Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-507-2021
https://doi.org/10.5194/cp-17-507-2021
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25 Feb 2021
Research article | Highlight paper |  | 25 Feb 2021

Lower oceanic δ13C during the last interglacial period compared to the Holocene

Shannon A. Bengtson, Laurie C. Menviel, Katrin J. Meissner, Lise Missiaen, Carlye D. Peterson, Lorraine E. Lisiecki, and Fortunat Joos

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Short summary
The last interglacial was a warm period that may provide insights into future climates. Here, we compile and analyse stable carbon isotope data from the ocean during the last interglacial and compare it to the Holocene. The data show that Atlantic Ocean circulation was similar during the last interglacial and the Holocene. We also establish a difference in the mean oceanic carbon isotopic ratio between these periods, which was most likely caused by burial and weathering carbon fluxes.