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The role of soil chemical properties, land use and plant diversity for microbial phosphorus in forest and grassland soils
Author(s) -
Sorkau Elisabeth,
Boch Steffen,
Boeddinghaus Runa S.,
Bonkowski Michael,
Fischer Markus,
Kandeler Ellen,
Klaus Valentin H.,
Kleinebecker Till,
Marhan Sven,
Müller Jörg,
Prati Daniel,
Schöning Ingo,
Schrumpf Marion,
Weinert Jan,
Oelmann Yvonne
Publication year - 2018
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.201700082
Subject(s) - grassland , soil water , abiotic component , environmental science , phosphorus , biomass (ecology) , soil carbon , agronomy , soil ph , ecology , biology , chemistry , soil science , organic chemistry
Management intensity modifies soil properties, e.g ., organic carbon (C org ) concentrations and soil pH with potential feedbacks on plant diversity. These changes might influence microbial P concentrations (P mic ) in soil representing an important component of the P cycle. Our objectives were to elucidate whether abiotic and biotic variables controlling P mic concentrations in soil are the same for forests and grasslands, and to assess the effect of region and management on P mic concentrations in forest and grassland soils as mediated by the controlling variables. In three regions of Germany, Schwäbische Alb, Hanich‐Dün, and Schorfheide‐Chorin, we studied forest and grassland plots (each n = 150) differing in plant diversity and land‐use intensity. In contrast to controls of microbial biomass carbon (C mic ), P mic was strongly influenced by soil pH, which in turn affected phosphorus (P) availability and thus microbial P uptake in forest and grassland soils. Furthermore, P mic concentrations in forest and grassland soils increased with increasing plant diversity. Using structural equation models, we could show that soil C org is the profound driver of plant diversity effects on P mic in grasslands. For both forest and grassland, we found regional differences in P mic attributable to differing environmental conditions (pH, soil moisture). Forest management and tree species showed no effect on P mic due to a lack of effects on controlling variables ( e.g ., C org ). We also did not find management effects in grassland soils which might be caused by either compensation of differently directed effects across sites or by legacy effects of former fertilization constraining the relevance of actual practices. We conclude that variables controlling P mic or C mic in soil differ in part and that regional differences in controlling variables are more important for P mic in soil than those induced by management.