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General relationships between abiotic soil properties and soil biota across spatial scales and different land-use types

Authors :
Rolf Daniel
Mark Maraun
Ellen Kandeler
Jörg Overmann
Melanie M. Pollierer
Marion Schrumpf
Fabian Alt
Ingo Schöning
Georgia Erdmann
Janine Groh
Volkmar Wolters
Astrid Näther
Heiko Nacke
Jan Weinert
Bärbel U. Foesel
Wolfgang W. Weisser
Waltraud X. Schulze
Annabel Meyer
Yvonne Oelmann
Doreen Berner
Christa Lang
Bernhard Klarner
Andrey Yurkov
Tesfaye Wubet
Andrea Polle
Stefan Scheu
Christiane Fischer
Dominik Begerow
François Buscot
Sven Marhan
Nadine Herold
Ernst Detlef Schulze
Klaus Birkhofer
Jessica L. M. Gutknecht
Michael Schloter
Roswitha B. Ehnes
Gertrud Lohaus
Tim Diekötter
Ibekwe, A. Mark
Source :
PLoS ONE 7:e43292 (2012), PLoS ONE, Vol 7, Iss 8, p e43292 (2012), PLoS One, PLoS ONE
Publication Year :
2012
Publisher :
Public Library of Science, 2012.

Abstract

Very few principles have been unraveled that explain the relationship between soil properties and soil biota across large spatial scales and different land-use types. Here, we seek these general relationships using data from 52 differently managed grassland and forest soils in three study regions spanning a latitudinal gradient in Germany. We hypothesize that, after extraction of variation that is explained by location and land-use type, soil properties still explain significant proportions of variation in the abundance and diversity of soil biota. If the relationships between predictors and soil organisms were analyzed individually for each predictor group, soil properties explained the highest amount of variation in soil biota abundance and diversity, followed by land-use type and sampling location. After extraction of variation that originated from location or land-use, abiotic soil properties explained significant amounts of variation in fungal, meso- and macrofauna, but not in yeast or bacterial biomass or diversity. Nitrate or nitrogen concentration and fungal biomass were positively related, but nitrate concentration was negatively related to the abundances of Collembola and mites and to the myriapod species richness across a range of forest and grassland soils. The species richness of earthworms was positively correlated with clay content of soils independent of sample location and land-use type. Our study indicates that after accounting for heterogeneity resulting from large scale differences among sampling locations and land-use types, soil properties still explain significant proportions of variation in fungal and soil fauna abundance or diversity. However, soil biota was also related to processes that act at larger spatial scales and bacteria or soil yeasts only showed weak relationships to soil properties. We therefore argue that more general relationships between soil properties and soil biota can only be derived from future studies that consider larger spatial scales and different land-use types. peerReviewed

Details

Language :
English
Database :
OpenAIRE
Journal :
PLoS ONE 7:e43292 (2012), PLoS ONE, Vol 7, Iss 8, p e43292 (2012), PLoS One, PLoS ONE
Accession number :
edsair.doi.dedup.....06e57db83b765f7c9e816b8134a5c026