Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle

Iodine has a significant impact on promoting the formation of new ultrafine aerosol particles and accelerating tropospheric ozone loss, thereby affecting radiative forcing and climate. Therefore, understanding the long-term natural evolution of iodine, and its coupling with climate variability, is k...

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Published in:Nature Communications
Main Authors: Corella, Juan Pablo, Maffezzoli, Niccolo, Spolaor, Andrea, Vallelonga, Paul, Cuevas, Carlos A., Scoto, Federico, Müller, Juliane, Vinther, Bo, Kjær, Helle A., Cozzi, Giulio, Edwards, Ross, Barbante, Carlo, Saiz-Lopez, Alfonso
Other Authors: Edwards, Ro
Format: Article in Journal/Newspaper
Language:unknown
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/10278/3757232
https://doi.org/10.1038/s41467-021-27642-5
https://www.nature.com/articles/s41467-021-27642-5
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author Corella, Juan Pablo
Maffezzoli, Niccolo
Spolaor, Andrea
Vallelonga, Paul
Cuevas, Carlos A.
Scoto, Federico
Müller, Juliane
Vinther, Bo
Kjær, Helle A.
Cozzi, Giulio
Edwards, Ross
Barbante, Carlo
Saiz-Lopez, Alfonso
author2 Corella, Juan Pablo
Maffezzoli, Niccolo
Spolaor, Andrea
Vallelonga, Paul
Cuevas, Carlos A.
Scoto, Federico
Müller, Juliane
Vinther, Bo
Kjær, Helle A.
Cozzi, Giulio
Edwards, Ro
Barbante, Carlo
Saiz-Lopez, Alfonso
author_facet Corella, Juan Pablo
Maffezzoli, Niccolo
Spolaor, Andrea
Vallelonga, Paul
Cuevas, Carlos A.
Scoto, Federico
Müller, Juliane
Vinther, Bo
Kjær, Helle A.
Cozzi, Giulio
Edwards, Ross
Barbante, Carlo
Saiz-Lopez, Alfonso
author_sort Corella, Juan Pablo
collection Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca)
container_issue 1
container_title Nature Communications
container_volume 13
description Iodine has a significant impact on promoting the formation of new ultrafine aerosol particles and accelerating tropospheric ozone loss, thereby affecting radiative forcing and climate. Therefore, understanding the long-term natural evolution of iodine, and its coupling with climate variability, is key to adequately assess its effect on climate on centennial to millennial timescales. Here, using two Greenland ice cores (NEEM and RECAP), we report the Arctic iodine variability during the last 127,000 years. We find the highest and lowest iodine levels recorded during interglacial and glacial periods, respectively, modulated by ocean bioproductivity and sea ice dynamics. Our sub-decadal resolution measurements reveal that high frequency iodine emission variability occurred in pace with Dansgaard/Oeschger events, highlighting the rapid Arctic ocean-ice-atmosphere iodine exchange response to abrupt climate changes. Finally, we discuss if iodine levels during past warmer-than-present climate phases can serve as analogues of future scenarios under an expected ice-free Arctic Ocean. We argue that the combination of natural biogenic ocean iodine release (boosted by ongoing Arctic warming and sea ice retreat) and anthropogenic ozone-induced iodine emissions may lead to a near future scenario with the highest iodine levels of the last 127,000 years.
