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

DIANA H. WALL; MARK A. BRADFORD; MARK G. ST. JOHN; JOHN A. TROFYMOW; VALERIE BEHAN‐PELLETIER; DAVID E. BIGNELL; J. MARK DANGERFIELD; WILLIAM J. PARTON; JOSEF RUSEK; WINFRIED VOIGT; VOLKMAR WOLTERS; HOLLEY ZADEH GARDEL; FRED O. AYUKE; RICHARD BASHFORD; OLGA I. BELJAKOVA; PATRICK J. BOHLEN; ALAIN BRAUMAN; STEPHEN FLEMMING; JOH R. HENSCHEL; DAN L. JOHNSON; T. HEFIN JONES; MARCELA KOVAROVA; J. MARTY KRANABETTER; LES KUTNY; KUO‐CHUAN LIN; MOHAMED MARYATI; DOMINIQUE MASSE; ANDREI POKARZHEVSKII; HOMATHEVI RAHMAN; MILLOR G. SABARÁ; JOERG‐ALFRED SALAMON; MICHAEL J. SWIFT; AMANDA VARELA; HERALDO L. VASCONCELOS; DON WHITE; XIAOMING ZOU
Global Change Biology · Vol. 14, Issue 11 · pp. 2661-2677 · 2008

Abstract

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.

Bibliographic Information

JournalGlobal Change Biology
PublisherWiley
Publication Date2008-11-01
Publication Year2008
Volume14
Issue11
Pages2661-2677
Document TypeJournal Article
Print ISSN1354-1013
eISSN1365-2486
DOI10.1111/j.1365-2486.2008.01672.x
SubjectConservation Science

Access Information

NARA Access Coverage1997-01-01~Current
Journal Homepagehttps://onlinelibrary.wiley.com/loi/13652486
Publisher PageOpen Publisher Page
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