Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea

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Autores principales: Risebrobakken, Bjørg, Jansen, Eystein, Andersson, Carin, Mjelde, Eirik, Hevroy, Kjersti
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2003
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author Risebrobakken, Bjørg
Jansen, Eystein
Andersson, Carin
Mjelde, Eirik
Hevroy, Kjersti
author_facet Risebrobakken, Bjørg
Jansen, Eystein
Andersson, Carin
Mjelde, Eirik
Hevroy, Kjersti
collection Datos científicos de ciencias marinas y ambientales
contents 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 Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_760166
institution PANGAEA
language en
publishDate 2003
publisher PANGAEA
record_format pangaea
spellingShingle Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea
Risebrobakken, Bjørg
Jansen, Eystein
Andersson, Carin
Mjelde, Eirik
Hevroy, Kjersti
CALYPSO; Calypso Corer; Giant box corer; GKG; IMAGES; IMAGES I; International Marine Global Change Study; JM97-948/2A; Marion Dufresne (1995); MD101__Campaign; MD952011; MD95-2011; Voring Plateau
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.
title Planktonic foraminiferal and stable oxygen isotope record of Holocene sediments from the Norwegian Sea
topic CALYPSO; Calypso Corer; Giant box corer; GKG; IMAGES; IMAGES I; International Marine Global Change Study; JM97-948/2A; Marion Dufresne (1995); MD101__Campaign; MD952011; MD95-2011; Voring Plateau
url https://doi.org/10.1594/PANGAEA.760166