Glacial to deglacial reservoir ages of surface waters in the southern South Pacific

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Autores principales: Küssner, Kevin, Sarnthein, Michael, Michel, Elisabeth, Mollenhauer, Gesine, Ronge, Thomas A, Siani, Giuseppe, Tiedemann, Ralf
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2020
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author Küssner, Kevin
Sarnthein, Michael
Michel, Elisabeth
Mollenhauer, Gesine
Ronge, Thomas A
Siani, Giuseppe
Tiedemann, Ralf
author_facet Küssner, Kevin
Sarnthein, Michael
Michel, Elisabeth
Mollenhauer, Gesine
Ronge, Thomas A
Siani, Giuseppe
Tiedemann, Ralf
collection Datos científicos de ciencias marinas y ambientales
contents Ocean sediment records document abrupt changes in glacial-to-deglacial circulation and mixing of the ocean, recorded as changes in 14C reservoir ages of surface waters. Here we present 14C-based high-resolution age records of four sediment cores from the western and eastern continental margins of the South Pacific. Global correlation of centennial-scale ocean variability requires centennial-scale precision in age control which can be established by means of 14C plateau tuning. The accuracy and precision of plateau tuning are now confirmed in two sediment cores off Chile; in one core by independent land-based age control of four tephra layers, in a second core by a suite of peak glacial sediment varves. The results from the cores support the model of a bipolar seesaw at the onset of fast deglacial Antarctic warming, moreover, they show that the Antarctic Cold Reversal immediately preceded the onset of the Younger Dryas cold spell. During peak glacial times, high reservoir ages reaching up to ~1500 yr and paired ice-rafted debris and sediment laminations may reflect seasonal sea ice and/or a melt water lid at high latitudes off southern Chile, likewise east of Southern New Zealand.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_922671
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Glacial to deglacial reservoir ages of surface waters in the southern South Pacific
Küssner, Kevin
Sarnthein, Michael
Michel, Elisabeth
Mollenhauer, Gesine
Ronge, Thomas A
Siani, Giuseppe
Tiedemann, Ralf
14C plateau tuning; ages of tephra layers; bipolar seesaw; centennial-scale ocean variability; deglacial variability; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Last Glacial Maximum; peak glacial sediment varves; planktic 14C reservoir ages; Radiocarbon chronology; southern South Pacific
Ocean sediment records document abrupt changes in glacial-to-deglacial circulation and mixing of the ocean, recorded as changes in 14C reservoir ages of surface waters. Here we present 14C-based high-resolution age records of four sediment cores from the western and eastern continental margins of the South Pacific. Global correlation of centennial-scale ocean variability requires centennial-scale precision in age control which can be established by means of 14C plateau tuning. The accuracy and precision of plateau tuning are now confirmed in two sediment cores off Chile; in one core by independent land-based age control of four tephra layers, in a second core by a suite of peak glacial sediment varves. The results from the cores support the model of a bipolar seesaw at the onset of fast deglacial Antarctic warming, moreover, they show that the Antarctic Cold Reversal immediately preceded the onset of the Younger Dryas cold spell. During peak glacial times, high reservoir ages reaching up to ~1500 yr and paired ice-rafted debris and sediment laminations may reflect seasonal sea ice and/or a melt water lid at high latitudes off southern Chile, likewise east of Southern New Zealand.
title Glacial to deglacial reservoir ages of surface waters in the southern South Pacific
topic 14C plateau tuning; ages of tephra layers; bipolar seesaw; centennial-scale ocean variability; deglacial variability; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Last Glacial Maximum; peak glacial sediment varves; planktic 14C reservoir ages; Radiocarbon chronology; southern South Pacific
url https://doi.org/10.1594/PANGAEA.922671