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Responses of soil respiration to experimental warming in an alpine steppe on the Tibetan Plateau

Bibliographic Data

ID15550335
AuthorsGuanqin Wang (0000-0003-2135-0993, Chinese Academy of Sciences), Fei Li (0009-0006-1479-2821, Chinese Academy of Sciences), Yunfeng Peng (0000-0002-4151-4206, Chinese Academy of Sciences), Jianchun Yu (0000-0002-8250-7475, Chinese Academy of Sciences), Dianye Zhang (0000-0002-1741-1135, Chinese Academy of Sciences), Guibiao Yang (Chinese Academy of Sciences, corresponding author), Kai Fang (0000-0003-2017-7092, Chinese Academy of Sciences), Jun Wang (0000-0003-4485-7201, Chinese Academy of Sciences), Anwar Mohammat (0000-0003-4437-877X, Chinese Academy of Sciences), Guoying Zhou (0000-0003-2485-6172, Chinese Academy of Sciences), Yuanhe Yang (0000-0002-5399-4606, Chinese Academy of Sciences, corresponding author)
Year2019
Volume14
Issue9
Pages094015-094015
Publication date2019-08-15
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab3bbc
OpenAlexW2966911599
LanguageEN
Citations received1
References cited52

High-latitude and high-altitude ecosystems store large amounts of carbon (C) and play a vital role in the global C cycle. Soil respiration ( R S ) in these ecosystems is believed to be extremely sensitive to climate warming and could potentially trigger positive C-climate feedback. However, this evidence is largely derived from wet ecosystems, with limited observations from dry ecosystems. Here, we explored the responses of R S , autotrophic ( R A ), and heterotrophic ( R H ) respiration under experimental warming in a dry ecosystem, an alpine steppe on the Tibetan Plateau. We assessed the effects of soil temperature and moisture dynamics on R S , R A, and R H and performed a meta-analysis to examine whether the warming effects observed were similar to those reported in wet ecosystems, including Tibetan alpine meadow and arctic ecosystem. Experimental warming did not alter R S , R A, and R H in this alpine steppe, likely because decreased soil moisture constrained positive warming effects. In contrast, the meta-analysis revealed that R S exhibited a significant increase under experimental warming in both the Tibetan alpine meadow and arctic wet tundra. These results demonstrate that R S exhibits different responses to climate warming between dry and wet ecosystems, suggesting potential more complex C-climate feedback in cold regions

Atmospheric sciences · Biology · Climate change · Ecosystem · Ecosystem respiration · Global warming · Plateau (mathematics · Primary production · Steppe · Terrestrial ecosystem · Tundra · Climate change and permafrost · Cryospheric studies and observations · Environmental Science · Peatlands and Wetlands Ecology · Ecology · Geology

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Unique citing works1
Citations per year0,33
Citation span2023 - 2023 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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