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Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent

Climate and litter quality are primary drivers of terrestrial decomposition and, based on evidence from multisite experiments at regional and global scales, are universally factored into global decomposition models. In contrast, soil animals are considered key regulators of decomposition at local sc...

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Autores principales: WALL, DIANA H, BRADFORD, MARK A, ST JOHN, MARK G, TROFYMOW, JOHN A, BEHAN-PELLETIER, VALERIE, BIGNELL, DAVID E, DANGERFIELD, J MARK, PARTON, WILLIAM J, RUSEK, JOSEF, VOIGT, WINFRIED, WOLTERS, VOLKMAR, GARDEL, HOLLEY ZADEH, AYUKE, FRED O, BASHFORD, RICHARD, BELJAKOVA, OLGA I, BOHLEN, PATRICK J, BRAUMAN, ALAIN, FLEMMING, STEPHEN, HENSCHEL, JOH R, JOHNSON, DAN L, JONES, T HEFIN, KOVAROVA, MARCELA, KRANABETTER, J MARTY, KUTNY, LES, LIN, KUO-CHUAN, MARYATI, MOHAMED, MASSE, DOMINIQUE, POKARZHEVSKII, ANDREI, RAHMAN, HOMATHEVI, SABARÁ, MILLOR G, SALAMON, JOERG-ALFRED, SWIFT, MICHAEL J, VARELA, AMANDA, VASCONCELOS, HERALDO L, WHITE, DON, ZOU, XIAOMING
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Blackwell Publishing Ltd 2008
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3597247/
http://dx.doi.org/10.1111/j.1365-2486.2008.01672.x
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author WALL, DIANA H
BRADFORD, MARK A
ST JOHN, MARK G
TROFYMOW, JOHN A
BEHAN-PELLETIER, VALERIE
BIGNELL, DAVID E
DANGERFIELD, J MARK
PARTON, WILLIAM J
RUSEK, JOSEF
VOIGT, WINFRIED
WOLTERS, VOLKMAR
GARDEL, HOLLEY ZADEH
AYUKE, FRED O
BASHFORD, RICHARD
BELJAKOVA, OLGA I
BOHLEN, PATRICK J
BRAUMAN, ALAIN
FLEMMING, STEPHEN
HENSCHEL, JOH R
JOHNSON, DAN L
JONES, T HEFIN
KOVAROVA, MARCELA
KRANABETTER, J MARTY
KUTNY, LES
LIN, KUO-CHUAN
MARYATI, MOHAMED
MASSE, DOMINIQUE
POKARZHEVSKII, ANDREI
RAHMAN, HOMATHEVI
SABARÁ, MILLOR G
SALAMON, JOERG-ALFRED
SWIFT, MICHAEL J
VARELA, AMANDA
VASCONCELOS, HERALDO L
WHITE, DON
ZOU, XIAOMING
author_facet WALL, DIANA H
BRADFORD, MARK A
ST JOHN, MARK G
TROFYMOW, JOHN A
BEHAN-PELLETIER, VALERIE
BIGNELL, DAVID E
DANGERFIELD, J MARK
PARTON, WILLIAM J
RUSEK, JOSEF
VOIGT, WINFRIED
WOLTERS, VOLKMAR
GARDEL, HOLLEY ZADEH
AYUKE, FRED O
BASHFORD, RICHARD
BELJAKOVA, OLGA I
BOHLEN, PATRICK J
BRAUMAN, ALAIN
FLEMMING, STEPHEN
HENSCHEL, JOH R
JOHNSON, DAN L
JONES, T HEFIN
KOVAROVA, MARCELA
KRANABETTER, J MARTY
KUTNY, LES
LIN, KUO-CHUAN
MARYATI, MOHAMED
MASSE, DOMINIQUE
POKARZHEVSKII, ANDREI
RAHMAN, HOMATHEVI
SABARÁ, MILLOR G
SALAMON, JOERG-ALFRED
SWIFT, MICHAEL J
VARELA, AMANDA
VASCONCELOS, HERALDO L
WHITE, DON
ZOU, XIAOMING
author_sort WALL, DIANA H
collection PubMed
description Climate and litter quality are primary drivers of terrestrial decomposition and, based on evidence from multisite experiments at regional and global scales, are universally factored into global decomposition models. In contrast, soil animals are considered key regulators of decomposition at local scales but their role at larger scales is unresolved. Soil animals are consequently excluded from global models of organic mineralization processes. Incomplete assessment of the roles of soil animals stems from the difficulties of manipulating invertebrate animals experimentally across large geographic gradients. This is compounded by deficient or inconsistent taxonomy. We report a global decomposition experiment to assess the importance of soil animals in C mineralization, in which a common grass litter substrate was exposed to natural decomposition in either control or reduced animal treatments across 30 sites distributed from 43°S to 68°N on six continents. Animals in the mesofaunal size range were recovered from the litter by Tullgren extraction and identified to common specifications, mostly at the ordinal level. The design of the trials enabled faunal contribution to be evaluated against abiotic parameters between sites. Soil animals increase decomposition rates in temperate and wet tropical climates, but have neutral effects where temperature or moisture constrain biological activity. Our findings highlight that faunal influences on decomposition are dependent on prevailing climatic conditions. We conclude that (1) inclusion of soil animals will improve the predictive capabilities of region- or biome-scale decomposition models, (2) soil animal influences on decomposition are important at the regional scale when attempting to predict global change scenarios, and (3) the statistical relationship between decomposition rates and climate, at the global scale, is robust against changes in soil faunal abundance and diversity.
