Magnetostratigraphy of sediment cores from the Greenland Sea

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Hauptverfasser: Nowaczyk, Norbert R, Antonow, Martin
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1997
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author Nowaczyk, Norbert R
Antonow, Martin
author_facet Nowaczyk, Norbert R
Antonow, Martin
collection Datos científicos de ciencias marinas y ambientales
contents High-resolution magnetostratigraphic analysis of three sediment cores from the base of the volcanic seamount Vesteris Banken in the Greenland Basin and one core from the Jan Mayen Fracture Zone revealed records of three pronounced geomagnetic events within the last 200 ka. Dating by stable carbon and oxygen isotope analysis, AMS14C measurements and biostratigraphic data (foraminifera abundances) yielded ages of 28-27 ka for the Mono Lake excursion, 37-33 ka for the Laschamp event, and 189-179 ka for the Biwa I event. In at least one of the cores the Laschamp event exhibits a full reversal of the local geomagnetic field vector. The same is true of the Biwa I event, documented in one of the cores.
format Dataset Open Access
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institution PANGAEA
language en
publishDate 1997
publisher PANGAEA
record_format pangaea
spellingShingle Magnetostratigraphy of sediment cores from the Greenland Sea
Nowaczyk, Norbert R
Antonow, Martin
ARK-V/2; ARK-VII/1; AWI_Paleo; Giant box corer; GIK21702-2 PS13/132; GIK21707-1 PS13/149; GIK21707-2 PS13/149; GIK21878-3 PS17/050; GIK21882-2 PS17/056; GIK21892-3 PS17/067; GKG; Greenland Sea; Jan Mayen Fracture Zone; KAL; Kasten corer; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13; PS17; PS1702-2; PS1707-1; PS1707-2; PS1878-3; PS1882-2; PS1892-3; Vesteris Banken
High-resolution magnetostratigraphic analysis of three sediment cores from the base of the volcanic seamount Vesteris Banken in the Greenland Basin and one core from the Jan Mayen Fracture Zone revealed records of three pronounced geomagnetic events within the last 200 ka. Dating by stable carbon and oxygen isotope analysis, AMS14C measurements and biostratigraphic data (foraminifera abundances) yielded ages of 28-27 ka for the Mono Lake excursion, 37-33 ka for the Laschamp event, and 189-179 ka for the Biwa I event. In at least one of the cores the Laschamp event exhibits a full reversal of the local geomagnetic field vector. The same is true of the Biwa I event, documented in one of the cores.
title Magnetostratigraphy of sediment cores from the Greenland Sea
topic ARK-V/2; ARK-VII/1; AWI_Paleo; Giant box corer; GIK21702-2 PS13/132; GIK21707-1 PS13/149; GIK21707-2 PS13/149; GIK21878-3 PS17/050; GIK21882-2 PS17/056; GIK21892-3 PS17/067; GKG; Greenland Sea; Jan Mayen Fracture Zone; KAL; Kasten corer; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13; PS17; PS1702-2; PS1707-1; PS1707-2; PS1878-3; PS1882-2; PS1892-3; Vesteris Banken
url https://doi.org/10.1594/PANGAEA.730507