_version_ 1867169500911108096
author Marienfeld, Peter
author_facet Marienfeld, Peter
collection Datos científicos de ciencias marinas y ambientales
contents The fjord system of Scoresby Sund on the east coast of Greenland has been the subject of two research cruises by RV Polarstern in 1988 and 1990. Most of the year, the fjord is covered by sea-ice. Sediment input takes place mostly via drifting icebergs during the short summer period. Depending on the distance to glaciers, surface sediments carry varying proportions of coarse ice-rafted debris (IRD). The degree of sediment reworking by scouring icebergs is controlled by the depth of the fjord, with the most intense reworking in areas shallower than about 450 m depth. Both IRD contribution and intensity of sediment scouring clearly control the distribution pattern of benthic organisms.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_738370
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle Sedimentology of the Scoresby Sund, East Greenland
Marienfeld, Peter
ARK-V/3b; ARK-VII/3b; AWI_Paleo; Giant box corer; GIK21709-2 PS13/151; GIK21710-1 PS13/156; GIK21712-1 PS13/160; GIK21713-1 PS13/161; GIK21714-1 PS13/165; GIK21715-2 PS13/166; GIK21716-1 PS13/167; GIK21717-1 PS13/169; GIK21733-1 PS13/240; GIK21734-1 PS13/247; GIK21735-2 PS13/249; GKG; Gravity corer (Kiel type); Greenland Shelf; King Oskar Fjord; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS17; PS17/252; PS17/260; PS17/275; PS17/276; PS17/277; PS17/281; PS17/282; PS17/283; PS1709-2; PS1710-1; PS1712-1; PS1713-1; PS1714-1; PS1715-2; PS1716-1; PS1717-1; PS1733-1; PS1734-1; PS1735-2; PS1928-1; PS1931-1; PS1940-1; PS1941-1; PS1942-1; PS1943-1; PS1944-1; PS1945-1; Scoresby Sund; SL
The fjord system of Scoresby Sund on the east coast of Greenland has been the subject of two research cruises by RV Polarstern in 1988 and 1990. Most of the year, the fjord is covered by sea-ice. Sediment input takes place mostly via drifting icebergs during the short summer period. Depending on the distance to glaciers, surface sediments carry varying proportions of coarse ice-rafted debris (IRD). The degree of sediment reworking by scouring icebergs is controlled by the depth of the fjord, with the most intense reworking in areas shallower than about 450 m depth. Both IRD contribution and intensity of sediment scouring clearly control the distribution pattern of benthic organisms.
title Sedimentology of the Scoresby Sund, East Greenland
topic ARK-V/3b; ARK-VII/3b; AWI_Paleo; Giant box corer; GIK21709-2 PS13/151; GIK21710-1 PS13/156; GIK21712-1 PS13/160; GIK21713-1 PS13/161; GIK21714-1 PS13/165; GIK21715-2 PS13/166; GIK21716-1 PS13/167; GIK21717-1 PS13/169; GIK21733-1 PS13/240; GIK21734-1 PS13/247; GIK21735-2 PS13/249; GKG; Gravity corer (Kiel type); Greenland Shelf; King Oskar Fjord; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS13 GRÖKORT; PS17; PS17/252; PS17/260; PS17/275; PS17/276; PS17/277; PS17/281; PS17/282; PS17/283; PS1709-2; PS1710-1; PS1712-1; PS1713-1; PS1714-1; PS1715-2; PS1716-1; PS1717-1; PS1733-1; PS1734-1; PS1735-2; PS1928-1; PS1931-1; PS1940-1; PS1941-1; PS1942-1; PS1943-1; PS1944-1; PS1945-1; Scoresby Sund; SL
url https://doi.org/10.1594/PANGAEA.738370