Search results for "Vulcano Island"

showing 10 items of 22 documents

Ludovico Sicardi, an unknown pioneer of the Volcanic Geochemical Monitoring

2018

On December of 1977, almost 100 years since its last eruption, intense volcanic activity took place in Vulcano Island (Sicily). The elevated fluxes and the temperature increase of the fumaroles in La Fossa Crater, as well as the variations in their chemical composition, alarmed the scientific community. During that period, in the city of Palermo, Marcello Carapezza along with his colleagues Mariano Valenza and Mario Nuccio, were studying the fumarolic field of Vulcano. After extended bibliographic research, Valenza discovered the studies of Ludovico Sicardi, which were focused on Vulcano, Stromboli, Vesuvio and Campi Flegrei. Considering the fact that Sicardi’s research was performed 60 yea…

Vulcano islandCarapezzafumarolic fieldSettore GEO/08 - Geochimica E Vulcanologia
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Tunable diode laser measurements of hydrothermal/volcanic CO2 and implications for the global CO2 budget

2014

Quantifying the CO2 flux sustained by low-temperature fumarolic fields in hydrothermal/volcanic environments has remained a challenge, to date. Here, we explored the potential of a commercial infrared tunable laser unit for quantifying such fumarolic volcanic/hydrothermal CO2 fluxes. Our field tests were conducted between April 2013 and March 2014 at Nea Kameni (Santorini, Greece), Hekla and Krýsuvík (Iceland) and Vulcano (Aeolian Islands, Italy). At these sites, the tunable laser was used to measure the path-integrated CO2 mixing ratios along cross sections of the fumaroles' atmospheric plumes. By using a tomographic post-processing routine, we then obtained, for each manifestation, the co…

lcsh:GeologyCO2 flux Nea Kameni Hekla volcano Krysuvik Vulcano islandlcsh:Stratigraphylcsh:QE1-996.5Settore GEO/08 - Geochimica E Vulcanologialcsh:QE640-699Solid Earth
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Pathways and fate of REE in the shallow hydrothermal aquifer of Vulcano island (Italy)

2019

Abstract We investigated the geochemical behaviour of major and Rare Earth Elements (REE), together with oxygen and deuterium isotopic composition in the aquifer of Vulcano, the southernmost island of the Aeolian archipelago (Italy). Studied wells, located at different distances from the crater, are characterised by different contributions of the rising volcanic fluids. In particular, those located in the proximity of La Fossa crater are affected by a strong interaction with volcanic-hydrothermal fluids and show REE behaviour similar to that of fresh rocks, suggesting a congruent dissolution of the solid matrix. Samples from the other wells, located in an area where the volcanic deposits ar…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesVulcano IslandSettore AGR/13 - Chimica AgrariaGeochemistryGeologyAquiferHydrothermal circulationWater-rock interaction010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationMatrix (geology)Settore GEO/08 - Geochimica E VulcanologiaImpact craterVolcanoGeochemistry and PetrologyFaciesRare earth elementSeawaterGroundwaterGeologyGroundwater0105 earth and related environmental sciences
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Effects of reduced pH on shell integrity of a common whelk from a natural undersea CO2 vent community off Vulcano Island, Italy.

2014

Hexaplex trunculus is a widespread Mediterranean gastropod mollusc that plays a crucial role in benthic ecosystem dynamics. Individuals occur in shallow, sublittoral habitats near Vulcano Island, Italy, where an undersea CO2 vent provides a gradient of seawater acidification mimicing future predicted levels of ocean acidification. Individuals were collected from three sites with declining pH [ambient ( pH 8.18), medium (pH 8.05) and low (pH 7.49)]. Dissolution of shells was clearly evident at the medium (smoothing of outer shell ) and low (pitting and holes) pH sites. Scanning electron microcroscopy will provide a qualitative comparative assessment of micro-scale impacts of shell dissolutio…

ocean acidification gastropod CO2 seep Vulcano Island
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Macroalgal responses to ocean acidification depend on nutrient and light levels. Frontiers in Marine Science

2015

Ocean acidification may benefit algae that are able to capitalize on increased carbon availability for photosynthesis, but it is expected to have adverse effects on calcified algae through dissolution. Shifts in dominance between primary producers will have knock-on effects on marine ecosystems and will likely vary regionally, depending on factors such as irradiance (light vs. shade) and nutrient levels (oligotrophic vs. eutrophic). Thus experiments are needed to evaluate interactive effects of combined stressors in the field. In this study, we investigated the physiological responses of macroalgae near a CO2 seep in oligotrophic waters off Vulcano (Italy). The algae were incubated in situ …

Settore BIO/07 - Ecologiaocean acidification macroalgae CO2 seep Vulcano Island Mediterranean
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Seawater Trace Metals in acidified condition: an accumulation study in the blue mussel Mytilus galloprovincialis off Vulcano Island submarine vents (…

