The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain).

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    • Source:
      Publisher: Nature Publishing Group Country of Publication: England NLM ID: 101563288 Publication Model: Electronic Cited Medium: Internet ISSN: 2045-2322 (Electronic) Linking ISSN: 20452322 NLM ISO Abbreviation: Sci Rep Subsets: PubMed not MEDLINE; MEDLINE
    • Publication Information:
      Original Publication: London : Nature Publishing Group, copyright 2011-
    • Abstract:
      The present work aims to characterize the ephemeral mineral assemblage related to the fumarolic fields of the Tajogaite volcano, formed in 2021 in La Palma Island (Canary Islands, Spain). A set of 73 samples was obtained after two sampling campaigns in different fumarole sectors of the studied area. Mineralization related to these fumaroles formed efflorescent patches located at variable distance from the main volcanic craters. Distal patches are predominantly whitish, while in the vicinities they typically show yellowish to orange colours. Field observations also revealed that fumaroles usually occur in elevated topographic areas as well as over fractured and porous volcanic pyroclastic materials. The mineralogical and textural characterisation of the Tajogaite fumaroles unfolds a complex mineral assemblage, comprising cryptocrystalline phases related to low (< 200 °C) and medium temperature (200-400 °C) conditions. In Tajogaite, we propose a classification of three different fumarolic mineralization types: (1) fluorides and chlorides located in proximal fumarolic areas (~ 300-180 °C); (2) native sulphur associated with gypsum, mascagnite and salammoniac (~ 120-100 °C) and (3) sulphates and alkaline carbonates typically occurred in distal fumarolic areas (< 100 °C). Finally, we present a schematic model of the formation of Tajogaite fumarolic mineralization and their compositional evolution developed during the cooling of the volcanic system.
      (© 2023. The Author(s).)
    • References:
      Sci Rep. 2022 Oct 21;12(1):17654. (PMID: 36271131)
      Science. 2004 Dec 3;306(5702):1740-5. (PMID: 15576610)
      Sci Data. 2022 Jul 28;9(1):435. (PMID: 35902600)
      Science. 2022 Mar 25;375(6587):1348-1349. (PMID: 35324304)
      Sci Rep. 2013;3:2107. (PMID: 23838703)
      Astrobiology. 2013 Nov;13(11):1049-64. (PMID: 24283927)
      Nat Commun. 2022 Jun 8;13(1):3174. (PMID: 35676272)
      Sci Rep. 2020 Oct 23;10(1):18181. (PMID: 33097774)
    • Grant Information:
      ProID-20211010027 Agencia Canaria de Investigación, Innovación y Sociedad de la Información
    • Publication Date:
      Date Completed: 20230419 Latest Revision: 20230421
    • Publication Date:
      20230421
    • Accession Number:
      PMC10113252
    • Accession Number:
      10.1038/s41598-023-33387-6
    • Accession Number:
      37072492