Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau

Abstract Understanding methane (CH4) emission from thermokarst lakes is crucial for predicting the impacts of abrupt thaw on the permafrost carbon-climate feedback. However, observational evidence, especially from high-altitude permafrost regions, is still scarce. Here, by combining field surveys, r...

Full description

Bibliographic Details
Published in:Nature Communications
Main Authors: Guibiao Yang, Zhihu Zheng, Benjamin W. Abbott, David Olefeldt, Christian Knoblauch, Yutong Song, Luyao Kang, Shuqi Qin, Yunfeng Peng, Yuanhe Yang
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Q
Ice
Online Access:https://doi.org/10.1038/s41467-023-38907-6
https://doaj.org/article/f0d5208d96cf4cfe904021a1f5fc7e8f
id ftdoajarticles:oai:doaj.org/article:f0d5208d96cf4cfe904021a1f5fc7e8f
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:f0d5208d96cf4cfe904021a1f5fc7e8f 2023-07-02T03:32:33+02:00 Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau Guibiao Yang Zhihu Zheng Benjamin W. Abbott David Olefeldt Christian Knoblauch Yutong Song Luyao Kang Shuqi Qin Yunfeng Peng Yuanhe Yang 2023-05-01T00:00:00Z https://doi.org/10.1038/s41467-023-38907-6 https://doaj.org/article/f0d5208d96cf4cfe904021a1f5fc7e8f EN eng Nature Portfolio https://doi.org/10.1038/s41467-023-38907-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-38907-6 2041-1723 https://doaj.org/article/f0d5208d96cf4cfe904021a1f5fc7e8f Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023) Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41467-023-38907-6 2023-06-11T00:37:29Z Abstract Understanding methane (CH4) emission from thermokarst lakes is crucial for predicting the impacts of abrupt thaw on the permafrost carbon-climate feedback. However, observational evidence, especially from high-altitude permafrost regions, is still scarce. Here, by combining field surveys, radio- and stable-carbon isotopic analyses, and metagenomic sequencing, we present multiple characteristics of CH4 emissions from 120 thermokarst lakes in 30 clusters along a 1100 km transect on the Tibetan Plateau. We find that thermokarst lakes have high CH4 emissions during the ice-free period (13.4 ± 1.5 mmol m−2 d−1; mean ± standard error) across this alpine permafrost region. Ebullition constitutes 84% of CH4 emissions, which are fueled primarily by young carbon decomposition through the hydrogenotrophic pathway. The relative abundances of methanogenic genes correspond to the observed CH4 fluxes. Overall, multiple parameters obtained in this study provide benchmarks for better predicting the strength of permafrost carbon-climate feedback in high-altitude permafrost regions. Article in Journal/Newspaper Ice permafrost Thermokarst Directory of Open Access Journals: DOAJ Articles Nature Communications 14 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Guibiao Yang
Zhihu Zheng
Benjamin W. Abbott
David Olefeldt
Christian Knoblauch
Yutong Song
Luyao Kang
Shuqi Qin
Yunfeng Peng
Yuanhe Yang
Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
topic_facet Science
Q
description Abstract Understanding methane (CH4) emission from thermokarst lakes is crucial for predicting the impacts of abrupt thaw on the permafrost carbon-climate feedback. However, observational evidence, especially from high-altitude permafrost regions, is still scarce. Here, by combining field surveys, radio- and stable-carbon isotopic analyses, and metagenomic sequencing, we present multiple characteristics of CH4 emissions from 120 thermokarst lakes in 30 clusters along a 1100 km transect on the Tibetan Plateau. We find that thermokarst lakes have high CH4 emissions during the ice-free period (13.4 ± 1.5 mmol m−2 d−1; mean ± standard error) across this alpine permafrost region. Ebullition constitutes 84% of CH4 emissions, which are fueled primarily by young carbon decomposition through the hydrogenotrophic pathway. The relative abundances of methanogenic genes correspond to the observed CH4 fluxes. Overall, multiple parameters obtained in this study provide benchmarks for better predicting the strength of permafrost carbon-climate feedback in high-altitude permafrost regions.
format Article in Journal/Newspaper
author Guibiao Yang
Zhihu Zheng
Benjamin W. Abbott
David Olefeldt
Christian Knoblauch
Yutong Song
Luyao Kang
Shuqi Qin
Yunfeng Peng
Yuanhe Yang
author_facet Guibiao Yang
Zhihu Zheng
Benjamin W. Abbott
David Olefeldt
Christian Knoblauch
Yutong Song
Luyao Kang
Shuqi Qin
Yunfeng Peng
Yuanhe Yang
author_sort Guibiao Yang
title Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
title_short Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
title_full Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
title_fullStr Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
title_full_unstemmed Characteristics of methane emissions from alpine thermokarst lakes on the Tibetan Plateau
title_sort characteristics of methane emissions from alpine thermokarst lakes on the tibetan plateau
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41467-023-38907-6
https://doaj.org/article/f0d5208d96cf4cfe904021a1f5fc7e8f
genre Ice
permafrost
Thermokarst
genre_facet Ice
permafrost
Thermokarst
op_source Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023)
op_relation https://doi.org/10.1038/s41467-023-38907-6
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-023-38907-6
2041-1723
https://doaj.org/article/f0d5208d96cf4cfe904021a1f5fc7e8f
op_doi https://doi.org/10.1038/s41467-023-38907-6
container_title Nature Communications
container_volume 14
container_issue 1
_version_ 1770272145136418816