1. Effects of warming on carbon emission and microbial abundances across different soil depths of a peatland in the permafrost region under anaerobic condition.
- Author
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Jiang, Lei, Song, Yanyu, Sun, Li, Song, Changchun, Wang, Xianwei, Ma, Xiuyan, Liu, Chao, and Gao, Jinli
- Subjects
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SOIL depth , *PERMAFROST , *MICROBIAL genes , *GLOBAL warming , *CARBON - Abstract
Peatlands in permafrost region are large carbon pools sensitive to global warming. However, the effects of increased temperature on carbon emissions and associated microbial abundances of peatlands under anaerobic condition remain largely unknown, especially when considering depths. For supplementing the deficiency about this, we collected soil from 0 to 150 cm depth of a permafrost peatland in the Great Hing'an Mountain and incubated at 5 and 15 °C for 55 days under anaerobic condition. Soil CO 2 and CH 4 emissions were detected during incubation, and inorganic nitrogen, dissolved organic carbon, and carbon-cycling microbial abundances were analyzed at the end of incubation. Results showed that emission rates and cumulative emissions amount of CO 2 and CH 4 at 15 °C across all soil depths were higher than those observed at 5 °C. Specifically, 0–20 cm and 20–40 cm layers had the highest CO 2 emission rates and cumulative emission amounts, whereas the 40–60 cm and 60–80 cm layers had the highest CH 4 emission rates and cumulative emission amounts. Mean temperature sensitivity (Q 10) values of CO 2 and CH 4 were 2.39 and 55.49 respectively. Q 10 values of bacteria, fungi, archaea, methanogen, and methanotroph abundances were 1.17, 3.85, 1.75, 1.68, and 1.66 respectively, which were calculated by the abundance ratio of microbial functional gene at 15 °C and 5 °C. Similar to the trend of CO 2 emissions, high bacteria, fungi, archaea, methanogen, and methanotroph functional gene abundances were also observed in 0–20 cm and 20–40 cm layers, and such abundances increased along with temperature increasing. In sum, elevated temperature enhances the carbon emission of peatland in permafrost region, and the warming simulated CO 2 emission is linked to the abundances of carbon-cycling microorganisms. • Soil CO 2 and CH 4 emissions at 15 °C are higher than at 5 °C across all soil depths. • Active layer soil has the highest CO 2 emission amounts in permafrost peatland. • CH 4 emissions are highest in the transition layer and its adjacent active layer. • Warming stimulated CO 2 emission is linked to C-cycling related microbial abundance. [ABSTRACT FROM AUTHOR]
- Published
- 2020
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