Cryptotephras in the marine sediment record of the Edisto Inlet, Ross Sea: Implications for the volcanology and tephrochronology of northern Victoria Land, Antarctica

We present the results of the tephrochronology study of a 14.49 m long marine sediment core (TR 17-08) collected in the Edisto Inlet, Ross Sea (Antarctica). The corecontains four cryptotephra layers at 55-56, 512-513, 517-518, and 524-525 cm of depth, which have been characterised by a detailed description of the texture,mineral assemblage, and single glass shards major and trace element geochemistry. The age model of the investigated sedimentary sequence, based on radiocarbondating, indicates that the topmost cryptotephra correlates with the widespread 1254 CE tephra erupted by a historical eruption (696 ± 2 cal yrs BP) o? MountRittmann, in northern Victoria Land. Deeper cryptotephra layers were derived from previously unknown explosive eruptions of Mount Melbourne volcano and wereemplaced between 1615 cal yrs BP and 1677 cal yrs BP, e.g. between the 3rd and 4th centuries CE. This discovery demonstrates that the Mount Melbourne volcaniccomplex has been highly active in historical times allowing signifcant progress in the current understanding of regional eruptive history. Moreover, from a tephfrochronological point of view, the detected cryptotephra provide new regional isochron markers to facilitate high-precision correlations and help stratigraphicallyconstrain changes in environmental and climatic conditions that are identifed by multidisciplinary studies