1. Terrestrial methane cycle perturbations during the onset of the Paleocene–Eocene Thermal Maximum
- Author
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J. Ian Raine, Erica M. Crouch, Richard D. Pancost, B. David A. Naafs, Elizabeth M. Kennedy, Dominic P. Strogen, Gordon N. Inglis, Megan Rohrssen, and Margaret E. Collinson
- Subjects
Paleontology ,chemistry.chemical_compound ,010504 meteorology & atmospheric sciences ,chemistry ,Carbon isotope excursion ,Geology ,010502 geochemistry & geophysics ,01 natural sciences ,Methane ,0105 earth and related environmental sciences - Abstract
Terrestrial methane (CH 4) emissions may have increased during the Paleocene-Eocene Thermal Maximum (PETM; ca. 56 Ma) and promoted additional warming, especially in the high latitudes. Although there is evidence for increased CH 4 cycling in a single Northern Hemisphere site, whether enhanced methane cycling was globally widespread is unknown because there have been no subsequent investigations. The mechanism of CH4 release is also unknown because a direct comparison between temperature and CH 4 cycling has so far not been possible. Here we use biomarkers to reconstruct temperature change and CH 4 cycling in a new PETM-aged succession in New Zealand. Our results indicate that the stable carbon isotopic composition (δ 13C) of bacterial hopanoids decreased to very low values (−60‰) during the onset of the PETM, indicating enhanced consumption of CH 4. These values are much lower than found in modern wetlands and suggest a major perturbation of the CH 4 cycle during the onset of the PETM. Low hopanoid δ 13C values do not persist into the early Eocene, despite evidence for elevated temperatures. This indicates that the terrestrial CH 4 cycle operates differently during transient compared to gradual warming events. Enhanced CH 4 cycling during the PETM may help to resolve the temperature data-model mismatch in the high latitudes and could yield higher estimates of Earth system sensitivity than expected from CO 2alone.
- Published
- 2021