Geological structure changes, including deformations and ruptures, developed in shallow
marine sediments are well recognized but were not systematically reviewed in previous …

Contourites are common morphological features along continental margins where currents
encounter the seafloor. They can provide long-term archives of palaeoceanography, may be …

Deep-sea coral distribution and composition are unknown in much of the global ocean, but
repurposing ocean industry surveys can fill that gap. In Santos Basin, southeast Brazil, areas …

Efforts to understand how Pleistocene climate changes were translated into fluctuations in
ice sheet extent and volume are limited by a lack of consensus about the glacial history of …

Pockmarks are prominent morphological features formed by fluid escape at the seafloor that
provide valuable information on past environmental conditions and ongoing sedimentary …

An association of authigenic pyrite and gypsum has been found in deep-sea sediments from
a core retrieved on the continental slope of the Santos Basin, South Atlantic. Pyrite occur …

In this study, we use inorganic (metal) and organic (bulk and molecular) markers in sediment
samples of the south-eastern Brazilian margin to investigate the response of geochemical …

New bathymetric and subsurface data from the Santos Basin, offshore southeast Brazil,
reveal sharp lateral morphological variations facing the margin-parallel (along-margin) flow …

The Patras Gulf Pockmark field is located in shallow waters offshore Patras City (Greece)
and is considered one of the most spectacular and best-documented fluid seepage activities …

Seafloor pockmarks are abundant around Aotearoa New Zealand, occurring across a
diverse range of tectonic, sedimentological and geomorphological settings. Globally, the …