The magnitude and impact of the 431 CE Tierra Blanca Joven eruption of Ilopango, El Salvador


Por: Smith, Victoria C., Costa, Antonio, Aguirre-Diaz, Gerardo, Pedrazzi, Dario, Scifo, Andrea, Plunkett, Gill, Poret, Mattieu, Tournigand, Pierre-Yves, Miles, Dan, Dee, Michael W., McConnell, Joseph R., Sunye-Puchol, Ivan, Harris, Pablo Davila, Sigl, Michael, Pilcher, Jonathan R., Chellman, Nathan, Gutierrez, Eduardo

Publicada: 20 oct 2020
Categoría: Multidisciplinary

Resumen:
The Tierra Blanca Joven (TBJ) eruption from Iopango volcano deposited thick ash over much of El Salvador when it was inhabited by the Maya, and rendered all areas within at least 80 km of the volcano uninhabitable for years to decades after the eruption. Nonetheless, the more widespread environmental and climatic impacts of this large eruption are not well known because the eruption magnitude and date are not well constrained. In this multifaceted study we have resolved the date of the eruption to 431 +/- 2 CE by identifying the ash layer in a well-dated, high-resolution Greenland ice-core record that is >7,000 km from Ilopango; and calculated that between 37 and 82 km(3) of magma was dispersed from an eruption coignimbrite column that rose to similar to 45 km by modeling the deposit thickness using state-of-the-art tephra dispersal methods. Sulfate records from an array of ice cores suggest stratospheric injection of 14 +/- 2 Tg S associated with the TBJ eruption, exceeding those of the historic eruption of Pinatubo in 1991. Based on these estimates it is likely that the TBJ eruption produced a cooling of around 0.5 degrees C for a few years after the eruption. The modeled dispersal and higher sulfate concentrations recorded in Antarctic ice cores imply that the cooling would have been more pronounced in the Southern Hemisphere. The new date confirms the eruption occurred within the Early Classic phase when Maya expanded across Central America.

Filiaciones:
Smith, Victoria C.:
 Univ Oxford, Sch Archaeol, Res Lab Archaeol & Hist Art, Oxford OX1 3TG, England

Costa, Antonio:
 Ist Nazl Geofis & Vulcanol, Sez Bologna, I-40128 Bologna, Italy

Aguirre-Diaz, Gerardo:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Queretaro 76230, Mexico

Pedrazzi, Dario:
 Inst Earth Sci Jaume Almera, Grp Volcanol, Lab Geol Proc Simulat SIMGEO UB CSIC, Lluis Sole i Sabaris S-N, Barcelona 08028, Spain

Scifo, Andrea:
 Univ Groningen, Ctr Isotope Res, NL-9747 AG Groningen, Netherlands

Plunkett, Gill:
 Queens Univ Belfast, Sch Nat & Built Environm, Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland

Poret, Mattieu:
 Univ Clermont Auvergne, CNRS, Inst Rech Dev, Lab Magmas & Volcans, F-63170 Clermont Ferrand, France

Tournigand, Pierre-Yves:
 Univ Padua, Dipartimento Geosci, I-35131 Padua, Italy

Miles, Dan:
 Univ Oxford, Sch Archaeol, Res Lab Archaeol & Hist Art, Oxford OX1 3TG, England

Dee, Michael W.:
 Univ Groningen, Ctr Isotope Res, NL-9747 AG Groningen, Netherlands

McConnell, Joseph R.:
 Desert Res Inst, Div Hydrol Sci, Reno, NV 89512 USA

Sunye-Puchol, Ivan:
 Univ Oxford, Sch Archaeol, Res Lab Archaeol & Hist Art, Oxford OX1 3TG, England

 Univ Nacl Autonoma Mexico, Ctr Geociencias, Queretaro 76230, Mexico

Harris, Pablo Davila:
 Inst Potosino Invest Cient & Tecnol, Div Geociencias Aplicadas, San Luis Potosi 78216, San Luis Potosi, Mexico

Sigl, Michael:
 Univ Bern, Phys, Climate & Environm Phys, CH-3012 Bern, Switzerland

 Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland

Pilcher, Jonathan R.:
 Queens Univ Belfast, Sch Nat & Built Environm, Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland

Chellman, Nathan:
 Desert Res Inst, Div Hydrol Sci, Reno, NV 89512 USA

Gutierrez, Eduardo:
 Minist Medio Ambiente & Recursos Nat, Gerencia Geol Observ Ambiental, San Salvador 76230, El Salvador
ISSN: 00278424
Editorial
NATL ACAD SCIENCES, 2101 CONSTITUTION AVE NW, WASHINGTON, DC 20418 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 117 Número: 42
Páginas: 26061-26068
WOS Id: 000580597300020
ID de PubMed: 32989145

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