OceanRep
A history of violence: magma incubation, timing and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala).
Cisneros de León, Alejandro, Schindlbeck-Belo, Julie C. , Kutterolf, Steffen , Danisík, Martin, Schmitt, Axel K., Freundt, Armin , Pérez, Wendy, Harvey, Janet C., Wang, Kuo‐Lung and Lee, Hao‐Yang (2021) A history of violence: magma incubation, timing and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala). Journal of Quaternary Science, 36 (2). pp. 169-179. DOI 10.1002/jqs.3265.
Preview |
Text
jqs.3265.pdf - Published Version Available under License Creative Commons: Attribution 4.0. Download (15MB) | Preview |
Other (Excel file)
jqs3265-sup-0001-sm_table_1_u-th_ages.xlsx - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (33kB) |
|
Other (Excel file)
jqs3265-sup-0002-sm_table_2_glass_chemistry.xlsx - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (1MB) |
|
Other (Excel file)
jqs3265-sup-0003-sm_table_3_u-th-he.xlsx - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (33kB) |
|
Other (Excel file)
jqs3265-sup-0004-sm_table_4_thickness_ig.xlsx - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (12kB) |
|
Preview |
Text
jqs3265-sup-0005-sup_fig_1.pdf - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (760kB) | Preview |
Text
jqs3265-sup-0006-supporting_material_1_methods.docx - Supplemental Material Available under License Creative Commons: Attribution-Noncommercial 4.0. Download (27kB) |
Abstract
The climactic Los Chocoyos (LCY) eruption from Atitlán caldera (Guatemala) is a key chronostratigraphic marker for the Quaternary period given the extensive distribution of its deposits that reached both the Pacific and Atlantic Oceans. Despite LCY tephra being an important marker horizon, a radioisotopic age for this eruption has remained elusive. Using zircon (U–Th)/He geochronology, we present the first radioisotopically determined eruption age for the LCY of 75 ± 2 ka. Additionally, the youngest zircon crystallization 238U–230Th rim ages in their respective samples constrain eruption age maxima for two other tephra units that erupted from Atitlán caldera, W-Fall (130 +16/−14 ka) and I-Fall eruptions (56 +8.2/−7.7 ka), which under- and overlie LCY tephra, respectively. Moreover, rim and interior zircon dating and glass chemistry suggest that before eruption silicic magma was stored for >80 kyr, with magma accumulation peaking within ca. 35 kyr before the LCY eruption during which the system may have developed into a vertically zoned magma chamber. Based on an updated distribution of LCY pyroclastic deposits, a new conservatively estimated volume of ~1220 ± 150 km3 is obtained (volcanic explosivity index VEI > 8), which confirms the LCY eruption as the first-ever recognized supereruption in Central America.
Document Type: | Article |
---|---|
Keywords: | 238U–230Th disequilibrium,(U–Th)/He, geochronology, tephrochronology, zircon |
Research affiliation: | OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems |
Main POF Topic: | PT3: Restless Earth |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Wiley |
Date Deposited: | 18 Jan 2021 07:09 |
Last Modified: | 07 Feb 2024 15:50 |
URI: | https://oceanrep.geomar.de/id/eprint/51594 |
Actions (login required)
View Item |
Copyright 2023 | GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel | All rights reserved
Questions, comments and suggestions regarding the GEOMAR repository are welcomed
at bibliotheksleitung@geomar.de !