format Article in Journal/Newspaper
genre Arctic
Arctic Ocean
Dansgaard-Oeschger events
Greenland
Greenland ice cores
Sea ice
genre_facet Arctic
Arctic Ocean
Dansgaard-Oeschger events
Greenland
Greenland ice cores
Sea ice
geographic Arctic
Arctic Ocean
Greenland
geographic_facet Arctic
Arctic Ocean
Greenland
id ftuniveneziairis:oai:iris.unive.it:10278/3757232
institution Open Polar
language unknown
op_collection_id ftuniveneziairis
op_doi https://doi.org/10.1038/s41467-021-27642-5
op_relation volume:13
issue:1
journal:NATURE COMMUNICATIONS
http://hdl.handle.net/10278/3757232
doi:10.1038/s41467-021-27642-5
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85122875627
https://www.nature.com/articles/s41467-021-27642-5
publishDate 2022
record_format openpolar
spelling ftuniveneziairis:oai:iris.unive.it:10278/3757232 2025-01-16T20:12:04+00:00 Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle Corella, Juan Pablo Maffezzoli, Niccolo Spolaor, Andrea Vallelonga, Paul Cuevas, Carlos A. Scoto, Federico Müller, Juliane Vinther, Bo Kjær, Helle A. Cozzi, Giulio Edwards, Ross Barbante, Carlo Saiz-Lopez, Alfonso Corella, Juan Pablo Maffezzoli, Niccolo Spolaor, Andrea Vallelonga, Paul Cuevas, Carlos A. Scoto, Federico Müller, Juliane Vinther, Bo Kjær, Helle A. Cozzi, Giulio Edwards, Ro Barbante, Carlo Saiz-Lopez, Alfonso 2022 http://hdl.handle.net/10278/3757232 https://doi.org/10.1038/s41467-021-27642-5 https://www.nature.com/articles/s41467-021-27642-5 unknown volume:13 issue:1 journal:NATURE COMMUNICATIONS http://hdl.handle.net/10278/3757232 doi:10.1038/s41467-021-27642-5 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85122875627 https://www.nature.com/articles/s41467-021-27642-5 Settore GEO/04 - Geografia Fisica e Geomorfologia info:eu-repo/semantics/article 2022 ftuniveneziairis https://doi.org/10.1038/s41467-021-27642-5 2024-03-21T18:21:48Z Iodine has a significant impact on promoting the formation of new ultrafine aerosol particles and accelerating tropospheric ozone loss, thereby affecting radiative forcing and climate. Therefore, understanding the long-term natural evolution of iodine, and its coupling with climate variability, is key to adequately assess its effect on climate on centennial to millennial timescales. Here, using two Greenland ice cores (NEEM and RECAP), we report the Arctic iodine variability during the last 127,000 years. We find the highest and lowest iodine levels recorded during interglacial and glacial periods, respectively, modulated by ocean bioproductivity and sea ice dynamics. Our sub-decadal resolution measurements reveal that high frequency iodine emission variability occurred in pace with Dansgaard/Oeschger events, highlighting the rapid Arctic ocean-ice-atmosphere iodine exchange response to abrupt climate changes. Finally, we discuss if iodine levels during past warmer-than-present climate phases can serve as analogues of future scenarios under an expected ice-free Arctic Ocean. We argue that the combination of natural biogenic ocean iodine release (boosted by ongoing Arctic warming and sea ice retreat) and anthropogenic ozone-induced iodine emissions may lead to a near future scenario with the highest iodine levels of the last 127,000 years. Article in Journal/Newspaper Arctic Arctic Ocean Dansgaard-Oeschger events Greenland Greenland ice cores Sea ice Università Ca’ Foscari Venezia: ARCA (Archivio Istituzionale della Ricerca) Arctic Arctic Ocean Greenland Nature Communications 13 1
spellingShingle Settore GEO/04 - Geografia Fisica e Geomorfologia
Corella, Juan Pablo
Maffezzoli, Niccolo
Spolaor, Andrea
Vallelonga, Paul
Cuevas, Carlos A.
Scoto, Federico
Müller, Juliane
Vinther, Bo
Kjær, Helle A.
Cozzi, Giulio
Edwards, Ross
Barbante, Carlo
Saiz-Lopez, Alfonso
Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title_full Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title_fullStr Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title_full_unstemmed Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title_short Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle
title_sort climate changes modulated the history of arctic iodine during the last glacial cycle
topic Settore GEO/04 - Geografia Fisica e Geomorfologia
topic_facet Settore GEO/04 - Geografia Fisica e Geomorfologia
url http://hdl.handle.net/10278/3757232
https://doi.org/10.1038/s41467-021-27642-5
https://www.nature.com/articles/s41467-021-27642-5