Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica

Peer reviewed: True Funder: École Polytechnique Fédérale de Lausanne Funder: Swiss Polar Institute Funder: Ferring Pharmaceuticals Inc. Funder: Natural Environment Research Council to the British Antarctic Survey’s Ice Dynamics and Paleoclimate program <jats:p>Here we present a case study for...

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Main Authors: Brown, JW, Moser, DE, Emanuelsson, DB, Thomas, ER
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/348333
https://doi.org/10.17863/CAM.95756
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spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/348333 2024-02-04T09:53:18+01:00 Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica Brown, JW Moser, DE Emanuelsson, DB Thomas, ER 2023-04-05T11:03:52Z text/xml application/zip application/pdf https://www.repository.cam.ac.uk/handle/1810/348333 https://doi.org/10.17863/CAM.95756 en eng eng MDPI AG http://dx.doi.org/10.3390/geosciences13030085 Geosciences (Switzerland) https://www.repository.cam.ac.uk/handle/1810/348333 doi:10.17863/CAM.95756 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 3705 Geology Eye Disease and Disorders of Vision Article 2023 ftunivcam https://doi.org/10.17863/CAM.95756 2024-01-11T23:26:37Z Peer reviewed: True Funder: École Polytechnique Fédérale de Lausanne Funder: Swiss Polar Institute Funder: Ferring Pharmaceuticals Inc. Funder: Natural Environment Research Council to the British Antarctic Survey’s Ice Dynamics and Paleoclimate program <jats:p>Here we present a case study for using visual stratigraphy to date a shallow firn core from coastal West Antarctica. The Mount Siple ice core has the potential to reconstruct climate in this data-sparse region over recent decades. Line scanned images of the 24 m firn core were used to generate a grey-scale, which displays variability consistent with annual cycles. The resulting Mount Siple age scale spans from 1998 ± 1 to 2017 CE. This study demonstrates that the seasonal changes in the grey-scale record provide an independent method of dating firn cores. However, the presence of melt layers at this site has introduced an error of ±1 year. Visual line stratigraphy has the unique advantage over traditional annual layer counting, based on chemical or isotopic species, of being non-destructive and relatively inexpensive. Visual line stratigraphy has proved to be an effective dating method for this site.</jats:p> Article in Journal/Newspaper Antarc* Antarctic Antarctica ice core Swiss Polar Institute West Antarctica Apollo - University of Cambridge Repository Antarctic West Antarctica Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Mount Siple ENVELOPE(-126.475,-126.475,-73.459,-73.459)
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language English
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
Eye Disease and Disorders of Vision
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
Eye Disease and Disorders of Vision
Brown, JW
Moser, DE
Emanuelsson, DB
Thomas, ER
Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
3705 Geology
Eye Disease and Disorders of Vision
description Peer reviewed: True Funder: École Polytechnique Fédérale de Lausanne Funder: Swiss Polar Institute Funder: Ferring Pharmaceuticals Inc. Funder: Natural Environment Research Council to the British Antarctic Survey’s Ice Dynamics and Paleoclimate program <jats:p>Here we present a case study for using visual stratigraphy to date a shallow firn core from coastal West Antarctica. The Mount Siple ice core has the potential to reconstruct climate in this data-sparse region over recent decades. Line scanned images of the 24 m firn core were used to generate a grey-scale, which displays variability consistent with annual cycles. The resulting Mount Siple age scale spans from 1998 ± 1 to 2017 CE. This study demonstrates that the seasonal changes in the grey-scale record provide an independent method of dating firn cores. However, the presence of melt layers at this site has introduced an error of ±1 year. Visual line stratigraphy has the unique advantage over traditional annual layer counting, based on chemical or isotopic species, of being non-destructive and relatively inexpensive. Visual line stratigraphy has proved to be an effective dating method for this site.</jats:p>
format Article in Journal/Newspaper
author Brown, JW
Moser, DE
Emanuelsson, DB
Thomas, ER
author_facet Brown, JW
Moser, DE
Emanuelsson, DB
Thomas, ER
author_sort Brown, JW
title Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
title_short Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
title_full Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
title_fullStr Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
title_full_unstemmed Visual Stratigraphy-Based Age Scale Developed for the Shallow Mount Siple Firn Core, Antarctica
title_sort visual stratigraphy-based age scale developed for the shallow mount siple firn core, antarctica
publisher MDPI AG
publishDate 2023
url https://www.repository.cam.ac.uk/handle/1810/348333
https://doi.org/10.17863/CAM.95756
long_lat ENVELOPE(-83.917,-83.917,-75.917,-75.917)
ENVELOPE(-126.475,-126.475,-73.459,-73.459)
geographic Antarctic
West Antarctica
Siple
Mount Siple
geographic_facet Antarctic
West Antarctica
Siple
Mount Siple
genre Antarc*
Antarctic
Antarctica
ice core
Swiss Polar Institute
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
ice core
Swiss Polar Institute
West Antarctica
op_relation https://www.repository.cam.ac.uk/handle/1810/348333
doi:10.17863/CAM.95756
op_doi https://doi.org/10.17863/CAM.95756
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