The Scotia Sea and surrounding Scotia Arc have evolved over the past 40 Ma, by extension
behind an east-migrating subduction zone, at the boundary between the South American …

Geophysical and geological data indicate that during the last glacial cycle a palaeo-ice
stream drained the Antarctic Peninsula Ice Sheet (APIS) through Marguerite Bay to the edge …

The present paper is mostly a synthesis of work conducted on the continental margin of the
Gulf of Cádiz using a broad database collected by several cruises and projects supported by …

Since 1995 several ice shelves in the Northern Antarctic Peninsula have collapsed and
triggered ice-mass unloading, invoking a solid Earth response that has been recorded at …

Fast-flowing ice streams and outlet glaciers currently account for as much as 90% of the
discharge from the Antarctic and Greenland Ice Sheets. Although the deformation of …

Geophysical data from the Antarctic Peninsula continental shelf reveal streamlined
subglacial bedforms in a cross‐shelf trough. Bedforms exhibit progressive elongation with …

The evolutionary and biogeographic history of the contemporary Antarctic terrestrial and
marine biotas reveals many components of ancient origin. For large elements of the …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

The presence of a complex bedform arrangement on the sea floor of the continental shelf in
the western Amundsen Sea Embayment, West Antarctica, indicates a multi-temporal record …

The upper mantle and transition zone beneath Antarctica and the surrounding oceans are
among the poorest‐imaged regions of the Earth's interior. Over the last 15 years, several …