The narrow seaway between Greenland and Norway, in Cretaceous time was over 1500 km
long and 300+ km wide, and partly of bathyal water depth during Aptian through …

Previous work has shown that some foraminiferal species thrive in organically enriched,
oxygen-depleted environments. Here, we comparelive'(stained) faunas in multicorer …

Investigations of macrobenthos were carried out within and beneath the oxygen minimum
zone (OMZ,< 0.5 mll− 1) during Fall 1994 on the Oman margin, NW Arabian Sea. Six …

The surface mixed layer of sediment, which ranges in thickness from a few centimeters to as
much as a meter, acts as a low-pass filter that damps high frequency signals before their …

We studied Upper Cretaceous and Lower Paleogene benthic foraminifera from the Agost
section (southeastern Spain) to infer paleobathymetrical changes and paleoenvironmental …

Abstract The Santana Group, consisting of the Barbalha, Crato, Ipubi and Romualdo
formations, records the post-rift sequence of the Gondwana break-up in the Araripe Basin …

At present, environmental impacts from offshore oil and gas activities are partly determined
by measuring changes in macrofauna diversity. Morphological identification of macrofauna …

Benthic foraminiferal assemblages belonging to a mixed carbonate–siliciclastic shelf
succession of the Oxfordian (Upper Jurassic) in the Prebetic, southern Spain, were …

Morphogroups offer a way of overcoming taxonomic differences and thereby making
comparisons between assemblages of different geological ages. Relating morphogroups to …

"... bangs have replaced whimpers and the geological record has become much more
exciting than it was thought to be." Derek Ager (1993) The New Catastro phism. Cambridge …