Daniel Rey

TL;DR: The influence of environmental parameters on the living benthic foraminiferal assemblages was studied and a most sensitive group of species to higher concentrations of heavy metals is identified, a widespread condition in this lagoon.

TL;DR: The low-field magnetic susceptibility ( χ ) of surficial sediments from the Ria de Pontevedra (NW Spain) shows a characteristic, hydrodynamically driven textural control, where diamagnetic sandy bioclastic carbonates occur toward the coastline, leaving the finer muddy sediments to be deposited in the central and deeper areas of the ria as discussed by the authors.

TL;DR: In this paper, the authors examined core samples from the inner, middle and outer parts of the Ria de Pontevedra and found an abundance of terrestrial intensive weathering products near the ria head, a dominance of shelf-derived sediment towards the mouth and the presence of several diagenetic minerals whose nature varies with location within the region.

TL;DR: In this paper, the authors present a synthesis of results from a MIGRATE working group that focused on the definition and assessment of hydrate in Europe, including the western and eastern margins of Greenland, the Barents Sea and onshore and offshore Svalbard, the Atlantic margin of Europe, extending south to the northwestern margin of Morocco, the Mediterranean Sea, the Sea of Marmara, and the western, southern margins of the Black Sea.