Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China

Methane (CH<sub>4</sub>) emission and environmental controls of CH<sub>4</sub>-cycling microorganisms are unclear in inland floodplains. Here, we examined soil CH<sub>4</sub> emissions and the community composition of CH<sub>4</sub>-cycling microorgani...

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Main Authors: Yijie Ren, Lianlian Zhu, Zhengmiao Deng, Yonghong Xie, Chengyi Zhang, Fengjin Xiao, Xinsheng Chen, Feng Li, Yeai Zou, Rong Sheng, Xiaoyan Zhang, Xian Chen
Format: Article
Language:English
Published: MDPI AG 2020-09-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/9/997
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author Yijie Ren
Lianlian Zhu
Zhengmiao Deng
Yonghong Xie
Chengyi Zhang
Fengjin Xiao
Xinsheng Chen
Feng Li
Yeai Zou
Rong Sheng
Xiaoyan Zhang
Xian Chen
author_facet Yijie Ren
Lianlian Zhu
Zhengmiao Deng
Yonghong Xie
Chengyi Zhang
Fengjin Xiao
Xinsheng Chen
Feng Li
Yeai Zou
Rong Sheng
Xiaoyan Zhang
Xian Chen
author_sort Yijie Ren
collection DOAJ
description Methane (CH<sub>4</sub>) emission and environmental controls of CH<sub>4</sub>-cycling microorganisms are unclear in inland floodplains. Here, we examined soil CH<sub>4</sub> emissions and the community composition of CH<sub>4</sub>-cycling microorganisms under three vegetation types—mudflat (MF, no vegetation cover), <i>Carex</i> meadow (CM, mainly <i>Carex brevicuspis</i>), and reed land (RL, mainly <i>Miscanthus sacchariflorus</i>)—from water-adjacent areas to higher-elevation land in the Dongting Lake floodplain, China. The results showed that CH<sub>4</sub> emission is the highest in CM, while significant absorption was observed in the RL site. The abundance ratio of methanogen/methanotroph was the highest in CM, intermediate in MF, and lowest in RL. The <i>Methanosarcinaceae</i> family represented the dominant methanogens in the three sampling sites (41.32–75.25%). The genus <i>Methylocystis</i> (60.85%, type II methanotrophs) was dominant in CM, while <i>Methylobacter</i> and <i>Methylosarcina</i> (type I methanotrophs) were the dominant genera in MF (51.00%) and RL (50.24%), respectively. Structural equation model analysis showed that methanogen and methanotroph abundance were affected by water table depth, soil water content, and pH indirectly through soil organic content, total nitrogen, microbial biomass carbon, and microbial biomass nitrogen. These results indicated that the Dongting Lake floodplain may change from a CH<sub>4</sub> source to a CH<sub>4</sub> sink with vegetation succession with an increase in elevation, and the methanogen/methanotroph ratio can be used as a proxy for CH<sub>4</sub> emission in wetland soils. The continuous increase in reed area combined with the decrease in <i>Carex</i> meadow may mitigate CH<sub>4</sub> emission and enhance the CH<sub>4</sub> sink function during the non-flood season in the Dongting Lake floodplain.
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spelling doaj.art-43cd6db7caa344da9b6dba576fc0ecdf2023-11-20T14:08:26ZengMDPI AGAtmosphere2073-44332020-09-0111999710.3390/atmos11090997Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, ChinaYijie Ren0Lianlian Zhu1Zhengmiao Deng2Yonghong Xie3Chengyi Zhang4Fengjin Xiao5Xinsheng Chen6Feng Li7Yeai Zou8Rong Sheng9Xiaoyan Zhang10Xian Chen11Key Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaNational Climate Center, China Meteorological Administration, Beijing 100081, ChinaNational Climate Center, China Meteorological Administration, Beijing 100081, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaKey Laboratory of Agro-ecological Processes in Subtropical Region, The Chinese Academy of Sciences, Changsha 410125, ChinaSchool of Agriculture, Sun Yat-sen University, Guangzhou 510275, ChinaHunan Research Center of Agricultural Microorganism Engineering Technology, Hunan Institute of Microbiology, Changsha 410009, ChinaMethane (CH<sub>4</sub>) emission and environmental controls of CH<sub>4</sub>-cycling microorganisms are unclear in inland floodplains. Here, we examined soil CH<sub>4</sub> emissions and the community composition of CH<sub>4</sub>-cycling microorganisms under three vegetation types—mudflat (MF, no vegetation cover), <i>Carex</i> meadow (CM, mainly <i>Carex brevicuspis</i>), and reed land (RL, mainly <i>Miscanthus sacchariflorus</i>)—from water-adjacent areas to higher-elevation land in the Dongting Lake floodplain, China. The results showed that CH<sub>4</sub> emission is the highest in CM, while significant absorption was observed in the RL site. The abundance ratio of methanogen/methanotroph was the highest in CM, intermediate in MF, and lowest in RL. The <i>Methanosarcinaceae</i> family represented the dominant methanogens in the three sampling sites (41.32–75.25%). The genus <i>Methylocystis</i> (60.85%, type II methanotrophs) was dominant in CM, while <i>Methylobacter</i> and <i>Methylosarcina</i> (type I methanotrophs) were the dominant genera in MF (51.00%) and RL (50.24%), respectively. Structural equation model analysis showed that methanogen and methanotroph abundance were affected by water table depth, soil water content, and pH indirectly through soil organic content, total nitrogen, microbial biomass carbon, and microbial biomass nitrogen. These results indicated that the Dongting Lake floodplain may change from a CH<sub>4</sub> source to a CH<sub>4</sub> sink with vegetation succession with an increase in elevation, and the methanogen/methanotroph ratio can be used as a proxy for CH<sub>4</sub> emission in wetland soils. The continuous increase in reed area combined with the decrease in <i>Carex</i> meadow may mitigate CH<sub>4</sub> emission and enhance the CH<sub>4</sub> sink function during the non-flood season in the Dongting Lake floodplain.https://www.mdpi.com/2073-4433/11/9/997methanotrophmethanogenDongting Lake floodplainvegetation typemethane flux
spellingShingle Yijie Ren
Lianlian Zhu
Zhengmiao Deng
Yonghong Xie
Chengyi Zhang
Fengjin Xiao
Xinsheng Chen
Feng Li
Yeai Zou
Rong Sheng
Xiaoyan Zhang
Xian Chen
Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
Atmosphere
methanotroph
methanogen
Dongting Lake floodplain
vegetation type
methane flux
title Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
title_full Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
title_fullStr Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
title_full_unstemmed Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
title_short Changes in Methane Emission and Community Composition of Methane-Cycling Microorganisms Along an Elevation Gradient in the Dongting Lake Floodplain, China
title_sort changes in methane emission and community composition of methane cycling microorganisms along an elevation gradient in the dongting lake floodplain china
topic methanotroph
methanogen
Dongting Lake floodplain
vegetation type
methane flux
url https://www.mdpi.com/2073-4433/11/9/997
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