Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard
Sediment core (gravity core) HH14-897-GC-MF was collected from Brepolen Bay, inner Hornsund, Svalbard (76°59.555' N; 016°24.313' E), from a water depth of 125 m, on 18.10.2014, during R/V Helmer Hanssen cruise. The total core length was 154 cm. The sampling site was located in a glacial ba...
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.946568 https://doi.org/10.1594/PANGAEA.946568 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946568 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
137Cs 210Pb dates Caesium-137 uncertainty Carbon organic total Carbon and nitrogen and sulfur (CNS) element analyzer Elementar Vario MAX Carbon Burial delta13C of organic carbon Depth bottom/max sediment/rock top/min fjord gamma-ray spectrometry Gamma spectrometer Canberra BE3830 glacimarine sedimentation Hornsund Lead-210 excess marine sediments Mass spectrometer Thermo Finnigan MAT 253 sediment accumulation rates Sediment core Spitsbergen Svalbard TOC Δδ13C |
spellingShingle |
137Cs 210Pb dates Caesium-137 uncertainty Carbon organic total Carbon and nitrogen and sulfur (CNS) element analyzer Elementar Vario MAX Carbon Burial delta13C of organic carbon Depth bottom/max sediment/rock top/min fjord gamma-ray spectrometry Gamma spectrometer Canberra BE3830 glacimarine sedimentation Hornsund Lead-210 excess marine sediments Mass spectrometer Thermo Finnigan MAT 253 sediment accumulation rates Sediment core Spitsbergen Svalbard TOC Δδ13C Szczuciński, Witold Dominiczak, Aleksander Apolinarska, Karina Woszczyk, Michał Forwick, Matthias Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
topic_facet |
137Cs 210Pb dates Caesium-137 uncertainty Carbon organic total Carbon and nitrogen and sulfur (CNS) element analyzer Elementar Vario MAX Carbon Burial delta13C of organic carbon Depth bottom/max sediment/rock top/min fjord gamma-ray spectrometry Gamma spectrometer Canberra BE3830 glacimarine sedimentation Hornsund Lead-210 excess marine sediments Mass spectrometer Thermo Finnigan MAT 253 sediment accumulation rates Sediment core Spitsbergen Svalbard TOC Δδ13C |
description |
Sediment core (gravity core) HH14-897-GC-MF was collected from Brepolen Bay, inner Hornsund, Svalbard (76°59.555' N; 016°24.313' E), from a water depth of 125 m, on 18.10.2014, during R/V Helmer Hanssen cruise. The total core length was 154 cm. The sampling site was located in a glacial bay formed after the termination of the Little Ice Age (Strzelecki et al., 2020; doi:10.1002/esp.4819). The dataset consists of gamma spectrometry measurements of excess 210Pb (calculated as a difference between the total 210Pb and the average of 214Pb and 214Bi) and 137Cs, total organic carbon (TOC) content, and delta 13C isotopic ratio of bulk organic matter. The data were obtained within a National Science Center (Poland) project: 'Impact of post-Little Ice Age glaciers retreat on sediment accumulation and carbon burial rates in subpolar fjords' and presented during conference presentations (e.g. Szczuciński et al. 2017). The excess 210Pb and 137Cs data were measured in the Institute of Geology at Adam Mickiewicz University in Poznań, Poland using a gamma detector Canberra BE3830, cooled with cryostat Cryo-Pulse®5 plus. The detector was placed in 10 cm thick lead shield walls and is equipped with a remote detector chamber option (RDC-6 inches) for low energy background reduction. The detector was commercially characterized by ISOCS (In-Situ Object Calibration Software) and LabSOCS (Laboratory Sourceless Object Calibration Software). Efficiencies for measured geometries were determined using LabSOCS code applying all corrections for sample geometry, matrix, and container type, and were verified with IAEA standards measurements. The results (spectra) were analyzed with Canberra GENIE-2000 v. 3.3 gamma spectrometry software and were presented with 2-sigma uncertainty ranges (Szczuciński, submitted). The age model was calculated using the serac package (Bruel and Sabatier, 2020; doi:10.1016/j.jenvrad.2020.106449), and verified with 137Cs depth profile, the time of glacier retreat from the coring site (Błaszczyk et al. 2013), and ... |
