(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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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 |
_version_ |
1809896404675461120 |