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Publikováno v:
Climate of the Past. 17:1507-1521
During the early part of the last glacial termination (17.2–15 ka) and coincident with a ∼35 ppm rise in atmospheric CO2, a sharp 0.3‰–0.4‰ decline in atmospheric δ13CO2 occurred, potentially constraining the key processes that account for
During the early last glacial termination (17.2–15 ka) atmospheric δ13C declined sharply by 0.3–0.4 ‰ as atmospheric pCO2 rose. This was the initial part of the atmospheric δ13C excursion that lasted for multiple thousand years. A similar δ1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f3e21530aced3e69b61fa8ce3a74f0dc
https://doi.org/10.5194/cp-2020-95
https://doi.org/10.5194/cp-2020-95