Webbläsaren som du använder stöds inte av denna webbplats. Alla versioner av Internet Explorer stöds inte längre, av oss eller Microsoft (läs mer här: * https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Var god och använd en modern webbläsare för att ta del av denna webbplats, som t.ex. nyaste versioner av Edge, Chrome, Firefox eller Safari osv.

Helena Filipsson, foto Erik Thor

Helena Filipsson

Professor

Helena Filipsson, foto Erik Thor

Oceanographic conditions in the deepest parts of the Kattegat, Scandinavia, revealed through recent benthic foraminifera and hydrography

Författare

  • K. Nordberg
  • H. Löfstedt Filipsson
  • B. Malmgren

Summary, in English

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 Kattegat has been identified. In the contexts of periodically occurring oxygen deficiency in the southern Kattegat, it is most relevant to study the environmental conditions in this area. Hydrographic data from the area inside and outside the sill area suggest that the deep-water on both sides of the sill do communicate. No evidence for stagnation in the deep area inside the sill was found. In addition to hydrography data, benthic foraminifera has been used as environmental tracers. Two characteristic benthic foraminiferal faunas have been defined one representing water depths; exceeding 80 m and one representing shallower depths. These faunas occur on both sides of the sill area. Two investigated deep depressions within the deep area inside the sill, the Alkor Depth (138 m) and Poseidon Depth (150 m) are marked by a fauna that is identical with that in the so-called Kattegat Trench. This suggests that the depressions are not more stagnant, if stagnant at all, than the surrounding Kattegat Trench and the Djupa Rannan Trench located outside the sill area. The information generated in this study is essential for the understanding of the processes resulting in oxygen deficiency in the deep water of the southern Kattegat.

Publiceringsår

1999-01-01

Språk

Engelska

Sidor

557-576

Publikation/Tidskrift/Serie

Estuarine, Coastal and Shelf Science

Volym

49

Issue

4

Dokumenttyp

Artikel i tidskrift

Förlag

Elsevier

Ämne

  • Oceanography, Hydrology, Water Resources

Nyckelord

  • Foraminifera
  • Hydrography
  • Kattegat
  • North Sea
  • Sill

Status

Published

ISBN/ISSN/Övrigt

  • ISSN: 0272-7714