TY - JOUR
T1 - Global decomposition experiment shows soil animal impacts on decomposition are climate-dependent
AU - Wall, Diana H.
AU - Bradford, Mark A.
AU - St. John, Mark G.
AU - Trofymow, John A.
AU - Behan-Pelletier, Valerie
AU - Bignell, David E.
AU - Dangerfield, J. Mark
AU - Parton, William J.
AU - Rusek, Josef
AU - Voigt, Winfried
AU - Wolters, Volkmar
AU - Gardel, Holley Zadeh
AU - Ayuke, Fredo O.
AU - Bashford, Richard
AU - Beljakova, Olga I.
AU - Bohlen, Patrick J.
AU - Brauman, Alain
AU - Flemming, Stephen
AU - Henschel, Joh R.
AU - Johnson, Dan L.
AU - Jones, T. Helfin
AU - Kovarova, Marcela
AU - Kranabetter, J. Marty
AU - Kutny, Les
AU - Lin, Kuo Chuan
AU - Maryati, Mohamed
AU - Masse, Dominique
AU - Pokarzhevskii, Andrei
AU - Rahman, Homathevi
AU - Sabará, Millor G.
AU - Salamon, Joerg Alfred
AU - Swift, Michael J.
AU - Varela, Amanda
AU - Vasconcelos, Heraldo L.
AU - White, Don
AU - Zou, Xiaoming
PY - 2008
Y1 - 2008
N2 - 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.
AB - 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.
KW - Climate decomposition index
KW - Decomposition
KW - Litter
KW - Mesofauna
KW - Soil biodiversity
KW - Soil carbon
KW - Soil fauna
UR - http://www.scopus.com/inward/record.url?scp=54449101622&partnerID=8YFLogxK
U2 - 10.1111/j.1365-2486.2008.01672.x
DO - 10.1111/j.1365-2486.2008.01672.x
M3 - Article
AN - SCOPUS:54449101622
SN - 1354-1013
VL - 14
SP - 2661
EP - 2677
JO - Global Change Biology
JF - Global Change Biology
IS - 11
ER -