Deep-water corals indicate the Red Sea survived the last glacial lowstand

M Morgan I. Chakraborty (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) A Arash Sharifi (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) F Francesca Benzoni (Red Sea Research Center, King Abdullah University of Science and Technology) F François L. H. Tissot (The Isotoparium, Division of Geological and Planetary Sciences, California Institute of Technology) A Ali Pourmand (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) M Marco Taviani (Istituto di Scienze Marine (CNR-ISMAR)) B Bolton Howes (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) P Peter K. Swart (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) C Choajin Lu (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami) M Mattie Rodrigue (OceanX) S Sam J. Purkis (Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami)

Abstract

The Red Sea, a nascent ocean basin connected to the Indian Ocean via a shallow strait, is assumed to have experienced significant environmental changes during the last glacial period due to a sea-level drop likely exceeding 110 m. This study investigates the hypothesis that hydrodynamic restriction led to severe ecological impacts, including basin-wide extinction due to elevated salinity followed by a short time of oxygen depletion. Uranium–Thorium dating of deep-water corals (DWCs) from 26 northern Red Sea sites reveals coral growth during and after the Last Glacial sea-level lowstand, indicating tolerable seawater chemistry. Additional geochemical data show no significant difference in Red Sea chemistry or temperature between the Latest Pleistocene and Holocene. A meta-analysis of 27 deep-sea cores reveals that while planktonic foraminifera experienced local extinction, other microfossil groups seemingly persisted. These findings suggest that the Red Sea survived the last sea-level lowstand, challenging the paradigm of a complete ecological collapse and providing insights into the resilience of marine ecosystems.

Article Details

Volume / Issue Vol. 122, Issue 8
Published February 25, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (11)

M

Morgan I. Chakraborty

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

A

Arash Sharifi

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

F

Francesca Benzoni

Red Sea Research Center, King Abdullah University of Science and Technology

F

François L. H. Tissot

The Isotoparium, Division of Geological and Planetary Sciences, California Institute of Technology

A

Ali Pourmand

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

M

Marco Taviani

Istituto di Scienze Marine (CNR-ISMAR)

B

Bolton Howes

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

P

Peter K. Swart

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

C

Choajin Lu

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami

M

Mattie Rodrigue

OceanX

S

Sam J. Purkis

Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami