Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia

Palaeoenvironmental changes since the late Younger Dryas are reconstructed in the southern Kattegat (Scandinavia) and provide a basis for correlating the whole of the North Sea-Skagerrak- Kattegat-Baltic region. The foraminiferal content of seven piston and three vibrocores were analysed. Radiocarbo...

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Published in:The Holocene
Main Author: Conradsen, Keld
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1995
Subjects:
Online Access:http://dx.doi.org/10.1177/095968369500500407
http://journals.sagepub.com/doi/pdf/10.1177/095968369500500407
id crsagepubl:10.1177/095968369500500407
record_format openpolar
spelling crsagepubl:10.1177/095968369500500407 2024-04-07T07:50:31+00:00 Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia Conradsen, Keld 1995 http://dx.doi.org/10.1177/095968369500500407 http://journals.sagepub.com/doi/pdf/10.1177/095968369500500407 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 5, issue 4, page 447-456 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 1995 crsagepubl https://doi.org/10.1177/095968369500500407 2024-03-08T03:20:45Z Palaeoenvironmental changes since the late Younger Dryas are reconstructed in the southern Kattegat (Scandinavia) and provide a basis for correlating the whole of the North Sea-Skagerrak- Kattegat-Baltic region. The foraminiferal content of seven piston and three vibrocores were analysed. Radiocarbon dates were obtained from four of the cores. Relatively warm water masses occurred in the shallow areas of the Kattegat during the late Younger Dryas and early Preboreal, while cold, arctic/ subarctic water masses occurred in deeper parts of the Kattegat and Skagerrak. Full interglacial temperature conditions developed in the southern Kattegat at 9600 BP. A sea-level rise is recorded at 9600-8200 BP, a period during which the Skagerrak-Kattegat area experienced a gradual warming. A change in sedimentological and environmental conditions occurred in the southern Kattegat at around 8000 BP, reflecting the opening of a connection to the Baltic and corresponding hydrographic changes. The modem general circulation pattern of the area was established after this event. A further rise in sea level is recorded after 8000 BP. A mid-Holocene alteration in hydrographic and sedimentation pattern in the area is marked by the reappearance of Nonionellina labradorica in the southern Kattegat. This alteration, previously dated to 4000 BP, is redated to 5500 BP and is interpreted as reflecting the well- defined late-Atlantic cooling of the North Atlantic region resulting in changed inflow/outflow pattern of water masses in the Kattegat. Article in Journal/Newspaper Arctic Foraminifera* North Atlantic Subarctic SAGE Publications Arctic Kattegat ENVELOPE(9.692,9.692,63.563,63.563) The Holocene 5 4 447 456
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
topic Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
spellingShingle Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
Conradsen, Keld
Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
topic_facet Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
description Palaeoenvironmental changes since the late Younger Dryas are reconstructed in the southern Kattegat (Scandinavia) and provide a basis for correlating the whole of the North Sea-Skagerrak- Kattegat-Baltic region. The foraminiferal content of seven piston and three vibrocores were analysed. Radiocarbon dates were obtained from four of the cores. Relatively warm water masses occurred in the shallow areas of the Kattegat during the late Younger Dryas and early Preboreal, while cold, arctic/ subarctic water masses occurred in deeper parts of the Kattegat and Skagerrak. Full interglacial temperature conditions developed in the southern Kattegat at 9600 BP. A sea-level rise is recorded at 9600-8200 BP, a period during which the Skagerrak-Kattegat area experienced a gradual warming. A change in sedimentological and environmental conditions occurred in the southern Kattegat at around 8000 BP, reflecting the opening of a connection to the Baltic and corresponding hydrographic changes. The modem general circulation pattern of the area was established after this event. A further rise in sea level is recorded after 8000 BP. A mid-Holocene alteration in hydrographic and sedimentation pattern in the area is marked by the reappearance of Nonionellina labradorica in the southern Kattegat. This alteration, previously dated to 4000 BP, is redated to 5500 BP and is interpreted as reflecting the well- defined late-Atlantic cooling of the North Atlantic region resulting in changed inflow/outflow pattern of water masses in the Kattegat.
format Article in Journal/Newspaper
author Conradsen, Keld
author_facet Conradsen, Keld
author_sort Conradsen, Keld
title Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
title_short Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
title_full Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
title_fullStr Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
title_full_unstemmed Late Younger Dryas to Holocene palaeoenvironments of the southern Kattegat, Scandinavia
title_sort late younger dryas to holocene palaeoenvironments of the southern kattegat, scandinavia
publisher SAGE Publications
publishDate 1995
url http://dx.doi.org/10.1177/095968369500500407
http://journals.sagepub.com/doi/pdf/10.1177/095968369500500407
long_lat ENVELOPE(9.692,9.692,63.563,63.563)
geographic Arctic
Kattegat
geographic_facet Arctic
Kattegat
genre Arctic
Foraminifera*
North Atlantic
Subarctic
genre_facet Arctic
Foraminifera*
North Atlantic
Subarctic
op_source The Holocene
volume 5, issue 4, page 447-456
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/095968369500500407
container_title The Holocene
container_volume 5
container_issue 4
container_start_page 447
op_container_end_page 456
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