The atmospheric bridge communicated the <i>δ</i><sup>13</sup>C decline during the last deglaciation to the global upper ocean

<p>During the early part of the last glacial termination (17.2–15 ka) and coincident with a <span class="inline-formula">∼35</span> ppm rise in atmospheric <span class="inline-formula">CO<sub>2</sub></span>, a sharp 0.3‰–0.4‰ decline in a...

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Bibliographic Details
Main Authors: J. Shao, L. D. Stott, L. Menviel, A. Ridgwell, M. Ödalen, M. Mohtadi
Format: Article
Language:English
Published: Copernicus Publications 2021-07-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/17/1507/2021/cp-17-1507-2021.pdf