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Maize phenology alters the distribution of enzyme activities in soil: Field estimates soil. A pronounced biotic control on EA was demonstrated by higher EA in rooted soil than in bare

Beech trees fuel soil animal food webs via root-derived nitrogen both the role of root-derived carbon (C) and nitrogen (N) for the nutrition of soil animal species

The persistence of bacterial diversity and ecosystem multifunctionality along a disturbance intensity gradient in karst soil approaches to topsoils sampled at rock-soil interfaces and adjacent bulk soil along an established gradient

The persistence of bacterial diversity and ecosystem multifunctionality along a disturbance intensity gradient in karst soil approaches to topsoils sampled at rock-soil interfaces and adjacent bulk soil along an established gradient

Estimates of soil renewal rates: applications for anti-erosion arrangement of the agricultural landscape of space-tim e scales) estimations of the soil loss tolerance

Archaeal lipids in soils and sediments: Water impact and consequences for microbial carbon sequestrationThe mineral protection of microbial necromass is critical for soil carbon stabilization. The water

Agrogenic evolution of automorphic chernozems in the forest-steppe zone (Belgorod oblast). Certain stages in the development of these soils during more than two centuries of their agricultural use

C/P stoichiometry of dying rice root defines the spatial distribution and dynamics of enzyme activities in root-detritusphere ratio). Root-detritus of low (59.0) and high (170.8) C/P ratios was produced in P-poor soil

Beech trees fuel soil animal food webs via root-derived nitrogen both the role of root-derived carbon (C) and nitrogen (N) for the nutrition of soil animal species

C/P stoichiometry of dying rice root defines the spatial distribution and dynamics of enzyme activities in root-detritusphere.05), whereas it decreased in the root-detritusphere of non-fertilised soil. We conclude that the decomposition

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