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Sci Rep. 2016 Feb 22;6:21561. doi: 10.1038/srep21561.

Heterotrophic respiration does not acclimate to continuous warming in a subtropical forest.

Wu C1,2,3, Liang N4, Sha L1,2, Xu X5, Zhang Y1,2, Lu H1,3, Song L1, Song Q1, Xie Y6.

Author information

1
Key laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, 666303, China.
2
Ailaoshan Station for Subtropical Forest Ecosystem Studies, Jingdong, 676209, China.
3
University of Chinese Academy of Sciences, Beijing, 100049, China.
4
Global Carbon Cycle Research Section, Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, 305-8506, Japan.
5
Key laboratory of Ecosystem Network Observation and Modelling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.
6
Jingdong Bureau of National Nature Reserve, Jingdong, Yunnan 676209, China.

Abstract

As heterotrophic respiration (R(H)) has great potential to increase atmospheric CO2 concentrations, it is important to understand warming effects on R(H) for a better prediction of carbon-climate feedbacks. However, it remains unclear how R(H) responds to warming in subtropical forests. Here, we carried out trenching alone and trenching with warming treatments to test the climate warming effect on R(H) in a subtropical forest in southwestern China. During the measurement period, warming increased annual soil temperature by 2.1 °C, and increased annual mean R(H) by 22.9%. Warming effect on soil temperature (WE(T)) showed very similar pattern with warming effect on R(H) (WE(RH)), decreasing yearly. Regression analyses suggest that WE(RH) was controlled by WE(T) and also regulated by the soil water content. These results showed that the decrease of WE(RH) was not caused by acclimation to the warmer temperature, but was instead due to decrease of WE(T). We therefore suggest that global warming will accelerate soil carbon efflux to the atmosphere, regulated by the change in soil water content in subtropical forests.

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