Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ...
Palaeoclimatic changes through the last 1200 calibrated years have been documented by high-resolution multi-proxy studies of three cores from about 400 m water depth on the North Icelandic shelf. Benthic and planktonic foraminiferal assemblages and stable isotope values, as well as ice rafted debris...
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Online Access: | https://dx.doi.org/10.1594/pangaea.900082 https://doi.pangaea.de/10.1594/PANGAEA.900082 |
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ftdatacite:10.1594/pangaea.900082 2024-02-04T10:01:33+01:00 Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... Knudsen, Karen Luise Eiriksson, Jón Jansen, Eystein Jiang, Hui Rytter, Frank Gudmundsdóttir, Esther Ruth 2019 application/zip https://dx.doi.org/10.1594/pangaea.900082 https://doi.pangaea.de/10.1594/PANGAEA.900082 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2004.08.012 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Benthic foraminifera Last millennium North Icelandic shelf Palaeoceanography Planktonic foraminifera Stable isotopes Composite Core Collection article Supplementary Publication Series of Datasets 2019 ftdatacite https://doi.org/10.1594/pangaea.90008210.1016/j.quascirev.2004.08.012 2024-01-05T00:50:36Z Palaeoclimatic changes through the last 1200 calibrated years have been documented by high-resolution multi-proxy studies of three cores from about 400 m water depth on the North Icelandic shelf. Benthic and planktonic foraminiferal assemblages and stable isotope values, as well as ice rafted debris (IRD) concentrations, are compared with diatom-based sea-surface water temperatures and the reconstructed mean temperature for the Northern Hemisphere. Changes in surface and bottom water characteristics are mainly due to variations in the strength of the relatively warm, high-salinity Irminger Current and the cold East Icelandic Current. The time period between 1200 and around 7–800 cal. (years) BP, including the Medieval Warm Period, was characterized by relatively high bottom and surface water temperatures due to the inflow of Atlantic water masses. After that, a general temperature decrease in the area marks the transition to a period with increased influence of the East Icelandic Current and, at the sea ... : Associated Projects and funding: HOLSMEER and PACLIVA projects funded by the European Commission's 5th Framework Programme (Contracts no. CT-2000-00060 and EVK2-2002-00143); PANIS project (Palaeoenvironments on the North Icelandic shelf); BIOICE project (Benthic Invertebrates of Icelandic Waters). Financial support by the Danish Natural Science Research Council, the Icelandic Research Council and the National Natural Science Foundation of China (Grant no. 40276013) ... Article in Journal/Newspaper Iceland Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Benthic foraminifera Last millennium North Icelandic shelf Palaeoceanography Planktonic foraminifera Stable isotopes Composite Core |
spellingShingle |
Benthic foraminifera Last millennium North Icelandic shelf Palaeoceanography Planktonic foraminifera Stable isotopes Composite Core Knudsen, Karen Luise Eiriksson, Jón Jansen, Eystein Jiang, Hui Rytter, Frank Gudmundsdóttir, Esther Ruth Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
topic_facet |
Benthic foraminifera Last millennium North Icelandic shelf Palaeoceanography Planktonic foraminifera Stable isotopes Composite Core |
description |
Palaeoclimatic changes through the last 1200 calibrated years have been documented by high-resolution multi-proxy studies of three cores from about 400 m water depth on the North Icelandic shelf. Benthic and planktonic foraminiferal assemblages and stable isotope values, as well as ice rafted debris (IRD) concentrations, are compared with diatom-based sea-surface water temperatures and the reconstructed mean temperature for the Northern Hemisphere. Changes in surface and bottom water characteristics are mainly due to variations in the strength of the relatively warm, high-salinity Irminger Current and the cold East Icelandic Current. The time period between 1200 and around 7–800 cal. (years) BP, including the Medieval Warm Period, was characterized by relatively high bottom and surface water temperatures due to the inflow of Atlantic water masses. After that, a general temperature decrease in the area marks the transition to a period with increased influence of the East Icelandic Current and, at the sea ... : Associated Projects and funding: HOLSMEER and PACLIVA projects funded by the European Commission's 5th Framework Programme (Contracts no. CT-2000-00060 and EVK2-2002-00143); PANIS project (Palaeoenvironments on the North Icelandic shelf); BIOICE project (Benthic Invertebrates of Icelandic Waters). Financial support by the Danish Natural Science Research Council, the Icelandic Research Council and the National Natural Science Foundation of China (Grant no. 40276013) ... |
format |
Article in Journal/Newspaper |
author |
Knudsen, Karen Luise Eiriksson, Jón Jansen, Eystein Jiang, Hui Rytter, Frank Gudmundsdóttir, Esther Ruth |
author_facet |
Knudsen, Karen Luise Eiriksson, Jón Jansen, Eystein Jiang, Hui Rytter, Frank Gudmundsdóttir, Esther Ruth |
author_sort |
Knudsen, Karen Luise |
title |
Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
title_short |
Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
title_full |
Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
title_fullStr |
Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
title_full_unstemmed |
Palaeoceanographic changes off North Iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
title_sort |
palaeoceanographic changes off north iceland through the last 1200 years: foraminifera, stable isotopes, diatoms and ice rafted debris ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.900082 https://doi.pangaea.de/10.1594/PANGAEA.900082 |
genre |
Iceland Planktonic foraminifera |
genre_facet |
Iceland Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2004.08.012 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.90008210.1016/j.quascirev.2004.08.012 |
_version_ |
1789967519230984192 |