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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Main Authors: Knudsen, Karen Luise, Eiriksson, Jón, Jansen, Eystein, Jiang, Hui, Rytter, Frank, Gudmundsdóttir, Esther Ruth
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.900082
https://doi.pangaea.de/10.1594/PANGAEA.900082
id ftdatacite:10.1594/pangaea.900082
record_format openpolar
spelling 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
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