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research article

Half of global methane emissions come from highly variable aquatic ecosystem sources

Rosentreter, Judith A.
•
Borges, Alberto V.
•
Deemer, Bridget R.
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April 5, 2021
Nature Geoscience

Atmospheric methane is a potent greenhouse gas that plays a major role in controlling the Earth’s climate. The causes of the renewed increase of methane concentration since 2007 are uncertain given the multiple sources and complex biogeochemistry. Here, we present a metadata analysis of methane fluxes from all major natural, impacted and human-made aquatic ecosystems. Our revised bottom-up global aquatic methane emissions combine diffusive, ebullitive and/or plant-mediated fluxes from 15 aquatic ecosystems. We emphasize the high variability of methane fluxes within and between aquatic ecosystems and a positively skewed distribution of empirical data, making global estimates sensitive to statistical assumptions and sampling design. We find aquatic ecosystems contribute (median) 41% or (mean) 53% of total global methane emissions from anthropogenic and natural sources. We show that methane emissions increase from natural to impacted aquatic ecosystems and from coastal to freshwater ecosystems. We argue that aquatic emissions will probably increase due to urbanization, eutrophication and positive climate feedbacks and suggest changes in land-use management as potential mitigation strategies to reduce aquatic methane emissions.

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Type
research article
DOI
10.1038/s41561-021-00715-2
Author(s)
Rosentreter, Judith A.
Borges, Alberto V.
Deemer, Bridget R.
Holgerson, Meredith A.
Liu, Shaoda
Song, Chunlin
Melack, John
Raymond, Peter A.
Duarte, Carlos M.
Allen, George H.
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Date Issued

2021-04-05

Published in
Nature Geoscience
Volume

14

Start page

225

End page

230

Subjects

methane emissions

•

global biogeochemistry

•

global change

•

aquatic ecosystems

Editorial or Peer reviewed

REVIEWED

Written at

EPFL

EPFL units
RIVER  
Available on Infoscience
April 6, 2021
Use this identifier to reference this record
https://infoscience.epfl.ch/handle/20.500.14299/177010
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