0000000000172538

AUTHOR

Leonardo Sagnotti

0000-0003-3944-201x

showing 3 related works from this author

Obsidians of Pantelleria (Strait of Sicily): A Petrographic, Geochemical and Magnetic Study of Known and New Geological Sources

2020

Abstract This paper provides new petrochemical and paleomagnetic data from obsidian sub-sources on the island of Pantelleria, exploited since the Neolithic. Data has been obtained from 14 obsidian samples from 4 locations: Fossa della Pernice (2 sites), Salto la Vecchia and Balata dei Turchi. Here, we aim to better characterize these obsidians using a cross-disciplinary and multi-analytical approach, to further understand their archaeological significance. Major element analyses (EMP) have enabled two compositional super-groups to be distinguished: (i) Fossa della Pernice, less peralkaline and (ii) Balata dei Turchi–Salto la Vecchia, distinctly more peralkaline and having almost identical c…

Bronze ageObsidianArcheology060102 archaeologyGeochemistrySettore GEO/07 - Petrologia E Petrografia06 humanities and the artsConservation010502 geochemistry & geophysics01 natural sciencesLipariEducationPetrographyArchaeologyUstica0601 history and archaeologyMagnetic studyGeologyCC1-960Pantelleria0105 earth and related environmental sciences
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Integrated stratigraphy of the Oligocene pelagic sequence in the Umbria- Marche basin (north-eastern Apennines, Italy): A potential Global Stratotype…

2008

The Oligocene represents an important time period from a wide range of perspectives and includes signifi cant climatic and eustatic variations. The pelagic succession of the Umbria-Marche Apennines (central Italy) includes a complete and continuous sequence of marly limestones and marls, with volcaniclastic layers that enable us to construct an integrated stratigraphic framework for this time period. We present here a synthesis of detailed biostratigraphic, magnetostratigraphic, and hemostratigraphic studies, along with geochronologic results from several biotite-rich volcaniclastic layers, which provide the means for an accurate and precise radiometric calibration of the Oligocene time sca…

Global Boundary Stratotype Section and PointPaleontologySequence (geology)PaleomagnetismStratotypeStratigraphyStage (stratigraphy)Section (archaeology)Period (geology)GeologyGeology
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New Insights into the Provenance of the Obsidian Fragments of the Island of Ustica (Palermo, Sicily)

2016

In this study we applied a multidisciplinary approach, coupling geophysical and geochemical measurements, to unveil the provenance of 170 obsidian flakes, collected on the volcanic island of Ustica (Sicily). On this island there are some prehistoric settlements dated from the Neolithic to the Middle Bronze Age. Despite not having geological outcrops of obsidian rocks, the countryside of Ustica is rich in fragments of this volcanic glass, imported from other source areas. The study of obsidian findings was carried out first through visual observations and density measurements. At least two different obsidian families have been distinguished, probably imported from Lipari and Pantelleria isla…

010506 paleontologyArcheologyHistoryProvenance060102 archaeologyVolcanic islandOutcrop06 humanities and the arts01 natural sciencesArchaeologyVolcanic glassPrehistorychemistry.chemical_compoundchemistryBronze Age0601 history and archaeologyGeology0105 earth and related environmental sciencesEMPAArchaeometry
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