format |
Dataset |
author |
Szczuciński, Witold Dominiczak, Aleksander Apolinarska, Karina Woszczyk, Michał Forwick, Matthias |
author_facet |
Szczuciński, Witold Dominiczak, Aleksander Apolinarska, Karina Woszczyk, Michał Forwick, Matthias |
author_sort |
Szczuciński, Witold |
title |
Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
title_short |
Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
title_full |
Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
title_fullStr |
Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
title_full_unstemmed |
Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard |
title_sort |
excess 210pb, 137cs, total organic carbon content, and δ13c isotopic ratio of bulk organic matter of sediment core hh14-897-gc-mf from hornsund, svalbard |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.946568 https://doi.org/10.1594/PANGAEA.946568 |
op_coverage |
MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 1.49 m |
long_lat |
ENVELOPE(15.865,15.865,76.979,76.979) ENVELOPE(-164.467,-164.467,-85.983,-85.983) |
geographic |
Svalbard Hornsund Hanssen |
geographic_facet |
Svalbard Hornsund Hanssen |
genre |
Arctic glacier Hornsund Svalbard Spitsbergen |
genre_facet |
Arctic glacier Hornsund Svalbard Spitsbergen |
op_relation |
Ruben, Manuel Jannis; Hefter, Jens; Schubotz, Florence; Geibert, Walter; Butzin, Martin; Gentz, Torben; Grotheer, Hendrik; Forwick, Matthias; Szczuciński, Witold; Mollenhauer, Gesine (2023): Fossil organic carbon utilization in marine Arctic fjord sediments by subsurface micro-organisms. Nature Geoscience, 16(7), 625-630, https://doi.org/10.1038/s41561-023-01198-z Szczuciński, Witold (2022): Age model analysis of sediment core HH14-897-GC-MF from Hornsund, Svalbard. PANGAEA, https://doi.org/10.1594/PANGAEA.946576 Szczuciński, Witold; Dominiczak, Aleksander; Apolinarska, Karina; Forwick, Matthias; Goslar, Tomasz; Moskalik, M; Strzelecki, M; Woszczyk, Michał (2017): Climate-driven variations in source-to-sink fluxes of sediment and carbon in High Arctic fjord (Hornsund, Svalbard). Toulouse 10-12 October 2017 - 33rd International Meeting Of Sedimentology -16ème Congrès Français De Sédimentologie – Abstract Book, 863 Szczuciński, Witold; et al. (submitted): Applications of gamma-emitting isotopes (210Pb and 137Cs) for assessment of sedimentary processes – insights from studies of lake, deltaic and continental shelf deposits. https://doi.pangaea.de/10.1594/PANGAEA.946568 https://doi.org/10.1594/PANGAEA.946568 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.94656810.1038/s41561-023-01198-z10.1594/PANGAEA.946576 |
_version_ |
1802639025277763584 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.946568 2024-06-23T07:48:42+00:00 Excess 210Pb, 137Cs, total organic carbon content, and δ13C isotopic ratio of bulk organic matter of sediment core HH14-897-GC-MF from Hornsund, Svalbard Szczuciński, Witold Dominiczak, Aleksander Apolinarska, Karina Woszczyk, Michał Forwick, Matthias MINIMUM DEPTH, sediment/rock: 0.01 m * MAXIMUM DEPTH, sediment/rock: 1.49 m 2022 text/tab-separated-values, 569 data points https://doi.pangaea.de/10.1594/PANGAEA.946568 https://doi.org/10.1594/PANGAEA.946568 en eng PANGAEA Ruben, Manuel Jannis; Hefter, Jens; Schubotz, Florence; Geibert, Walter; Butzin, Martin; Gentz, Torben; Grotheer, Hendrik; Forwick, Matthias; Szczuciński, Witold; Mollenhauer, Gesine (2023): Fossil organic carbon utilization in marine Arctic fjord sediments by subsurface