Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland

We have reconstructed chronology for the disturbed bottom parts of the GRIP and GISP2 ice cores using the combined paleoatmospheric records of CH₄ concentration and δ¹⁸O[subscript atm] in the trapped gases. Our reconstructed ages for basal ice samples are based on comparison of published measurement...

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Main Authors: Suwa, Makoto, von Fischer, Joseph C., Bender, Michael L., Landais, Amaelle, Brook, Edward J.
Other Authors: Geosciences
Format: Article in Journal/Newspaper
Language:English
unknown
Published: American Geophysical Union
Subjects:
Online Access:https://ir.library.oregonstate.edu/concern/articles/8g84mr653
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spelling ftoregonstate:ir.library.oregonstate.edu:8g84mr653 2024-09-15T18:09:35+00:00 Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland Suwa, Makoto von Fischer, Joseph C. Bender, Michael L. Landais, Amaelle Brook, Edward J. Geosciences https://ir.library.oregonstate.edu/concern/articles/8g84mr653 English [eng] eng unknown American Geophysical Union https://ir.library.oregonstate.edu/concern/articles/8g84mr653 In Copyright Article ftoregonstate 2024-07-22T18:06:06Z We have reconstructed chronology for the disturbed bottom parts of the GRIP and GISP2 ice cores using the combined paleoatmospheric records of CH₄ concentration and δ¹⁸O[subscript atm] in the trapped gases. Our reconstructed ages for basal ice samples are based on comparison of published measurements of CH₄ and δ¹⁸O[subscript atm] from the disturbed section of the GRIP and GISP2 cores with the same properties in the Vostok ice core. NGRIP δ¹⁸O[subscript ice] values are also used to constrain the chronology during the end of marine isotope stage 5e. For each sample, we assign an age that represents the unique or most probable time of gas trapping, given its gas composition. Of 157 samples with CH₄ and δ¹⁸O[subscript atm] data, 10 give unique ages. Twenty-five newly measured values of the triple isotope composition of O₂ from the disturbed section of the GISP2 core add a third time-dependent gas property that agrees with our reconstruction. Our reconstruction supports earlier conclusions of Landais et al. (2003) that the disturbed section primarily includes ice from the last interglacial (MIS 5e) and the penultimate glacial period (MIS 6). The oldest ice in the basal layer of GISP2 and GRIP has an age ≥237 ka. The climate history we derive suggests that the last interglacial at Summit, Greenland, around 127 ka was slightly warmer than the current interglacial period. Reduction of various ion concentrations in ice and thickening of the ice sheet during Termination II was similar to that in Termination I. Keywords: chronology, Termination II, ice core Article in Journal/Newspaper Greenland GRIP ice core Ice Sheet NGRIP ScholarsArchive@OSU (Oregon State University)
institution Open Polar
collection ScholarsArchive@OSU (Oregon State University)
op_collection_id ftoregonstate
language English
unknown
description We have reconstructed chronology for the disturbed bottom parts of the GRIP and GISP2 ice cores using the combined paleoatmospheric records of CH₄ concentration and δ¹⁸O[subscript atm] in the trapped gases. Our reconstructed ages for basal ice samples are based on comparison of published measurements of CH₄ and δ¹⁸O[subscript atm] from the disturbed section of the GRIP and GISP2 cores with the same properties in the Vostok ice core. NGRIP δ¹⁸O[subscript ice] values are also used to constrain the chronology during the end of marine isotope stage 5e. For each sample, we assign an age that represents the unique or most probable time of gas trapping, given its gas composition. Of 157 samples with CH₄ and δ¹⁸O[subscript atm] data, 10 give unique ages. Twenty-five newly measured values of the triple isotope composition of O₂ from the disturbed section of the GISP2 core add a third time-dependent gas property that agrees with our reconstruction. Our reconstruction supports earlier conclusions of Landais et al. (2003) that the disturbed section primarily includes ice from the last interglacial (MIS 5e) and the penultimate glacial period (MIS 6). The oldest ice in the basal layer of GISP2 and GRIP has an age ≥237 ka. The climate history we derive suggests that the last interglacial at Summit, Greenland, around 127 ka was slightly warmer than the current interglacial period. Reduction of various ion concentrations in ice and thickening of the ice sheet during Termination II was similar to that in Termination I. Keywords: chronology, Termination II, ice core
author2 Geosciences
format Article in Journal/Newspaper
author Suwa, Makoto
von Fischer, Joseph C.
Bender, Michael L.
Landais, Amaelle
Brook, Edward J.
spellingShingle Suwa, Makoto
von Fischer, Joseph C.
Bender, Michael L.
Landais, Amaelle
Brook, Edward J.
Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
author_facet Suwa, Makoto
von Fischer, Joseph C.
Bender, Michael L.
Landais, Amaelle
Brook, Edward J.
author_sort Suwa, Makoto
title Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
title_short Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
title_full Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
title_fullStr Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
title_full_unstemmed Chronology reconstruction for the disturbed bottom section of the GISP2 and the GRIP ice cores: Implications for Termination II in Greenland
title_sort chronology reconstruction for the disturbed bottom section of the gisp2 and the grip ice cores: implications for termination ii in greenland
publisher American Geophysical Union
url https://ir.library.oregonstate.edu/concern/articles/8g84mr653
genre Greenland
GRIP
ice core
Ice Sheet
NGRIP
genre_facet Greenland
GRIP
ice core
Ice Sheet
NGRIP
op_relation https://ir.library.oregonstate.edu/concern/articles/8g84mr653
op_rights In Copyright
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