Soil microorganisms are clearly a key component of both natural and managed ecosystems.
Despite the challenges of surviving in soil, a gram of soil can contain thousands of individual …

The rhizosphere is the interface between plant roots and soil where interactions among a
myriad of microorganisms and invertebrates affect biogeochemical cycling, plant growth and …

Microbial communities play important roles in all ecosystems and yet a comprehensive
understanding of the ecological processes governing the assembly of these communities is …

Background The relative importance of stochasticity versus determinism in soil bacterial
communities is unclear, as are the possible influences that alter the balance between these …

The continuous increase of the greenhouse gas nitrous oxide (N2O) in the atmosphere due
to increasing anthropogenic nitrogen input in agriculture has become a global concern. In …

Microorganisms drive much of the Earth's nitrogen (N) cycle, but we still lack a global
overview of the abundance and composition of the microorganisms carrying out soil N …

For centuries ecologists have studied how the diversity and functional traits of plant and
animal communities vary across biomes. In contrast, we have only just begun exploring …

The understanding of nitrogen (N) cycling in forest ecosystems has undergone a major shift
in the past decade as molecular methods are being used to link microorganisms to key …

Maintaining stability of ecosystem functions in the face of global change calls for a better
understanding regulatory factors of functionally specialized microbial groups and their …

Autotrophic archaeal and bacterial ammonia-oxidisers (AOA and AOB) drive soil nitrification.
Ammonia limitation, mixotrophy, and pH have been suggested as factors providing niche …