Sediment fluxes dominate glacial–interglacial changes in ocean carbon inventory: results from factorial simulations over the past 780 000 years

<p>Atmospheric CO<span class="inline-formula"><sub>2</sub></span> concentrations varied over ice age cycles due to net exchange fluxes of carbon between land, ocean, marine sediments, lithosphere, and the atmosphere. Marine sediments and polar ice cores archiv...

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Bibliographic Details
Main Authors: M. Adloff, A. Jeltsch-Thömmes, F. Pöppelmeier, T. F. Stocker, F. Joos
Format: Article
Language:English
Published: Copernicus Publications 2025-02-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/21/571/2025/cp-21-571-2025.pdf
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