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spelling pubmed-35972472013-03-19 Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent WALL, DIANA H BRADFORD, MARK A ST JOHN, MARK G TROFYMOW, JOHN A BEHAN-PELLETIER, VALERIE BIGNELL, DAVID E DANGERFIELD, J MARK PARTON, WILLIAM J RUSEK, JOSEF VOIGT, WINFRIED WOLTERS, VOLKMAR GARDEL, HOLLEY ZADEH AYUKE, FRED O BASHFORD, RICHARD BELJAKOVA, OLGA I BOHLEN, PATRICK J BRAUMAN, ALAIN FLEMMING, STEPHEN HENSCHEL, JOH R JOHNSON, DAN L JONES, T HEFIN KOVAROVA, MARCELA KRANABETTER, J MARTY KUTNY, LES LIN, KUO-CHUAN MARYATI, MOHAMED MASSE, DOMINIQUE POKARZHEVSKII, ANDREI RAHMAN, HOMATHEVI SABARÁ, MILLOR G SALAMON, JOERG-ALFRED SWIFT, MICHAEL J VARELA, AMANDA VASCONCELOS, HERALDO L WHITE, DON ZOU, XIAOMING Glob Chang Biol Original Articles Climate and litter quality are primary drivers of terrestrial decomposition and, based on evidence from multisite experiments at regional and global scales, are universally factored into global decomposition models. In contrast, soil animals are considered key regulators of decomposition at local scales but their role at larger scales is unresolved. Soil animals are consequently excluded from global models of organic mineralization processes. Incomplete assessment of the roles of soil animals stems from the difficulties of manipulating invertebrate animals experimentally across large geographic gradients. This is compounded by deficient or inconsistent taxonomy. We report a global decomposition experiment to assess the importance of soil animals in C mineralization, in which a common grass litter substrate was exposed to natural decomposition in either control or reduced animal treatments across 30 sites distributed from 43°S to 68°N on six continents. Animals in the mesofaunal size range were recovered from the litter by Tullgren extraction and identified to common specifications, mostly at the ordinal level. The design of the trials enabled faunal contribution to be evaluated against abiotic parameters between sites. Soil animals increase decomposition rates in temperate and wet tropical climates, but have neutral effects where temperature or moisture constrain biological activity. Our findings highlight that faunal influences on decomposition are dependent on prevailing climatic conditions. We conclude that (1) inclusion of soil animals will improve the predictive capabilities of region- or biome-scale decomposition models, (2) soil animal influences on decomposition are important at the regional scale when attempting to predict global change scenarios, and (3) the statistical relationship between decomposition rates and climate, at the global scale, is robust against changes in soil faunal abundance and diversity. Blackwell Publishing Ltd 2008-11 /pmc/articles/PMC3597247/ http://dx.doi.org/10.1111/j.1365-2486.2008.01672.x Text en Journal compilation © 2008 Blackwell Publishing http://creativecommons.org/licenses/by/2.5/ Re-use of this article is permitted in accordance with the Creative Commons Deed, Attribution 2.5, which does not permit commercial exploitation.
spellingShingle Original Articles
WALL, DIANA H
BRADFORD, MARK A
ST JOHN, MARK G
TROFYMOW, JOHN A
BEHAN-PELLETIER, VALERIE
BIGNELL, DAVID E
DANGERFIELD, J MARK
PARTON, WILLIAM J
RUSEK, JOSEF
VOIGT, WINFRIED
WOLTERS, VOLKMAR
GARDEL, HOLLEY ZADEH
AYUKE, FRED O
BASHFORD, RICHARD
BELJAKOVA, OLGA I
BOHLEN, PATRICK J
BRAUMAN, ALAIN
FLEMMING, STEPHEN
HENSCHEL, JOH R
JOHNSON, DAN L
JONES, T HEFIN
KOVAROVA, MARCELA
KRANABETTER, J MARTY
KUTNY, LES
LIN, KUO-CHUAN
MARYATI, MOHAMED
MASSE, DOMINIQUE
POKARZHEVSKII, ANDREI
RAHMAN, HOMATHEVI
SABARÁ, MILLOR G
SALAMON, JOERG-ALFRED
SWIFT, MICHAEL J
VARELA, AMANDA
VASCONCELOS, HERALDO L
WHITE, DON
ZOU, XIAOMING
Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title_full Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title_fullStr Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title_full_unstemmed Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title_short Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
title_sort global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
topic Original Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3597247/
http://dx.doi.org/10.1111/j.1365-2486.2008.01672.x
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