(Table 1) Age determination of sediment core KC073 ...

We present a high-resolution paleoceanographic record of deglaciation based on diatom assemblages from a core located just south of the Polar Front in the southwest Atlantic. Core KC073 is from a sediment drift at the mouth of the Falkland Trough and contains sediments from the Last Glacial Maximum...

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Bibliographic Details
Main Authors: Allen, Claire Susannah, Pike, Jennifer, Pudsey, Carol J, Leventer, Amy
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.837085
https://doi.pangaea.de/10.1594/PANGAEA.837085
id ftdatacite:10.1594/pangaea.837085
record_format openpolar
spelling ftdatacite:10.1594/pangaea.837085 2024-09-15T17:46:32+00:00 (Table 1) Age determination of sediment core KC073 ... Allen, Claire Susannah Pike, Jennifer Pudsey, Carol J Leventer, Amy 2005 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.837085 https://doi.pangaea.de/10.1594/PANGAEA.837085 en eng PANGAEA https://dx.doi.org/10.1029/2004pa001055 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Laboratory code/label DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Age, dated standard deviation Carbon Calendar age, maximum/old Calendar age, minimum/young Calendar age Calendar age, standard deviation Kasten corer Age, 14C AMS Age, 14C calibrated, CALIB 4.4 Stuiver et al., 2003 dataset Supplementary Dataset Dataset 2005 ftdatacite https://doi.org/10.1594/pangaea.83708510.1029/2004pa001055 2024-08-01T10:59:23Z We present a high-resolution paleoceanographic record of deglaciation based on diatom assemblages from a core located just south of the Polar Front in the southwest Atlantic. Core KC073 is from a sediment drift at the mouth of the Falkland Trough and contains sediments from the Last Glacial Maximum (LGM) to present, dated using radiocarbon dates on bulk organic matter and radiolarian stratigraphy. The site lies along the path of the Antarctic Circumpolar Current (ACC) and immediately downstream of where North Atlantic Deep Water (NADW) is entrained into the ACC. Significant variations in ocean conditions are reflected in high-amplitude changes in diatom concentrations and assemblage composition. The diatom assemblage at the LGM indicates that winter sea ice extent was at least 5° farther north than present until at least 19.0 ka (calendar years) and summer sea ice may have occasionally extended over the site, but for the most part it lay to the south. During deglaciation, Chaetoceros resting spores (CRS) ... : Age corrected using the regional 14C correction age of 1300 years B.P. and calibrated using CALIB 4.4. ... Dataset Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Laboratory code/label
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated
Age, dated standard deviation
Carbon
Calendar age, maximum/old
Calendar age, minimum/young
Calendar age
Calendar age, standard deviation
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.4 Stuiver et al., 2003
spellingShingle Laboratory code/label
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated
Age, dated standard deviation
Carbon
Calendar age, maximum/old
Calendar age, minimum/young
Calendar age
Calendar age, standard deviation
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.4 Stuiver et al., 2003
Allen, Claire Susannah
Pike, Jennifer
Pudsey, Carol J
Leventer, Amy
(Table 1) Age determination of sediment core KC073 ...
topic_facet Laboratory code/label
DEPTH, sediment/rock
Depth, top/min
Depth, bottom/max
Age, dated
Age, dated standard deviation
Carbon
Calendar age, maximum/old
Calendar age, minimum/young
Calendar age
Calendar age, standard deviation
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.4 Stuiver et al., 2003
description We present a high-resolution paleoceanographic record of deglaciation based on diatom assemblages from a core located just south of the Polar Front in the southwest Atlantic. Core KC073 is from a sediment drift at the mouth of the Falkland Trough and contains sediments from the Last Glacial Maximum (LGM) to present, dated using radiocarbon dates on bulk organic matter and radiolarian stratigraphy. The site lies along the path of the Antarctic Circumpolar Current (ACC) and immediately downstream of where North Atlantic Deep Water (NADW) is entrained into the ACC. Significant variations in ocean conditions are reflected in high-amplitude changes in diatom concentrations and assemblage composition. The diatom assemblage at the LGM indicates that winter sea ice extent was at least 5° farther north than present until at least 19.0 ka (calendar years) and summer sea ice may have occasionally extended over the site, but for the most part it lay to the south. During deglaciation, Chaetoceros resting spores (CRS) ... : Age corrected using the regional 14C correction age of 1300 years B.P. and calibrated using CALIB 4.4. ...
format Dataset
author Allen, Claire Susannah
Pike, Jennifer
Pudsey, Carol J
Leventer, Amy
author_facet Allen, Claire Susannah
Pike, Jennifer
Pudsey, Carol J
Leventer, Amy
author_sort Allen, Claire Susannah
title (Table 1) Age determination of sediment core KC073 ...
title_short (Table 1) Age determination of sediment core KC073 ...
title_full (Table 1) Age determination of sediment core KC073 ...
title_fullStr (Table 1) Age determination of sediment core KC073 ...
title_full_unstemmed (Table 1) Age determination of sediment core KC073 ...
title_sort (table 1) age determination of sediment core kc073 ...
publisher PANGAEA
publishDate 2005
url https://dx.doi.org/10.1594/pangaea.837085
https://doi.pangaea.de/10.1594/PANGAEA.837085
genre Antarc*
Antarctic
NADW
North Atlantic Deep Water
North Atlantic
Sea ice
genre_facet Antarc*
Antarctic
NADW
North Atlantic Deep Water
North Atlantic
Sea ice
op_relation https://dx.doi.org/10.1029/2004pa001055
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.83708510.1029/2004pa001055
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