Age determinations of sediment cores from the Baffin Shelf ...

Cores HU82-034-057 and HU84-035-008, Resolution Basin, SE Baffin Shelf, contain 200 and 450 cm, respectively, of sediment that spans the Younger Dryas chron. In both cores the interval is bracketed by 14C dates on foraminifera or molluscs. These sites were close to the margin of the late Wisconsin (...

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Main Authors: Andrews, John T, Evans, L W, Williams, Kerstin M, Briggs, W M, Jull, A J Timothy, Erlenkeuser, Helmut, Hardy, Iris A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1990
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.727068
https://doi.pangaea.de/10.1594/PANGAEA.727068
id ftdatacite:10.1594/pangaea.727068
record_format openpolar
spelling ftdatacite:10.1594/pangaea.727068 2024-01-28T10:04:39+01:00 Age determinations of sediment cores from the Baffin Shelf ... Andrews, John T Evans, L W Williams, Kerstin M Briggs, W M Jull, A J Timothy Erlenkeuser, Helmut Hardy, Iris A 1990 application/zip https://dx.doi.org/10.1594/pangaea.727068 https://doi.pangaea.de/10.1594/PANGAEA.727068 en eng PANGAEA https://dx.doi.org/10.1029/pa005i006p00921 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Piston corer Collection article Supplementary Publication Series of Datasets 1990 ftdatacite https://doi.org/10.1594/pangaea.72706810.1029/pa005i006p00921 2024-01-04T14:12:42Z Cores HU82-034-057 and HU84-035-008, Resolution Basin, SE Baffin Shelf, contain 200 and 450 cm, respectively, of sediment that spans the Younger Dryas chron. In both cores the interval is bracketed by 14C dates on foraminifera or molluscs. These sites were close to the margin of the late Wisconsin (Foxe) ice sheet as it flowed toward the Labrador Sea. Prior to 11 ka, both cores record moderate to high accumulations of foraminifera, relatively high del 18O values in planktonic foraminifera, and low values of detrital carbonate. The diatom and percent opal records imply occasional seasonally open water conditions. During part of the Younger Dryas chron both the diatom and opal analyses imply a shutoff of biogenic silica production, suggesting surface water conditions affected by increased sea ice and/or reduced nutrients. In addition, the Younger Dryas interval is marked by an increase in coarse sand and detrital carbonate, a decrease in total organic carbon and foraminifera, and high rates of sediment ... : Supplement to: Andrews, John T; Evans, L W; Williams, Kerstin M; Briggs, W M; Jull, A J Timothy; Erlenkeuser, Helmut; Hardy, Iris A (1990): Cryosphere/ocean interactions at the margin of the Laurentide ice sheet during the Younger Dryas chron: SE Baffin Shelf, Northwest Territories. Paleoceanography, 5(6), 921-935 ... Article in Journal/Newspaper Baffin Ice Sheet Labrador Sea Northwest Territories Planktonic foraminifera Sea ice DataCite Metadata Store (German National Library of Science and Technology) Briggs ENVELOPE(-63.017,-63.017,-64.517,-64.517) Northwest Territories
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Piston corer
spellingShingle Piston corer
Andrews, John T
Evans, L W
Williams, Kerstin M
Briggs, W M
Jull, A J Timothy
Erlenkeuser, Helmut
Hardy, Iris A
Age determinations of sediment cores from the Baffin Shelf ...
topic_facet Piston corer
description Cores HU82-034-057 and HU84-035-008, Resolution Basin, SE Baffin Shelf, contain 200 and 450 cm, respectively, of sediment that spans the Younger Dryas chron. In both cores the interval is bracketed by 14C dates on foraminifera or molluscs. These sites were close to the margin of the late Wisconsin (Foxe) ice sheet as it flowed toward the Labrador Sea. Prior to 11 ka, both cores record moderate to high accumulations of foraminifera, relatively high del 18O values in planktonic foraminifera, and low values of detrital carbonate. The diatom and percent opal records imply occasional seasonally open water conditions. During part of the Younger Dryas chron both the diatom and opal analyses imply a shutoff of biogenic silica production, suggesting surface water conditions affected by increased sea ice and/or reduced nutrients. In addition, the Younger Dryas interval is marked by an increase in coarse sand and detrital carbonate, a decrease in total organic carbon and foraminifera, and high rates of sediment ... : Supplement to: Andrews, John T; Evans, L W; Williams, Kerstin M; Briggs, W M; Jull, A J Timothy; Erlenkeuser, Helmut; Hardy, Iris A (1990): Cryosphere/ocean interactions at the margin of the Laurentide ice sheet during the Younger Dryas chron: SE Baffin Shelf, Northwest Territories. Paleoceanography, 5(6), 921-935 ...
format Article in Journal/Newspaper
author Andrews, John T
Evans, L W
Williams, Kerstin M
Briggs, W M
Jull, A J Timothy
Erlenkeuser, Helmut
Hardy, Iris A
author_facet Andrews, John T
Evans, L W
Williams, Kerstin M
Briggs, W M
Jull, A J Timothy
Erlenkeuser, Helmut
Hardy, Iris A
author_sort Andrews, John T
title Age determinations of sediment cores from the Baffin Shelf ...
title_short Age determinations of sediment cores from the Baffin Shelf ...
title_full Age determinations of sediment cores from the Baffin Shelf ...
title_fullStr Age determinations of sediment cores from the Baffin Shelf ...
title_full_unstemmed Age determinations of sediment cores from the Baffin Shelf ...
title_sort age determinations of sediment cores from the baffin shelf ...
publisher PANGAEA
publishDate 1990
url https://dx.doi.org/10.1594/pangaea.727068
https://doi.pangaea.de/10.1594/PANGAEA.727068
long_lat ENVELOPE(-63.017,-63.017,-64.517,-64.517)
geographic Briggs
Northwest Territories
geographic_facet Briggs
Northwest Territories
genre Baffin
Ice Sheet
Labrador Sea
Northwest Territories
Planktonic foraminifera
Sea ice
genre_facet Baffin
Ice Sheet
Labrador Sea
Northwest Territories
Planktonic foraminifera
Sea ice
op_relation https://dx.doi.org/10.1029/pa005i006p00921
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.72706810.1029/pa005i006p00921
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