Temperature, soil moisture, and microbial controls on CO2 and CH4 emissions from a permafrost peatland. Issue 5 (14th June 2021)

• Record Type: Journal Article
• Authors: Song, Yanyu; Song, Changchun; Hou, Aixin; Sun, Li; Wang, Xianwei; Ma, Xiuyan; Jiang, Lei; Liu, Chao; Gao, Jinli
• Is Part Of: Environmental progress & sustainable energy. Volume 40:Issue 5(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-06-14
• Subjects: carbon cycling -- climate warming -- greenhouse gasses -- methane -- microbial mechanism; Environmental engineering -- Periodicals; Sustainable engineering -- Periodicals; Environmental chemistry -- Periodicals; 333.7
• DOI: 10.1002/ep.13693
• Languages: English
• ISSNs: 1944-7442

Abstract

Abstract: Peatlands are significant carbon dioxide (CO2 ) sinks and methane (CH4 ) sources. In this study, we investigated changes in CO2 and CH4 emissions from topsoil (0–20 cm) to subsoil (20–40 cm) in a permafrost peatland, and the related soil microbial abundance in response to increasing temperature and soil water content by using an incubation experiment. Our results indicated that CO2 and CH4 emissions from the permafrost peatland are highly sensitive to temperature and soil water content. CO2 emissions from topsoil and subsoil at 15°C were 3.36 and 2.74 times larger, respectively, compared to those at 5°C under the field moisture condition, and were 1.70 times larger under the waterlogged treatment in both topsoil and subsoil. CH4 emissions from 0–20 to 20–40 cm soils at 15°C were 34 and 83 times larger, respectively, than those at 5°C under the original state and 17 and 32 times larger under the waterlogged treatment. These results indicated that CH4 emissions are more sensitive than CO2 emissions, and waterlogged conditions could decrease temperature sensitivity of CO2 and CH4 emissions. Microbial analyses showed that the cumulative emissions amount of CO2 positively correlated with bacterial, fungal, and methanotroph abundances. Positive relationships were observed between CH4 emissions and abundances of bacteria, fungi, and archaea. These findings suggested that changes in temperature and water content alter CO2 and CH4 emissions from permafrost peatlands through controlling abundances of soil bacteria, fungi, archaea, and methanotrophs. These variables bear importance in accurately estimating C emissions from permafrost peatlands.