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

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 Eart...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: M. P. S. Badger, T. B. Chalk, G. L. Foster, P. R. Bown, S. J. Gibbs, P. F. Sexton, D. N. Schmidt, H. Pälike, A. Mackensen, R. D. Pancost
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
ice core
Online Access:https://doi.org/10.5194/cp-15-539-2019
https://doaj.org/article/05f1c31f9be14e5fadebfcb7cb3466bb
Description
Summary: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 kyr, 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 Pliocene and across a Pleistocene glacial–interglacial cycle at Ocean Drilling Program (ODP) Site 999. 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 .

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