Atmospheric methane lifetime during the Last Glacial Maximum was reduced owing to dust-mediated chlorine chemistry

Atmospheric methane (CH 4 ) plays a central role in Earth’s climate, yet the drivers of its decline during the high-dust conditions of glacial periods, such as the Last Glacial Maximum (LGM), remain uncertain. Previous explanations imply source-driven changes, assuming an atmospheric lifetime comparable to that of present day. Recent work shows that interactions between mineral dust and sea salt aerosols produce CH 4 -removing chlorine radicals. In this work, we show that during the LGM, CH 4 lifetime shortened to 7.8 years, 20% lower than that of present day. Chlorine contributed ~15% of global CH 4 loss, fourfold that of present day. Our results reproduce ice core CH 4 isotopic evidence, demonstrating that stronger-than-assumed atmospheric sinks can explain CH 4 variability without invoking substantial source changes, highlighting the overlooked role of chlorine chemistry in the glacial CH 4 budget.

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Publication Details

Journal
Science
Published
2026-09-17
DOI
https://doi.org/10.1126/science.aec4071
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

Atmospheric methane lifetime during the Last Glacial Maximum was reduced owing to dust-mediated chlorine chemistry

Nicolás J. Cosentino, Juan Pablo Corella, Rafael P. Fernández, Samuel Albani et al.
Science
Atmospheric chemistry and aerosols
article

Atmospheric methane lifetime during the Last Glacial Maximum was reduced owing to dust-mediated chlorine chemistry

Nicolás J. Cosentino, Juan Pablo Corella, Rafael P. Fernández, Samuel Albani, Carlos A. Cuevas, Alfonso Saiz‐Lopez, Jennifer Campos Ayala, N. M. Mahowald, Markus Grimmer, Michaela Mühl, Andrea Spolaor, J. H. M. M. Schmitt, Julián Villamayor, Daphne Meidan, Hubertus Fischer
article en

Abstract

Atmospheric methane (CH 4 ) plays a central role in Earth’s climate, yet the drivers of its decline during the high-dust conditions of glacial periods, such as the Last Glacial Maximum (LGM), remain uncertain. Previous explanations imply source-driven changes, assuming an atmospheric lifetime comparable to that of present day. Recent work shows that interactions between mineral dust and sea salt aerosols produce CH 4 -removing chlorine radicals. In this work, we show that during the LGM, CH 4 lifetime shortened to 7.8 years, 20% lower than that of present day. Chlorine contributed ~15% of global CH 4 loss, fourfold that of present day. Our results reproduce ice core CH 4 isotopic evidence, demonstrating that stronger-than-assumed atmospheric sinks can explain CH 4 variability without invoking substantial source changes, highlighting the overlooked role of chlorine chemistry in the glacial CH 4 budget.

ScienceVol. 393(6817)
Institut polytechnique de Grenoble (FR), University of Bern (CH), Centre National de la Recherche Scientifique (FR), Oeschger Centre for Climate Change Research (CH), Consejo Nacional de Investigaciones Científicas y Técnicas (AR), Cornell University (US), Instituto Interdisciplinario de Ciencias Básicas (AR), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Museo Nacional de Ciencias Naturales (ES), Institut des Géosciences de l'Environnement (FR), Institute of Astronomy and Space Physics (AR), Instituto Franco-Argentino sobre Estudios de Clima y sus Impactos (AR), National Research Council (IT), Institut de Recherche pour le Développement (FR), University of Milano-Bicocca (IT), Université Grenoble Alpes (FR)
Association du Syndrome de Lowe, Svensk Njurmedicinsk Förening, Deutsches Museum
Life below water
Openalex Percentile: Top 15%
Atmospheric chemistry and aerosols
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