Oceanographic conditions in the deepest parts of the Kattegat, Scandinavia, revealed through recent benthic foraminifera and hydrography
The Kattegat has, since the 1980s, been subject to extensive investigations focusing on various aspects of the marine environment. The most important reasons for this concentration of work are marine eutrophication, periodically occurring oxygen deficiency in the bottom-water and subsequent benthic mortality. In this study a previously not discussed sill area separating two deep areas in the Katte
