Background The dynamics of phosphorus (P) in the environment is important for regulating
nutrient cycles in natural and managed ecosystems and an integral part in assessing …

There has been much soil phosphorus (P) research in the last decades, but few basic
publications exist summarizing the current state of knowledge on ecologically relevant P …

Soils represent the largest phosphorus (P) reserves on land and determining the amount is
a critical first step for identifying sites where ecosystem functioning is potentially limited by P …

Phosphorus availability may shape plant–microorganism–soil interactions in forest
ecosystems. Our aim was to quantify the interactions between soil P availability and P …

Understanding and quantification of phosphorus (P) fluxes are key requirements for
predictions of future forest ecosystems changes as well as for transferring lessons learned …

Controlled experiments have shown that global changes decouple the biogeochemical
cycles of carbon (C), nitrogen (N), and phosphorus (P), resulting in shifting stoichiometry that …

Biogeochemical weathering of bedrock is the most important input of silicon (Si) and
phosphorus (P) to forest ecosystems. While soil microbes, and in particular P-solubilizing …

Although phosphorus (P) is a limiting nutrient for plant growth in subtropical forests, the
effects of forest succession on soil P dynamics, which in turn influences P availability, are …

Plants mediate water fluxes within the soil–vegetation–atmosphere continuum. This water
transfer in soils, through plants, into the atmosphere can be effectively traced by stable …

Tracing and quantifying water fluxes in the hydrological cycle is crucial for understanding the
current state of ecohydrological systems and their vulnerability to environmental change …