Caroline P. Slomp

TL;DR: In this article, the authors reviewed the key factors determining the fluxes of nitrogen (N) and phosphorus (P) associated with submarine groundwater discharge and presented a compilation of measured rates, in particular, the water residence time and the redox conditions in coastal aquifers and sediments determine fluxes and ratios of N and P in SGD.

TL;DR: The Baltic Sea is unique for coastal marine ecosystems experiencing N losses in hypoxic waters below the halocline, and Nutrient load reductions are needed to reduce the extent, severity, and effects of hypoxia.

TL;DR: In this article, the authors synthesize biological, geochemical, and physically focused CH4 climate feedback literature, bringing together the key findings of these disciplines, and discuss environment-specific feedback processes, including the microbial, physical, and geochemical interlinkages and the timescales on which they operate.

TL;DR: In this paper, it was shown that the reactive iron oxyhydroxide phase in a large variety of lacustrine and marine environments is nanophase goethite (α-FeOOH), rather than the assumed surface-complex-stabilized, two-line ferrihydrite and accompanying mixture of clay and oxy-roxide Fe-bearing phases.

TL;DR: In this paper, a combination of pore water and solid phase analysis was used to determine whether authigenic carbonate fluorapatite (CFA) is currently forming in the sediment at two locations (OMEX I and II) on the North Atlantic continental platform Goban Spur (southwest of Ireland).