Sorry, you need to enable JavaScript to visit this website.

Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores

TitoloMultiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores
Tipo di pubblicazioneArticolo su Rivista peer-reviewed
Anno di Pubblicazione2019
AutoriNarcisi, B.M., Petit J.R., Delmonte B., Batanova V., and Savarino J.
RivistaQuaternary Science Reviews
Volume210
Paginazione164-174
ISSN02773791
Parole chiaveAntarctic plateau, Antarctic rifting volcanism, antarctica, Cryptotephra, East Antarctica, explosive volcanism, Geochemistry, Glacial geology, glass, Glass shards, Grain size, heterogeneity, Ice, Ice core, igneous geochemistry, Indonesia, Microstructure, rifting, Samalas AD 1257 eruption, tephra, Victoria Land, volcanic eruption, volcanic glass, Volcanic isochron, Volcanoes
Abstract

Strong volcanic signals simultaneously recorded in polar ice sheets are commonly assigned to major low-latitude eruptions that dispersed large quantities of aerosols in the global atmosphere with the potential of inducing climate perturbations. Parent eruptions responsible for specific events are typically deduced from matching to a known volcanic eruption having coincidental date. However, more robust source linkage can be achieved only through geochemical characterisation of the airborne volcanic glass products (tephra) sometimes preserved in the polar strata. We analysed fine-grained tephra particles extracted from layers of the AD 1259 major bipolar volcanic signal in four East Antarctic ice cores drilled in different widely-spaced locations on the Antarctic Plateau. The very large database of glass-shard geochemistry combined with grain size analyses consistently indicate that the material was sourced from multiple distinct eruptions. These are the AD 1257 mega-eruption of Samalas volcano in Indonesia, recently proposed to be the single event responsible for the polar signal, as well as a newly-identified Antarctic eruption, which occurred in northern Victoria Land in AD 1259. Finally, a further eruption that took place somewhere outside of Antarctica has also contributed to tephra deposition. Our high-resolution, multiple-site approach was critical for revealing spatial heterogeneity of tephra at the continental scale. Evidence from ice-core tephra indicates recurrent explosive activity at the Antarctic volcanoes and could have implications for improved reconstruction of post-volcanic effects on climate from proxy polar records. © 2019 Elsevier Ltd

Note

cited By 0

URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85062839283&doi=10.1016%2fj.quascirev.2019.03.005&partnerID=40&md5=29fbba63af0f373a03e8847800d0643f
DOI10.1016/j.quascirev.2019.03.005
Citation KeyNarcisi2019164