On Synchronous Supereruptions

The Youngest Toba Tuff (YTT) supereruption from Toba Caldera in Sumatra at ca. 74,000 years BP is the largest volcanic event recorded in the Pleistocene. Intriguingly, recent radioisotopic dating of the near antipodal Los Chocoyos (LCY) supereruption from the Atitlán caldera in Guatemala finds an id...

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Published in:Frontiers in Earth Science
Main Authors: Alejandro Cisneros de León, Tushar Mittal, Shanaka L. de Silva, Stephen Self, Axel K. Schmitt, Steffen Kutterolf
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2022
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2022.827252
https://doaj.org/article/d352fe1c99d24c4687bdd1bfda93d563
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spelling ftdoajarticles:oai:doaj.org/article:d352fe1c99d24c4687bdd1bfda93d563 2023-05-15T16:39:15+02:00 On Synchronous Supereruptions Alejandro Cisneros de León Tushar Mittal Shanaka L. de Silva Stephen Self Axel K. Schmitt Steffen Kutterolf 2022-04-01T00:00:00Z https://doi.org/10.3389/feart.2022.827252 https://doaj.org/article/d352fe1c99d24c4687bdd1bfda93d563 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2022.827252/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2022.827252 https://doaj.org/article/d352fe1c99d24c4687bdd1bfda93d563 Frontiers in Earth Science, Vol 10 (2022) Atitlán caldera Toba caldera Los Chocoyos Youngest Toba Tuff Antipode Science Q article 2022 ftdoajarticles https://doi.org/10.3389/feart.2022.827252 2022-12-31T11:58:47Z The Youngest Toba Tuff (YTT) supereruption from Toba Caldera in Sumatra at ca. 74,000 years BP is the largest volcanic event recorded in the Pleistocene. Intriguingly, recent radioisotopic dating of the near antipodal Los Chocoyos (LCY) supereruption from the Atitlán caldera in Guatemala finds an identical age within uncertainties to that of YTT. This opens the question of whether these synchronous supereruptions may be a coincidence or could be a consequence of each other? Using the known eruptive record from the past 2 Myr, we find that the likelihood of having two near antipodal supereruptions (>1,000 km3 tephra volume) within centuries (<400 years), as suggested by volcanic proxies and annual counting layer chronology in the ice core records, is very small (0.086%), requiring a non-random cause and effect. Considering this analysis, we speculate that one potential physical mechanism that could explain the temporal relationship between these supereruptions is that seismic energy released during YTT eruption focused on the antipodal region, where concentrated stresses ultimately promoted the eruption of the perched LCY magma system (or vice versa). This supereruption “double-whammy” may thus be the more compelling source of the significant environmental impacts often attributed individually to the YTT supereruption. Improving the existing age information of YTT and LCY, and a better understanding of caldera collapse events will enable further testing of the hypothesis that synchronous supereruptions do not result by pure chance. Article in Journal/Newspaper ice core Directory of Open Access Journals: DOAJ Articles Frontiers in Earth Science 10
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Atitlán caldera
Toba caldera
Los Chocoyos
Youngest Toba Tuff
Antipode
Science
Q
spellingShingle Atitlán caldera
Toba caldera
Los Chocoyos
Youngest Toba Tuff
Antipode
Science
Q
Alejandro Cisneros de León
Tushar Mittal
Shanaka L. de Silva
Stephen Self
Axel K. Schmitt
Steffen Kutterolf
On Synchronous Supereruptions
topic_facet Atitlán caldera
Toba caldera
Los Chocoyos
Youngest Toba Tuff
Antipode
Science
Q
description The Youngest Toba Tuff (YTT) supereruption from Toba Caldera in Sumatra at ca. 74,000 years BP is the largest volcanic event recorded in the Pleistocene. Intriguingly, recent radioisotopic dating of the near antipodal Los Chocoyos (LCY) supereruption from the Atitlán caldera in Guatemala finds an identical age within uncertainties to that of YTT. This opens the question of whether these synchronous supereruptions may be a coincidence or could be a consequence of each other? Using the known eruptive record from the past 2 Myr, we find that the likelihood of having two near antipodal supereruptions (>1,000 km3 tephra volume) within centuries (<400 years), as suggested by volcanic proxies and annual counting layer chronology in the ice core records, is very small (0.086%), requiring a non-random cause and effect. Considering this analysis, we speculate that one potential physical mechanism that could explain the temporal relationship between these supereruptions is that seismic energy released during YTT eruption focused on the antipodal region, where concentrated stresses ultimately promoted the eruption of the perched LCY magma system (or vice versa). This supereruption “double-whammy” may thus be the more compelling source of the significant environmental impacts often attributed individually to the YTT supereruption. Improving the existing age information of YTT and LCY, and a better understanding of caldera collapse events will enable further testing of the hypothesis that synchronous supereruptions do not result by pure chance.
format Article in Journal/Newspaper
author Alejandro Cisneros de León
Tushar Mittal
Shanaka L. de Silva
Stephen Self
Axel K. Schmitt
Steffen Kutterolf
author_facet Alejandro Cisneros de León
Tushar Mittal
Shanaka L. de Silva
Stephen Self
Axel K. Schmitt
Steffen Kutterolf
author_sort Alejandro Cisneros de León
title On Synchronous Supereruptions
title_short On Synchronous Supereruptions
title_full On Synchronous Supereruptions
title_fullStr On Synchronous Supereruptions
title_full_unstemmed On Synchronous Supereruptions
title_sort on synchronous supereruptions
publisher Frontiers Media S.A.
publishDate 2022
url https://doi.org/10.3389/feart.2022.827252
https://doaj.org/article/d352fe1c99d24c4687bdd1bfda93d563
genre ice core
genre_facet ice core
op_source Frontiers in Earth Science, Vol 10 (2022)
op_relation https://www.frontiersin.org/articles/10.3389/feart.2022.827252/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2022.827252
https://doaj.org/article/d352fe1c99d24c4687bdd1bfda93d563
op_doi https://doi.org/10.3389/feart.2022.827252
container_title Frontiers in Earth Science
container_volume 10
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