Millennial variations in atmospheric CO2 during the early Holocene (11.7–7.4 ka)

We present a new high-resolution record of atmospheric CO2 from the Siple Dome ice core, Antarctica, over the early Holocene (11.7–7.4 ka) that quantifies natural CO2 variability on millennial timescales under interglacial climate conditions. Atmospheric CO2 decreased by ∼10 ppm between 11.3 and 7.3...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Shin, Jinhwa, Ahn, Jinho, Chowdhry Beeman, Jai, Lee, Hun-Gyu, Seo, Jaemyeong Mango, Brook, Edward J.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
article
Verlagsveröffentlichung
Pacific
Siple
Siple Dome
Antarc*
Antarctica
ice core
North Atlantic
Online Access:https://doi.org/10.5194/cp-18-2063-2022
https://noa.gwlb.de/receive/cop_mods_00062552
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061800/cp-18-2063-2022.pdf
https://cp.copernicus.org/articles/18/2063/2022/cp-18-2063-2022.pdf
Description
Summary:We present a new high-resolution record of atmospheric CO2 from the Siple Dome ice core, Antarctica, over the early Holocene (11.7–7.4 ka) that quantifies natural CO2 variability on millennial timescales under interglacial climate conditions. Atmospheric CO2 decreased by ∼10 ppm between 11.3 and 7.3 ka. The decrease was punctuated by local minima at 11.1, 10.1, 9.1, and 8.3 ka with an amplitude of 2–4 ppm. Although the explanations of carbon cycle mechanisms remain uncertain due to insufficient paleoclimate records and model simulations, these variations correlate with proxies for solar forcing and local climate in the southeast Atlantic polar front, eastern equatorial Pacific, and North Atlantic. Additional CO2 measurements using better-quality ice cores and carbon cycle models are needed to confirm the observation.

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