Thermogenic methane beneath the North Greenland Ice Sheet revealed by isotopic and geological evidence

Glacial meltwater has been increasingly recognised as a potential source of atmospheric methane, yet its origin and variability in the High Arctic remain poorly constrained. In this study, we present measurements of methane concentration and carbon‑isotope composition in meltwater draining the northern Greenland Ice Sheet. Here we show that methane concentrations (12-20 nM) are significantly lower than those reported from other Greenland catchments, despite clear evidence of subglacial input. Isotopic signatures and regional geological context indicate that this methane is predominantly thermogenic, reflecting a geological source that is largely independent of subglacial microbial activity. These findings advance current understanding of methane sources beneath the Greenland Ice Sheet, revealing a thermogenic contribution alongside microbial methane in Arctic methane cycling. In this work we highlight the need to account for geological methane reservoirs when assessing present and future cryosphere-carbon feedbacks.

Authors

Institutions

Publication Details

Journal
Nature Communications
Published
2026-07-24
DOI
https://doi.org/10.1038/s41467-026-75951-4
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Thermogenic methane beneath the North Greenland Ice Sheet revealed by isotopic and geological evidence

Camille Akhoudas, Changxun Yu, Christian Stranne, Martin Jakobsson et al.
Nature Communications
Methane Hydrates and Related Phenomena
article

Thermogenic methane beneath the North Greenland Ice Sheet revealed by isotopic and geological evidence

Camille Akhoudas, Changxun Yu, Christian Stranne, Martin Jakobsson, Wei‐Li Hong, Julie Lattaud, Nina Kirchner, J. Prytherch, Marcelo Ketzer, Henrik Drake, K. Faehnrich, Matt O’Regan, Cheng Chang, M. Sundberg
article en

Abstract

Glacial meltwater has been increasingly recognised as a potential source of atmospheric methane, yet its origin and variability in the High Arctic remain poorly constrained. In this study, we present measurements of methane concentration and carbon‑isotope composition in meltwater draining the northern Greenland Ice Sheet. Here we show that methane concentrations (12-20 nM) are significantly lower than those reported from other Greenland catchments, despite clear evidence of subglacial input. Isotopic signatures and regional geological context indicate that this methane is predominantly thermogenic, reflecting a geological source that is largely independent of subglacial microbial activity. These findings advance current understanding of methane sources beneath the Greenland Ice Sheet, revealing a thermogenic contribution alongside microbial methane in Arctic methane cycling. In this work we highlight the need to account for geological methane reservoirs when assessing present and future cryosphere-carbon feedbacks.

Nature CommunicationsVol. 17(1)
Uppsala University (SE), Stockholm University (SE), Linnaeus University (SE), Bolin Centre for Climate Research (SE), Östersjöcentrum, The University of Adelaide (AU)
Polarforskningssekretariatet, Rolex, Svenska Forskningsrådet Formas, Crafoordska Stiftelsen, Vetenskapsrådet, Australian Research Council
Life below water
Openalex Percentile: Top 15%
Methane Hydrates and Related Phenomena
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.