Age model of sediment core MSM45/19_2 ...
The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic.Radiocarbon dating was done to...
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Online Access: | https://dx.doi.org/10.1594/pangaea.945717 https://doi.pangaea.de/10.1594/PANGAEA.945717 |
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ftdatacite:10.1594/pangaea.945717 2024-02-04T10:01:17+01:00 Age model of sediment core MSM45/19_2 ... Lochte, Annalena Antonia Schneider, Ralph R 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.945717 https://doi.pangaea.de/10.1594/PANGAEA.945717 en eng PANGAEA http://calib.org https://dx.doi.org/10.1038/s41467-019-08408-6 https://dx.doi.org/10.1017/s0033822200014788 https://dx.doi.org/10.1016/0012-821x(94)90112-0 https://dx.doi.org/10.1038/ngeo285 https://dx.doi.org/10.1016/j.quaint.2011.08.023 https://dx.doi.org/10.1002/2016pa003051 https://dx.doi.org/10.1016/j.marmicro.2017.07.002 https://dx.doi.org/10.1017/s0033822200013904 http://calib.org Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 8.2 ka event Age model Holocene Labrador Sea radiocarbon age model DEPTH, sediment/rock Calendar age Gravity corer Age, 14C calibrated MSM45 Maria S. Merian Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94571710.1038/s41467-019-08408-610.1017/s003382220001478810.1016/0012-821x(94)90112-010.1038/ngeo28510.1016/j.quaint.2011.08.02310.1002/2016pa00305110.1016/j.marmicro.2017.07.00210.1017/s0033822200013904 2024-01-05T01:36:27Z The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic.Radiocarbon dating was done to secure the chorology of core MSM45-19-2 for further palaeoceanographic interpretations. The chronology of core MSM45-19-2 is based on linear interpolation of the calibrated (median probability)14C AMS ages. The sedimentation rate varies between 0.037 and 1.22 cm per year and decreases toward the top of the core, which may be related to stronger current activity during the late Holocene leading to winnowing of fine particles (e.g. Rashid et al., 2017) or a shift of the sediment deposition center toward the outer shelf after sea-level high stand was reached. In addition, decreased glacial meltwater runoff after 7 ka BP corresponding to the end of significant Laurentide Ice Sheet melting (Carlson et al., 2008) would ... Dataset Ice Sheet Labrador Sea DataCite Metadata Store (German National Library of Science and Technology) Canada Labrador Shelf ENVELOPE(-58.000,-58.000,56.000,56.000) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
8.2 ka event Age model Holocene Labrador Sea radiocarbon age model DEPTH, sediment/rock Calendar age Gravity corer Age, 14C calibrated MSM45 Maria S. Merian |
spellingShingle |
8.2 ka event Age model Holocene Labrador Sea radiocarbon age model DEPTH, sediment/rock Calendar age Gravity corer Age, 14C calibrated MSM45 Maria S. Merian Lochte, Annalena Antonia Schneider, Ralph R Age model of sediment core MSM45/19_2 ... |
topic_facet |
8.2 ka event Age model Holocene Labrador Sea radiocarbon age model DEPTH, sediment/rock Calendar age Gravity corer Age, 14C calibrated MSM45 Maria S. Merian |
description |
The presented data originates from the 1306cm long gravity core MSM45-19-2 (58°45.68 N, 61°56.25 W, 202m water depth) taken during R/V Maria S. Merian cruise MSM45 in August 2015 at 202 m water depth on the northern Labrador Shelf, northeast Canada, northwest Atlantic.Radiocarbon dating was done to secure the chorology of core MSM45-19-2 for further palaeoceanographic interpretations. The chronology of core MSM45-19-2 is based on linear interpolation of the calibrated (median probability)14C AMS ages. The sedimentation rate varies between 0.037 and 1.22 cm per year and decreases toward the top of the core, which may be related to stronger current activity during the late Holocene leading to winnowing of fine particles (e.g. Rashid et al., 2017) or a shift of the sediment deposition center toward the outer shelf after sea-level high stand was reached. In addition, decreased glacial meltwater runoff after 7 ka BP corresponding to the end of significant Laurentide Ice Sheet melting (Carlson et al., 2008) would ... |
format |
Dataset |
author |
Lochte, Annalena Antonia Schneider, Ralph R |
author_facet |
Lochte, Annalena Antonia Schneider, Ralph R |
author_sort |
Lochte, Annalena Antonia |
title |
Age model of sediment core MSM45/19_2 ... |
title_short |
Age model of sediment core MSM45/19_2 ... |
title_full |
Age model of sediment core MSM45/19_2 ... |
title_fullStr |
Age model of sediment core MSM45/19_2 ... |
title_full_unstemmed |
Age model of sediment core MSM45/19_2 ... |
title_sort |
age model of sediment core msm45/19_2 ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.945717 https://doi.pangaea.de/10.1594/PANGAEA.945717 |
long_lat |
ENVELOPE(-58.000,-58.000,56.000,56.000) |
geographic |
Canada Labrador Shelf |
geographic_facet |
Canada Labrador Shelf |
genre |
Ice Sheet Labrador Sea |
genre_facet |
Ice Sheet Labrador Sea |
op_relation |
http://calib.org https://dx.doi.org/10.1038/s41467-019-08408-6 https://dx.doi.org/10.1017/s0033822200014788 https://dx.doi.org/10.1016/0012-821x(94)90112-0 https://dx.doi.org/10.1038/ngeo285 https://dx.doi.org/10.1016/j.quaint.2011.08.023 https://dx.doi.org/10.1002/2016pa003051 https://dx.doi.org/10.1016/j.marmicro.2017.07.002 https://dx.doi.org/10.1017/s0033822200013904 http://calib.org |
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.94571710.1038/s41467-019-08408-610.1017/s003382220001478810.1016/0012-821x(94)90112-010.1038/ngeo28510.1016/j.quaint.2011.08.02310.1002/2016pa00305110.1016/j.marmicro.2017.07.00210.1017/s0033822200013904 |
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1789967048037629952 |