Sedimentology on two cores from Scoresby Sund, Greenland

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Autor principal: Marienfeld, Peter
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1992
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author Marienfeld, Peter
author_facet Marienfeld, Peter
collection Datos científicos de ciencias marinas y ambientales
contents Reconstruction of the postglacial palaeoenvironmental evolution was the main objective of marine geological investigations in the Scorcsby Sund fjord system. For this purpose, samples of marine sediments, taken on RV Polarstern cruises ARK-V/3b and ARK-VII/3b in 1988 and 1990, have been analysed. All investigated fjord sediments are paratills. However, remarkable changes in sediment fabric and composition occur with depth in cores. They are attributable to different modes of sediment deposition. Therefore, a subdivision of the postglacial palaeoenvironmental history into periods of considerably different sedimentary conditions is feasible. The change of sedimentary fades with time is interpreted by deposition under changing climatic conditions during the postglacial. Displacements of cyclonic and anticyclonic centers in the atmosphere change amount of precipitation at the east coast of Greenland. Precipitation strongly influences extension of local ice caps of coastal areas and duration of coverage of the fjords by sea ice. These factors again control the sedimentary regime in the fjord system.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_763190
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle Sedimentology on two cores from Scoresby Sund, Greenland
Marienfeld, Peter
ARK-V/3b; AWI_Paleo; GIK21718-1 PS13/170; GIK21719-1 PS13/172; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1718-1; PS1719-1; Quaternary Environment of the Eurasian North; QUEEN; Scoresby Sund; SL
Reconstruction of the postglacial palaeoenvironmental evolution was the main objective of marine geological investigations in the Scorcsby Sund fjord system. For this purpose, samples of marine sediments, taken on RV Polarstern cruises ARK-V/3b and ARK-VII/3b in 1988 and 1990, have been analysed. All investigated fjord sediments are paratills. However, remarkable changes in sediment fabric and composition occur with depth in cores. They are attributable to different modes of sediment deposition. Therefore, a subdivision of the postglacial palaeoenvironmental history into periods of considerably different sedimentary conditions is feasible. The change of sedimentary fades with time is interpreted by deposition under changing climatic conditions during the postglacial. Displacements of cyclonic and anticyclonic centers in the atmosphere change amount of precipitation at the east coast of Greenland. Precipitation strongly influences extension of local ice caps of coastal areas and duration of coverage of the fjords by sea ice. These factors again control the sedimentary regime in the fjord system.
title Sedimentology on two cores from Scoresby Sund, Greenland
topic ARK-V/3b; AWI_Paleo; GIK21718-1 PS13/170; GIK21719-1 PS13/172; Gravity corer (Kiel type); Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS1718-1; PS1719-1; Quaternary Environment of the Eurasian North; QUEEN; Scoresby Sund; SL
url https://doi.org/10.1594/PANGAEA.763190