TY - GEN
T1 - Geochemical Evidence for Photic Zone Euxinia During Greenhouse Climate in the Tethys Sea, Egypt
AU - Fathy, Douaa
AU - Wagreich, Michael
AU - Sami, Mabrouk
N1 - Publisher Copyright:
© 2022, The Author(s), under exclusive license to Springer Nature Switzerland AG.
PY - 2022
Y1 - 2022
N2 - Upper cretaceous organic-rich sediments are good archives for the paleoceanographic changes. Here, a comprehensive set of geochemical, biological, and mineralogical data have been applied in order to evaluate the role of euxinia on the organic matter during deposition. The total organic matter of these organic-rich sediments reaches up to 23 wt%. They have significant concentrations of redox-sensitive trace elements such as Mo, Cu, Zn, Ni, Cd, U, and V. The values of redox proxies (e.g., U/Mo, V/(V + Ni), V/Ni, Ni/Co, V/Cr, U/Th, U authigenic) and the size of framboids pyrite suggest that the Upper Cretaceous organic-rich sediments were deposited under a euxinic water column environment. The molecular fossils data also point to the predominance of the sulfidic anoxic conditions during deposition. The good correlation between TOC and redox proxies indicates that the oxygen-depleted conditions play a significant role in the preservation of that organic matter.
AB - Upper cretaceous organic-rich sediments are good archives for the paleoceanographic changes. Here, a comprehensive set of geochemical, biological, and mineralogical data have been applied in order to evaluate the role of euxinia on the organic matter during deposition. The total organic matter of these organic-rich sediments reaches up to 23 wt%. They have significant concentrations of redox-sensitive trace elements such as Mo, Cu, Zn, Ni, Cd, U, and V. The values of redox proxies (e.g., U/Mo, V/(V + Ni), V/Ni, Ni/Co, V/Cr, U/Th, U authigenic) and the size of framboids pyrite suggest that the Upper Cretaceous organic-rich sediments were deposited under a euxinic water column environment. The molecular fossils data also point to the predominance of the sulfidic anoxic conditions during deposition. The good correlation between TOC and redox proxies indicates that the oxygen-depleted conditions play a significant role in the preservation of that organic matter.
KW - Cretaceous
KW - Depositional environment
KW - Egypt
KW - Euxinia
KW - Greenhouse climate
KW - Organic matter
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U2 - 10.1007/978-3-030-73026-0_85
DO - 10.1007/978-3-030-73026-0_85
M3 - Conference contribution
AN - SCOPUS:85128951079
SN - 9783030730253
T3 - Advances in Science, Technology and Innovation
SP - 373
EP - 374
BT - Advances in Geophysics, Tectonics and Petroleum Geosciences - Proceedings of the 2nd Springer Conference of the Arabian Journal of Geosciences CAJG-2, Tunisia 2019
A2 - Meghraoui, Mustapha
A2 - Sundararajan, Narasimman
A2 - Banerjee, Santanu
A2 - Hinzen, Klaus-G.
A2 - Eshagh, Mehdi
A2 - Roure, François
A2 - Chaminé, Helder I.
A2 - Maouche, Said
A2 - Michard, André
PB - Springer Nature
T2 - 2nd Springer Conference of the Arabian Journal of Geosciences, CAJG-2 2019
Y2 - 25 November 2019 through 28 November 2019
ER -