id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.51882
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.51882 2023-05-15T15:42:25+02:00 Clay mineralogy and stable isotopes on core PS2049-4 Bonn, Wolfgang J LATITUDE: -69.086880 * LONGITUDE: 0.889800 * DATE/TIME START: 1991-03-01T15:33:00 * DATE/TIME END: 1991-03-01T15:33:00 * MINIMUM DEPTH, sediment/rock: 0.010 m * MAXIMUM DEPTH, sediment/rock: 2.190 m 1997-02-21 text/tab-separated-values, 384 data points https://doi.pangaea.de/10.1594/PANGAEA.51882 https://doi.org/10.1594/PANGAEA.51882 en eng PANGAEA https://doi.org/10.1594/PANGAEA.729792 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 https://doi.pangaea.de/10.1594/PANGAEA.51882 https://doi.org/10.1594/PANGAEA.51882 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Amphibole ANT-IX/3 AWI_Paleo Chlorite Counting >63 µm fraction DEPTH sediment/rock Feldspar Grain size sieving/settling tube Gravity corer (Kiel type) Illite Kaolinite Lazarev Sea Mass spectrometer Finnigan MAT 251 Micronodules Minerals Neogloboquadrina pachyderma sinistral δ13C δ18O Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS18 PS18/196 PS2049-4 Quartz Radiolarians Sand Silt Size fraction < 0.002 mm clay SL Smectite Talc (Area 9.37Å) X-ray diffraction TEXTUR clay fraction Dataset 1997 ftpangaea https://doi.org/10.1594/PANGAEA.51882 https://doi.org/10.1594/PANGAEA.729792 https://doi.org/10.2312/BzP_0180_1995 2023-01-20T09:17:01Z Dataset Berichte zur Polarforschung Lazarev Sea Neogloboquadrina pachyderma Polar Research Polarforschung Reports on polar research PANGAEA - Data Publisher for Earth & Environmental Science Lazarev ENVELOPE(12.917,12.917,-69.967,-69.967) Lazarev Sea ENVELOPE(7.000,7.000,-68.000,-68.000) ENVELOPE(0.889800,0.889800,-69.086880,-69.086880)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Amphibole
ANT-IX/3
AWI_Paleo
Chlorite
Counting >63 µm fraction
DEPTH
sediment/rock
Feldspar
Grain size
sieving/settling tube
Gravity corer (Kiel type)
Illite
Kaolinite
Lazarev Sea
Mass spectrometer Finnigan MAT 251
Micronodules
Minerals
Neogloboquadrina pachyderma sinistral
δ13C
δ18O
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS18
PS18/196
PS2049-4
Quartz
Radiolarians
Sand
Silt
Size fraction < 0.002 mm
clay
SL
Smectite
Talc (Area
9.37Å)
X-ray diffraction TEXTUR
clay fraction
spellingShingle Amphibole
ANT-IX/3
AWI_Paleo
Chlorite
Counting >63 µm fraction
DEPTH
sediment/rock
Feldspar
Grain size
sieving/settling tube
Gravity corer (Kiel type)
Illite
Kaolinite
Lazarev Sea
Mass spectrometer Finnigan MAT 251
Micronodules
Minerals
Neogloboquadrina pachyderma sinistral
δ13C
δ18O
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS18
PS18/196
PS2049-4
Quartz
Radiolarians
Sand
Silt
Size fraction < 0.002 mm
clay
SL
Smectite
Talc (Area
9.37Å)
X-ray diffraction TEXTUR
clay fraction
Bonn, Wolfgang J
Clay mineralogy and stable isotopes on core PS2049-4
topic_facet Amphibole
ANT-IX/3
AWI_Paleo
Chlorite
Counting >63 µm fraction
DEPTH
sediment/rock
Feldspar
Grain size
sieving/settling tube
Gravity corer (Kiel type)
Illite
Kaolinite
Lazarev Sea
Mass spectrometer Finnigan MAT 251
Micronodules
Minerals
Neogloboquadrina pachyderma sinistral
δ13C
δ18O
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Polarstern
PS18
PS18/196
PS2049-4
Quartz
Radiolarians
Sand
Silt
Size fraction < 0.002 mm
clay
SL
Smectite
Talc (Area
9.37Å)
X-ray diffraction TEXTUR
clay fraction
format Dataset
author Bonn, Wolfgang J
author_facet Bonn, Wolfgang J
author_sort Bonn, Wolfgang J
title Clay mineralogy and stable isotopes on core PS2049-4
title_short Clay mineralogy and stable isotopes on core PS2049-4
title_full Clay mineralogy and stable isotopes on core PS2049-4
title_fullStr Clay mineralogy and stable isotopes on core PS2049-4
title_full_unstemmed Clay mineralogy and stable isotopes on core PS2049-4
title_sort clay mineralogy and stable isotopes on core ps2049-4
publisher PANGAEA
publishDate 1997
url https://doi.pangaea.de/10.1594/PANGAEA.51882
https://doi.org/10.1594/PANGAEA.51882
op_coverage LATITUDE: -69.086880 * LONGITUDE: 0.889800 * DATE/TIME START: 1991-03-01T15:33:00 * DATE/TIME END: 1991-03-01T15:33:00 * MINIMUM DEPTH, sediment/rock: 0.010 m * MAXIMUM DEPTH, sediment/rock: 2.190 m
long_lat ENVELOPE(12.917,12.917,-69.967,-69.967)
ENVELOPE(7.000,7.000,-68.000,-68.000)
ENVELOPE(0.889800,0.889800,-69.086880,-69.086880)
geographic Lazarev
Lazarev Sea
geographic_facet Lazarev
Lazarev Sea
genre Berichte zur Polarforschung
Lazarev Sea
Neogloboquadrina pachyderma
Polar Research
Polarforschung
Reports on polar research
genre_facet Berichte zur Polarforschung
Lazarev Sea
Neogloboquadrina pachyderma
Polar Research
Polarforschung
Reports on polar research
op_relation https://doi.org/10.1594/PANGAEA.729792
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
https://doi.pangaea.de/10.1594/PANGAEA.51882
https://doi.org/10.1594/PANGAEA.51882
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.51882
https://doi.org/10.1594/PANGAEA.729792
https://doi.org/10.2312/BzP_0180_1995
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