Nitrogen (N) is used in many of life's fundamental biomolecules, and it is also a participant in
environmental redox chemistry. Biogeochemical processes control the amount and form of N …

Ocean biogeochemical models describe the ocean's circulation, physical properties,
biogeochemical properties and their transformations using coupled differential equations …

Dissolved oxygen (O2) is essential for most ocean ecosystems, fuelling organisms'
respiration and facilitating the cycling of carbon and nutrients. Oxygen measurements have …

Climate-driven redistribution of tuna threatens to disrupt the economies of Pacific Small
Island Develo** States (SIDS) and sustainable management of the world's largest tuna …

The biological carbon pump (BCP) stores∼ 1,700 Pg C from the atmosphere in the ocean
interior, but the magnitude and direction of future changes in carbon sequestration by the …

Climate change is driving an expansion of marine oxygen-deficient zones, which may alter
the global cycles of carbon, sulfur, nitrogen, and trace metals. Currently, however, we lack a …

The global ocean's oxygen inventory is declining in response to global warming, but the
future of the low-oxygen tropics is uncertain. We report new evidence for tropical …

Abstract The North Pacific Subtropical Gyre (NPSG) is an oligotrophic environment where a
number of mesoscale eddies occur. With continuous measurements from Biogeochemical …

The global ocean is losing oxygen with warming. Observations and Earth system model
projections, however, suggest that this global ocean deoxygenation does not equate to a …

Oxygen deficient zones (ODZs) in the tropical ocean exert a profound influence on global
biogeochemical cycles, but the factors that regulate their long‐term structure and sensitivity …