The prokaryotic and eukaryotic microorganisms that drive the pelagic ocean's
biogeochemical cycles are currently facing an unprecedented set of comprehensive …

Surface ocean biogeochemistry and photochemistry regulate ocean–atmosphere fluxes of
trace gases critical for Earth's atmospheric chemistry and climate. The oceanic processes …

Ocean acidification (OA), caused by seawater CO2 uptake, has significant impacts on
marine calcifying organisms and phototrophs. However, the response of bacterial …

Ocean acidification (OA), arising from the influx of anthropogenically generated carbon,
poses a massive threat to the ocean ecosystems. Our knowledge of the effects of elevated …

Anthropogenic CO2 emissions are causing oceans to become more acidic, with
consequences for all marine life including microorganisms. Studies reveal that from the …

Ammonia-oxidizing microorganisms are an important source of the greenhouse gas nitrous
oxide (N2O) in aquatic environments. Identifying the impact of pH on N2O production by …

Transformation and mobilization of bioessential elements in the biosphere, lithosphere,
atmosphere, and hydrosphere constitute the Earth's biogeochemical cycles, which are …

N2 fixation and ammonia oxidation (AO) are the two most important processes in the
nitrogen (N) cycle of biological soil crusts (BSCs). We studied the short-term response of …

Climate change has profound impacts on marine biodiversity and biodiversity changes in
turn might affect the community sensitivity to impacts of abiotic changes. We used mesocosm …

The strong seasonal variability in physical-chemical conditions of the Eastern South Pacific
Ocean creates an ideal setting to study spatiotemporal distribution of key marine microbial …