Abstract Purpose of Review The changes or updates in ocean biogeochemistry component
have been mapped between CMIP5 and CMIP6 model versions, and an assessment made …

The marine trace gas dimethylsulfide (DMS) supplies sulfur to the atmosphere at a rate of 15–
40 Tg S per year, contributing to the production of atmospheric sulfate aerosols that …

The marine dissolved organic carbon (DOC) pool is an important player in the functioning of
marine ecosystems. DOC is at the interface between the chemical and the biological worlds …

CO 2 hydrogenation is an attractive way to store and utilize carbon dioxide generated by
industrial processes, as well as to produce valuable chemicals from renewable and …

Anthropogenic emissions to the atmosphere have increased the flux of nutrients, especially
nitrogen, to the ocean, but they have also altered the acidity of aerosol, cloud water, and …

Oceans have the capacity to absorb large amounts of carbon dioxide (CO 2) because CO 2
dissolves and reacts in seawater to form bicarbonate (HCO 3−) and protons (H+). About a …

Characteristics and trends of surface ocean dimethylsulfide (DMS) concentrations and fluxes
into the atmosphere of four Earth system models (ESMs: CNRM-ESM2-1, MIROC-ES2L …

A key component of the marine sulfur cycle is the climate-active gas dimethylsulfide (DMS),
which is synthesized by a range of organisms from phytoplankton to corals, and accounts for …

Oceanic dimethyl sulfide (DMS) emissions have been recognized as a biological regulator
of climate by contributing to cloud formation. Despite decades of research, the climatic role …

The effects of climate change (CC) on contaminants and their potential consequences to
marine ecosystem services and human wellbeing are of paramount importance, as they …