Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea
High-resolution records from IMAGES core MD95-2011 in the eastern Norwegian Sea provide evidence for relatively large- and small-scale high-latitude climate variability throughout the Holocene. During the early and mid-Holocene a situation possibly driven by consistent stronger westerlies increased...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.760166 2023-05-15T15:05:12+02:00 Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea Risebrobakken, Bjørg Jansen, Eystein Andersson, Carin Mjelde, Eirik Hevroy, Kjersti MEDIAN LATITUDE: 66.969738 * MEDIAN LONGITUDE: 7.639330 * SOUTH-BOUND LATITUDE: 66.969660 * WEST-BOUND LONGITUDE: 7.639330 * NORTH-BOUND LATITUDE: 66.969830 * EAST-BOUND LONGITUDE: 7.639330 * DATE/TIME START: 1995-06-08T00:00:00 * DATE/TIME END: 1995-06-08T00:00:00 2003-05-10 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.760166 https://doi.org/10.1594/PANGAEA.760166 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.760166 https://doi.org/10.1594/PANGAEA.760166 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Bjerknes Centre for Climate Research Supplement to: Risebrobakken, Bjørg; Jansen, Eystein; Andersson, Carin; Mjelde, Eirik; Hevroy, Kjersti (2003): A high-resolution study of Holocene paleoclimatic and paleoceanographic changes in the Nordic Seas. Paleoceanography, 18(1), 1017, https://doi.org/10.1029/2002PA000764 CALYPSO Calypso Corer Giant box corer GKG IMAGES IMAGES I International Marine Global Change Study JM97-948/2A Marion Dufresne (1995) MD101 MD952011 MD95-2011 Voring Plateau Dataset 2003 ftpangaea https://doi.org/10.1594/PANGAEA.760166 https://doi.org/10.1029/2002PA000764 2023-01-20T07:32:10Z High-resolution records from IMAGES core MD95-2011 in the eastern Norwegian Sea provide evidence for relatively large- and small-scale high-latitude climate variability throughout the Holocene. During the early and mid-Holocene a situation possibly driven by consistent stronger westerlies increased the eastward influence of Arctic intermediate and near-surface waters. For the late Holocene a relaxation of the atmospheric forcing resulted in increased influence of Atlantic water. The main changes in Holocene climate show no obvious connection to changing solar irradiance, and spectral analysis reveals no consistent signature for any periodic behavior of Holocene climate at millennial or centennial timescales. There are, however, indications of consistent multidecadal variability. Dataset Arctic Foraminifera* Norwegian Sea PANGAEA - Data Publisher for Earth & Environmental Science Arctic Norwegian Sea ENVELOPE(7.639330,7.639330,66.969830,66.969660) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
CALYPSO Calypso Corer Giant box corer GKG IMAGES IMAGES I International Marine Global Change Study JM97-948/2A Marion Dufresne (1995) MD101 MD952011 MD95-2011 Voring Plateau |
spellingShingle |
CALYPSO Calypso Corer Giant box corer GKG IMAGES IMAGES I International Marine Global Change Study JM97-948/2A Marion Dufresne (1995) MD101 MD952011 MD95-2011 Voring Plateau Risebrobakken, Bjørg Jansen, Eystein Andersson, Carin Mjelde, Eirik Hevroy, Kjersti Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
topic_facet |
CALYPSO Calypso Corer Giant box corer GKG IMAGES IMAGES I International Marine Global Change Study JM97-948/2A Marion Dufresne (1995) MD101 MD952011 MD95-2011 Voring Plateau |
description |
High-resolution records from IMAGES core MD95-2011 in the eastern Norwegian Sea provide evidence for relatively large- and small-scale high-latitude climate variability throughout the Holocene. During the early and mid-Holocene a situation possibly driven by consistent stronger westerlies increased the eastward influence of Arctic intermediate and near-surface waters. For the late Holocene a relaxation of the atmospheric forcing resulted in increased influence of Atlantic water. The main changes in Holocene climate show no obvious connection to changing solar irradiance, and spectral analysis reveals no consistent signature for any periodic behavior of Holocene climate at millennial or centennial timescales. There are, however, indications of consistent multidecadal variability. |
format |
Dataset |
author |
Risebrobakken, Bjørg Jansen, Eystein Andersson, Carin Mjelde, Eirik Hevroy, Kjersti |
author_facet |
Risebrobakken, Bjørg Jansen, Eystein Andersson, Carin Mjelde, Eirik Hevroy, Kjersti |
author_sort |
Risebrobakken, Bjørg |
title |
Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
title_short |
Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
title_full |
Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
title_fullStr |
Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
title_full_unstemmed |
Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea |
title_sort |
planktonic foraminiferal and stable oxygen isotope record of holocene sediments from the norwegian sea |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.760166 https://doi.org/10.1594/PANGAEA.760166 |
op_coverage |
MEDIAN LATITUDE: 66.969738 * MEDIAN LONGITUDE: 7.639330 * SOUTH-BOUND LATITUDE: 66.969660 * WEST-BOUND LONGITUDE: 7.639330 * NORTH-BOUND LATITUDE: 66.969830 * EAST-BOUND LONGITUDE: 7.639330 * DATE/TIME START: 1995-06-08T00:00:00 * DATE/TIME END: 1995-06-08T00:00:00 |
long_lat |
ENVELOPE(7.639330,7.639330,66.969830,66.969660) |
geographic |
Arctic Norwegian Sea |
geographic_facet |
Arctic Norwegian Sea |
genre |
Arctic Foraminifera* Norwegian Sea |
genre_facet |
Arctic Foraminifera* Norwegian Sea |
op_source |
Bjerknes Centre for Climate Research Supplement to: Risebrobakken, Bjørg; Jansen, Eystein; Andersson, Carin; Mjelde, Eirik; Hevroy, Kjersti (2003): A high-resolution study of Holocene paleoclimatic and paleoceanographic changes in the Nordic Seas. Paleoceanography, 18(1), 1017, https://doi.org/10.1029/2002PA000764 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.760166 https://doi.org/10.1594/PANGAEA.760166 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.760166 https://doi.org/10.1029/2002PA000764 |
_version_ |
1766336942432059392 |