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Autor principal: Blanz, Thomas
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1992
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Acceso en línea:https://doi.org/10.1594/PANGAEA.785253
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author Blanz, Thomas
author_facet Blanz, Thomas
collection Datos científicos de ciencias marinas y ambientales
contents For the first time detailed physical properties were measured in addition to sedimentological parameters of near surface sediments of Kattegat channel system. This study has been accomplished on two sediment cores of different waterdepth of each Alkor-deep and Littorina-deep. The sediments of Littorina-deep, which have been dated with 210Pb-method, turned out to be surprisingly recent, with sedimentation rates up to 3,2 cm/year. Differences in physical properties lead to the assumption of lower sedimentation rates in Alkor-deep, the velocities of bottom and deepwater currents could be the cause of these differences in sedimentation rates. In Alkor-deep, the morphology runs parallel to the main direction of the bottom current. Therefore higher current velocities can be reached, which favor the erosion of fine sediment particles. Littorina-deep is located rectangular to the main direction of bottom currents. This might lead to an 'overflow' situation instead of a 'flow through'.
format Dataset Open Access
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institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle (Table 2) Presence of plant remains in sediment core GIK14973, northern Kattegat
Blanz, Thomas
Calcium carbonate; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK14973; KAL; Kasten corer; Littorina-Deep, Kattegat; Plant debris; POS170; Poseidon
For the first time detailed physical properties were measured in addition to sedimentological parameters of near surface sediments of Kattegat channel system. This study has been accomplished on two sediment cores of different waterdepth of each Alkor-deep and Littorina-deep. The sediments of Littorina-deep, which have been dated with 210Pb-method, turned out to be surprisingly recent, with sedimentation rates up to 3,2 cm/year. Differences in physical properties lead to the assumption of lower sedimentation rates in Alkor-deep, the velocities of bottom and deepwater currents could be the cause of these differences in sedimentation rates. In Alkor-deep, the morphology runs parallel to the main direction of the bottom current. Therefore higher current velocities can be reached, which favor the erosion of fine sediment particles. Littorina-deep is located rectangular to the main direction of bottom currents. This might lead to an 'overflow' situation instead of a 'flow through'.
title (Table 2) Presence of plant remains in sediment core GIK14973, northern Kattegat
topic Calcium carbonate; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK14973; KAL; Kasten corer; Littorina-Deep, Kattegat; Plant debris; POS170; Poseidon
url https://doi.org/10.1594/PANGAEA.785253