Beryllium isotope variations recorded in the Adélie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency

The Adélie Basin is a relatively small (∼1600 km2), semi-enclosed continental shelf bathymetric depression located adjacent to the Wilkes Subglacial Basin, a basin underlying a sector of the East Antarctic Ice Sheet that contains ∼3–4 meters sea level equivalent of ice. Located within the Adélie Bas...

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Bibliographic Details
Published in:Quaternary Science Advances
Main Authors: Behrens, Bethany C., Yokoyama, Yusuke, Miyairi, Yosuke, Sproson, Adam D., Yamane, Masako, Jimenez-espejo, Francisco J., Mckay, Robert M., Johnson, Katelyn M., Escutia, Carlota, Dunbar, Robert B.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2022
Subjects:
Holocene
East Antarctica
Cosmogenic nuclides
Beryllium isotopes
Scavenging
Antarctic
East Antarctic Ice Sheet
Wilkes Subglacial Basin
Antarc*
Antarctica
Ice Sheet
Ice Shelf
Online Access:https://archimer.ifremer.fr/doc/00766/87821/93372.pdf
https://doi.org/10.1016/j.qsa.2022.100054
https://archimer.ifremer.fr/doc/00766/87821/
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Summary:The Adélie Basin is a relatively small (∼1600 km2), semi-enclosed continental shelf bathymetric depression located adjacent to the Wilkes Subglacial Basin, a basin underlying a sector of the East Antarctic Ice Sheet that contains ∼3–4 meters sea level equivalent of ice. Located within the Adélie Basin is a ∼184 m thick laminated sediment deposit, the Adélie Drift, ideal for examining regional changes in ice sheet and ocean dynamics. Here, we examine the ratio of reactive beryllium-10 to reactive beryllium-9 ((10Be/9Be)reac) in a marine sediment core obtained from the Adélie Drift to assess these changes during the Holocene epoch (11.7 ka BP to present). The (10Be/9Be)reac record provides insight into changes in freshwater input, primary productivity, and scavenging efficiency, while removing the influence of particle size on 10Be concentration. During the early Holocene, (10Be/9Be)reac ratios indicate increased meltwater discharge from ca. 11.7 to 10 ka BP, as grounded ice retreated from the Adélie Basin and adjacent bathymetric highs. After ∼10 ka BP, beryllium isotopes are influenced by scavenging efficiency and dilution controlled by ocean currents and accumulation rate, operating alongside meltwater input, suggesting there are additional factors to consider when using (10Be/9Be)reac as a proxy for ice shelf cover and glacial dynamics.

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