▪ Abstract Most of our knowledge of biodiversity and its causes in the deep-sea benthos
derives from regional-scale sampling studies of the macrofauna. Improved sampling …

Subaqueous sediment density flows are one of the volumetrically most important processes
for moving sediment across our planet, and form the largest sediment accumulations on …

The outer parts of a number of small Late Jurassic sandy deep‐water fans in the northern
North Sea are dominated by the stacked deposits of co‐genetic sandy and muddy gravity …

Microbial community samples were collected from the anoxic zone of the Cariaco Basin at
depths of 320, 500, and 1,310 m on a November 1996 cruise and were used to construct …

Turbidite records along ocean margins and in lake basins are increasingly used as
paleoseismic proxies. However, the slope remobilization processes that formed the …

The hadal zone largely comprises a series of subduction trenches that do not form part of the
continental shelf-slope rise to abyssal plain continuum. Instead they form geographically …

Monthly hydrographic, primary production, bacterial production, and settling particulate
carbon flux observations were collected between November 1995 and December 1997 at …

The hydrography of the Cariaco Basin (temperature, salinity, density, dissolved oxygen
concentration) was studied using monthly observations collected between November 1995 …

The submerged portions of the North Anatolia Fault system beneath the Marmara Sea were
studied with high-resolution multibeam bathymetry, subbottom profiling and sediment cores …

During the late glacial, marine isotope Stage 2, the Marmara Sea transformed into a
brackish lake as global sea-level fell below the sill in the Dardanelles Strait. A record of the …