Sedimentology on cores off the South Orkney Plateau
Grab samples and cores for sedimentological studies were retrieved along a N-S transect of the South Orkney Plateau margin. On the basis of morphology, the margin has been subdivided into shelf, upper continental slope, and a lower slope region cut by basins and ridges. Grain size, Sand component, a...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1991
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.860528 https://doi.org/10.1594/PANGAEA.860528 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860528 |
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openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
ANT-II/3 AWI_Paleo Giant box corer GKG Gravity corer (Kiel type) KL_Mk Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer Meischner small Polarstern PS04 PS04/254 PS04/256 PS04/257 PS04/258 PS1167-10 PS1169-1 PS1170-1 PS1170-4 PS1171-1 SL South Orkney Weddell Sea |
spellingShingle |
ANT-II/3 AWI_Paleo Giant box corer GKG Gravity corer (Kiel type) KL_Mk Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer Meischner small Polarstern PS04 PS04/254 PS04/256 PS04/257 PS04/258 PS1167-10 PS1169-1 PS1170-1 PS1170-4 PS1171-1 SL South Orkney Weddell Sea Grünig, Sigrun Sedimentology on cores off the South Orkney Plateau |
topic_facet |
ANT-II/3 AWI_Paleo Giant box corer GKG Gravity corer (Kiel type) KL_Mk Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer Meischner small Polarstern PS04 PS04/254 PS04/256 PS04/257 PS04/258 PS1167-10 PS1169-1 PS1170-1 PS1170-4 PS1171-1 SL South Orkney Weddell Sea |
description |
Grab samples and cores for sedimentological studies were retrieved along a N-S transect of the South Orkney Plateau margin. On the basis of morphology, the margin has been subdivided into shelf, upper continental slope, and a lower slope region cut by basins and ridges. Grain size, Sand component, and clay mineralogy were determined as well as water, organic carbon and carbonate contents. In addition, vane shear strength, magnetic intensity and the proportion of ice-rafted debris were measured, dating was done by detailed magnetic stratigraphy, the biofluctuation of the radiolarian Cycladophora davisiana and 230-Thorium analyses. Sediment facies distribution is controlled by numerous factors such as regional bathymetry and circulation, biogenic productivity, seasonal ice cover and the deposition of terrigenous detritus by ice-rafting, bottom water transport and/or slumping. The complex interrelationship between these factors results in three main categories of sediment facies. The diamict facies is interpreted as an interglacial facies. It is composed of clayey silt and silt and is characterised by a large component of coarse, ice-rafted material such as gravel and sand (IRD). This generally strongly bioturbated sediment contains radiolarian and diatom-rich layers as well as horizons of lower water and organic carbon content. Magnetic intensities, related to volcanic ash particles, glauconite, and micromanganese nodules as well as a large quantity of rock fragments, are low. The biosiliceous and IRD content decreases from north to south along the South Orkney transect because of seasonal ice margin fluctuations, thus resulting in barren and IRD-poor interglacial deposits in the southern region. Apart from ice-rafting and biogenic productivity, bottom currents also exert a strong control on the distribution of this facies. Strong and fluctuating bottom current influence is documented by the sediment structures in this facies. The homogenous clay facies was deposited during glacial periods. These silty clays are ... |
format |
Other/Unknown Material |
author |
Grünig, Sigrun |
author_facet |
Grünig, Sigrun |
author_sort |
Grünig, Sigrun |
title |
Sedimentology on cores off the South Orkney Plateau |
title_short |
Sedimentology on cores off the South Orkney Plateau |
title_full |
Sedimentology on cores off the South Orkney Plateau |
title_fullStr |
Sedimentology on cores off the South Orkney Plateau |
title_full_unstemmed |
Sedimentology on cores off the South Orkney Plateau |
title_sort |
sedimentology on cores off the south orkney plateau |
publisher |
PANGAEA |
publishDate |
1991 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.860528 https://doi.org/10.1594/PANGAEA.860528 |
op_coverage |
MEDIAN LATITUDE: -63.569845 * MEDIAN LONGITUDE: -44.463850 * SOUTH-BOUND LATITUDE: -63.959160 * WEST-BOUND LONGITUDE: -44.608299 * NORTH-BOUND LATITUDE: -63.458301 * EAST-BOUND LONGITUDE: -44.047000 * DATE/TIME START: 1983-12-12T00:00:00 * DATE/TIME END: 1983-12-13T00:00:00 |
long_lat |
ENVELOPE(-44.608299,-44.047000,-63.458301,-63.959160) |
genre |
Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research Weddell Sea |
genre_facet |
Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research Weddell Sea |
op_source |
Supplement to: Grünig, Sigrun (1991): Quartäre Sedimentationsprozesse am Kontinentalhang des Süd-Orkney-Plateaus im nordwestlichen Weddellmeer (Antarktis) (Quaternary sedimentation processes on the continental margin of the South Orkney Plateau, NW Weddell Sea (Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 75, 196 pp, https://doi.org/10.2312/BzP_0075_1991 |
op_relation |
