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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Bibliographic Details
Main Authors: Lochte, Annalena Antonia, Schneider, Ralph R
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.945717
https://doi.pangaea.de/10.1594/PANGAEA.945717
id ftdatacite:10.1594/pangaea.945717
record_format openpolar
spelling 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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