TY  - JOUR
A1  - Sorkau, Elisabeth
A1  - Boch, Steffen
A1  - Boeddinghaus, Runa S.
A1  - Bonkowski, Michael
A1  - Fischer, Markus
A1  - Kandeler, Ellen
A1  - Klaus, Valentin H.
A1  - Kleinebecker, Till
A1  - Marhan, Sven
A1  - Müller, Jörg
A1  - Prati, Daniel
A1  - Schoening, Ingo
A1  - Schrumpf, Marion
A1  - Weinert, Jan
A1  - Oelmann, Yvonne
T1  - The role of soil chemical properties, land use and plant diversity for microbial phosphorus in forest and grassland soils
JF  - Journal of plant nutrition and soil science = Zeitschrift für Pflanzenernährung und Bodenkunde
N2  - 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 Pcycle. 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, Schwabische Alb, Hanich-Dun, 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 Puptake 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.
KW  - age class forest
KW  - land-use intensity
KW  - meadow
KW  - microbes
KW  - pasture
KW  - unmanaged forest
Y1  - 2018
U6  - https://doi.org/10.1002/jpln.201700082
SN  - 1436-8730
SN  - 1522-2624
VL  - 181
IS  - 2
SP  - 185
EP  - 197
PB  - Wiley-VCH
CY  - Weinheim
ER  -