(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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Bibliographic Details
Main Authors: Vogt, Christoph, Knies, Jochen
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
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
Svalbard
Greenland
Bear Island
Arctic
Greenland Sea
Storfjorden
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.853649
https://doi.org/10.1594/PANGAEA.853649
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.853649
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)

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