Sedimentology on Quaternary depoits from the Weddell Sea continental slope
Sedimentological, geochemical (in particular biogenic content) and physical properties from the Weddell, Lazarev and Cosmonaut seas along the Antarctic continental margin were analysed in order to reconstruct the late Quaternary productivity and sedimentary processes of this region. Seven undisturbe...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2009
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.729792 https://doi.org/10.1594/PANGAEA.729792 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.729792 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
ANT-IX/3 ANT-VI/3 ANT-VIII/6 Atka Bay AWI_Paleo Fram Strait Gravity corer (Kiel type) Lazarev Sea Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS12 PS12/248 PS12/536 PS1575-1 PS16 PS16/534 PS16/541 PS1648-1 PS18 PS18/184 PS18/185 PS18/186 PS18/187 PS18/191 PS18/192 PS18/193 PS18/194 PS18/196 PS18/198 PS18/203 PS18/204 PS1821-6 PS1824-1 PS2037-3 PS2038-2 PS2039-1 PS2040-2 PS2044-1 PS2045-3 PS2046-1 PS2047-3 PS2049-4 PS2050-1 PS2055-2 PS2056-1 Silicon Cycling in the World Ocean SINOPS SL South Orkney |
spellingShingle |
ANT-IX/3 ANT-VI/3 ANT-VIII/6 Atka Bay AWI_Paleo Fram Strait Gravity corer (Kiel type) Lazarev Sea Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS12 PS12/248 PS12/536 PS1575-1 PS16 PS16/534 PS16/541 PS1648-1 PS18 PS18/184 PS18/185 PS18/186 PS18/187 PS18/191 PS18/192 PS18/193 PS18/194 PS18/196 PS18/198 PS18/203 PS18/204 PS1821-6 PS1824-1 PS2037-3 PS2038-2 PS2039-1 PS2040-2 PS2044-1 PS2045-3 PS2046-1 PS2047-3 PS2049-4 PS2050-1 PS2055-2 PS2056-1 Silicon Cycling in the World Ocean SINOPS SL South Orkney Bonn, Wolfgang J Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
topic_facet |
ANT-IX/3 ANT-VI/3 ANT-VIII/6 Atka Bay AWI_Paleo Fram Strait Gravity corer (Kiel type) Lazarev Sea Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS12 PS12/248 PS12/536 PS1575-1 PS16 PS16/534 PS16/541 PS1648-1 PS18 PS18/184 PS18/185 PS18/186 PS18/187 PS18/191 PS18/192 PS18/193 PS18/194 PS18/196 PS18/198 PS18/203 PS18/204 PS1821-6 PS1824-1 PS2037-3 PS2038-2 PS2039-1 PS2040-2 PS2044-1 PS2045-3 PS2046-1 PS2047-3 PS2049-4 PS2050-1 PS2055-2 PS2056-1 Silicon Cycling in the World Ocean SINOPS SL South Orkney |
description |
Sedimentological, geochemical (in particular biogenic content) and physical properties from the Weddell, Lazarev and Cosmonaut seas along the Antarctic continental margin were analysed in order to reconstruct the late Quaternary productivity and sedimentary processes of this region. Seven undisturbed sediment cores were chosen. The sediments represent a depositional period from 400,000 years to the recent time. The late Quaternary climatic changes influence changes in the paleoenvironmental and the geological conditions, directly forced by the behaviour of the Antarctic ice sheet. All investigated cores are positioned within the oscillating ice sheet area and reflect the influence of the ice sheet in response to the climatic cycles. The organic carbon, carbonate, biogenic opal, and barium contents were measured, andlor calculated, together with the determination by XRD of the terrigenous components such as quartz and plagioclase (expressed as relative to corundum standard). The contents of organic carbon and carbonate in general are very low. The results provide an indication that organic carbon content is a preservation signal and not a productivity signal. Carbonate is not correlated with biogenic opal and biogenic barium. Profiles of biogenic opal and barium were measured within the sediment cores providing a qualitative and quantitative tool to estimate changes in paleoproductivity over the investigated time. Generally, good correlations between the barium and opal records of the sediment cores indicate that dissolution of opal in the water column and the sediment does not obscure the surface productivity signal. Therefore, opal can be used in combination with other proxies for paleoproductivity discussions in this area. Maximum paleoproductivity rates (PPmax) during peak warm stages reach values between 82-345 gC/m2/a and maximum export productivity rates (Pnew, max) between 14-177 gC/m2/a, that are representative of high-productivity areas. They are drastically reduced during glacial times (PPmax = 14-107 ... |
