(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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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 |
_version_ |
1810494751703564288 |