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Redox evolution and the development of oxygen...
Journal article

Redox evolution and the development of oxygen minimum zones in the Eastern Mediterranean Levantine basin during the early Holocene

Abstract

Oxygen Minimum Zones (OMZs) are expanding in modern oceans due to anthropogenically-driven climate and environmental change. In the Eastern Mediterranean Sea (EMS), OMZs developed in the early Holocene as a result of decreased intermediate water ventilation, increasing temperature, and increased Nile discharge and primary productivity. Here, we report benthic foraminiferal numbers (BFN) and species abundances, together with redox-sensitive …

Authors

Zirks E; Krom M; Schmiedl G; Katz T; Xiong Y; Alcott LJ; Poulton SW; Goodman-Tchernov B

Journal

Geochimica et Cosmochimica Acta, Vol. 297, , pp. 82–100

Publisher

Elsevier

Publication Date

3 2021

DOI

10.1016/j.gca.2021.01.009

ISSN

0016-7037