format |
Other/Unknown Material |
author |
Bonn, Wolfgang J |
author_facet |
Bonn, Wolfgang J |
author_sort |
Bonn, Wolfgang J |
title |
Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
title_short |
Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
title_full |
Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
title_fullStr |
Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
title_full_unstemmed |
Sedimentology on Quaternary depoits from the Weddell Sea continental slope |
title_sort |
sedimentology on quaternary depoits from the weddell sea continental slope |
publisher |
PANGAEA |
publishDate |
2009 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.729792 https://doi.org/10.1594/PANGAEA.729792 |
op_coverage |
MEDIAN LATITUDE: -68.870024 * MEDIAN LONGITUDE: 3.942645 * SOUTH-BOUND LATITUDE: -69.773380 * WEST-BOUND LONGITUDE: -43.335500 * NORTH-BOUND LATITUDE: -62.849500 * EAST-BOUND LONGITUDE: 37.480500 * DATE/TIME START: 1987-12-26T13:05:00 * DATE/TIME END: 1991-03-06T18:15:00 |
long_lat |
ENVELOPE(-43.335500,37.480500,-62.849500,-69.773380) |
genre |
Antarc* Antarctic Berichte zur Polarforschung Fram Strait Ice Sheet Lazarev Sea Polar Research Polarforschung Reports on polar research Weddell Sea |
genre_facet |
Antarc* Antarctic Berichte zur Polarforschung Fram Strait Ice Sheet Lazarev Sea Polar Research Polarforschung Reports on polar research Weddell Sea |
op_source |
Supplement to: Bonn, Wolfgang J (1995): Biogenopal und biogenes Barium als Indikatoren für spätquartäre Produktivitätsänderungen am antarktischen Kontinentalhang, atlantischer Sektor (Biogenic opal and barium: Indicators for late Quarternary changes in productivity at the Antarctic continental margin, Atlantic Sector). Berichte zur Polarforschung = Reports on Polar Research, 180, 186 pp, https://doi.org/10.2312/BzP_0180_1995 |
op_relation |
Bonn, Wolfgang J; Fütterer, Dieter K; Grobe, Hannes (1994): Quaternary sedimentation at the Antarctic continental margin. Terra Antartica, 1(2), 319-320, hdl:10013/epic.10991.d001 Bonn, Wolfgang J; Gingele, Franz; Grobe, Hannes; Mackensen, Andreas; Fütterer, Dieter K (1998): Palaeoproductivity at the Antarctic continental margin: opal and barium records for the last 400 ka. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 195-211, https://doi.org/10.1016/S0031-0182(97)00144-2 https://doi.pangaea.de/10.1594/PANGAEA.729792 https://doi.org/10.1594/PANGAEA.729792 |
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.72979210.2312/BzP_0180_199510.1016/S0031-0182(97)00144-2 |
_version_ |
1810289085363781632 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.729792 2024-09-15T17:48:05+00:00 Sedimentology on Quaternary depoits from the Weddell Sea continental slope Bonn, Wolfgang J MEDIAN LATITUDE: -68.870024 * MEDIAN LONGITUDE: 3.942645 * SOUTH-BOUND LATITUDE: -69.773380 * WEST-BOUND LONGITUDE: -43.335500 * NORTH-BOUND LATITUDE: -62.849500 * EAST-BOUND LONGITUDE: 37.480500 * DATE/TIME START: 1987-12-26T13:05:00 * DATE/TIME END: 1991-03-06T18:15:00 2009 application/zip, 44 datasets https://doi.pangaea.de/10.1594/PANGAEA.729792 https://doi.org/10.1594/PANGAEA.729792 en eng PANGAEA Bonn, Wolfgang J; Fütterer, Dieter K; Grobe, Hannes (1994): Quaternary sedimentation at the Antarctic continental margin. Terra Antartica, 1(2), 319-320, hdl:10013/epic.10991.d001 Bonn, Wolfgang J; Gingele, Franz; Grobe, Hannes; Mackensen, Andreas; Fütterer, Dieter K (1998): Palaeoproductivity at the Antarctic continental margin: opal and barium records for the last 400 ka. