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 core contains four cryptotephra layers at 55–56, 512–513, 517–518, and 524–525 cm of depth, which have been characterised by a detailed des...

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Bibliographic Details
Published in:Quaternary Science Advances
Main Authors: Alessio Di Roberto, Giuseppe Re, Bianca Scateni, Maurizio Petrelli, Tommaso Tesi, Lucilla Capotondi, Caterina Morigi, Giacomo Galli, Ester Colizza, Romana Melis, Fiorenza Torricella, Patrizia Giordano, Federico Giglio, Andrea Gallerani, Karen Gariboldi
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2023
Subjects:
Geography. Anthropology. Recreation
G
Archaeology
CC1-960
Ross Sea
Victoria Land
Edisto
Mount Melbourne
Rittmann
Mount Rittmann
Edisto Inlet
Antarc*
Antarctica
Online Access:https://doi.org/10.1016/j.qsa.2023.100079
https://doaj.org/article/b79ad8ef0b6949d58e75a59cff6ea53f
Description
Summary: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 core contains 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 radiocarbon dating, indicates that the topmost cryptotephra correlates with the widespread 1254 CE tephra erupted by a historical eruption (696 ± 2 cal yrs BP) of Mount Rittmann, in northern Victoria Land. Deeper cryptotephra layers were derived from previously unknown explosive eruptions of Mount Melbourne volcano and were emplaced 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 volcanic complex has been highly active in historical times allowing significant progress in the current understanding of regional eruptive history. Moreover, from a tephrochronological point of view, the detected cryptotephra provide new regional isochron markers to facilitate high-precision correlations and help stratigraphically constrain changes in environmental and climatic conditions that are identified by multidisciplinary studies.

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