Climate models with biogeochemical components predict declines in oceanic dissolved
oxygen with global warming. In coastal regimes oxygen deficits represent acute ecosystem …

The intensity, duration and frequency of coastal hypoxia (oxygen concentration< 63 μM) are
increasing due to human alteration of coastal ecosystems and changes in oceanographic …

Organic carbon processing at the seafloor is studied by biogeochemists to quantify burial
and respiration, by organic geochemists to elucidate compositional changes and by …

Decreasing concentrations of dissolved oxygen in the ocean are considered one of the main
threats to marine ecosystems as they jeopardize the growth of higher organisms. They also …

Accurate representation of the remineralization of sinking organic matter is crucial for
reliable projections of the marine carbon cycle. Both water temperature and oxygen …

To assess whether the oxygen minimum zone (OMZ) across the Pakistan Margin causes
differences in the lability of sedimentary organic matter, sediments were collected in the core …

Decreasing concentrations of dissolved oxygen and the resulting expansion of anaerobic
ecosystems is a major threat to marine ecosystem services because it favors the formation of …

To quantify how fish farming modifies short‐term benthic carbon cycling in fjord
environments and the role of hydrodynamics in modifying effects on the benthos, we …

Deep-sea sediments cover∼ 70% of Earth's surface and represent the largest interface
between the biological and geological cycles of carbon. Diatoms and zooplankton faecal …

Oxygen minimum zones (OMZs) impinging on continental margins present sharp gradients
ideal for testing environmental factors thought to influence C cycling and other benthic …