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 195-211, https://doi.org/10.1016/S0031-0182(97)00144-2 https://doi.pangaea.de/10.1594/PANGAEA.729792 https://doi.org/10.1594/PANGAEA.729792 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Bonn, Wolfgang J (1995): Biogenopal und biogenes Barium als Indikatoren für spätquartäre Produktivitätsänderungen am antarktischen Kontinentalhang, atlantischer Sektor (Biogenic opal and barium: Indicators for late Quarternary changes in productivity at the Antarctic continental margin, Atlantic Sector). Berichte zur Polarforschung = Reports on Polar Research, 180, 186 pp, https://doi.org/10.2312/BzP_0180_1995 ANT-IX/3 ANT-VI/3 ANT-VIII/6 Atka Bay AWI_Paleo Fram Strait Gravity corer (Kiel type) Lazarev Sea Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS12 PS12/248 PS12/536 PS1575-1 PS16 PS16/534 PS16/541 PS1648-1 PS18 PS18/184 PS18/185 PS18/186 PS18/187 PS18/191 PS18/192 PS18/193 PS18/194 PS18/196 PS18/198 PS18/203 PS18/204 PS1821-6 PS1824-1 PS2037-3 PS2038-2 PS2039-1 PS2040-2 PS2044-1 PS2045-3 PS2046-1 PS2047-3 PS2049-4 PS2050-1 PS2055-2 PS2056-1 Silicon Cycling in the World Ocean SINOPS SL South Orkney dataset publication series 2009 ftpangaea https://doi.org/10.1594/PANGAEA.72979210.2312/BzP_0180_199510.1016/S0031-0182(97)00144-2 2024-07-24T02:31:20Z Sedimentological, geochemical (in particular biogenic content) and physical properties from the Weddell, Lazarev and Cosmonaut seas along the Antarctic continental margin were analysed in order to reconstruct the late Quaternary productivity and sedimentary processes of this region. Seven undisturbed sediment cores were chosen. The sediments represent a depositional period from 400,000 years to the recent time. The late Quaternary climatic changes influence changes in the paleoenvironmental and the geological conditions, directly forced by the behaviour of the Antarctic ice sheet. All investigated cores are positioned within the oscillating ice sheet area and reflect the influence of the ice sheet in response to the climatic cycles. The organic carbon, carbonate, biogenic opal, and barium contents were measured, andlor calculated, together with the determination by XRD of the terrigenous components such as quartz and plagioclase (expressed as relative to corundum standard). The contents of organic carbon and carbonate in general are very low. The results provide an indication that organic carbon content is a preservation signal and not a productivity signal. Carbonate is not correlated with biogenic opal and biogenic barium. Profiles of biogenic opal and barium were measured within the sediment cores providing a qualitative and quantitative tool to estimate changes in paleoproductivity over the investigated time. Generally, good correlations between the barium and opal records of the sediment cores indicate that dissolution of opal in the water column and the sediment does not obscure the surface productivity signal. Therefore, opal can be used in combination with other proxies for paleoproductivity discussions in this area. Maximum paleoproductivity rates (PPmax) during peak warm stages reach values between 82-345 gC/m2/a and maximum export productivity rates (Pnew, max) between 14-177 gC/m2/a, that are representative of high-productivity areas. They are drastically reduced during glacial times (PPmax = 14-107 ... Other/Unknown Material Antarc* Antarctic Berichte zur Polarforschung Fram Strait Ice Sheet Lazarev Sea Polar Research Polarforschung Reports on polar research Weddell Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-43.335500,37.480500,-62.849500,-69.773380) |