Data from: The influence of soil communities on the temperature sensitivity of soil respiration

Soil respiration represents a major carbon flux between terrestrial ecosystems and the atmosphere, and is expected to accelerate under climate warming. Despite its importance in climate change forecasts, however, our understanding of the effects of temperature on soil respiration (RS) is incomplete....

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Main Authors: Johnston, Alice S.A., Sibly, Richard M.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/10255/dryad.187174
https://doi.org/10.5061/dryad.416kv03
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spelling ftdryad:oai:v1.datadryad.org:10255/dryad.187174 2023-05-15T18:40:07+02:00 Data from: The influence of soil communities on the temperature sensitivity of soil respiration Johnston, Alice S.A. Sibly, Richard M. 2018-08-27T18:56:25Z http://hdl.handle.net/10255/dryad.187174 https://doi.org/10.5061/dryad.416kv03 unknown doi:10.5061/dryad.416kv03/1 doi:10.5061/dryad.416kv03/3 doi:10.5061/dryad.416kv03/2 doi:10.5061/dryad.416kv03/4 doi:10.1038/s41559-018-0648-6 doi:10.5061/dryad.416kv03 Johnston ASA, Sibly RM (2018) The influence of soil communities on the temperature sensitivity of soil respiration. Nature Ecology & Evolution 2(10): 1597-1602. http://hdl.handle.net/10255/dryad.187174 Soil biota Soil community Metabolic rate Individual mass Population abundance Temperature sensitivity Soil respiration Biome Tundra Boreal forest Temperate forest Temperate grassland Tropical forest Article 2018 ftdryad https://doi.org/10.5061/dryad.416kv03 https://doi.org/10.5061/dryad.416kv03/1 https://doi.org/10.5061/dryad.416kv03/3 https://doi.org/10.5061/dryad.416kv03/2 https://doi.org/10.5061/dryad.416kv03/4 https://doi.org/10.1038/s41559-018-0648-6 2020-01-01T16:13:05Z Soil respiration represents a major carbon flux between terrestrial ecosystems and the atmosphere, and is expected to accelerate under climate warming. Despite its importance in climate change forecasts, however, our understanding of the effects of temperature on soil respiration (RS) is incomplete. Using a metabolic ecology approach we link soil biota metabolism, community composition and heterotrophic activity, to predict RS rates across five biomes. We find that accounting for the ecological mechanisms underpinning decomposition processes predicts climatological RS variations observed in an independent dataset (n = 312). The importance of community composition is evident because without it RS is substantially underestimated. With increasing temperature, we predict a latitudinal increase in RS temperature sensitivity, with Q10 values ranging between 2.33 ±0.01 in tropical forests to 2.72 ±0.03 in tundra. This global trend has been widely observed, but has not previously been linked to soil communities. Article in Journal/Newspaper Tundra Dryad Digital Repository (Duke University)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic Soil biota
Soil community
Metabolic rate
Individual mass
Population abundance
Temperature sensitivity
Soil respiration
Biome
Tundra
Boreal forest
Temperate forest
Temperate grassland
Tropical forest
spellingShingle Soil biota
Soil community
Metabolic rate
Individual mass
Population abundance
Temperature sensitivity
Soil respiration
Biome
Tundra
Boreal forest
Temperate forest
Temperate grassland
Tropical forest
Johnston, Alice S.A.
Sibly, Richard M.
Data from: The influence of soil communities on the temperature sensitivity of soil respiration
topic_facet Soil biota
Soil community
Metabolic rate
Individual mass
Population abundance
Temperature sensitivity
Soil respiration
Biome
Tundra
Boreal forest
Temperate forest
Temperate grassland
Tropical forest
description Soil respiration represents a major carbon flux between terrestrial ecosystems and the atmosphere, and is expected to accelerate under climate warming. Despite its importance in climate change forecasts, however, our understanding of the effects of temperature on soil respiration (RS) is incomplete. Using a metabolic ecology approach we link soil biota metabolism, community composition and heterotrophic activity, to predict RS rates across five biomes. We find that accounting for the ecological mechanisms underpinning decomposition processes predicts climatological RS variations observed in an independent dataset (n = 312). The importance of community composition is evident because without it RS is substantially underestimated. With increasing temperature, we predict a latitudinal increase in RS temperature sensitivity, with Q10 values ranging between 2.33 ±0.01 in tropical forests to 2.72 ±0.03 in tundra. This global trend has been widely observed, but has not previously been linked to soil communities.
format Article in Journal/Newspaper
author Johnston, Alice S.A.
Sibly, Richard M.
author_facet Johnston, Alice S.A.
Sibly, Richard M.
author_sort Johnston, Alice S.A.
title Data from: The influence of soil communities on the temperature sensitivity of soil respiration
title_short Data from: The influence of soil communities on the temperature sensitivity of soil respiration
title_full Data from: The influence of soil communities on the temperature sensitivity of soil respiration
title_fullStr Data from: The influence of soil communities on the temperature sensitivity of soil respiration
title_full_unstemmed Data from: The influence of soil communities on the temperature sensitivity of soil respiration
title_sort data from: the influence of soil communities on the temperature sensitivity of soil respiration
publishDate 2018
url http://hdl.handle.net/10255/dryad.187174
https://doi.org/10.5061/dryad.416kv03
genre Tundra
genre_facet Tundra
op_relation doi:10.5061/dryad.416kv03/1
doi:10.5061/dryad.416kv03/3
doi:10.5061/dryad.416kv03/2
doi:10.5061/dryad.416kv03/4
doi:10.1038/s41559-018-0648-6
doi:10.5061/dryad.416kv03
Johnston ASA, Sibly RM (2018) The influence of soil communities on the temperature sensitivity of soil respiration. Nature Ecology & Evolution 2(10): 1597-1602.
http://hdl.handle.net/10255/dryad.187174
op_doi https://doi.org/10.5061/dryad.416kv03
https://doi.org/10.5061/dryad.416kv03/1
https://doi.org/10.5061/dryad.416kv03/3
https://doi.org/10.5061/dryad.416kv03/2
https://doi.org/10.5061/dryad.416kv03/4
https://doi.org/10.1038/s41559-018-0648-6
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