Brehme, Isa (1992): Sedimentfazies und Bodenwasserstrom am Kontinentalhang des nordwestlichen Weddellmeeres (Sediment facies and bottomwater current on the continental slope in the northwestern Weddell Sea). Berichte zur Polarforschung = Reports on Polar Research, 110, 127 pp, https://doi.org/10.2312/BzP_0110_1992 Fütterer, Dieter K (1984): Die Expedition ANTARKTIS-II mit FS POLARSTERN 1983/84. Berichte zur Polarforschung = Reports on Polar Research, 18, 92 pp, https://doi.org/10.2312/BzP_0018_1984 Fütterer, Dieter K; Grobe, Hannes; Grünig, Sigrun (1988): Quaternary sediment patterns in the Weddell Sea: relations and environmental conditions. Paleoceanography, 3(5), 551-561, https://doi.org/10.1029/PA003i005p00551 https://doi.pangaea.de/10.1594/PANGAEA.860528 https://doi.org/10.1594/PANGAEA.860528 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.86052810.2312/BzP_0075_199110.2312/BzP_0110_199210.2312/BzP_0018_198410.1029/PA003i005p00551 |
_version_ |
1810436287667109888 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860528 2024-09-15T17:59:14+00:00 Sedimentology on cores off the South Orkney Plateau Grünig, Sigrun MEDIAN LATITUDE: -63.569845 * MEDIAN LONGITUDE: -44.463850 * SOUTH-BOUND LATITUDE: -63.959160 * WEST-BOUND LONGITUDE: -44.608299 * NORTH-BOUND LATITUDE: -63.458301 * EAST-BOUND LONGITUDE: -44.047000 * DATE/TIME START: 1983-12-12T00:00:00 * DATE/TIME END: 1983-12-13T00:00:00 1991 application/zip, 14 datasets https://doi.pangaea.de/10.1594/PANGAEA.860528 https://doi.org/10.1594/PANGAEA.860528 en eng PANGAEA Brehme, Isa (1992): Sedimentfazies und Bodenwasserstrom am Kontinentalhang des nordwestlichen Weddellmeeres (Sediment facies and bottomwater current on the continental slope in the northwestern Weddell Sea). Berichte zur Polarforschung = Reports on Polar Research, 110, 127 pp, https://doi.org/10.2312/BzP_0110_1992 Fütterer, Dieter K (1984): Die Expedition ANTARKTIS-II mit FS POLARSTERN 1983/84. Berichte zur Polarforschung = Reports on Polar Research, 18, 92 pp, https://doi.org/10.2312/BzP_0018_1984 Fütterer, Dieter K; Grobe, Hannes; Grünig, Sigrun (1988): Quaternary sediment patterns in the Weddell Sea: relations and environmental conditions. Paleoceanography, 3(5), 551-561, https://doi.org/10.1029/PA003i005p00551 https://doi.pangaea.de/10.1594/PANGAEA.860528 https://doi.org/10.1594/PANGAEA.860528 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Grünig, Sigrun (1991): Quartäre Sedimentationsprozesse am Kontinentalhang des Süd-Orkney-Plateaus im nordwestlichen Weddellmeer (Antarktis) (Quaternary sedimentation processes on the continental margin of the South Orkney Plateau, NW Weddell Sea (Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 75, 196 pp, https://doi.org/10.2312/BzP_0075_1991 ANT-II/3 AWI_Paleo Giant box corer GKG Gravity corer (Kiel type) KL_Mk Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer Meischner small Polarstern PS04 PS04/254 PS04/256 PS04/257 PS04/258 PS1167-10 PS1169-1 PS1170-1 PS1170-4 PS1171-1 SL South Orkney Weddell Sea dataset publication series 1991 ftpangaea https://doi.org/10.1594/PANGAEA.86052810.2312/BzP_0075_199110.2312/BzP_0110_199210.2312/BzP_0018_198410.1029/PA003i005p00551 2024-07-24T02:31:21Z Grab samples and cores for sedimentological studies were retrieved along a N-S transect of the South Orkney Plateau margin. On the basis of morphology, the margin has been subdivided into shelf, upper continental slope, and a lower slope region cut by basins and ridges. Grain size, Sand component, and clay mineralogy were determined as well as water, organic carbon and carbonate contents. In addition, vane shear strength, magnetic intensity and the proportion of ice-rafted debris were measured, dating was done by detailed magnetic stratigraphy, the biofluctuation of the radiolarian Cycladophora davisiana and 230-Thorium analyses. Sediment facies distribution is controlled by numerous factors such as regional bathymetry and circulation, biogenic productivity, seasonal ice cover and the deposition of terrigenous detritus by ice-rafting, bottom water transport and/or slumping. The complex interrelationship between these factors results in three main categories of sediment facies. The diamict facies is interpreted as an interglacial facies. It is composed of clayey silt and silt and is characterised by a large component of coarse, ice-rafted material such as gravel and sand (IRD). This generally strongly bioturbated sediment contains radiolarian and diatom-rich layers as well as horizons of lower water and organic carbon content. Magnetic intensities, related to volcanic ash particles, glauconite, and micromanganese nodules as well as a large quantity of rock fragments, are low. The biosiliceous and IRD content decreases from north to south along the South Orkney transect because of seasonal ice margin fluctuations, thus resulting in barren and IRD-poor interglacial deposits in the southern region. Apart from ice-rafting and biogenic productivity, bottom currents also exert a strong control on the distribution of this facies. Strong and fluctuating bottom current influence is documented by the sediment structures in this facies. The homogenous clay facies was deposited during glacial periods. These silty clays are ... Other/Unknown Material Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research Weddell Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-44.608299,-44.047000,-63.458301,-63.959160) |