Depositional and organic carbon-controlled regimes during the Coniacian-Santonian event
- Autor(en)
- Ahmed Mansour, Michael Wagreich, Thomas Gentzis, Seare Ocubalidet, Sameh S. Tahoun, Ashraf M.T. Elewa
- Abstrakt
Geochemical and palynological proxies were determined for 31 samples representing the upper Coniacian-lowermost Campanian Abu Roash A Member, collected from the BED2-3 well. This was done to assess the prevailing paleoredox conditions, productivity levels, and water-column settings to: (1) understand controls and mechanisms related to accumulation of organic carbon within the sedimentary record; (2) assess principal environmental processes that triggered the preservation of organic matter-poor, calcareous shale and limestone facies of the Abo Roash A Member; and (3) to interpret the paleoceanographic settings and confirm the occurrence of either Oceanic Anoxic Event 3 (OAE3) or Cretaceous Oceanic Red Beds (CORBs) within the Abu Gharadig Basin in the southern part of the Tethyan Ocean, Egypt. Sedimentation rates were reconstructed based on the biostratigraphic-age constraints of marine dinoflagellate cysts (dinocysts). Trace elements-based ratios and relationships were used in order to study the role of clastic terrestrial input. Three groups of dinocysts and freshwater Pediastrum algae were used to study the water-column conditions. Results showed that the Abu Roash A Member was deposited under oxic to intermittently dysoxic conditions in a distal inner to middle neritic environment, with varying sedimentation rates from 32 to 119 mm kyr−1. Productivity appeared to be a significant factor for determining magnitudes of the organic carbon accumulation; however, low productivity was prevalent during deposition. Carbonate content was high, which resulted in dilution of organic matter during varied rates of sediment input. Such results indicate that the paleoceanographic conditions in the southern Tethys witnessed the absence of prevalent oceanic anoxia (i.e., the Coniacian-Santonian OAE 3) and deposition of the CORBs as in several parts of the Tethys, the Pacific, and the Indian oceans.
- Organisation(en)
- Institut für Geologie
- Externe Organisation(en)
- Minya University, Core Laboratories N.V., Cairo University
- Journal
- Marine and Petroleum Geology
- Band
- 115
- Anzahl der Seiten
- 18
- ISSN
- 0264-8172
- DOI
- https://doi.org/10.1016/j.marpetgeo.2020.104285
- Publikationsdatum
- 05-2020
- Peer-reviewed
- Ja
- ÖFOS 2012
- 105105 Geochemie, 105121 Sedimentologie
- Schlagwörter
- ASJC Scopus Sachgebiete
- Economic Geology, Geology, Geophysics, Oceanography, Stratigraphy
- Sustainable Development Goals
- SDG 14 – Leben unter Wasser
- Link zum Portal
- https://ucris.univie.ac.at/portal/de/publications/depositional-and-organic-carboncontrolled-regimes-during-the-coniaciansantonian-event(6a78d513-80d1-4485-9ddf-ec760f8509f9).html