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• W3020341520 abstract "It is well established that soil microbial communities remain active during much of the Arctic winter, despite soil temperatures that are often well below −10°C 1 . Overwinter microbial activity has important effects on global carbon (C) budgets 2 , nutrient cycling and vegetation community composition 3 . Microbial respiration is highly temperature sensitive in frozen soils, as liquid water and solute availability decrease rapidly with declining temperature 4 . Thus, temperature is considered the ultimate control on overwinter soil microbial activity in the Arctic. Warmer winter soils are thought to yield greater microbial respiration of available C, greater overwinter CO 2 efflux and a flush of nutrients that could be available for plant uptake at thaw 3 . Rising air temperature, combined with changes in timing and/or depth of snowpack development, is leading to warmer Arctic winter soils 5 . Using observational and experimental approaches in the field and in the laboratory, we demonstrate that persistently warm winter soils can lead to labile C starvation of the microbial community and reduced respiration rates, despite the high C content of most arctic soils. If Arctic winter soil temperatures continue to rise, microbial C limitation will reduce cold season CO 2 emissions and alter soil nutrient cycling, if not countered by greater labile C inputs." @default.
• W3020341520 created "2020-05-01" @default.
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• W3020341520 date "2020-04-25" @default.
• W3020341520 modified "2023-09-25" @default.
• W3020341520 title "Labile carbon limits late winter microbial activity near Arctic treeline" @default.
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• W3020341520 doi "https://doi.org/10.1101/2020.04.24.058198" @default.
• W3020341520 hasPublicationYear "2020" @default.
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