Multiple sources for tephra from AD 1259 volcanic signal in Antarctic ice cores. (15th April 2019)

• Record Type: Journal Article
• Authors: Narcisi, Biancamaria; Petit, Jean Robert; Delmonte, Barbara; Batanova, Valentina; Savarino, Joël
• Is Part Of: Quaternary science reviews. Volume 210(2019)
• Page Start: 164
• Page End: 174
• Publication Date: 2019-04-15
• Subjects: Cryptotephra -- Antarctica -- Ice cores -- Volcanic isochron -- Glass shard microanalysis -- Antarctic rifting volcanism -- Samalas AD 1257 eruption; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2019.03.005
• Languages: English
• ISSNs: 0277-3791

Abstract

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. Highlights: Significant tephra concentration in AD 1259 volcanic signal from four Antarctic ice cores. Compositional heterogeneity of tephra suggests sourcing from multiple distinct eruptions. Linkage of the Antarctic ice signal with the Samalas AD 1257 eruption confirmed. A new Antarctic eruption that occurred in AD 1259 has been also identified. Antarctic regional-scale effects of local volcanic activity conceivable.