This paper is the first comprehensive synthesis of what is currently known about the different
natural and anthropogenic fluxes of rhenium (Re) on Earth's surface. We highlight the …

High-resolution Os isotope stratigraphy can aid in reconstructing Pleistocene ice sheet
fluctuation and elucidating the role of local and regional weathering fluxes on the marine Os …

Compared to continental crust, marine sediments accumulating beneath O 2 depleted
waters are enriched in Re and Mo, with Re/Mo ratios that vary by more than two orders of …

Horizon scanning is an increasingly common strategy to identify key research needs and
frame future agendas in science. Here, we present the results of the first such exercise for …

The nitrogen (N) isotopic composition (δ 15 N) of bulk sedimentary N (δ 15 N bulk) is a
common tool for studying past biogeochemical cycling in the paleoceanographic record …

The proposed Anthropocene Global Boundary Stratotype Section and Point (GSSP)
candidate site of West Flower Garden Bank (27.8762° N, 93.8147° W) is an open ocean …

Deep-sea corals are important components of the benthos in the Gulf of Mexico, because
they provide structural complexity to associated species of fish and invertebrates, and they …

The oxidation of petrogenic organic carbon (OCpetro) is a source of carbon dioxide to the
atmosphere over geological timescales. The rates of OCpetro oxidation in locations that …

Compound-specific stable isotopes of amino acids (CSI-AA) from proteinaceous deep-sea
coral skeletons have the potential to improve paleoreconstructions of plankton community …

Ongoing human activities are known to affect nitrogen cycling on coral reefs, but the full
history of anthropogenic impact is unclear due to a lack of continuous records. We have …