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题名: In-depth analysis of core methanogenic communities from high elevation permafrost-affected wetlands
作者: Yang, Sizhong1, 2; Liebner, Susanne1; Winkel, Matthias1; Alawi, Mashal1; Horn, Fabian1; Doerfer, Corina3; Ollivier, Julien4; He, Jin-Sheng5, 6; Jin, Huijun2; Kuehn, Peter3; Schloter, Michael4; Scholten, Thomas3; Wagner, Dirk1
刊名: SOIL BIOLOGY & BIOCHEMISTRY
出版日期: 2017-08-01
卷号: 111, 页码:66-77
关键词: Methanogenic archaea ; Wetland ; mcTA gene ; Frozen ground ; Tibetan Plateau ; Biogeography ; Methanoregula
DOI: 10.1016/j.soilbio.2017.03.007
文章类型: Article
英文摘要: The organic carbon of permafrost affected soils is receiving particular attention with respect to its fate and potential feedback to global warming. The structural and activity changes of methanogenic communities in the degrading permafrost-affected wetlands on the Tibetan Plateau can serve as fundamental elements for modelling feedback interaction of ecosystems to climate change. Hence, we aimed at anticipating if and how the rapid environmental changes occurring especially on the high altitude Tibetan platform will affect methanogenic communities. We identified methanogenic community composition, activity and abundance in wetland soils with different hydrological settings, permafrost extent and soil properties and pinpoint the environmental controls. We show that despite a pronounced natural gradient, the Tibetan high elevation wetland soils host a large methanogenic core microbiome. Hydrogenotrophic methanogens, in particular Methanoregula, and H2-dependent methanogenesis were overall dominant although acetoclastic methanogens in addition to hydrogenotrophs were among the dominating taxa in a minerotrophic fen. Tracing the Methanoregula community of the Tibetan Plateau using public databases revealed its global relevance in natural terrestrial habitats. Unlike the composition, the activity and abundance of methanogens varied strongly in the studied soils with higher values in alpine swamps than in alpine meadows. This study indicates that in the course of current wetland and permafrost degradation and the loss in soil moisture, a decrease in the methane production potential is expected on the high Tibetan Plateau but it will not lead to pronounced changes within the methanogenic community structure. (C) 2017 The Authors. Published by Elsevier Ltd.
WOS标题词: Science & Technology ; Life Sciences & Biomedicine
类目[WOS]: Soil Science
研究领域[WOS]: Agriculture
关键词[WOS]: QINGHAI-TIBET PLATEAU ; METHANE EMISSIONS ; MICROBIAL COMMUNITY ; THAWING PERMAFROST ; POLYGONAL TUNDRA ; ZOIGE WETLAND ; LENA DELTA ; PEAT BOG ; CARBON ; ECOSYSTEMS
收录类别: SCI
项目资助者: German Federal Ministry of Education and Research (BMBF)(03G081013 ; Helmholtz Association (HGF)(VH-NG-919) ; 03G0810C ; 03G0810A)
语种: 英语
WOS记录号: WOS:000401877800008
Citation statistics:
内容类型: 期刊论文
URI标识: http://210.75.249.4/handle/363003/7087
Appears in Collections:中国科学院西北高原生物研究所_期刊论文

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作者单位: 1.GFZ German Res Ctr Geosci, Sect Geomicrobiol 5 3, D-14473 Potsdam, Germany
2.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soils Engn, Lanzhou 730000, Peoples R China
3.Univ Tubingen, Dept Geosci, D-72074 Tubingen, Germany
4.Helmholtz Zentrum Munchen, Res Unit Comparat Microbiome Anal, D-85764 Neuherberg, Germany
5.Chinese Acad Sci, Northwest Inst Plateau Biol, Key Lab Adaptat & Evolut Plateau Biota, Xining 810008, Peoples R China
6.Peking Univ, Coll Urban & Environm Sci, Dept Ecol, Beijing 100871, Peoples R China
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