micro-organisms. Nature Geoscience, 16(7), 625-630, https://doi.org/10.1038/s41561-023-01198-z Szczuciński, Witold (2022): Age model analysis of sediment core HH14-897-GC-MF from Hornsund, Svalbard. PANGAEA, https://doi.org/10.1594/PANGAEA.946576 Szczuciński, Witold; Dominiczak, Aleksander; Apolinarska, Karina; Forwick, Matthias; Goslar, Tomasz; Moskalik, M; Strzelecki, M; Woszczyk, Michał (2017): Climate-driven variations in source-to-sink fluxes of sediment and carbon in High Arctic fjord (Hornsund, Svalbard). Toulouse 10-12 October 2017 - 33rd International Meeting Of Sedimentology -16ème Congrès Français De Sédimentologie – Abstract Book, 863 Szczuciński, Witold; et al. (submitted): Applications of gamma-emitting isotopes (210Pb and 137Cs) for assessment of sedimentary processes – insights from studies of lake, deltaic and continental shelf deposits. https://doi.pangaea.de/10.1594/PANGAEA.946568 https://doi.org/10.1594/PANGAEA.946568 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess 137Cs 210Pb dates Caesium-137 uncertainty Carbon organic total Carbon and nitrogen and sulfur (CNS) element analyzer Elementar Vario MAX Carbon Burial delta13C of organic carbon Depth bottom/max sediment/rock top/min fjord gamma-ray spectrometry Gamma spectrometer Canberra BE3830 glacimarine sedimentation Hornsund Lead-210 excess marine sediments Mass spectrometer Thermo Finnigan MAT 253 sediment accumulation rates Sediment core Spitsbergen Svalbard TOC Δδ13C Dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94656810.1038/s41561-023-01198-z10.1594/PANGAEA.946576 2024-06-12T14:17:12Z Sediment core (gravity core) HH14-897-GC-MF was collected from Brepolen Bay, inner Hornsund, Svalbard (76°59.555' N; 016°24.313' E), from a water depth of 125 m, on 18.10.2014, during R/V Helmer Hanssen cruise. The total core length was 154 cm. The sampling site was located in a glacial bay formed after the termination of the Little Ice Age (Strzelecki et al., 2020; doi:10.1002/esp.4819). The dataset consists of gamma spectrometry measurements of excess 210Pb (calculated as a difference between the total 210Pb and the average of 214Pb and 214Bi) and 137Cs, total organic carbon (TOC) content, and delta 13C isotopic ratio of bulk organic matter. The data were obtained within a National Science Center (Poland) project: 'Impact of post-Little Ice Age glaciers retreat on sediment accumulation and carbon burial rates in subpolar fjords' and presented during conference presentations (e.g. Szczuciński et al. 2017). The excess 210Pb and 137Cs data were measured in the Institute of Geology at Adam Mickiewicz University in Poznań, Poland using a gamma detector Canberra BE3830, cooled with cryostat Cryo-Pulse®5 plus. The detector was placed in 10 cm thick lead shield walls and is equipped with a remote detector chamber option (RDC-6 inches) for low energy background reduction. The detector was commercially characterized by ISOCS (In-Situ Object Calibration Software) and LabSOCS (Laboratory Sourceless Object Calibration Software). Efficiencies for measured geometries were determined using LabSOCS code applying all corrections for sample geometry, matrix, and container type, and were verified with IAEA standards measurements. The results (spectra) were analyzed with Canberra GENIE-2000 v. 3.3 gamma spectrometry software and were presented with 2-sigma uncertainty ranges (Szczuciński, submitted). The age model was calculated using the serac package (Bruel and Sabatier, 2020; doi:10.1016/j.jenvrad.2020.106449), and verified with 137Cs depth profile, the time of glacier retreat from the coring site (Błaszczyk et al. 2013), and ... Dataset Arctic glacier Hornsund Svalbard Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science Svalbard Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Hanssen ENVELOPE(-164.467,-164.467,-85.983,-85.983) |