Submarine groundwater discharge (SGD) is now recognized as an important process of the
hydrological cycle worldwide and plays a major role as a conveyor of dissolved compounds …

The biogeochemical cycles of trace elements and their isotopes (TEIs) constitute an active
area of oceanographic research due to their role as essential nutrients for marine organisms …

Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …

Retrograde clay mineral reactions (reverse weathering), including glauconite formation, are
first-order controls on element sequestration in marine sediments. Here, we report …

Rising temperatures in the Arctic Ocean region are responsible for changes such as
reduced ice cover, permafrost thawing, and increased river discharge, which, together, alter …

Land to ocean transfer of material largely controls the chemical composition of seawater and
the global element cycles. Oceanic isotopic budgets of chemical species, macro-and …

Quantifying fluxes of trace elements and their isotopes (TEIs) at the ocean's sediment–water
boundary is a pre-eminent challenge to understand their role in the present, past and future …

Dissolved manganese (Mn) is a biologically essential element. Moreover, its oxidised form is
involved in removing itself and several other trace elements from ocean waters. Here we …

Upwelling of subsurface waters injects macronutrients (fixed N, P, and Si) and micronutrient
trace metals (TMs) into surface waters supporting elevated primary production in Eastern …

Hydrothermal activity occurs in all ocean basins, releasing high concentrations of key trace
elements and isotopes (TEIs) into the oceans. Importantly, the calculated rate of entrainment …