The Department of Marine Sciences, University of Gothenburg, (https://www.gu.se/en/marina-vetenskaper) combines extensive scientific competence with unique

Chemical weathering of silicate rocks occurs along a continuum from terrestrial to marine environments.

Benthic fluxes are important sources of nutrients and dissolved carbon to the water column. Yet, most approaches for quantifying benthic fluxes are labor intensive and cover relatively small areas of...

The land along the coast is often hydrologically disconnected from the prevailing river systems. Water flow and nutrient transport from these disconnected coastal subcatchments follow diffusive pathwa...

This study uses sediment eDNA metabarcoding to assess the diversity and distribution of meiofauna in Siberian seas, marking the first application of this technique in the region. Our results reveal t....

Can climate catastrophe be stymied by tweaking seawater chemistry?

Eutrophication stimulates nitrous oxide emissions in coastal lagoons Excess nitrate induces incomplete denitrification, leading to high nitrous oxide effluxes in sediments Nitrous oxide emission...

A rapidly-retreating marine-terminating glacier exported CH4 to nearshore waters N2O was undersaturated near the glacier front The regional CO2 sink greatly outweighs CH4 and N2O emissions

Groundwater is a hidden, steady source of CO2 to coastal waters.

Groundwater is a hidden, steady source of CO2 to coastal waters.