(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region
A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assem...
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Language: | English |
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PANGAEA
2009
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.853649 https://doi.org/10.1594/PANGAEA.853649 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.853649 |
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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 |
ARK-IX/4 ARK-VIII/2 ARK-VIII/3 AWI_Paleo Barents Sea BC Bear Island Trough Box corer Center for Marine Environmental Sciences Chlorite DEPTH sediment/rock Elevation of event Event label Giant box corer GKG Gravity corer (Kiel type) HE153 HE153/1239-2 HE153/1240-2 HE153/1241-2 HE153/1242-2 HE153/1243-2 HE153/1244-2 HE153/1245-2 HE153/1246-2 HE153/1249-2 HE153/1250-2 HE153/1251-2 HE153/1254-2 HE153/1255-2 HE153/1258-1 HE153/1260-2 HE153/1261-2 HE153/1262-2 HE153/1263-2 HE153/1264-2 HE153/1265-2 HE153/1266-2 HE153/1267-2 HE153/1268-2 HE153/1269-2 HE153/1270-2 HE153/1272-2 HE153/1273-2 HE153/1274-2 HE153/1275-2 HE153/1276-2 HE153/1278-2 HE153/1279-2 |
spellingShingle |
ARK-IX/4 ARK-VIII/2 ARK-VIII/3 AWI_Paleo Barents Sea BC Bear Island Trough Box corer Center for Marine Environmental Sciences Chlorite DEPTH sediment/rock Elevation of event Event label Giant box corer GKG Gravity corer (Kiel type) HE153 HE153/1239-2 HE153/1240-2 HE153/1241-2 HE153/1242-2 HE153/1243-2 HE153/1244-2 HE153/1245-2 HE153/1246-2 HE153/1249-2 HE153/1250-2 HE153/1251-2 HE153/1254-2 HE153/1255-2 HE153/1258-1 HE153/1260-2 HE153/1261-2 HE153/1262-2 HE153/1263-2 HE153/1264-2 HE153/1265-2 HE153/1266-2 HE153/1267-2 HE153/1268-2 HE153/1269-2 HE153/1270-2 HE153/1272-2 HE153/1273-2 HE153/1274-2 HE153/1275-2 HE153/1276-2 HE153/1278-2 HE153/1279-2 Vogt, Christoph Knies, Jochen (Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
topic_facet |
ARK-IX/4 ARK-VIII/2 ARK-VIII/3 AWI_Paleo Barents Sea BC Bear Island Trough Box corer Center for Marine Environmental Sciences Chlorite DEPTH sediment/rock Elevation of event Event label Giant box corer GKG Gravity corer (Kiel type) HE153 HE153/1239-2 HE153/1240-2 HE153/1241-2 HE153/1242-2 HE153/1243-2 HE153/1244-2 HE153/1245-2 HE153/1246-2 HE153/1249-2 HE153/1250-2 HE153/1251-2 HE153/1254-2 HE153/1255-2 HE153/1258-1 HE153/1260-2 HE153/1261-2 HE153/1262-2 HE153/1263-2 HE153/1264-2 HE153/1265-2 HE153/1266-2 HE153/1267-2 HE153/1268-2 HE153/1269-2 HE153/1270-2 HE153/1272-2 HE153/1273-2 HE153/1274-2 HE153/1275-2 HE153/1276-2 HE153/1278-2 HE153/1279-2 |
description |
A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assemblages are related to the sub-Barents Sea geology because the Quaternary sediment cover is rather thin. Additionally, land masses like Svalbard and northern Scandinavia dominate the clay mineral signal with their erosional products. Dense bottom water, very often of brine origin, that flows within deep troughs, such as the Storfjorden or Bear Island Trough, transport the clay mineral signal from their origin to the Norwegian-Greenland Sea. |
format |
Dataset |
author |
Vogt, Christoph Knies, Jochen |
author_facet |
Vogt, Christoph Knies, Jochen |
author_sort |
Vogt, Christoph |
title |
(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
title_short |
(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
