UGC Approved Journal no 63975(19)
New UGC Peer-Reviewed Rules

ISSN: 2349-5162 | ESTD Year : 2014
Volume 12 | Issue 10 | October 2025

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Published in:

Volume 12 Issue 3
March-2025
eISSN: 2349-5162

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Published Paper ID:
JETIR2503121


Registration ID:
556371

Page Number

b173-b200

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Title

CHARACTERIZATION OF LOWEST OXYGEN ENVIRONMENTS WITHIN ANCIENT UPWELLING ENVIRONMENTS: A CASE STUDY FROM THE CAMPANIAN-MAASTRICHTIAN AT WEST-CENTRAL SINAI, EGYPT

Abstract

The Late Cretaceous Period was characterized by nutrient-rich conditions driven by intense coastal upwelling. This upwelling system, fueled by strong coastal winds, particularly during the Maastrichtian, elevated nutrient levels in surface waters, as evidenced by geochemical proxies and benthic foraminiferal data. Benthic foraminifera, widely used as indicators of past ocean depths and depositional environments, were studied in the Campanian-Maastrichtian (C-M) marine rocks of the Sudr Formation from the Gabal Nezazzat section (west-central Sinai, Egypt). Nine planktonic foraminiferal zones are recorded through the Nezzazat section, ranging from CF9 to CF1. A total of 71 samples, comprising 69 species across 35 genera, were analyzed to infer species diversity, interrelationships, and changes in palaeo-environmental conditions, palaeo-oxygenation, palaeo-productivity, and palaeo-depth within the C-M successions. The Campanian deposits were formed in outer neritic to upper bathyal environments (201.6–539.84 m), characterized by low organic matter flux (HOFS: 4.5% to 9%), low total organic carbon (TOC < 3), and well-oxygenated conditions (BFOI: 33.3 to 67.3; oxic >0.3 mL/L O₂). The transition from the Campanian to the Maastrichtian occurred in outer neritic to deeper bathyal settings, maintaining low productivity and well-oxygenated conditions. Early Maastrichtian deposits indicate shallower depositional environments (113.5–479.75 m) with reduced oxygen availability at the seafloor (BFOI: 40–60; dysoxic 0.1–0.3 mL/L O₂), associated with increased organic matter flux and higher TOC values (>4). These conditions deepened through the late Maastrichtian, with upwelling-driven nutrient enrichment persisting throughout the period

Key Words

low-oxygen, Campanian-Maastrichtian, Gebel Nazzazat, Sinai, Benthic foraminiferal

Cite This Article

"CHARACTERIZATION OF LOWEST OXYGEN ENVIRONMENTS WITHIN ANCIENT UPWELLING ENVIRONMENTS: A CASE STUDY FROM THE CAMPANIAN-MAASTRICHTIAN AT WEST-CENTRAL SINAI, EGYPT", International Journal of Emerging Technologies and Innovative Research (www.jetir.org), ISSN:2349-5162, Vol.12, Issue 3, page no.b173-b200, March-2025, Available :http://www.jetir.org/papers/JETIR2503121.pdf

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2349-5162 | Impact Factor 7.95 Calculate by Google Scholar

An International Scholarly Open Access Journal, Peer-Reviewed, Refereed Journal Impact Factor 7.95 Calculate by Google Scholar and Semantic Scholar | AI-Powered Research Tool, Multidisciplinary, Monthly, Multilanguage Journal Indexing in All Major Database & Metadata, Citation Generator

Cite This Article

"CHARACTERIZATION OF LOWEST OXYGEN ENVIRONMENTS WITHIN ANCIENT UPWELLING ENVIRONMENTS: A CASE STUDY FROM THE CAMPANIAN-MAASTRICHTIAN AT WEST-CENTRAL SINAI, EGYPT", International Journal of Emerging Technologies and Innovative Research (www.jetir.org | UGC and issn Approved), ISSN:2349-5162, Vol.12, Issue 3, page no. ppb173-b200, March-2025, Available at : http://www.jetir.org/papers/JETIR2503121.pdf

Publication Details

Published Paper ID: JETIR2503121
Registration ID: 556371
Published In: Volume 12 | Issue 3 | Year March-2025
DOI (Digital Object Identifier):
Page No: b173-b200
Country: Suez, Suez, Egypt .
Area: Science
ISSN Number: 2349-5162
Publisher: IJ Publication


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