'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia

Previous reports have suggested climatic fluctuations as a possible factor controlling 'blooms' of the toxic dinoflagellate Gymnodinium catenatum Graham 1943 that occurred in Scandinavian waters at about 4000 and between 2000 and 300 BP. Evidence of climatic fluctuations associated with th...

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Published in:The Holocene
Main Authors: Thorsen, Thor A., Dale, Barrie, Nordberg, Kjell
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1995
Subjects:
Online Access:http://dx.doi.org/10.1177/095968369500500406
http://journals.sagepub.com/doi/pdf/10.1177/095968369500500406
id crsagepubl:10.1177/095968369500500406
record_format openpolar
spelling crsagepubl:10.1177/095968369500500406 2023-05-15T17:47:06+02:00 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia Thorsen, Thor A. Dale, Barrie Nordberg, Kjell 1995 http://dx.doi.org/10.1177/095968369500500406 http://journals.sagepub.com/doi/pdf/10.1177/095968369500500406 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 5, issue 4, page 435-446 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 1995 crsagepubl https://doi.org/10.1177/095968369500500406 2022-08-12T11:31:58Z Previous reports have suggested climatic fluctuations as a possible factor controlling 'blooms' of the toxic dinoflagellate Gymnodinium catenatum Graham 1943 that occurred in Scandinavian waters at about 4000 and between 2000 and 300 BP. Evidence of climatic fluctuations associated with the younger 'blooms', which correspond to the Mediaeval Warm Epoch, is presented here from detailed dinoflagellate cyst records in a 860-cm sediment core from the southern Kattegat. Peak concentrations of the cosmopolitan cyst Operculodinium centrocarpum (Deflandre and Cookson) Wall 1967 suggest environmental changes at about 2000 BP associated with the initial phase of the 'blooms', and at about 300 BP corresponding to the waning phase. Since G. catenatum is only recorded in small amounts from the region today, and otherwise is more characteristic of warmer water, its 'blooms' are considered probable evidence of warmer sea-surface temperatures between 2000 and 300 BP. Supporting evidence for this is provided by peak concentrations of G. catenatum dated to about 830 BP. The occurrence of the extremely cold oceanic species Impagidinium pallidum Bujak 1984 and the cold-water species Protoperidinium conicoides (Paulsen) Balech 1974 in two consecutive samples at 400 BP probably indicate increased influence of colder oceanic waters from the Norwegian Sea. This corresponds to the beginning of the 'Little Ice Age' which most likely contributed to the subsequent waning of the 'blooms'. Article in Journal/Newspaper Norwegian Sea SAGE Publications (via Crossref) Kattegat ENVELOPE(9.692,9.692,63.563,63.563) Norwegian Sea The Holocene 5 4 435 446
institution Open Polar
collection SAGE Publications (via Crossref)
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
Thorsen, Thor A.
Dale, Barrie
Nordberg, Kjell
'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
topic_facet Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
description Previous reports have suggested climatic fluctuations as a possible factor controlling 'blooms' of the toxic dinoflagellate Gymnodinium catenatum Graham 1943 that occurred in Scandinavian waters at about 4000 and between 2000 and 300 BP. Evidence of climatic fluctuations associated with the younger 'blooms', which correspond to the Mediaeval Warm Epoch, is presented here from detailed dinoflagellate cyst records in a 860-cm sediment core from the southern Kattegat. Peak concentrations of the cosmopolitan cyst Operculodinium centrocarpum (Deflandre and Cookson) Wall 1967 suggest environmental changes at about 2000 BP associated with the initial phase of the 'blooms', and at about 300 BP corresponding to the waning phase. Since G. catenatum is only recorded in small amounts from the region today, and otherwise is more characteristic of warmer water, its 'blooms' are considered probable evidence of warmer sea-surface temperatures between 2000 and 300 BP. Supporting evidence for this is provided by peak concentrations of G. catenatum dated to about 830 BP. The occurrence of the extremely cold oceanic species Impagidinium pallidum Bujak 1984 and the cold-water species Protoperidinium conicoides (Paulsen) Balech 1974 in two consecutive samples at 400 BP probably indicate increased influence of colder oceanic waters from the Norwegian Sea. This corresponds to the beginning of the 'Little Ice Age' which most likely contributed to the subsequent waning of the 'blooms'.
format Article in Journal/Newspaper
author Thorsen, Thor A.
Dale, Barrie
Nordberg, Kjell
author_facet Thorsen, Thor A.
Dale, Barrie
Nordberg, Kjell
author_sort Thorsen, Thor A.
title 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
title_short 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
title_full 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
title_fullStr 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
title_full_unstemmed 'Blooms' of the toxic dinoflagellate Gymnodinium catenatum as evidence of climatic fluctuations in the late Holocene of southwestern Scandinavia
title_sort 'blooms' of the toxic dinoflagellate gymnodinium catenatum as evidence of climatic fluctuations in the late holocene of southwestern scandinavia
publisher SAGE Publications
publishDate 1995
url http://dx.doi.org/10.1177/095968369500500406
http://journals.sagepub.com/doi/pdf/10.1177/095968369500500406
long_lat ENVELOPE(9.692,9.692,63.563,63.563)
geographic Kattegat
Norwegian Sea
geographic_facet Kattegat
Norwegian Sea
genre Norwegian Sea
genre_facet Norwegian Sea
op_source The Holocene
volume 5, issue 4, page 435-446
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/095968369500500406
container_title The Holocene
container_volume 5
container_issue 4
container_start_page 435
op_container_end_page 446
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