Insensitivity of alkenone carbon isotopes to atmospheric CO 2 at low to moderate CO 2 levels

• Published in: Climate of the Past
• Main Authors: Badger, Marcus, Chalk, Thomas B, Foster, Gavin L, Bown, Paul R, Gibbs, Samantha J, Sexton, Philip, Schmidt, Daniela N, Pälike, Heiko, Mackensen, A, Pancost, Richard D
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2019
• Subjects: ice core
• Online Access: https://oro.open.ac.uk/57510/; https://oro.open.ac.uk/57510/1/cp-2018-152.pdf; https://oro.open.ac.uk/57510/8/57510FINAL.pdf; https://doi.org/10.5194/cp-15-539-2019

Atmospheric p CO 2 is a critical component of the global carbon system and is considered to be the major control of Earth’s past, present and future climate. Accurate and precise reconstructions of its concentration through geological time are, therefore, crucial to our understanding of the Earth system. Ice core records document p CO 2 for the past 800 kyrs, but at no point during this interval were CO 2 levels higher than today. Interpretation of older p CO 2 has been hampered by discrepancies during some time intervals between two of the main ocean-based proxy methods used to reconstruct p CO 2 : the carbon isotope fractionation that occurs during photosynthesis as recorded by haptophyte biomarkers (alkenones) and the boron isotope composition (δ 11 B) of foraminifer shells. Here we present alkenone and δ 11 B-based p CO 2 reconstructions generated from the same samples from the Plio-Pleistocene at ODP Site 999 across a glacial-interglacial cycle. We find a muted response to p CO 2 in the alkenone record compared to contemporaneous ice core and δ 11 B records, suggesting caution in the interpretation of alkenone-based records at low p CO 2 levels. This is possibly caused by the physiology of CO 2 uptake in the haptophytes. Our new understanding resolves some of the inconsistencies between the proxies and highlights that caution may be required when interpreting alkenone-based reconstructions of p CO 2 .