2013

Seawater Trace Metals Mytilus galloprovincialisVulcano Island
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Georeferenced cartography dataset of the La Fossa crater fumarolic field at Vulcano Island (Aeolian Archipelago, Italy): conversion and comparison of…

2011

The present study illustrates the procedures applied for the coordinate system conversion of the historical fumarole positions at La Fossa crater, to allow their comparison with newly acquired global positioning system (GPS) data. Due to the absence of ground control points in the field and on both the old Gauss Boaga and the new UTM WGS 1984 maps, we had to model the transformation errors between the two systems using differential GPS techniques. Once corrected, the maps show a residual Easting shifting, due to erroneous georeferencing of the original base maps; this is corrected by morphological comparative methods. The good correspondence between the corrected positions of the historical…

business.industrylcsh:QC801-809lcsh:QC851-999ResidualFumarole GPS Map Vulcano IslandField (geography)Fumarolelcsh:Geophysics. Cosmic physicsGeophysicsImpact craterGeoreferenceGlobal Positioning Systemlcsh:Meteorology. ClimatologyDifferential GPSbusinessCartographyAeolian archipelagoGeologyAnnals of Geophysics
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Microbial Biofilms Along a Geochemical Gradient at the Shallow-Water Hydrothermal System of Vulcano Island, Mediterranean Sea

2022

Shallow water hydrothermal vents represent highly dynamic environments where strong geochemical gradients can shape microbial communities. Recently, these systems are being widely used for investigating the effects of ocean acidification on biota as vent emissions can release high CO2 concentrations causing local pH reduction. However, other gas species, as well as trace elements and metals, are often released in association with CO2 and can potentially act as confounding factors. In this study, we evaluated the composition, diversity and inferred functional profiles of microbial biofilms in Levante Bay (Vulcano Island, Italy, Mediterranean Sea), a well-studied shallow-water hydrothermal ve…

Vulcano islandMicrobiology (medical)sulfide oxidizing bacteriaEpsilonproteobacteria/Campylobacteriafungiactive microbial communitiesmicrobial biofilmsshallow-water hydrothermal ventsocean acidificationMicrobiologyGammaproteobacteriaFrontiers in Microbiology
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Long-time variation of soil CO2 fluxes at the summit crater of Vulcano (Italy)

2012

Here, we report the first continuous data of geochemical parameters acquired directly from the active summit crater of Vulcano. This approach provides a means to better investigate deep geochemical processes associated with the degassing system of Vulcano Island. In particular, we report on soil CO2 fluxes from the upper part of Vulcano, a closed-conduit volcano, from September 2007 to October 2010. Large variations in the soil CO2 and plume SO2 fluxes (order of magnitude), coinciding with other discontinuous geochemical parameters (CO2 concentrations in fumarole gas) and physical parameters (increase of shallow seismic activity and fumarole temperatures) have been recorded. The results fro…

geographygeography.geographical_feature_categorySummitEarth scienceCo2 fluxFumaroleContinuous dataPlumeImpact craterVolcanoGeochemistry and PetrologyVulcano Island Geochemical monitoring CO2 flux CO2 fumaroles SO2 fluxSedimentologyGeologyBulletin of Volcanology
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Continuous SO2 flux measurements for Vulcano Island, Italy

2012

<p>The La Fossa cone of Vulcano Island (Aeolian Archipelago, Italy) is a closed conduit volcano. Today, Vulcano Island is characterized by sulfataric activity, with a large fumarolic field that is mainly located in the summit area. A scanning differential optical absorption spectroscopy instrument designed by the Optical Sensing Group of Chalmers University of Technology in Göteborg, Sweden, was installed in the framework of the European project "Network for Observation of Volcanic and Atmospheric Change", in March 2008. This study presents the first dataset of SO<sub>2</sub> plume fluxes recorded for a closed volcanic system. Between 2008 and 2010, the SO<sub>2</…

Vulcano Islanddata setSO2lcsh:QC851-999fumaroleNetwork for Observation of Volcanic and Atmospheric ChangeVulcanoFlux (metallurgy)Optical sensingemissionsulfur dioxideSicilyGeomorphologyAeolian archipelagoLipari Islandvolcanology Fossa Cratergeographygeography.geographical_feature_categoryplumeDifferential optical absorption spectroscopylcsh:QC801-809Atmospheric changedegassingSettore GEO/08 - Geochimica E VulcanologiaPlumelcsh:Geophysics. Cosmic physicsGeophysicsOceanographyDifferential optical absorption spectroscopyItalyVolcanoMessina [Sicily]lcsh:Meteorology. ClimatologyGeologyAnnals of Geophysics
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