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...

Full description

Bibliographic Details
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
_version_ 1821770744597577728
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
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 1
container_title Nature Communications
container_volume 12
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
genre Antarc*
Antarctic
Antarctica
ice core
genre_facet Antarc*
Antarctic
Antarctica
ice core
geographic Antarctic
The Antarctic
Argentina
Fernandez
geographic_facet Antarctic
The Antarctic
Argentina
Fernandez
id ftconicet:oai:ri.conicet.gov.ar:11336/173339
institution Open Polar
language English
long_lat ENVELOPE(-62.233,-62.233,-63.250,-63.250)
op_collection_id ftconicet
op_doi https://doi.org/10.1038/s41467-021-26109-x
op_relation 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
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
publisher Nature Publishing Group
record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/173339 2025-01-16T19:37:39+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 The Antarctic Argentina Fernandez ENVELOPE(-62.233,-62.233,-63.250,-63.250) Nature Communications 12 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
title 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_short Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_sort antarctic ozone hole modifies iodine geochemistry on the antarctic plateau
topic OZONE HOLE
IODINE RECYCLING
ANTARCTIC PLATEAU
DOME-C
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet OZONE HOLE
IODINE RECYCLING
ANTARCTIC PLATEAU
DOME-C
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/173339