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Noble gas isotopes at Deception Island (Antarctica) reveal degassing‑derived eruptions and cosmogenic helium signatures: implications for the current high levels of volcanic activity and geochronology of its eruptive history

Antonio M. Álvarez-Valero1, Hirochika Sumino2, Antonio Caracausi3, Lara Arribas1, Antonio Polo Sánchez1, Adelina Geyer4, Ray Burgess5, Helena Albert6, Meritxell Aulinas6, Masao Ban7, Javier Borrajo8, Marcos García-Arias1, Gabor Kereszturi9, Jose A. Lozano Rodríguez10

  • Affiliations: 1Departamento de Geología, Universidad de Salamanca, 37008, Salamanca, Spain; 2Research Center for Advanced Science and Technology, University of Tokyo, 153-8904 Tokyo, Japan; 3Geosciences Barcelona (GEO3BCN-CSIC), 08028 Barcelona, Spain; 4 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, 90146 Palermo, Italy; 5 Department of Earth and Environmental Sciences, University of Manchester, ManchesterM13 9PL, UK; 6 Departamento de Mineralogía, Petrología y Geología Aplicada, Universidad de Barcelona, 08028 Barcelona, Spain; 7Department of Science, Yamagata University, 990-8560 Yamagata, Japan; 8Departamento de Ciencias Biomédicas y del Diagnóstico, Universidad de Salamanca, 37007, Salamanca, Spain; 9 Volcanic Risk Solutions, School of Agriculture and Environment, Massey University, 11222 Palmerston North, New Zealand; 10Instituto Español de Oceanografía, Centro Oceanográfico de Canarias, 38180, Santa Cruz de Tenerife, Spain 

  • Presentation type: Poster

  • Presentation time: Monday 16:30 - 18:30, Room Poster Hall

  • Poster Board Number: 171

  • Programme No: 3.3.10

  • Theme 3 > Session 3

Abstract

Deception Island is one of the most active volcanoes in Antarctica with more than twenty explosive eruptions in the past two centuries. Any future volcanic eruption(s) is a serious concern for scientists, tourists, marine ecosystems and even for global oceanographic processes. Currently, it is highly challenging to carry-out -at least- low frequency volcanic gas monitoring at Deception Island because of the arduous climatic conditions and its remote location. We managed to do it for connecting the information of He, Ne, and Ar isotopes measured in olivine samples of the main past eruptive events with their on-going bubbling emissions at surface. Results reveal (i) ascending primitive magmas outgassed volatiles with a MORB-like He isotopic signature as at present day data; (ii) intensive degassing (fractionated 4He/40Ar*), before the beginning of the main eruptive episodes, as nowadays. All this demonstrates how the pre-eruptive noble gas signals of volcanic activity is an important step toward a better understanding of the magmatic dynamics and has the potential to improve eruption forecasting. We also describe the cosmogenic signal (i.e. high 3He/4He ratios of 56-910 RA) in the crystal lattice of olivine phenocrysts (total fusion in crushed poweder) much higher than the magmatic values previously obtained in the inclusions of the same olivines. The cosmogenic details reveal age ranges of c. 4-6 Ma and c. 4 ka for the pre-caldera and syn-caldera deposits, respectively, thus being the first quantitative geochronological approach to date the formation of Deception Island.