Age model and geochemistry data of sediment core GeoTü SL167 ...
The data sets contains the age model as well as bulk organic and n-alkane data of sediment core GeoTü SL167 to reconstruct changes of the oxygen minimum zone strength for the late Quaternary. The age model is based on 14C AMS measurements of planktonic foraminifera and is calibrated with the BACON v...
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Online Access: | https://dx.doi.org/10.1594/pangaea.964226 https://doi.pangaea.de/10.1594/PANGAEA.964226 |
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ftdatacite:10.1594/pangaea.964226 2024-06-09T07:49:07+00:00 Age model and geochemistry data of sediment core GeoTü SL167 ... Burdanowitz, Nicole Schmiedl, Gerhard Gaye, Birgit Munz, Philipp Schulz, Hartmut 2024 application/zip https://dx.doi.org/10.1594/pangaea.964226 https://doi.pangaea.de/10.1594/PANGAEA.964226 en eng PANGAEA https://dx.doi.org/10.5194/bg-21-1477-2024 https://dx.doi.org/10.1214/11-ba618 https://dx.doi.org/10.2312/cr_m74 https://dx.doi.org/10.5194/cp-17-1735-2021 https://dx.doi.org/10.1017/s0033822200038339 https://dx.doi.org/10.1017/s0033822200064778 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Age model Arabian Sea Denitrification n-alkanes OMZ Quaternary Cluster of Excellence Climate, Climatic Change, and Society CLICCS article Collection Bundled Publication of Datasets 2024 ftdatacite https://doi.org/10.1594/pangaea.96422610.5194/bg-21-1477-202410.1214/11-ba61810.2312/cr_m7410.5194/cp-17-1735-202110.1017/s003382220003833910.1017/s0033822200064778 2024-05-13T11:55:52Z The data sets contains the age model as well as bulk organic and n-alkane data of sediment core GeoTü SL167 to reconstruct changes of the oxygen minimum zone strength for the late Quaternary. The age model is based on 14C AMS measurements of planktonic foraminifera and is calibrated with the BACON v. 2.5.6 software for R (Blauuw & Christen, 2011) and a marine reservoir age of ΔR = 93 ± 61 years. The ΔR is based on the weighted mean of two regional marine reservoir corrections (Muscat) by Southon et al. (2002) using the marine calibration database (Reimer and Reimer, 2001, http://calib.org/marine/). Total organic carbon and nitrogen measurements were carried out with an Euro EA3000 elemental analyser and δ15N measurements with a Thermo Scientific Flash EA1112 coupled to a Finnigan MAT 252 IRMS. Total organic carbon mass accumulation rates (TOC MAR) based on calculation using the organic carbon content and total mass accumulation rates. A description of the calculation of the total mass accumulations rates ... Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Reimer ENVELOPE(-86.200,-86.200,-77.800,-77.800) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Age model Arabian Sea Denitrification n-alkanes OMZ Quaternary Cluster of Excellence Climate, Climatic Change, and Society CLICCS |
spellingShingle |
Age model Arabian Sea Denitrification n-alkanes OMZ Quaternary Cluster of Excellence Climate, Climatic Change, and Society CLICCS Burdanowitz, Nicole Schmiedl, Gerhard Gaye, Birgit Munz, Philipp Schulz, Hartmut Age model and geochemistry data of sediment core GeoTü SL167 ... |
topic_facet |
Age model Arabian Sea Denitrification n-alkanes OMZ Quaternary Cluster of Excellence Climate, Climatic Change, and Society CLICCS |
description |
The data sets contains the age model as well as bulk organic and n-alkane data of sediment core GeoTü SL167 to reconstruct changes of the oxygen minimum zone strength for the late Quaternary. The age model is based on 14C AMS measurements of planktonic foraminifera and is calibrated with the BACON v. 2.5.6 software for R (Blauuw & Christen, 2011) and a marine reservoir age of ΔR = 93 ± 61 years. The ΔR is based on the weighted mean of two regional marine reservoir corrections (Muscat) by Southon et al. (2002) using the marine calibration database (Reimer and Reimer, 2001, http://calib.org/marine/). Total organic carbon and nitrogen measurements were carried out with an Euro EA3000 elemental analyser and δ15N measurements with a Thermo Scientific Flash EA1112 coupled to a Finnigan MAT 252 IRMS. Total organic carbon mass accumulation rates (TOC MAR) based on calculation using the organic carbon content and total mass accumulation rates. A description of the calculation of the total mass accumulations rates ... |
format |
Article in Journal/Newspaper |
author |
Burdanowitz, Nicole Schmiedl, Gerhard Gaye, Birgit Munz, Philipp Schulz, Hartmut |
author_facet |
Burdanowitz, Nicole Schmiedl, Gerhard Gaye, Birgit Munz, Philipp Schulz, Hartmut |
author_sort |
Burdanowitz, Nicole |
title |
Age model and geochemistry data of sediment core GeoTü SL167 ... |
title_short |
Age model and geochemistry data of sediment core GeoTü SL167 ... |
title_full |
Age model and geochemistry data of sediment core GeoTü SL167 ... |
title_fullStr |
Age model and geochemistry data of sediment core GeoTü SL167 ... |
title_full_unstemmed |
Age model and geochemistry data of sediment core GeoTü SL167 ... |
title_sort |
age model and geochemistry data of sediment core geotü sl167 ... |
publisher |
PANGAEA |
publishDate |
2024 |
url |
https://dx.doi.org/10.1594/pangaea.964226 https://doi.pangaea.de/10.1594/PANGAEA.964226 |
long_lat |
ENVELOPE(-86.200,-86.200,-77.800,-77.800) |
geographic |
Reimer |
geographic_facet |
Reimer |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.5194/bg-21-1477-2024 https://dx.doi.org/10.1214/11-ba618 https://dx.doi.org/10.2312/cr_m74 https://dx.doi.org/10.5194/cp-17-1735-2021 https://dx.doi.org/10.1017/s0033822200038339 https://dx.doi.org/10.1017/s0033822200064778 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.96422610.5194/bg-21-1477-202410.1214/11-ba61810.2312/cr_m7410.5194/cp-17-1735-202110.1017/s003382220003833910.1017/s0033822200064778 |
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1801381314427879424 |