Understanding the nature of organic matter flux in the ocean remains a major goal of
oceanography because it impacts some of the most important processes in the ocean …

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 …

The biological carbon pump (BCP) comprises wide-ranging processes that set carbon
supply, consumption, and storage in the oceans' interior. It is becoming increasingly evident …

Sinking particulate organic carbon out of the surface ocean sequesters carbon on decadal to
millennial timescales. Predicting the particulate carbon flux is therefore critical for …

Quantitative knowledge about the burial of sedimentary components at the seafloor has
wide‐ranging implications in ocean science, from global climate to continental weathering …

Abstract 230Th normalization is a valuable paleoceanographic tool for reconstructing high‐
resolution sediment fluxes during the late Pleistocene (last~ 500,000 years). As its …

The biological pump supplies carbon to the oceans' interior, driving long-term carbon
sequestration and providing energy for deep-sea ecosystems,. Its efficiency is set by …

Export of sinking particles from the surface ocean is critical for carbon sequestration and to
provide energy to the deep biosphere. The magnitude and spatial patterns of this export …

Processes controlling dissolved barium (dBa) were investigated along the GEOTRACES
GA03 North Atlantic and GP16 Eastern Tropical Pacific transects, which traversed similar …

Organic matter (OM) plays a significant role in the formation of oxygen minimum zones
(OMZs) and associated biogeochemical cycling. OM supply processes to the OMZ include …