Volcanic activity and gas emissions along the South Sandwich Arc

• Published in: Bulletin of Volcanology
• Main Authors: Liu, Emma, Wood, Kieran, Aiuppa, Alessandro, Giudice, Gaetano, Bitetto, Marcello, Fischer, Tobias P., Kilbride, Brendan T. McCormick, Plank, Terry, Hart, Tom
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2020
• Subjects: South Sandwich Volcanic Arc; Volcanic activity; volcanic gas emissions; Saunders Island; South Sandwich Islands
• Online Access: https://research.manchester.ac.uk/en/publications/576e010f-f9eb-4816-9b11-63b7d01b4f0a; https://doi.org/10.1007/s00445-020-01415-2; https://research-information.bris.ac.uk/en/publications/77cba48e-d8c7-4a6e-8c3a-a850dcc6b313

The South Sandwich Volcanic Arc is one of the most remote and enigmatic arcs on Earth. Sporadic observations from rare cloud-free satellite images—and even rarer in situ reports—provide glimpses into a dynamic arc system characterised by persistent gas emissions and frequent eruptive activity. Our understanding of the state of volcanic activity along this arc is incomplete compared to arcs globally. To fill this gap, we present here detailed geological and volcanological observations made during an expedition to the South Sandwich Islands in January 2020. We report the first in situ measurements of gas chemistry, emission rate and carbon isotope composition from along the arc. We show that Mt. Michael on Saunders Island is a persistent source of gas emissions, releasing 145 ± 59 t day −1 SO 2 in a plume characterised by a CO 2 /SO 2 molar ratio of 1.8 ± 0.2. Combining this CO 2 /SO 2 ratio with our independent SO 2 emission rate measured near simultaneously, we derive a CO 2 flux of 179 ± 76 t day −1 . Outgassing from low temperature (90–100 °C) fumaroles is pervasive at the active centres of Candlemas and Bellingshausen, with measured gas compositions indicative of interaction between magmatic fluids and hydrothermal systems. Carbon isotope measurements of dilute plume and fumarole gases from along the arc indicate a magmatic δ 13 C of − 4.5 ± 2.0‰. Interpreted most simply, this result suggests a carbon source dominated by mantle-derived carbon. However, based on a carbon mass balance from sediment core ODP 701, we show that mixing between depleted upper mantle and a subduction component composed of sediment and altered crust is also permissible. We conclude that, although remote, the South Sandwich Volcanic Arc is an ideal tectonic setting in which to explore geochemical processes in a young, developing arc.