Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland

The importance of the stable isotopes in tree rings for the study of the climate variations caused by volcanic eruptions is still unclear. We studied δ 18 O, δD, δ 13 C stable isotopes of larch and cembran pine cellulose around four major eruptions with annual resolution, along with a superposed epo...

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Published in:Geosciences
Main Authors: Tito Arosio, Stéphane Affolter, Kurt Nicolussi, Michael Sigl, Malin Michelle Ziehmer-Wenz, Christian Schlüchter, Emmanuel Schaad, Rafael Stähli, Markus Christian Leuenberger
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2022
Subjects:
Online Access:https://doi.org/10.3390/geosciences12100371
https://doaj.org/article/00ec2e07eefd4187bf0d3249e0c16be0
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spelling ftdoajarticles:oai:doaj.org/article:00ec2e07eefd4187bf0d3249e0c16be0 2023-05-15T16:51:18+02:00 Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland Tito Arosio Stéphane Affolter Kurt Nicolussi Michael Sigl Malin Michelle Ziehmer-Wenz Christian Schlüchter Emmanuel Schaad Rafael Stähli Markus Christian Leuenberger 2022-10-01T00:00:00Z https://doi.org/10.3390/geosciences12100371 https://doaj.org/article/00ec2e07eefd4187bf0d3249e0c16be0 EN eng MDPI AG https://www.mdpi.com/2076-3263/12/10/371 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences12100371 2076-3263 https://doaj.org/article/00ec2e07eefd4187bf0d3249e0c16be0 Geosciences, Vol 12, Iss 371, p 371 (2022) volcanic eruption tree rings stable isotope fluid inclusion Alps climate Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.3390/geosciences12100371 2022-12-30T20:29:08Z The importance of the stable isotopes in tree rings for the study of the climate variations caused by volcanic eruptions is still unclear. We studied δ 18 O, δD, δ 13 C stable isotopes of larch and cembran pine cellulose around four major eruptions with annual resolution, along with a superposed epoch analysis of 34 eruptions with 5-year resolution. Initial analysis of the tropical Tambora (1815 CE) and Samalas (1257 CE) eruptions showed a post-eruption decrease in δ 18 O values attributed to post-volcanic cooling and increased summer precipitation in Southern Europe, as documented by observations and climate simulations. The post-volcanic cooling was captured by the δD of speleothem fluid inclusion. The δ 18 O decrease was also observed in the analysis of 34 major tropical eruptions over the last 2000 years. In contrast, the eruptions of c. 750, 756, and 764 CE attributed to Icelandic volcanoes left no significant responses in the cellulose isotopes. Further analysis of all major Icelandic eruptions in the last 2000 years showed no consistent isotopic fingerprints, with the exception of lower post-volcanic δ 13 C values in larch. In summary, the δ 18 O values of cellulose can provide relevant information on climatic and hydroclimatic variations following major tropical volcanic eruptions, even when using the 5-year resolution wood samples of the Alpine Tree-Ring Isotope Record database. Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Lower Post ENVELOPE(-128.482,-128.482,59.925,59.925) Geosciences 12 10 371
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic volcanic eruption
tree rings
stable isotope
fluid inclusion
Alps
climate
Geology
QE1-996.5
spellingShingle volcanic eruption
tree rings
stable isotope
fluid inclusion
Alps
climate
Geology
QE1-996.5
Tito Arosio
Stéphane Affolter
Kurt Nicolussi
Michael Sigl
Malin Michelle Ziehmer-Wenz
Christian Schlüchter
Emmanuel Schaad
Rafael Stähli
Markus Christian Leuenberger
Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
topic_facet volcanic eruption
tree rings
stable isotope
fluid inclusion
Alps
climate
Geology
QE1-996.5
description The importance of the stable isotopes in tree rings for the study of the climate variations caused by volcanic eruptions is still unclear. We studied δ 18 O, δD, δ 13 C stable isotopes of larch and cembran pine cellulose around four major eruptions with annual resolution, along with a superposed epoch analysis of 34 eruptions with 5-year resolution. Initial analysis of the tropical Tambora (1815 CE) and Samalas (1257 CE) eruptions showed a post-eruption decrease in δ 18 O values attributed to post-volcanic cooling and increased summer precipitation in Southern Europe, as documented by observations and climate simulations. The post-volcanic cooling was captured by the δD of speleothem fluid inclusion. The δ 18 O decrease was also observed in the analysis of 34 major tropical eruptions over the last 2000 years. In contrast, the eruptions of c. 750, 756, and 764 CE attributed to Icelandic volcanoes left no significant responses in the cellulose isotopes. Further analysis of all major Icelandic eruptions in the last 2000 years showed no consistent isotopic fingerprints, with the exception of lower post-volcanic δ 13 C values in larch. In summary, the δ 18 O values of cellulose can provide relevant information on climatic and hydroclimatic variations following major tropical volcanic eruptions, even when using the 5-year resolution wood samples of the Alpine Tree-Ring Isotope Record database.
format Article in Journal/Newspaper
author Tito Arosio
Stéphane Affolter
Kurt Nicolussi
Michael Sigl
Malin Michelle Ziehmer-Wenz
Christian Schlüchter
Emmanuel Schaad
Rafael Stähli
Markus Christian Leuenberger
author_facet Tito Arosio
Stéphane Affolter
Kurt Nicolussi
Michael Sigl
Malin Michelle Ziehmer-Wenz
Christian Schlüchter
Emmanuel Schaad
Rafael Stähli
Markus Christian Leuenberger
author_sort Tito Arosio
title Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
title_short Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
title_full Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
title_fullStr Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
title_full_unstemmed Variable Response in Alpine Tree-Ring Stable Isotopes Following Volcanic Eruptions in the Tropics and Iceland
title_sort variable response in alpine tree-ring stable isotopes following volcanic eruptions in the tropics and iceland
publisher MDPI AG
publishDate 2022
url https://doi.org/10.3390/geosciences12100371
https://doaj.org/article/00ec2e07eefd4187bf0d3249e0c16be0
long_lat ENVELOPE(-128.482,-128.482,59.925,59.925)
geographic Lower Post
geographic_facet Lower Post
genre Iceland
genre_facet Iceland
op_source Geosciences, Vol 12, Iss 371, p 371 (2022)
op_relation https://www.mdpi.com/2076-3263/12/10/371
https://doaj.org/toc/2076-3263
doi:10.3390/geosciences12100371
2076-3263
https://doaj.org/article/00ec2e07eefd4187bf0d3249e0c16be0
op_doi https://doi.org/10.3390/geosciences12100371
container_title Geosciences
container_volume 12
container_issue 10
container_start_page 371
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