1. A history of violence: magma incubation, timing and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala)
- Author
-
Alejandro Cisneros de León, Armin Freundt, Kuo-Lung Wang, Steffen Kutterolf, Julie Schindlbeck-Belo, Wendy Perez, Axel K. Schmitt, Janet C. Harvey, Martin Danišík, Hao-Yang Lee, Schindlbeck‐Belo, Julie C., 1 Institut für Geowissenschaften Universität Heidelberg, Im Neuenheimer Feld 234‐236 Germany, Kutterolf, Steffen, 2 GEOMAR Helmholtz Centre for Ocean Research Kiel SFB574, Wischhofstraße 1‐3 Kiel 24148 Germany, Danišík, Martin, 3 GeoHistory Facility, John de Laeter Centre, TIGeR Curtin University Perth WA 6845 Australia, Schmitt, Axel K., Freundt, Armin, Pérez, Wendy, Harvey, Janet C., Wang, Kuo‐Lung, 4 Institute of Earth Sciences, Academia Sinica Taipei 11529 Taiwan, and Lee, Hao‐Yang
- Subjects
010504 meteorology & atmospheric sciences ,551.701 ,geochronology ,Geochemistry ,Paleontology ,zircon ,010502 geochemistry & geophysics ,01 natural sciences ,238U–230Th disequilibrium ,Arts and Humanities (miscellaneous) ,Geochronology ,Magma ,Earth and Planetary Sciences (miscellaneous) ,Caldera ,Tephra ,Tephrochronology ,Incubation ,tephrochronology ,Geology ,(U–Th)/He ,0105 earth and related environmental sciences ,Zircon - 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., Deutsche Forschungsgemeinschaft SCH 2521/6‐1
- Published
- 2021