Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73

Temperature and salinity reconstructions for two 1000-year high-resolution sedimentary records, located at the boundary between Atlantic and Arctic surface waters on the North Icelandic shelf, are based on transfer functions and oxygen isotopes for planktonic and benthic foraminifera. There is a gen...

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Main Authors: Knudsen, Karen Luise, Eiriksson, Jón, Bartels-Jonsdottir, Helga B
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.900268
https://doi.pangaea.de/10.1594/PANGAEA.900268
id ftdatacite:10.1594/pangaea.900268
record_format openpolar
spelling ftdatacite:10.1594/pangaea.900268 2023-05-15T15:00:58+02:00 Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73 Knudsen, Karen Luise Eiriksson, Jón Bartels-Jonsdottir, Helga B 2019 application/zip https://dx.doi.org/10.1594/pangaea.900268 https://doi.pangaea.de/10.1594/PANGAEA.900268 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1016/j.marmicro.2011.11.002 https://dx.doi.org/10.1177/0959683613479677 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Benthic and planktonic foraminifera Last millennium North Icelandic shelf Stable isotopes article Supplementary Collection of Datasets Collection 2019 ftdatacite https://doi.org/10.1594/pangaea.900268 https://doi.org/10.1016/j.marmicro.2011.11.002 https://doi.org/10.1177/0959683613479677 2022-02-09T13:17:41Z Temperature and salinity reconstructions for two 1000-year high-resolution sedimentary records, located at the boundary between Atlantic and Arctic surface waters on the North Icelandic shelf, are based on transfer functions and oxygen isotopes for planktonic and benthic foraminifera. There is a general increase of Arctic Water indicator species at the transition from the Medieval Warm Period into the Little Ice Age (LIA) and a subsequent return of Atlantic Water indicator species towards the end of the LIA and in the 20th century.The timing of the reconstructed temperature changes, both at the beginning and at the end of the LIA, appears to be slightly different for the different water masses. The earliest temperature change is seen in the bottom and subsurface waters, where a cooling is reconstructed as early as AD 1150-1200 at both locations, whereas previously published diatom-based and alkenone-based sea-surface temperature reconstructions show a change at AD 1300, coinciding with the air temperature shift in the area. Our results show the need of a thorough understanding of the oceanography in the study area, as well as the different living habitat for the biological proxies used for the temperature estimates. : Project affiliation and funding:European Commission MILLENNIUM Integrated Project (grant 017008).Unpublished pre - 1000 cal. BP isotope data provided by K. L. Knudsen and J. Eiríksson, funded by the Danish Natural Science Research Council, the Icelandic Research Council, and the European Commission's 5th Framework Programme PACLIVA (EVK2-2002-00143). Article in Journal/Newspaper Arctic Foraminifera* Iceland Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Arctic Knudsen ENVELOPE(16.057,16.057,67.137,67.137)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Benthic and planktonic foraminifera
Last millennium
North Icelandic shelf
Stable isotopes
spellingShingle Benthic and planktonic foraminifera
Last millennium
North Icelandic shelf
Stable isotopes
Knudsen, Karen Luise
Eiriksson, Jón
Bartels-Jonsdottir, Helga B
Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
topic_facet Benthic and planktonic foraminifera
Last millennium
North Icelandic shelf
Stable isotopes
description Temperature and salinity reconstructions for two 1000-year high-resolution sedimentary records, located at the boundary between Atlantic and Arctic surface waters on the North Icelandic shelf, are based on transfer functions and oxygen isotopes for planktonic and benthic foraminifera. There is a general increase of Arctic Water indicator species at the transition from the Medieval Warm Period into the Little Ice Age (LIA) and a subsequent return of Atlantic Water indicator species towards the end of the LIA and in the 20th century.The timing of the reconstructed temperature changes, both at the beginning and at the end of the LIA, appears to be slightly different for the different water masses. The earliest temperature change is seen in the bottom and subsurface waters, where a cooling is reconstructed as early as AD 1150-1200 at both locations, whereas previously published diatom-based and alkenone-based sea-surface temperature reconstructions show a change at AD 1300, coinciding with the air temperature shift in the area. Our results show the need of a thorough understanding of the oceanography in the study area, as well as the different living habitat for the biological proxies used for the temperature estimates. : Project affiliation and funding:European Commission MILLENNIUM Integrated Project (grant 017008).Unpublished pre - 1000 cal. BP isotope data provided by K. L. Knudsen and J. Eiríksson, funded by the Danish Natural Science Research Council, the Icelandic Research Council, and the European Commission's 5th Framework Programme PACLIVA (EVK2-2002-00143).
format Article in Journal/Newspaper
author Knudsen, Karen Luise
Eiriksson, Jón
Bartels-Jonsdottir, Helga B
author_facet Knudsen, Karen Luise
Eiriksson, Jón
Bartels-Jonsdottir, Helga B
author_sort Knudsen, Karen Luise
title Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
title_short Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
title_full Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
title_fullStr Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
title_full_unstemmed Oceanographic changes through the last millennium off North Iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: Knudsen, Karen Luise; Eiriksson, Jón; Bartels-Jonsdottir, Helga B (2012): Oceanographic changes through the last millennium off North Iceland: Temperature and salinity reconstructions based on foraminifera and stable isotopes. Marine Micropaleontology, 84-85, 54-73
title_sort oceanographic changes through the last millennium off north iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes, supplement to: knudsen, karen luise; eiriksson, jón; bartels-jonsdottir, helga b (2012): oceanographic changes through the last millennium off north iceland: temperature and salinity reconstructions based on foraminifera and stable isotopes. marine micropaleontology, 84-85, 54-73
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.900268
https://doi.pangaea.de/10.1594/PANGAEA.900268
long_lat ENVELOPE(16.057,16.057,67.137,67.137)
geographic Arctic
Knudsen
geographic_facet Arctic
Knudsen
genre Arctic
Foraminifera*
Iceland
Planktonic foraminifera
genre_facet Arctic
Foraminifera*
Iceland
Planktonic foraminifera
op_relation https://dx.doi.org/10.1016/j.marmicro.2011.11.002
https://dx.doi.org/10.1177/0959683613479677
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/pangaea.900268
https://doi.org/10.1016/j.marmicro.2011.11.002
https://doi.org/10.1177/0959683613479677
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