Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ...
Instrumental monitoring of the climate at high northern latitudes has documented the ongoing warming of the last few decades. Climate modelling has also demonstrated that the global warming signal will be amplified in the polar region. Such temperature increases would have important implications on...
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ftdatacite:10.1594/pangaea.841926 2024-09-15T17:57:45+00:00 Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... Wilson, Laurie J Hald, Morten Godtliebsen, Fred 2011 application/zip https://dx.doi.org/10.1594/pangaea.841926 https://doi.pangaea.de/10.1594/PANGAEA.841926 en eng PANGAEA https://dx.doi.org/10.1177/0959683610385718 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Multiple investigations JM050704 Jan Mayen International Polar Year 2007-2008 IPY article Collection Supplementary Publication Series of Datasets 2011 ftdatacite https://doi.org/10.1594/pangaea.84192610.1177/0959683610385718 2024-08-01T10:52:43Z Instrumental monitoring of the climate at high northern latitudes has documented the ongoing warming of the last few decades. Climate modelling has also demonstrated that the global warming signal will be amplified in the polar region. Such temperature increases would have important implications on the ecosystem and biota of the Barents Sea. This study therefore aims to reconstruct the climatic changes of the Barents Sea based on benthic foraminifera over approximately the last 1400 years at the decadal to sub-decadal scale. Oxygen and carbon isotope analysis and benthic foraminiferal species counts indicate an overall warming trend of approximately 2.6°C through the 1400-year record. In addition, the well-documented cooling period equating to the 'Little Ice Age' is evident between c. 1650 and 1850. Most notably, a series of highly fluctuating temperatures are observed over the last century. An increase of 1.5°C is shown across this period. Thus for the first time we are able to demonstrate that the recent ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper Barents Sea International Polar Year IPY Jan Mayen DataCite |
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English |
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Multiple investigations JM050704 Jan Mayen International Polar Year 2007-2008 IPY |
spellingShingle |
Multiple investigations JM050704 Jan Mayen International Polar Year 2007-2008 IPY Wilson, Laurie J Hald, Morten Godtliebsen, Fred Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
topic_facet |
Multiple investigations JM050704 Jan Mayen International Polar Year 2007-2008 IPY |
description |
Instrumental monitoring of the climate at high northern latitudes has documented the ongoing warming of the last few decades. Climate modelling has also demonstrated that the global warming signal will be amplified in the polar region. Such temperature increases would have important implications on the ecosystem and biota of the Barents Sea. This study therefore aims to reconstruct the climatic changes of the Barents Sea based on benthic foraminifera over approximately the last 1400 years at the decadal to sub-decadal scale. Oxygen and carbon isotope analysis and benthic foraminiferal species counts indicate an overall warming trend of approximately 2.6°C through the 1400-year record. In addition, the well-documented cooling period equating to the 'Little Ice Age' is evident between c. 1650 and 1850. Most notably, a series of highly fluctuating temperatures are observed over the last century. An increase of 1.5°C is shown across this period. Thus for the first time we are able to demonstrate that the recent ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... |
format |
Article in Journal/Newspaper |
author |
Wilson, Laurie J Hald, Morten Godtliebsen, Fred |
author_facet |
Wilson, Laurie J Hald, Morten Godtliebsen, Fred |
author_sort |
Wilson, Laurie J |
title |
Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
title_short |
Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
title_full |
Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
title_fullStr |
Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
title_full_unstemmed |
Radiocarbon age, and sedimentation and accumulation rate of core JM05-G001 obtained during Jan Mayen cruise JM050704 to the Barents Sea ... |
title_sort |
radiocarbon age, and sedimentation and accumulation rate of core jm05-g001 obtained during jan mayen cruise jm050704 to the barents sea ... |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://dx.doi.org/10.1594/pangaea.841926 https://doi.pangaea.de/10.1594/PANGAEA.841926 |
genre |
Barents Sea International Polar Year IPY Jan Mayen |
genre_facet |
Barents Sea International Polar Year IPY Jan Mayen |
op_relation |
https://dx.doi.org/10.1177/0959683610385718 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.84192610.1177/0959683610385718 |
_version_ |
1810433910318825472 |