Increasing phosphorus (P) inputs induced by anthropogenic activities have increased P
availability in soils considerably, with dramatic effects on carbon (C) cycling and storage …

Dissolved organic matter (DOM) plays a vital role in biogeochemical processes and in
determining the responses of soil organic matter (SOM) to global change. Although the …

Unprecedented nitrogen (N) inputs into terrestrial ecosystems have profoundly altered soil N
cycling. Ammonia oxidizers and denitrifiers are the main producers of nitrous oxide (N2O) …

Low soil phosphorus (P) bioavailability causes the widespread occurrence of P‐limited
terrestrial ecosystems around the globe. Exploring the factors influencing soil P …

Soil microbiology has entered into the big data era, but the challenges in bridging laboratory‐
, field‐, and model‐based studies of ecosystem functions still remain. Indeed, the limitation …

Microorganisms govern soil nutrient cycling. It is therefore critical to understand their
responses to human-induced increases in N and P inputs. We investigated microbial …

Many studies have used the relative activities of extracellular enzymes associated with
microbial carbon (C), nitrogen (N) and phosphorus (P) acquisition to infer the relative C vs …

Soil priming is a microbial‐driven process, which determines key soil–climate feedbacks in
response to fresh carbon inputs. Despite its importance, the microbial traits behind this …

Saline and alkaline soils are a challenge for sustainable crop production. The use of organic
and inorganic amendments is a common practice to increase the fertility of salt-affected soils …

Soil microbial functional genes are linked with carbon (C) as well as nitrogen (N) cycling
processes, and their relative abundances are strongly affected by ecosystem managements …