Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon

Abstract Warming is altering the way soils function in ecosystems both directly by changing microbial physiology and indirectly by causing shifts in microbial community composition. Some of these warming‐driven changes are short term, but others may persist over time. Here, we took advantage of a lo...

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Main Authors: Katharine L. Stuble, Shuang Ma, Junyi Liang, Yiqi Luo, Aimée T. Classen, Lara Souza
Format: Article
Language:English
Published: Wiley 2019-05-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1002/ecs2.2715
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author Katharine L. Stuble
Shuang Ma
Junyi Liang
Yiqi Luo
Aimée T. Classen
Lara Souza
author_facet Katharine L. Stuble
Shuang Ma
Junyi Liang
Yiqi Luo
Aimée T. Classen
Lara Souza
author_sort Katharine L. Stuble
collection DOAJ
description Abstract Warming is altering the way soils function in ecosystems both directly by changing microbial physiology and indirectly by causing shifts in microbial community composition. Some of these warming‐driven changes are short term, but others may persist over time. Here, we took advantage of a long‐term (14 yr) warming experiment in a tallgrass prairie to tease apart the influence of short‐ and long‐term warming on litter decomposition. We collected soils originating from warmed and control plots and incubated them with a common litter substrate in a reciprocal design under elevated and ambient growth chamber temperatures. Litter decomposition was 40% higher in soils that were warmed in the field for 14 yr (long‐term warming) relative to soils derived from ambient plots. Short‐term warming in the laboratory had less of an impact on decomposition—decomposition increased by 12% under laboratory warming. Using a two‐pool soil carbon model to explore how different carbon pools may be responding, we found that long‐term warming accelerated the turnover of labile, not recalcitrant, carbon in these prairie soils—a result that is likely due to shifts in soil community activity/composition. Taken together, our results offer experimental evidence that warming‐induced changes in the soil community that occur over 14 yr of warming have long‐lasting effects on carbon turnover.
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spelling doaj.art-dec93ab93ba543b3bc2c0b8d1fee2bb92022-12-22T01:29:17ZengWileyEcosphere2150-89252019-05-01105n/an/a10.1002/ecs2.2715Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbonKatharine L. Stuble0Shuang Ma1Junyi Liang2Yiqi Luo3Aimée T. Classen4Lara Souza5The Holden Arboretum Kirtland Ohio 44094 USADepartment of Biological Sciences Northern Arizona University Flagstaff Arizona 86011 USADepartment of Microbiology and Plant Biology University of Oklahoma Norman Ohio 73019 USADepartment of Biological Sciences Northern Arizona University Flagstaff Arizona 86011 USARubenstein School of Environment and Natural Resources University of Vermont Burlington Vermont 05405 USAThe Oklahoma Biological Survey Norman Oklahoma 73019 USAAbstract Warming is altering the way soils function in ecosystems both directly by changing microbial physiology and indirectly by causing shifts in microbial community composition. Some of these warming‐driven changes are short term, but others may persist over time. Here, we took advantage of a long‐term (14 yr) warming experiment in a tallgrass prairie to tease apart the influence of short‐ and long‐term warming on litter decomposition. We collected soils originating from warmed and control plots and incubated them with a common litter substrate in a reciprocal design under elevated and ambient growth chamber temperatures. Litter decomposition was 40% higher in soils that were warmed in the field for 14 yr (long‐term warming) relative to soils derived from ambient plots. Short‐term warming in the laboratory had less of an impact on decomposition—decomposition increased by 12% under laboratory warming. Using a two‐pool soil carbon model to explore how different carbon pools may be responding, we found that long‐term warming accelerated the turnover of labile, not recalcitrant, carbon in these prairie soils—a result that is likely due to shifts in soil community activity/composition. Taken together, our results offer experimental evidence that warming‐induced changes in the soil community that occur over 14 yr of warming have long‐lasting effects on carbon turnover.https://doi.org/10.1002/ecs2.2715carbon turn overclimate changedecompositiondirect and indirect effectsmicrobial activitymicrobial composition
spellingShingle Katharine L. Stuble
Shuang Ma
Junyi Liang
Yiqi Luo
Aimée T. Classen
Lara Souza
Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
Ecosphere
carbon turn over
climate change
decomposition
direct and indirect effects
microbial activity
microbial composition
title Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
title_full Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
title_fullStr Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
title_full_unstemmed Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
title_short Long‐term impacts of warming drive decomposition and accelerate the turnover of labile, not recalcitrant, carbon
title_sort long term impacts of warming drive decomposition and accelerate the turnover of labile not recalcitrant carbon
topic carbon turn over
climate change
decomposition
direct and indirect effects
microbial activity
microbial composition
url https://doi.org/10.1002/ecs2.2715
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