(Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...

ESR-spectra of foraminifera in arctic sediment cores display the [CO2]- -signal (g=2.0006). Research on the thermal behaviour of the [CO2]- -signal shows that both natural and artificial irradiation generates a precursor and a thermal unstable component of the [CO2]- -signal. The precursor can be tr...

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Bibliographic Details
Main Authors: Hoffmann, Dirk L, Woda, Clemens, Strobl, Christopher, Mangini, Augusto
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.120604
https://doi.pangaea.de/10.1594/PANGAEA.120604
id ftdatacite:10.1594/pangaea.120604
record_format openpolar
spelling ftdatacite:10.1594/pangaea.120604 2024-09-09T19:26:52+00:00 (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ... Hoffmann, Dirk L Woda, Clemens Strobl, Christopher Mangini, Augusto 2001 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.120604 https://doi.pangaea.de/10.1594/PANGAEA.120604 en eng PANGAEA https://dx.doi.org/10.1016/s0277-3791(00)00059-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Age model, optional Method comment Equivalent dose Dose rate, standard deviation Thorium-232 Thorium-232, standard deviation Thorium-230 Thorium-230, standard deviation Uranium-238 Uranium-238, standard deviation Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, standard deviation Potassium Potassium, standard deviation Water content, wet mass Water content, standard deviation Age, dated Age, dated standard deviation Piston corer BGR type Age model, stable isotope stratigraphy Calculated from mass/volume Age, electron spin resonance ESR ARK-IV/3 Polarstern dataset Supplementary Dataset Dataset 2001 ftdatacite https://doi.org/10.1594/pangaea.12060410.1016/s0277-3791(00)00059-7 2024-06-17T09:47:39Z ESR-spectra of foraminifera in arctic sediment cores display the [CO2]- -signal (g=2.0006). Research on the thermal behaviour of the [CO2]- -signal shows that both natural and artificial irradiation generates a precursor and a thermal unstable component of the [CO2]- -signal. The precursor can be transfered to the stable radical, and unstable radicals can be removed by heating. The signal-change by heating depends on the irradiation dose. Because of the varying response on thermal treatment, the dose-response curves show systematic differences depending on the applied procedure (single- or multi-aliquot method with or without heating). A model for the description of the [CO2]- -signal-change is presented. The combination of two exponential saturation functions seems to be an adequate analytical description of the dose-response curve of the [CO2]- -signal in foraminifera. Due to the limited thermal stability this signal can be used for dating foraminifera with ages up to about 190 ka. ... : Samples at 0.37-4.63 from core PS1535-8, samples at 5.48 and 7 m from core PS1535-10 ... Dataset Arctic Foraminifera* DataCite Arctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Age model, optional
Method comment
Equivalent dose
Dose rate, standard deviation
Thorium-232
Thorium-232, standard deviation
Thorium-230
Thorium-230, standard deviation
Uranium-238
Uranium-238, standard deviation
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, standard deviation
Potassium
Potassium, standard deviation
Water content, wet mass
Water content, standard deviation
Age, dated
Age, dated standard deviation
Piston corer BGR type
Age model, stable isotope stratigraphy
Calculated from mass/volume
Age, electron spin resonance ESR
ARK-IV/3
Polarstern
spellingShingle DEPTH, sediment/rock
Age model, optional
Method comment
Equivalent dose
Dose rate, standard deviation
Thorium-232
Thorium-232, standard deviation
Thorium-230
Thorium-230, standard deviation
Uranium-238
Uranium-238, standard deviation
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, standard deviation
Potassium
Potassium, standard deviation
Water content, wet mass
Water content, standard deviation
Age, dated
Age, dated standard deviation
Piston corer BGR type
Age model, stable isotope stratigraphy
Calculated from mass/volume
Age, electron spin resonance ESR
ARK-IV/3
Polarstern
Hoffmann, Dirk L
Woda, Clemens
Strobl, Christopher
Mangini, Augusto
(Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
topic_facet DEPTH, sediment/rock
Age model, optional
Method comment
Equivalent dose
Dose rate, standard deviation
Thorium-232
Thorium-232, standard deviation
Thorium-230
Thorium-230, standard deviation
Uranium-238
Uranium-238, standard deviation
Uranium-234/Uranium-238 activity ratio
Uranium-234/Uranium-238 activity ratio, standard deviation
Potassium
Potassium, standard deviation
Water content, wet mass
Water content, standard deviation
Age, dated
Age, dated standard deviation
Piston corer BGR type
Age model, stable isotope stratigraphy
Calculated from mass/volume
Age, electron spin resonance ESR
ARK-IV/3
Polarstern
description ESR-spectra of foraminifera in arctic sediment cores display the [CO2]- -signal (g=2.0006). Research on the thermal behaviour of the [CO2]- -signal shows that both natural and artificial irradiation generates a precursor and a thermal unstable component of the [CO2]- -signal. The precursor can be transfered to the stable radical, and unstable radicals can be removed by heating. The signal-change by heating depends on the irradiation dose. Because of the varying response on thermal treatment, the dose-response curves show systematic differences depending on the applied procedure (single- or multi-aliquot method with or without heating). A model for the description of the [CO2]- -signal-change is presented. The combination of two exponential saturation functions seems to be an adequate analytical description of the dose-response curve of the [CO2]- -signal in foraminifera. Due to the limited thermal stability this signal can be used for dating foraminifera with ages up to about 190 ka. ... : Samples at 0.37-4.63 from core PS1535-8, samples at 5.48 and 7 m from core PS1535-10 ...
format Dataset
author Hoffmann, Dirk L
Woda, Clemens
Strobl, Christopher
Mangini, Augusto
author_facet Hoffmann, Dirk L
Woda, Clemens
Strobl, Christopher
Mangini, Augusto
author_sort Hoffmann, Dirk L
title (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
title_short (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
title_full (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
title_fullStr (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
title_full_unstemmed (Table 1) Radionuclides and ESR dating of sediment cores PS1535-10 and PS1535-8 ...
title_sort (table 1) radionuclides and esr dating of sediment cores ps1535-10 and ps1535-8 ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.120604
https://doi.pangaea.de/10.1594/PANGAEA.120604
geographic Arctic
geographic_facet Arctic
genre Arctic
Foraminifera*
genre_facet Arctic
Foraminifera*
op_relation https://dx.doi.org/10.1016/s0277-3791(00)00059-7
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.12060410.1016/s0277-3791(00)00059-7
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