Matches in SemOpenAlex for { <https://semopenalex.org/work/W2606329532> ?p ?o ?g. }
- W2606329532 endingPage "114" @default.
- W2606329532 startingPage "104" @default.
- W2606329532 abstract "Methane (CH4) oxidation plays a critical role in mitigating global warming. However, the key environmental drivers shaping CH4 oxidation rate at regional and sub-regional scales in grassland ecosystems remain poorly understood. In this study, we collected soils from 21 sites at the regional scale across three steppes of China, including grasslands in Inner Mongolia Plateau (IMP), Xinjiang Autonomous Region (XAR) and Tibetan Plateau (TP). Potential CH4 oxidation rate was measured, and the compositions and abundances of methanotrophs were analyzed by quantitative PCR (qPCR) and Miseq sequencing technique. The factors controlling CH4 oxidation potential at regional and sub-regional scales were evaluated by means of partial least squares path modeling (PLS-PM) and multiple regression on distance matrices (MRM). The results showed that the compositions and abundances of methanotrophs varied at different sub-regions. Type I methanotrophs were predominant in soils from the Inner Mongolia steppe and Xinjiang Autonomous Region, whereas pxmA methanotrophs mainly distributed in the Tibetan alpine steppe soil. Measured environmental variables explained the variations of CH4 oxidation potential well at both regional and sub-regional scales in these Chinese grassland ecosystems. However, the contributions of different variables to CH4 oxidation potential were scale-dependent. At the regional scale, total nitrogen (TN) was the environmental variable that best explained the potential CH4 oxidation rate, and its influence might be mainly associated with its effects on plant growth and methanotrophic community traits. At sub-regional scales, the main controlling variables were total organic carbon (TOC) and soil texture in Inner Mongolia steppe, aridity index (AI) and mean annual temperature (MAT) in Xinjiang Autonomous Region, and TN in Tibetan alpine steppe. These results further suggested that the impacts of environmental variables on CH4 oxidation rate were realized either through their effects on methanotrophic communities, and/or by affecting soil properties in the grassland ecosystems." @default.
- W2606329532 created "2017-04-28" @default.
- W2606329532 creator A5028457946 @default.
- W2606329532 creator A5038146039 @default.
- W2606329532 creator A5041861338 @default.
- W2606329532 creator A5047376512 @default.
- W2606329532 creator A5048774004 @default.
- W2606329532 creator A5059706692 @default.
- W2606329532 creator A5085694379 @default.
- W2606329532 date "2017-08-01" @default.
- W2606329532 modified "2023-10-15" @default.
- W2606329532 title "Scale-dependent key drivers controlling methane oxidation potential in Chinese grassland soils" @default.
- W2606329532 cites W1765708425 @default.
- W2606329532 cites W1799065907 @default.
- W2606329532 cites W1855544175 @default.
- W2606329532 cites W1888548133 @default.
- W2606329532 cites W1898629807 @default.
- W2606329532 cites W1907393055 @default.
- W2606329532 cites W1977380527 @default.
- W2606329532 cites W1985544238 @default.
- W2606329532 cites W1990320472 @default.
- W2606329532 cites W1992313621 @default.
- W2606329532 cites W1993661462 @default.
- W2606329532 cites W1996622455 @default.
- W2606329532 cites W1997976059 @default.
- W2606329532 cites W2002664482 @default.
- W2606329532 cites W2002709469 @default.
- W2606329532 cites W2010115883 @default.
- W2606329532 cites W2015743167 @default.
- W2606329532 cites W2021171178 @default.
- W2606329532 cites W2022364875 @default.
- W2606329532 cites W2042765141 @default.
- W2606329532 cites W2045939163 @default.
- W2606329532 cites W2054107288 @default.
- W2606329532 cites W2057422885 @default.
- W2606329532 cites W2066988911 @default.
- W2606329532 cites W2070734693 @default.
- W2606329532 cites W2072970694 @default.
- W2606329532 cites W2078204332 @default.
- W2606329532 cites W2088090850 @default.
- W2606329532 cites W2094265060 @default.
- W2606329532 cites W2098240442 @default.
- W2606329532 cites W2111989634 @default.
- W2606329532 cites W2112776483 @default.
- W2606329532 cites W2113801249 @default.
- W2606329532 cites W2114163760 @default.
- W2606329532 cites W2115545645 @default.
- W2606329532 cites W2121258973 @default.
- W2606329532 cites W2123416613 @default.
- W2606329532 cites W2124351063 @default.
- W2606329532 cites W2136231645 @default.
- W2606329532 cites W2136312598 @default.
- W2606329532 cites W2137580674 @default.
- W2606329532 cites W2140128739 @default.
- W2606329532 cites W2144668179 @default.
- W2606329532 cites W2147785369 @default.
- W2606329532 cites W2149844070 @default.
- W2606329532 cites W2154418676 @default.
- W2606329532 cites W2154736508 @default.
- W2606329532 cites W2156068910 @default.
- W2606329532 cites W2166687012 @default.
- W2606329532 cites W2166822119 @default.
- W2606329532 cites W2546680399 @default.
- W2606329532 cites W2569075688 @default.
- W2606329532 doi "https://doi.org/10.1016/j.soilbio.2017.04.005" @default.
- W2606329532 hasPublicationYear "2017" @default.
- W2606329532 type Work @default.
- W2606329532 sameAs 2606329532 @default.
- W2606329532 citedByCount "63" @default.
- W2606329532 countsByYear W26063295322018 @default.
- W2606329532 countsByYear W26063295322019 @default.
- W2606329532 countsByYear W26063295322020 @default.
- W2606329532 countsByYear W26063295322021 @default.
- W2606329532 countsByYear W26063295322022 @default.
- W2606329532 countsByYear W26063295322023 @default.
- W2606329532 crossrefType "journal-article" @default.
- W2606329532 hasAuthorship W2606329532A5028457946 @default.
- W2606329532 hasAuthorship W2606329532A5038146039 @default.
- W2606329532 hasAuthorship W2606329532A5041861338 @default.
- W2606329532 hasAuthorship W2606329532A5047376512 @default.
- W2606329532 hasAuthorship W2606329532A5048774004 @default.
- W2606329532 hasAuthorship W2606329532A5059706692 @default.
- W2606329532 hasAuthorship W2606329532A5085694379 @default.
- W2606329532 hasConcept C100970517 @default.
- W2606329532 hasConcept C104577883 @default.
- W2606329532 hasConcept C105895522 @default.
- W2606329532 hasConcept C110872660 @default.
- W2606329532 hasConcept C127313418 @default.
- W2606329532 hasConcept C134306372 @default.
- W2606329532 hasConcept C159390177 @default.
- W2606329532 hasConcept C159750122 @default.
- W2606329532 hasConcept C18903297 @default.
- W2606329532 hasConcept C205649164 @default.
- W2606329532 hasConcept C2775835988 @default.
- W2606329532 hasConcept C2776191655 @default.
- W2606329532 hasConcept C2780030769 @default.
- W2606329532 hasConcept C33923547 @default.
- W2606329532 hasConcept C39432304 @default.