Articles | Volume 16, issue 12
https://doi.org/10.5194/tc-16-4887-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-4887-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
New 10Be exposure ages improve Holocene ice sheet thinning history near the grounding line of Pope Glacier, Antarctica
Jonathan R. Adams
CORRESPONDING AUTHOR
British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET,
UK
Department of Earth Science & Engineering, Imperial College London,
London SW7 2AZ, UK
Joanne S. Johnson
British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET,
UK
Stephen J. Roberts
British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET,
UK
Philippa J. Mason
Department of Earth Science & Engineering, Imperial College London,
London SW7 2AZ, UK
Keir A. Nichols
Department of Earth Science & Engineering, Imperial College London,
London SW7 2AZ, UK
Ryan A. Venturelli
Department of Geology and Geological Engineering, Colorado School of
Mines, Golden, CO 80401, USA
Klaus Wilcken
Australian Nuclear Science and Technology Organization (ANSTO), New
Illawarra Road, Lucas Heights, NSW 2234, Australia
Greg Balco
Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA
Brent Goehring
Department of Earth & Environmental Sciences, Tulane University, New
Orleans, LA 70118, USA
Brenda Hall
School of Earth and Climate Sciences and the Climate Change Institute,
University of Maine, Orono, ME 04469, USA
John Woodward
Department of Geography and Environmental Sciences, Northumbria
University, Newcastle-upon-Tyne NE1 8ST, UK
Dylan H. Rood
Department of Earth Science & Engineering, Imperial College London,
London SW7 2AZ, UK
Data sets
Beryllium-10 exposure ages for Pope Glacier from a scoria cone 1.5 km west of Mount Murphy in the Amundsen Sea Embayment Jonathan R. Adams, Dylan H. Rood, Klaus Wilcken, Stephen J. Roberts, and Joanne S. Johnson https://doi.org/10.5285/8F275626-5F22-48DF-95E5-CDC8F204A897
Short summary
Glaciers in West Antarctica are experiencing significant ice loss. Geological data provide historical context for ongoing ice loss in West Antarctica, including constraints on likely future ice sheet behaviour in response to climatic warming. We present evidence from rare isotopes measured in rocks collected from an outcrop next to Pope Glacier. These data suggest that Pope Glacier thinned faster and sooner after the last ice age than previously thought.
Glaciers in West Antarctica are experiencing significant ice loss. Geological data provide...