Glacial Southern Ocean deep water Nd isotopic composition dominated by benthic modification

Glacial Southern Ocean deep water Nd isotopic composition dominated by benthic modification

Abstract The deep Southern Ocean (SO) circulation plays a key role in the storage and release of CO2 in Earth’s climate system. The uptake and release of CO2 strongly depend on the redistribution of well and poorly ventilated deep ocean water masses. Recently, evidence was found for possible stronge...

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Bibliographic Details
Main Authors: Moritz Hallmaier, Eva M. Rückert, Yugeng Chen, Jasmin M. Link, Riccardo Lizio, Gerrit Lohmann, Marcus Gutjahr, Norbert Frank
Format: Article
Language:English
Published: Nature Portfolio 2025-01-01
Series:Scientific Reports
Subjects:
Southern Ocean
Ocean circulation
Neodymium isotopes
Benthic flux
Carbon storage
Online Access:https://doi.org/10.1038/s41598-025-86350-y
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https://doi.org/10.1038/s41598-025-86350-y

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