Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning Maud Land, East Antarctica

The East Antarctic Ice Sheet stores a vast amount of freshwater, which makes it the single largest potential contributor to future sea-level rise. However, the lack of well-constrained geological records of past ice sheet changes impedes model validation, hampers mass balance estimates, and inhibits...

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Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Suganuma, Yusuke, Kaneda, Heitaro, Mas e Braga, Martim, Ishiwa, Takeshige, Koyama, Takushi, Newall, Jennifer C., Okuno, Jun’ichi, Obase, Takashi, Saito, Fuyuki, Rogozhina, Irina, Andersen, Jane Lund, Kawamata, Moto, Hirabayashi, Motohiro, Lifton, Nathaniel A., Fredin, Ola, Harbor, Jonathan M., Stroeven, Arjen P., Abe-Ouchi, Ayako
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Antarctic
Dronning Maud Land
East Antarctic Ice Sheet
East Antarctica
Antarc*
Antarctica
Ice Sheet
Ice Shelf
Online Access:https://pure.au.dk/portal/en/publications/04e82b2e-2279-437e-9116-4d46e5c45398
https://doi.org/10.1038/s43247-022-00599-z
http://www.scopus.com/inward/record.url?scp=85141570252&partnerID=8YFLogxK
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Summary:The East Antarctic Ice Sheet stores a vast amount of freshwater, which makes it the single largest potential contributor to future sea-level rise. However, the lack of well-constrained geological records of past ice sheet changes impedes model validation, hampers mass balance estimates, and inhibits examination of ice loss mechanisms. Here we identify rapid ice-sheet thinning in coastal Dronning Maud Land from Early to Middle Holocene (9000–5000 years ago) using a deglacial chronology based on in situ cosmogenic nuclide surface exposure dates from central Dronning Maud Land, in concert with numerical simulations of regional and continental ice-sheet evolution. Regional sea-level changes reproduced from our refined ice-load history show a highstand at 9000–8000 years ago. We propose that sea-level rise and a concomitant influx of warmer Circumpolar Deep Water triggered ice shelf breakup via the marine ice sheet instability mechanism, which led to rapid thinning of upstream coastal ice sheet sectors.

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