The Dome Fuji ice core DF2021 chronology (0–207 kyr BP)
International audience Abstract. We present an age model for the 651 m deep Skytrain Ice Rise ice core. The top 2000 years have previously been dated using age markers interpolated through annual layer counting. Below this, we align the Skytrain core to the AICC2012 age model using tie points in the...
Published in: | Quaternary Science Reviews |
---|---|
Main Authors: | , , , , , , , |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2022
|
Subjects: | |
Online Access: | https://hal.science/hal-03849027 https://hal.science/hal-03849027/document https://hal.science/hal-03849027/file/oyabu-QSR2022.pdf https://doi.org/10.1016/j.quascirev.2022.107754 |
id |
ftinsu:oai:HAL:hal-03849027v1 |
---|---|
record_format |
openpolar |
spelling |
ftinsu:oai:HAL:hal-03849027v1 2024-04-28T08:24:13+00:00 The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) Oyabu, Ikumi Kawamura, Kenji Buizert, Christo Parrenin, Frédéric Orsi, Anais Kitamura, Kyotaro Aoki, Shuji Nakazawa, Takakiyo Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) 2022-10 https://hal.science/hal-03849027 https://hal.science/hal-03849027/document https://hal.science/hal-03849027/file/oyabu-QSR2022.pdf https://doi.org/10.1016/j.quascirev.2022.107754 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2022.107754 hal-03849027 https://hal.science/hal-03849027 https://hal.science/hal-03849027/document https://hal.science/hal-03849027/file/oyabu-QSR2022.pdf doi:10.1016/j.quascirev.2022.107754 info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-03849027 Quaternary Science Reviews, 2022, 294, pp.107754. ⟨10.1016/j.quascirev.2022.107754⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2022 ftinsu https://doi.org/10.1016/j.quascirev.2022.107754 2024-04-05T00:31:05Z International audience Abstract. We present an age model for the 651 m deep Skytrain Ice Rise ice core. The top 2000 years have previously been dated using age markers interpolated through annual layer counting. Below this, we align the Skytrain core to the AICC2012 age model using tie points in the ice and air phase, and apply the Paleochrono program to obtain the best fit to the tie points and glaciological constraints. In the gas phase, ties are made using methane and, in critical sections, δ18Oair; in the ice phase ties are through 10Be across the Laschamps Event, and through ice chemistry related to long-range dust transport and deposition. This strategy provides a good outcome to about 108 ka (~605 m). Beyond that there are signs of flow disturbance, with a section of ice probably repeated. Nonetheless values of CH4 and δ18Oair confirm that part of the last interglacial (LIG), from about 117–126 ka (617–628 m), is present and in chronological order. Below this there are clear signs of stratigraphic disturbance, with rapid oscillation of values in both the ice and gas phase at the base of the LIG section. Based on methane values, the warmest part of the LIG and the coldest part of the penultimate glacial are missing from our record. Ice below 631 m appears to be of age >150 ka. Article in Journal/Newspaper ice core Institut national des sciences de l'Univers: HAL-INSU Quaternary Science Reviews 294 107754 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Oyabu, Ikumi Kawamura, Kenji Buizert, Christo Parrenin, Frédéric Orsi, Anais Kitamura, Kyotaro Aoki, Shuji Nakazawa, Takakiyo The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
topic_facet |
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience Abstract. We present an age model for the 651 m deep Skytrain Ice Rise ice core. The top 2000 years have previously been dated using age markers interpolated through annual layer counting. Below this, we align the Skytrain core to the AICC2012 age model using tie points in the ice and air phase, and apply the Paleochrono program to obtain the best fit to the tie points and glaciological constraints. In the gas phase, ties are made using methane and, in critical sections, δ18Oair; in the ice phase ties are through 10Be across the Laschamps Event, and through ice chemistry related to long-range dust transport and deposition. This strategy provides a good outcome to about 108 ka (~605 m). Beyond that there are signs of flow disturbance, with a section of ice probably repeated. Nonetheless values of CH4 and δ18Oair confirm that part of the last interglacial (LIG), from about 117–126 ka (617–628 m), is present and in chronological order. Below this there are clear signs of stratigraphic disturbance, with rapid oscillation of values in both the ice and gas phase at the base of the LIG section. Based on methane values, the warmest part of the LIG and the coldest part of the penultimate glacial are missing from our record. Ice below 631 m appears to be of age >150 ka. |
author2 |
Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) |
format |
Article in Journal/Newspaper |
author |
Oyabu, Ikumi Kawamura, Kenji Buizert, Christo Parrenin, Frédéric Orsi, Anais Kitamura, Kyotaro Aoki, Shuji Nakazawa, Takakiyo |
author_facet |
Oyabu, Ikumi Kawamura, Kenji Buizert, Christo Parrenin, Frédéric Orsi, Anais Kitamura, Kyotaro Aoki, Shuji Nakazawa, Takakiyo |
author_sort |
Oyabu, Ikumi |
title |
The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
title_short |
The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
title_full |
The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
title_fullStr |
The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
title_full_unstemmed |
The Dome Fuji ice core DF2021 chronology (0–207 kyr BP) |
title_sort |
dome fuji ice core df2021 chronology (0–207 kyr bp) |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-03849027 https://hal.science/hal-03849027/document https://hal.science/hal-03849027/file/oyabu-QSR2022.pdf https://doi.org/10.1016/j.quascirev.2022.107754 |
genre |
ice core |
genre_facet |
ice core |
op_source |
ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-03849027 Quaternary Science Reviews, 2022, 294, pp.107754. ⟨10.1016/j.quascirev.2022.107754⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2022.107754 hal-03849027 https://hal.science/hal-03849027 https://hal.science/hal-03849027/document https://hal.science/hal-03849027/file/oyabu-QSR2022.pdf doi:10.1016/j.quascirev.2022.107754 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2022.107754 |
container_title |
Quaternary Science Reviews |
container_volume |
294 |
container_start_page |
107754 |
_version_ |
1797584663369220096 |