Temperature sensitivity of soil respiration rates enhanced by microbial community response

dc.contributor.author
Karhu, Kristiina
dc.contributor.author
Auffret, Marc D.
dc.contributor.author
Dungait, Jennifer A. J.
dc.contributor.author
Hopkins, David W.
dc.contributor.author
Prosser, James I.
dc.contributor.author
Singh, Brajesh K.
dc.contributor.author
Subke, Jens-Arne
dc.contributor.author
Wookey, Philip A.
dc.contributor.author
Ågren, Göran I.
dc.contributor.author
Sebastià, Ma. T.
dc.contributor.author
Gouriveau, Fabrice
dc.contributor.author
Bergkvist, Göran
dc.contributor.author
Meir, Patrick
dc.contributor.author
Nottingham, Andrew T.
dc.contributor.author
Salinas, Norma
dc.contributor.author
Hartley, Iain P.
dc.date.accessioned
2024-12-05T21:52:05Z
dc.date.available
2024-12-05T21:52:05Z
dc.date.issued
2020-11-16T13:22:59Z
dc.date.issued
2020-11-16T13:22:59Z
dc.date.issued
2014-09-03
dc.identifier
https://doi.org/10.1038/nature13604
dc.identifier
1476-4687
dc.identifier
http://hdl.handle.net/10459.1/69886
dc.identifier.uri
http://hdl.handle.net/10459.1/69886
dc.description.abstract
Soils store about four times as much carbon as plant biomass1, and soil microbial respiration releases about 60 petagrams of carbon per year to the atmosphere as carbon dioxide2. Short-term experiments have shown that soil microbial respiration increases exponentially with temperature3. This information has been incorporated into soil carbon and Earth-system models, which suggest that warming-induced increases in carbon dioxide release from soils represent an important positive feedback loop that could influence twenty-first-century climate change4. The magnitude of this feedback remains uncertain, however, not least because the response of soil microbial communities to changing temperatures has the potential to either decrease5,6,7 or increase8,9 warming-induced carbon losses substantially. Here we collect soils from different ecosystems along a climate gradient from the Arctic to the Amazon and investigate how microbial community-level responses control the temperature sensitivity of soil respiration. We find that the microbial community-level response more often enhances than reduces the mid- to long-term (90 days) temperature sensitivity of respiration. Furthermore, the strongest enhancing responses were observed in soils with high carbon-to-nitrogen ratios and in soils from cold climatic regions. After 90 days, microbial community responses increased the temperature sensitivity of respiration in high-latitude soils by a factor of 1.4 compared to the instantaneous temperature response. This suggests that the substantial carbon stores in Arctic and boreal soils could be more vulnerable to climate warming than currently predicted.
dc.description.abstract
This work was carried out with Natural Environment Research Council (NERC) funding (grant number NE/H022333/1). K.K. was supported by an Academy of Finland post-doctoral research grant while finalizing this manuscript. P.M. was supported by ARC FT110100457 and NERC NE/G018278/1, and B.K.S by the Grain Research and Development Corporation and ARC DP130104841.
dc.language
eng
dc.publisher
Springer Nature
dc.relation
Versió preprint del document publicat a: https://doi.org/10.1038/nature13604
dc.relation
Nature, 2014, vol. 513, p. 81-84
dc.rights
(c) Nature Publishing Group, a division of Macmillan Publishers Limited, 2014
dc.rights
info:eu-repo/semantics/openAccess
dc.subject
Biogeochemistry
dc.subject
Climate-change ecology
dc.title
Temperature sensitivity of soil respiration rates enhanced by microbial community response
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/submittedVersion


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