about
Aridity modulates N availability in arid and semiarid Mediterranean grasslands.Decoupling of soil nutrient cycles as a function of aridity in global drylands.Are there links between responses of soil microbes and ecosystem functioning to elevated CO2, N deposition and warming? A global perspective.Structure and functioning of dryland ecosystems in a changing world.Do biotic interactions modulate ecosystem functioning along stress gradients? Insights from semi-arid plant and biological soil crust communitiesPlant species richness and ecosystem multifunctionality in global drylandsClimate and litter quality differently modulate the effects of soil fauna on litter decomposition across biomes.Dual mechanisms regulate ecosystem stability under decade-long warming and hay harvest.Is manure an alternative to topsoil in road embankment restoration?Asymmetric responses of primary productivity to precipitation extremes: A synthesis of grassland precipitation manipulation experiments.Side-effects of plant domestication: ecosystem impacts of changes in litter quality.Shrub encroachment can reverse desertification in semi-arid Mediterranean grasslands.Functional traits determine plant co-occurrence more than environment or evolutionary relatedness in global drylands.Biogeographic bases for a shift in crop C : N : P stoichiometries during domestication.Changes in rainfall amount and frequency do not affect the outcome of the interaction between the shrub Retama sphaerocarpa and its neighbouring grasses in two semiarid communities.Plant responses to soil heterogeneity and global environmental change.Ecosystem development in roadside grasslands: biotic control, plant-soil interactions, and dispersal limitations.Soil nutrient heterogeneity modulates ecosystem responses to changes in the identity and richness of plant functional groupsClimate mediates the biodiversity-ecosystem stability relationship globallyEarthworms modify plant biomass and nitrogen capture under conditions of soil nutrient heterogeneity and elevated atmospheric CO 2 concentrationsHuman impacts and aridity differentially alter soil N availability in drylands worldwideSoil characteristics determine soil carbon and nitrogen availability during leaf litter decomposition regardless of litter qualityEarly-successional vegetation changes after roadside prairie restoration modify processes related with soil functioning by changing microbial functional diversityImpact of simulated changes in rainfall regime and nutrient deposition on the relative dominance and isotopic composition of ruderal plants in anthropogenic grasslandsTemporal dynamics of herbivory and water availability interactively modulate the outcome of a grass-shrub interaction in a semi-arid ecosystemDominant plant species modulate responses to hydroseeding, irrigation and fertilization during the restoration of semiarid motorway slopesPathways regulating decreased soil respiration with warming in a biocrust-dominated drylandAspects of soil lichen biodiversity and aggregation interact to influence subsurface microbial functionCommunity-aggregated plant traits interact with soil nutrient heterogeneity to determine ecosystem functioningBiological Soil Crust Microsites Are the Main Contributor to Soil Respiration in a Semiarid EcosystemSoil microbial respiration adapts to ambient temperature in global drylandsDifferential responses of carbon-degrading enzyme activities to warming: Implications for soil respirationPlant domestication disrupts biodiversity effects across major crop typesTRY plant trait database - enhanced coverage and open accessIncreasing microbial carbon use efficiency with warming predicts soil heterotrophic respiration globally
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P50
description
onderzoeker
@nl
researcher
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հետազոտող
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name
Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
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type
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Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
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prefLabel
Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
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Pablo García-Palacios
@nl
P106
P1153
32867755600
P21
P31
P496
0000-0002-6367-4761