U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...

Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of...

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Bibliographic Details
Main Authors: Liebetrau, Volker, Krause, Stefan
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.825734
https://doi.pangaea.de/10.1594/PANGAEA.825734
id ftdatacite:10.1594/pangaea.825734
record_format openpolar
spelling ftdatacite:10.1594/pangaea.825734 2024-09-15T18:38:27+00:00 U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... Liebetrau, Volker Krause, Stefan 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.825734 https://doi.pangaea.de/10.1594/PANGAEA.825734 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.824947 https://dx.doi.org/10.1126/science.1246298 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Sample code/label Location Description Sample mass non-silicates, total Age, dated Age, error Uranium-238 Error, absolute Thorium-232 Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, error, absolute Thorium-230/Thorium-232 activity ratio Uranium-238/Thorium-232 activity ratio Thorium-230/Uranium-234 activity ratio δ13C, carbonate δ18O, carbonate Carbonates Age model Submersible JAGO MC-ICP-MS, isotope dilution Calculated Mass spectrometer, Finnigan, MAT 253 X-ray diffractometry Philips PW1710 MSM21/4 Maria S. Merian Dataset dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.82573410.1594/pangaea.82494710.1126/science.1246298 2024-07-03T13:10:33Z Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of cogenetic origin.Uncertainties presented on 2 sigma level.HyBIS U-measurements were performed on Quadrupole Inductively Coupled Plasma Mass Spectrometer (Q-ICP-MS) on limited precision level.Note 1: The sample weight represents the analysed amount dissolved in 4 N Acetic Acid and 2.25 N HNO3 (marked by -2), respectively, at room temperature over 2 hours. Remaining material was 2 x centrifuged, dried down and weighed for recalculation of the dissolved sample weight.Note 2: The equivalent percentage of the analysed non-silicate fraction represented by the sample weight. X-ray diffraction analyses indicated aragonite as the main non-silicate and easily dissolvable phase. ... Dataset Svalbard DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Sample code/label
Location
Description
Sample mass
non-silicates, total
Age, dated
Age, error
Uranium-238
Error, absolute
Thorium-232
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, error, absolute
Thorium-230/Thorium-232 activity ratio
Uranium-238/Thorium-232 activity ratio
Thorium-230/Uranium-234 activity ratio
δ13C, carbonate
δ18O, carbonate
Carbonates
Age model
Submersible JAGO
MC-ICP-MS, isotope dilution
Calculated
Mass spectrometer, Finnigan, MAT 253
X-ray diffractometry Philips PW1710
MSM21/4
Maria S. Merian
spellingShingle Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Sample code/label
Location
Description
Sample mass
non-silicates, total
Age, dated
Age, error
Uranium-238
Error, absolute
Thorium-232
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, error, absolute
Thorium-230/Thorium-232 activity ratio
Uranium-238/Thorium-232 activity ratio
Thorium-230/Uranium-234 activity ratio
δ13C, carbonate
δ18O, carbonate
Carbonates
Age model
Submersible JAGO
MC-ICP-MS, isotope dilution
Calculated
Mass spectrometer, Finnigan, MAT 253
X-ray diffractometry Philips PW1710
MSM21/4
Maria S. Merian
Liebetrau, Volker
Krause, Stefan
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
topic_facet Event label
Latitude of event
Longitude of event
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Sample code/label
Location
Description
Sample mass
non-silicates, total
Age, dated
Age, error
Uranium-238
Error, absolute
Thorium-232
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, error, absolute
Thorium-230/Thorium-232 activity ratio
Uranium-238/Thorium-232 activity ratio
Thorium-230/Uranium-234 activity ratio
δ13C, carbonate
δ18O, carbonate
Carbonates
Age model
Submersible JAGO
MC-ICP-MS, isotope dilution
Calculated
Mass spectrometer, Finnigan, MAT 253
X-ray diffractometry Philips PW1710
MSM21/4
Maria S. Merian
description Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of cogenetic origin.Uncertainties presented on 2 sigma level.HyBIS U-measurements were performed on Quadrupole Inductively Coupled Plasma Mass Spectrometer (Q-ICP-MS) on limited precision level.Note 1: The sample weight represents the analysed amount dissolved in 4 N Acetic Acid and 2.25 N HNO3 (marked by -2), respectively, at room temperature over 2 hours. Remaining material was 2 x centrifuged, dried down and weighed for recalculation of the dissolved sample weight.Note 2: The equivalent percentage of the analysed non-silicate fraction represented by the sample weight. X-ray diffraction analyses indicated aragonite as the main non-silicate and easily dissolvable phase. ...
format Dataset
author Liebetrau, Volker
Krause, Stefan
author_facet Liebetrau, Volker
Krause, Stefan
author_sort Liebetrau, Volker
title U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
title_short U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
title_full U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
title_fullStr U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
title_full_unstemmed U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
title_sort u-th isotope systematics and light stable isotope data of carbonate enriched sediments at masox and hybis sites (methane seepage off svalbard) from jago dives during cruise maria s. merian msm21/4 ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.825734
https://doi.pangaea.de/10.1594/PANGAEA.825734
genre Svalbard
genre_facet Svalbard
op_relation https://dx.doi.org/10.1594/pangaea.824947
https://dx.doi.org/10.1126/science.1246298
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.82573410.1594/pangaea.82494710.1126/science.1246298
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