title_full |
(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
title_fullStr |
(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
title_full_unstemmed |
(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
title_sort |
(table 1) sample locations and clay mineral data of sediment surface samples from the barents sea region |
publisher |
PANGAEA |
publishDate |
2009 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.853649 https://doi.org/10.1594/PANGAEA.853649 |
op_coverage |
MEDIAN LATITUDE: 76.291341 * MEDIAN LONGITUDE: 20.062106 * SOUTH-BOUND LATITUDE: 70.440000 * WEST-BOUND LONGITUDE: 5.934500 * NORTH-BOUND LATITUDE: 82.166660 * EAST-BOUND LONGITUDE: 43.576667 * DATE/TIME START: 1991-06-23T16:22:00 * DATE/TIME END: 2001-09-12T00:00:00 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m |
long_lat |
ENVELOPE(-67.250,-67.250,-68.151,-68.151) ENVELOPE(5.934500,43.576667,82.166660,70.440000) |
geographic |
Svalbard Barents Sea Greenland Bear Island |
geographic_facet |
Svalbard Barents Sea Greenland Bear Island |
genre |
Arctic Barents Sea Bear Island Greenland Greenland Sea Storfjorden Svalbard |
genre_facet |
Arctic Barents Sea Bear Island Greenland Greenland Sea Storfjorden Svalbard |
op_source |
Supplement to: Vogt, Christoph; Knies, Jochen (2009): Sediment pathways in the western Barents Sea inferred from clay mineral assemblages in surface sediments. Norwegian Journal of Geology, 89(1-2), 41-55, https://www.geologi.no/images/njg/2009/1-2/Vogt_print.pdf |
op_relation |
Stein, Ruediger; Grobe, Hannes; Wahsner, Monika (1994): Organic carbon, carbonate, and clay mineral distributions in eastern central Arctic Ocean surface sediments. Marine Geology, 119(3-4), 269-285, https://doi.org/10.1016/0025-3227(94)90185-6 Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis. Boreas, 28(1), 215-233, https://doi.org/10.1111/j.1502-3885.1999.tb00216.x Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Distribution of clay minerals in surface sediments of the Eurasian Arctic Ocean. PANGAEA, https://doi.org/10.1594/PANGAEA.57249 Winkelmann, Daniel (2003): Reconstruction of recent and late Holocene sedimentation processes on the continental shelf west off Spitsbergen. MSc Thesis, Tech. Univ. of Freiberg, Germany, 156 pp Winkelmann, Daniel; Knies, Jochen (2005): Recent distribution and accumulation of organic carbon on the continental margin west off Spitsbergen. Geochemistry, Geophysics, Geosystems, 6(9), Q09012, https://doi.org/10.1029/2005GC000916 https://doi.pangaea.de/10.1594/PANGAEA.853649 https://doi.org/10.1594/PANGAEA.853649 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.853649 https://doi.org/10.1016/0025-3227(94)90185-6 https://doi.org/10.1111/j.1502-3885.1999.tb00216.x https://doi.org/10.1594/PANGAEA.57249 https://doi.org/10.1029/2005GC000916 |
_version_ |
1766301083658878976 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.853649 2023-05-15T14:27:22+02:00 (Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region Vogt, Christoph Knies, Jochen MEDIAN LATITUDE: 76.291341 * MEDIAN LONGITUDE: 20.062106 * SOUTH-BOUND LATITUDE: 70.440000 * WEST-BOUND LONGITUDE: 5.934500 * NORTH-BOUND LATITUDE: 82.166660 * EAST-BOUND LONGITUDE: 43.576667 * DATE/TIME START: 1991-06-23T16:22:00 * DATE/TIME END: 2001-09-12T00:00:00 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m 2009-10-01 text/tab-separated-values, 781 data points