(Table 1) Radiocarbon ages and different calibrated ages for sediment core HLY0503-18TC obtained during the HOTRAX expedition

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Hauptverfasser: Hanslik, Daniela, Jakobsson, Martin, Backman, Jan, Björck, Svante, Sellén, Emma, O'Regan, Matthew, Fornaciari, Eliana, Skog, Göran
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Sprache:en
Veröffentlicht: PANGAEA 2010
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author Hanslik, Daniela
Jakobsson, Martin
Backman, Jan
Björck, Svante
Sellén, Emma
O'Regan, Matthew
Fornaciari, Eliana
Skog, Göran
author_facet Hanslik, Daniela
Jakobsson, Martin
Backman, Jan
Björck, Svante
Sellén, Emma
O'Regan, Matthew
Fornaciari, Eliana
Skog, Göran
collection Datos científicos de ciencias marinas y ambientales
contents A short sediment core from a local depression forming an intra basin on the Lomonosov Ridge, was retrieved during the Healy-Oden Trans-Arctic Expedition 2005 (HOTRAX). It contains a record of the Marine Isotope Stages (MIS) 1-3 showing exceptionally high abundances of calcareous microfossils during parts of MIS 3. Based on radiocarbon dating, linear sedimentation rates of 7-9 cm/ka persist during the last deglaciation. The Last Glacial Maximum (LGM) is partly characterized by a hiatus. Planktic foraminiferal abundance variations of Neogloboquadrina pachyderma sinistral and calcareous nannofossils reflect changes in Arctic Ocean summer sea ice coverage and probably inflow of subpolar North Atlantic water. Calibration of the radiocarbon ages, using modeled reservoir corrections from previous studies and the microfossil abundance record of the studied core, results in marine reservoir ages of 1400 years or more, at least during the last deglaciation. Paired benthic-planktic radiocarbon dated foraminiferal samples indicate a slow decrease in age difference between surface and bottom waters from the Lateglacial to the Holocene, suggesting circulation and ventilation changes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_810548
institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Radiocarbon ages and different calibrated ages for sediment core HLY0503-18TC obtained during the HOTRAX expedition
Hanslik, Daniela
Jakobsson, Martin
Backman, Jan
Björck, Svante
Sellén, Emma
O'Regan, Matthew
Fornaciari, Eliana
Skog, Göran
Age, 14C calibrated; Age, 14C conventional; Age, 14C milieu/reservoir corrected and calibrated; Age, dated; Age, dated, standard deviation; Age, dated material; Calendar age; Calendar age, standard deviation; DEPTH, sediment/rock; Healy; Healy-Oden Trans Arctic Expedition 2005 (HOTRAX05); HLY0503; HLY0503-18TC; International Polar Year (2007-2008); IPY; Lomonosov Ridge, Arctic Ocean; Method comment; Sample ID; TC; Trigger corer
A short sediment core from a local depression forming an intra basin on the Lomonosov Ridge, was retrieved during the Healy-Oden Trans-Arctic Expedition 2005 (HOTRAX). It contains a record of the Marine Isotope Stages (MIS) 1-3 showing exceptionally high abundances of calcareous microfossils during parts of MIS 3. Based on radiocarbon dating, linear sedimentation rates of 7-9 cm/ka persist during the last deglaciation. The Last Glacial Maximum (LGM) is partly characterized by a hiatus. Planktic foraminiferal abundance variations of Neogloboquadrina pachyderma sinistral and calcareous nannofossils reflect changes in Arctic Ocean summer sea ice coverage and probably inflow of subpolar North Atlantic water. Calibration of the radiocarbon ages, using modeled reservoir corrections from previous studies and the microfossil abundance record of the studied core, results in marine reservoir ages of 1400 years or more, at least during the last deglaciation. Paired benthic-planktic radiocarbon dated foraminiferal samples indicate a slow decrease in age difference between surface and bottom waters from the Lateglacial to the Holocene, suggesting circulation and ventilation changes.
title (Table 1) Radiocarbon ages and different calibrated ages for sediment core HLY0503-18TC obtained during the HOTRAX expedition
topic Age, 14C calibrated; Age, 14C conventional; Age, 14C milieu/reservoir corrected and calibrated; Age, dated; Age, dated, standard deviation; Age, dated material; Calendar age; Calendar age, standard deviation; DEPTH, sediment/rock; Healy; Healy-Oden Trans Arctic Expedition 2005 (HOTRAX05); HLY0503; HLY0503-18TC; International Polar Year (2007-2008); IPY; Lomonosov Ridge, Arctic Ocean; Method comment; Sample ID; TC; Trigger corer
url https://doi.org/10.1594/PANGAEA.810548