Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau

Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV radiation on terrestrial and marine ecosyste...

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Published in:Nature Communications
Main Authors: Spolaor, Andrea, Burgay, François, Fernandez, Rafael Pedro, Turetta, Clara, Cuevas, Carlos A., Kim, Kitae, Kinnison, Douglas E., Lamarque, Jean-François, de Blasi, Fabrizio, Barbaro, Elena, Corella, Juan Pablo, Vallelonga, Paul, Frezzotti, Massimo, Barbante, Carlo, Saiz López, Alfonso
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group
Subjects:
Online Access:http://hdl.handle.net/11336/173339
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/173339 2024-11-03T14:50:18+00:00 Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau Spolaor, Andrea Burgay, François Fernandez, Rafael Pedro Turetta, Clara Cuevas, Carlos A. Kim, Kitae Kinnison, Douglas E. Lamarque, Jean-François de Blasi, Fabrizio Barbaro, Elena Corella, Juan Pablo Vallelonga, Paul Frezzotti, Massimo Barbante, Carlo Saiz López, Alfonso application/pdf http://hdl.handle.net/11336/173339 eng eng Nature Publishing Group info:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/s41467-021-26109-x info:eu-repo/semantics/altIdentifier/doi/10.1038/s41467-021-26109-x http://hdl.handle.net/11336/173339 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ OZONE HOLE IODINE RECYCLING ANTARCTIC PLATEAU DOME-C https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1038/s41467-021-26109-x 2024-10-04T09:34:02Z Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV radiation on terrestrial and marine ecosystems are well established; however, the impact on geochemical cycles of ice photoactive elements, such as iodine, remains mostly unexplored. Here, we present the first iodine record from the inner Antarctic Plateau (Dome C) that covers approximately the last 212 years (1800-2012 CE). Our results show that the iodine concentration in ice remained constant during the pre-ozone hole period (1800-1974 CE) but has declined twofold since the onset of the ozone hole era (~1975 CE), closely tracking the total ozone evolution over Antarctica. Based on ice core observations, laboratory measurements and chemistry-climate model simulations, we propose that the iodine decrease since ~1975 is caused by enhanced iodine re-emission from snowpack due to the ozone hole-driven increase in UV radiation reaching the Antarctic Plateau. These findings suggest the potential for ice core iodine records from the inner Antarctic Plateau to be as an archive for past stratospheric ozone trends. Fil: Spolaor, Andrea. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Polari.; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Burgay, François. Universita' Ca' Foscari Di Venezia; Italia. Paul Scherrer Institute; Suiza Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina Fil: Turetta, Clara. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Polari.; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Cuevas, Carlos A. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; ... Article in Journal/Newspaper Antarc* Antarctic Antarctica ice core CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Argentina Fernandez ENVELOPE(-62.233,-62.233,-63.250,-63.250) The Antarctic Nature Communications 12 1
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic OZONE HOLE
IODINE RECYCLING
ANTARCTIC PLATEAU
DOME-C
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle OZONE HOLE
IODINE RECYCLING
ANTARCTIC PLATEAU
DOME-C
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Clara
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-François
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Vallelonga, Paul
Frezzotti, Massimo
Barbante, Carlo
Saiz López, Alfonso
Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
topic_facet OZONE HOLE
IODINE RECYCLING
ANTARCTIC PLATEAU
DOME-C
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV radiation on terrestrial and marine ecosystems are well established; however, the impact on geochemical cycles of ice photoactive elements, such as iodine, remains mostly unexplored. Here, we present the first iodine record from the inner Antarctic Plateau (Dome C) that covers approximately the last 212 years (1800-2012 CE). Our results show that the iodine concentration in ice remained constant during the pre-ozone hole period (1800-1974 CE) but has declined twofold since the onset of the ozone hole era (~1975 CE), closely tracking the total ozone evolution over Antarctica. Based on ice core observations, laboratory measurements and chemistry-climate model simulations, we propose that the iodine decrease since ~1975 is caused by enhanced iodine re-emission from snowpack due to the ozone hole-driven increase in UV radiation reaching the Antarctic Plateau. These findings suggest the potential for ice core iodine records from the inner Antarctic Plateau to be as an archive for past stratospheric ozone trends. Fil: Spolaor, Andrea. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Polari.; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Burgay, François. Universita' Ca' Foscari Di Venezia; Italia. Paul Scherrer Institute; Suiza Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina Fil: Turetta, Clara. Consiglio Nazionale Delle Ricerche. Istituto Di Scienze Polari.; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Cuevas, Carlos A. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; ...
format Article in Journal/Newspaper
author Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Clara
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-François
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Vallelonga, Paul
Frezzotti, Massimo
Barbante, Carlo
Saiz López, Alfonso
author_facet Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Clara
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-François
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Vallelonga, Paul
Frezzotti, Massimo
Barbante, Carlo
Saiz López, Alfonso
author_sort Spolaor, Andrea
title Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_short Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_full Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_fullStr Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_full_unstemmed Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_sort antarctic ozone hole modifies iodine geochemistry on the antarctic plateau
publisher Nature Publishing Group
url http://hdl.handle.net/11336/173339
long_lat ENVELOPE(-62.233,-62.233,-63.250,-63.250)
geographic Antarctic
Argentina
Fernandez
The Antarctic
geographic_facet Antarctic
Argentina
Fernandez
The Antarctic
genre Antarc*
Antarctic
Antarctica
ice core
genre_facet Antarc*
Antarctic
Antarctica
ice core
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info:eu-repo/semantics/altIdentifier/doi/10.1038/s41467-021-26109-x
http://hdl.handle.net/11336/173339
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
op_doi https://doi.org/10.1038/s41467-021-26109-x
container_title Nature Communications
container_volume 12
container_issue 1
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