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Journal Abstract Search

325 related items for PubMed ID: 27590882

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  • 3. Temperature sensitivity of SOM decomposition is linked with a K-selected microbial community.
    Li H, Yang S, Semenov MV, Yao F, Ye J, Bu R, Ma R, Lin J, Kurganova I, Wang X, Deng Y, Kravchenko I, Jiang Y, Kuzyakov Y.
    Glob Chang Biol; 2021 Jun; 27(12):2763-2779. PubMed ID: 33709545
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  • 6. Warming enhances old organic carbon decomposition through altering functional microbial communities.
    Cheng L, Zhang N, Yuan M, Xiao J, Qin Y, Deng Y, Tu Q, Xue K, Van Nostrand JD, Wu L, He Z, Zhou X, Leigh MB, Konstantinidis KT, Schuur EA, Luo Y, Tiedje JM, Zhou J.
    ISME J; 2017 Aug; 11(8):1825-1835. PubMed ID: 28430189
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  • 7. Temperature-dependent shift from labile to recalcitrant carbon sources of arctic heterotrophs.
    Biasi C, Rusalimova O, Meyer H, Kaiser C, Wanek W, Barsukov P, Junger H, Richter A.
    Rapid Commun Mass Spectrom; 2005 Aug; 19(11):1401-8. PubMed ID: 15880633
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  • 12. Similar response of labile and resistant soil organic matter pools to changes in temperature.
    Fang C, Smith P, Moncrieff JB, Smith JU.
    Nature; 2005 Jan 06; 433(7021):57-9. PubMed ID: 15635408
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  • 16. Molecular-level methods for monitoring soil organic matter responses to global climate change.
    Feng X, Simpson MJ.
    J Environ Monit; 2011 May 06; 13(5):1246-54. PubMed ID: 21416081
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  • 19. Warming and increased precipitation indirectly affect the composition and turnover of labile-fraction soil organic matter by directly affecting vegetation and microorganisms.
    Chen Q, Niu B, Hu Y, Luo T, Zhang G.
    Sci Total Environ; 2020 Apr 20; 714():136787. PubMed ID: 31982765
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