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  • 1
    Publication Date: 2019-03-27
    Description: This paper discusses the first geochemical characterization of obsidian fragments from the prehistoric site of Roccapalumba (Palermo, Italy). The Neolithic age of the prehistoric settlement was constrained by pottery and flint tools discovered in the same archaeological context. To define the provenance of the investigated obsidian artifacts major and trace element analyses have been carried out by using scanning electron microscopy (SEM–EDX) and inductively coupled plasma mass spectrometry (LA–ICP–MS). The comparison with literature data of the Central Mediterranean source areas, based on trace elements content and their ratios allow of constraining a provenance of the Roccapalumba obsidians from the Lipari Island. The obsidian lava flow from Gabellotto Valley is the most probable source of volcanic glass at Lipari and also the most exploited in the Mediterranean area for manufactured tools. The obtained results can contribute in reconstructing the trade/exchange and procurement relationships occurred between the prehistoric human groups inhabiting Sicily during Neolithic age.
    Description: Published
    Description: 151-167
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Description: JCR Journal
    Keywords: Roccapalumba ; trace elements ; obsidian ; Neolithic ; SEM-EDX, ; Lipari Island ; LA-ICP-MS ; Archaeology and Archaeometry
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2019-03-26
    Description: The geological, biological and geochemical features of a particular field of hydrothermal vents, discovered in the Panarea Volcanic Complex during a research survey carried out in 2015, are described for the first time. The site, located at 70-80 m depth off the South-western coast of the islet of Basiluzzo, was named Smoking Land for the presence of a large number of wide and high active chimneys and was characterized in terms of dissolved benthic fluxes, associated macrofauna and megafauna communities and preliminary mineralogy and geochemistry of chimney structures. On the whole field, a total of 39 chimneys, different in size and shape, were closely observed and described; 14 of them showed emission of low temperature hydrothermal fluids of marine origin characterized by acidified chemical conditions. The CTD and benthic chamber measurements highlighted that the Smoking Land is able to form a sea water bottom layer characterized by variable acidity and high DIC and trace elements concentrations; these characteristics weaken moving away from the chimney mouths. The SEM-EDS analysis of the collected solid samples revealed a chimney structure principally composed by amorphous and low crystalline Fe-oxyhydroxides of hydrothermal origins. The ROV explorations revealed a wide coverage of red algae (Peyssonnelia spp.) colonized by the green algae Flabiella petiolata and by suspension feeders, mainly sponges, but also bryozoans, and tubicolous polychaetes. Although novent-exclusive species were identified, the benthic communities found in association to the chimneys included more taxa than those observed in the surrounding no-vent rocky areas. These first findings evidence a submarine dynamic habitat where geological, chemical and biological processes are intimately connected, making the Smoking Land an important site in terms of marine heritage that should be safeguarded and protected.
    Description: Published
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: hydrothermal fluids ; marine environment ; new shallow water hydrothermal vents over the Panarea volcanic area
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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