https://doi.pangaea.de/10.1594/PANGAEA.853649 https://doi.org/10.1594/PANGAEA.853649 en eng PANGAEA Stein, Ruediger; Grobe, Hannes; Wahsner, Monika (1994): Organic carbon, carbonate, and clay mineral distributions in eastern central Arctic Ocean surface sediments. Marine Geology, 119(3-4), 269-285, https://doi.org/10.1016/0025-3227(94)90185-6 Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Clay-mineral distribution in surface sediments of the Eurasian Arctic Ocean and continental margin as indicator for source areas and transport pathways - a synthesis. Boreas, 28(1), 215-233, https://doi.org/10.1111/j.1502-3885.1999.tb00216.x Wahsner, Monika; Müller, Claudia; Stein, Ruediger; Ivanov, Gennadiy I; Levitan, Mikhail A; Shelekhova, E S; Tarasov, Gennadiy A (1999): Distribution of clay minerals in surface sediments of the Eurasian Arctic Ocean. PANGAEA, https://doi.org/10.1594/PANGAEA.57249 Winkelmann, Daniel (2003): Reconstruction of recent and late Holocene sedimentation processes on the continental shelf west off Spitsbergen. MSc Thesis, Tech. Univ. of Freiberg, Germany, 156 pp Winkelmann, Daniel; Knies, Jochen (2005): Recent distribution and accumulation of organic carbon on the continental margin west off Spitsbergen. Geochemistry, Geophysics, Geosystems, 6(9), Q09012, https://doi.org/10.1029/2005GC000916 https://doi.pangaea.de/10.1594/PANGAEA.853649 https://doi.org/10.1594/PANGAEA.853649 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Vogt, Christoph; Knies, Jochen (2009): Sediment pathways in the western Barents Sea inferred from clay mineral assemblages in surface sediments. Norwegian Journal of Geology, 89(1-2), 41-55, https://www.geologi.no/images/njg/2009/1-2/Vogt_print.pdf ARK-IX/4 ARK-VIII/2 ARK-VIII/3 AWI_Paleo Barents Sea BC Bear Island Trough Box corer Center for Marine Environmental Sciences Chlorite DEPTH sediment/rock Elevation of event Event label Giant box corer GKG Gravity corer (Kiel type) HE153 HE153/1239-2 HE153/1240-2 HE153/1241-2 HE153/1242-2 HE153/1243-2 HE153/1244-2 HE153/1245-2 HE153/1246-2 HE153/1249-2 HE153/1250-2 HE153/1251-2 HE153/1254-2 HE153/1255-2 HE153/1258-1 HE153/1260-2 HE153/1261-2 HE153/1262-2 HE153/1263-2 HE153/1264-2 HE153/1265-2 HE153/1266-2 HE153/1267-2 HE153/1268-2 HE153/1269-2 HE153/1270-2 HE153/1272-2 HE153/1273-2 HE153/1274-2 HE153/1275-2 HE153/1276-2 HE153/1278-2 HE153/1279-2 Dataset 2009 ftpangaea https://doi.org/10.1594/PANGAEA.853649 https://doi.org/10.1016/0025-3227(94)90185-6 https://doi.org/10.1111/j.1502-3885.1999.tb00216.x https://doi.org/10.1594/PANGAEA.57249 https://doi.org/10.1029/2005GC000916 2023-01-20T09:06:21Z A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assemblages are related to the sub-Barents Sea geology because the Quaternary sediment cover is rather thin. Additionally, land masses like Svalbard and northern Scandinavia dominate the clay mineral signal with their erosional products. Dense bottom water, very often of brine origin, that flows within deep troughs, such as the Storfjorden or Bear Island Trough, transport the clay mineral signal from their origin to the Norwegian-Greenland Sea. Dataset Arctic Barents Sea Bear Island Greenland Greenland Sea Storfjorden Svalbard PANGAEA - Data Publisher for Earth & Environmental Science Svalbard Barents Sea Greenland Bear Island ENVELOPE(-67.250,-67.250,-68.151,-68.151) ENVELOPE(5.934500,43.576667,82.166660,70.440000) |