The trophic resource continuum (TRC) in euphotic zones of the world's oceans is the
spectrum of conditions from the richest runoff and upwelling areas to the most nutrient …

Reconstruction of Atlantic Ocean vertical and meridional water characteristics is based on
combined synoptic fossil census data, stable isotope records, and measurements of …

At two locations in the Atlantic Ocean (DSDP Sites 367 and 530) early to middle Cretaceous
organic-carbon-rich beds (“black shales”) were found to have significantly lower δ 15 N …

The proportion of the organic carbon produced in oceanic surface waters that is buried in the
underlying sediments is highly variable. The organic-carbon preservation factor, the …

The distribution of sapropelic sediments in the early South Atlantic Ocean is used to test
palaeocirculation models related to oxygen-deficient conditions. The data presented here …

Abstract The Middle Cambrian to Tremadoc Scandinavian alum shales are highly
condensed sediments, notably enriched in organic matter. Sedimentological studies alone …

An extensive and abrupt biotic turnover marking the Cenomanian-Turonian (Cretaceous)
stage boundary occurred just prior to maximum transgression of the Middle Cretaceous …

The field of paleoceanography experienced continued growth during the last three years.
The First International Conference on Paleoceanography was held in Zürich, Switzerland, in …

A simple steady-state 1-D model of the oceanic particulate organic carbon, dissolved
oxygen and dissolved phosphate system has been developed to study global and basin …

Foraminifera have been a very successful group of protozoans for over 500 million years.
Loeblich and Tappan recogtuzed 220 foraminifera1 families;'species counts exceed 25,000 …