Millennial variations in atmospheric CO 2 during the early Holocene (11.7–7.4 ka)

• Published in: Climate of the Past
• Main Authors: J. Shin, J. Ahn, J. Chowdhry Beeman, H.-G. Lee, J. M. Seo, E. J. Brook
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Environmental pollution; TD172-193.5; Environmental protection; TD169-171.8; Environmental sciences; GE1-350; Pacific; Siple; Siple Dome; Antarc*; Antarctica; ice core; North Atlantic
• Online Access: https://doi.org/10.5194/cp-18-2063-2022; https://doaj.org/article/033e89919070428da3887f4286f127f3

We present a new high-resolution record of atmospheric CO 2 from the Siple Dome ice core, Antarctica, over the early Holocene (11.7–7.4 ka) that quantifies natural CO 2 variability on millennial timescales under interglacial climate conditions. Atmospheric CO 2 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 CO 2 measurements using better-quality ice cores and carbon cycle models are needed to confirm the observation.