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

The Ad´elie 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 m sea level equivalent of ice. Located within the Ad´elie Basin...

Full description

Bibliographic Details
Published in:Quaternary Science Advances
Main Authors: Behrens, Bethany C., Jiménez Espejo, Francisco J., Escutia Dotti, Carlota
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2022
Subjects:
Online Access:https://hdl.handle.net/10481/79749
https://doi.org/10.1016/j.qsa.2022.100054
id ftunivgranada:oai:digibug.ugr.es:10481/79749
record_format openpolar
spelling ftunivgranada:oai:digibug.ugr.es:10481/79749 2023-05-15T13:36:43+02:00 Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency Behrens, Bethany C. Jiménez Espejo, Francisco J. Escutia Dotti, Carlota 2022-04-18 https://hdl.handle.net/10481/79749 https://doi.org/10.1016/j.qsa.2022.100054 eng eng Elsevier Bethany C. Behrens. [et al.]. Beryllium isotope variations recorded in the Adélie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency, Quaternary Science Advances, Volume 7, 2022, 100054, ISSN 2666-0334, [https://doi.org/10.1016/j.qsa.2022.100054] https://hdl.handle.net/10481/79749 doi:10.1016/j.qsa.2022.100054 Attribution-NonCommercial-NoDerivatives 4.0 Internacional http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess Holocene East Antarctica Cosmogenic nuclides Beryllium isotopes Scavenging info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftunivgranada https://doi.org/10.1016/j.qsa.2022.100054 2023-04-04T23:23:53Z The Ad´elie 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 m sea level equivalent of ice. Located within the Ad´elie Basin is a ~184 m thick laminated sediment deposit, the Ad´elie 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 Ad´elie 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 Ad´elie 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. Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT) Japan Society for the Promotion of Science Grants-in-Aid for Scientific Research (KAKENHI) 20H00193 Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT) Japan Society for the Promotion of Science 20J21145 PE17712 P18791 New Zealand Ministry of Business, Innovation and Employment (MBIE) ANTA1801 Ministry of Science and Innovation, Spain (MICINN) Spanish Government CTM2017-89711-C2-1-P European Union through FEDER funds Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf DIGIBUG: Repositorio Institucional de la Universidad de Granada Antarctic East Antarctica East Antarctic Ice Sheet New Zealand Wilkes Subglacial Basin ENVELOPE(145.000,145.000,-75.000,-75.000) Quaternary Science Advances 7 100054
institution Open Polar
collection DIGIBUG: Repositorio Institucional de la Universidad de Granada
op_collection_id ftunivgranada
language English
topic Holocene
East Antarctica
Cosmogenic nuclides
Beryllium isotopes
Scavenging
spellingShingle Holocene
East Antarctica
Cosmogenic nuclides
Beryllium isotopes
Scavenging
Behrens, Bethany C.
Jiménez Espejo, Francisco J.
Escutia Dotti, Carlota
Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
topic_facet Holocene
East Antarctica
Cosmogenic nuclides
Beryllium isotopes
Scavenging
description The Ad´elie 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 m sea level equivalent of ice. Located within the Ad´elie Basin is a ~184 m thick laminated sediment deposit, the Ad´elie 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 Ad´elie 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 Ad´elie 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. Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT) Japan Society for the Promotion of Science Grants-in-Aid for Scientific Research (KAKENHI) 20H00193 Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT) Japan Society for the Promotion of Science 20J21145 PE17712 P18791 New Zealand Ministry of Business, Innovation and Employment (MBIE) ANTA1801 Ministry of Science and Innovation, Spain (MICINN) Spanish Government CTM2017-89711-C2-1-P European Union through FEDER funds
format Article in Journal/Newspaper
author Behrens, Bethany C.
Jiménez Espejo, Francisco J.
Escutia Dotti, Carlota
author_facet Behrens, Bethany C.
Jiménez Espejo, Francisco J.
Escutia Dotti, Carlota
author_sort Behrens, Bethany C.
title Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
title_short Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
title_full Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
title_fullStr Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
title_full_unstemmed Beryllium isotope variations recorded in the Ad´elie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency
title_sort beryllium isotope variations recorded in the ad´elie basin, east antarctica reflect holocene changes in ice dynamics, productivity, and scavenging efficiency
publisher Elsevier
publishDate 2022
url https://hdl.handle.net/10481/79749
https://doi.org/10.1016/j.qsa.2022.100054
long_lat ENVELOPE(145.000,145.000,-75.000,-75.000)
geographic Antarctic
East Antarctica
East Antarctic Ice Sheet
New Zealand
Wilkes Subglacial Basin
geographic_facet Antarctic
East Antarctica
East Antarctic Ice Sheet
New Zealand
Wilkes Subglacial Basin
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
op_relation Bethany C. Behrens. [et al.]. Beryllium isotope variations recorded in the Adélie Basin, East Antarctica reflect Holocene changes in ice dynamics, productivity, and scavenging efficiency, Quaternary Science Advances, Volume 7, 2022, 100054, ISSN 2666-0334, [https://doi.org/10.1016/j.qsa.2022.100054]
https://hdl.handle.net/10481/79749
doi:10.1016/j.qsa.2022.100054
op_rights Attribution-NonCommercial-NoDerivatives 4.0 Internacional
http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1016/j.qsa.2022.100054
container_title Quaternary Science Advances
container_volume 7
container_start_page 100054
_version_ 1766082927107506176