Articles | Volume 17, issue 1
Clim. Past, 17, 507–528, 2021
Clim. Past, 17, 507–528, 2021

Research article 25 Feb 2021

Research article | 25 Feb 2021

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

Shannon A. Bengtson et al.

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Cited articles

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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.