age assignment. The stratigraphic analysis of the relations and ranges of these fauna led to the recognition of five biozones; Dicarinella primitiva or Huberella huberi or Marginotruncana sinuosa for the Coniacian, while Dicarinella concavata and Dicarinella asymetrica for the Santonian. Also, the Coniacian/Santonian boundary was delineated, considering the appearance of Dicarinella concavata and disappearance of Huberella huberi, as well as the increase of Marginotruncanids (M. renzi, M. sigali, M. marginata, M. pseudolinneiana….etc.). Furthermore, the black shales found in the middle part of the Matulla Formation were attributed to the Coniacian-Santonian Oceanic Anoxic Event (OAE3). The occurrence of black shales with planktic foraminifera during the Coniacian–Santonian interval in several countries belonging to five continents, was the main impetus to render this event a global event.
},
year = {2024}
}
TY - JOUR T1 - A New Epistemological Insight of the Coniacian-Santonian Oceanic Anoxic Event (OAE3) AU - Ahmed Aly Ismail Y1 - 2024/02/21 PY - 2024 N1 - https://doi.org/10.11648/j.ajbio.20241201.14 DO - 10.11648/j.ajbio.20241201.14 T2 - American Journal of BioScience JF - American Journal of BioScience JO - American Journal of BioScience SP - 22 EP - 34 PB - Science Publishing Group SN - 2330-0167 UR - https://doi.org/10.11648/j.ajbio.20241201.14 AB - Eighteen planktic and eleven benthic foraminiferal species were recorded from the dark grey to black shale facies of the Matulla Formation in Abu Zeneima area, West-Central Sinai, Egypt. The faunal assemblage is dominated by cosmopolitan whiteinellids, marginotruncanids, Dicarinellids, Contusotruncanids and Heterohelicids. The planktic species with high taxonomic diversity were used to zone the Coniacian and Santonian stages, as well as define the Coniacian/ Santonian boundary, while benthic foraminifera is of minor contribution in age assignment. The stratigraphic analysis of the relations and ranges of these fauna led to the recognition of five biozones; Dicarinella primitiva or Huberella huberi or Marginotruncana sinuosa for the Coniacian, while Dicarinella concavata and Dicarinella asymetrica for the Santonian. Also, the Coniacian/Santonian boundary was delineated, considering the appearance of Dicarinella concavata and disappearance of Huberella huberi, as well as the increase of Marginotruncanids (M. renzi, M. sigali, M. marginata, M. pseudolinneiana….etc.). Furthermore, the black shales found in the middle part of the Matulla Formation were attributed to the Coniacian-Santonian Oceanic Anoxic Event (OAE3). The occurrence of black shales with planktic foraminifera during the Coniacian–Santonian interval in several countries belonging to five continents, was the main impetus to render this event a global event. VL - 12 IS - 1 ER -
Geology Department, Faculty of Science, Ain Shams University, Cairo, Egypt
