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Earth-Prints is an open archive created and maintained by Istituto Nazionale di Geofisica e Vulcanologia. This digital collection allows users to browse, search and access manuscripts, journal articles, theses, conference materials, books, book-chapters, web products.

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  • PublicationOpen Access
    Hard-bottom benthic communities in two semi-submerged marine caves (Adriatic Sea): an updated baseline with insights on short-term recreational boating impacts
    (Oxford : Elsevier Science Limited, 2026-04-24)
    Tursi, Andrea
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    Chimienti, Giovanni
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    Bottalico, Antonella
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    Schiavo, Antonella
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    Longo, Caterina
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    Mastrototaro, Francesco
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    We investigated two semi-submerged marine caves within the Tremiti Islands Marine Protected Area (South Italy, Adriatic Sea), integrating geomorphological mapping, video-transects, qualitative sampling, and an assessment of recreational boating. High-resolution 3D surveys were used to characterize cave morphology. Benthic assemblages were analysed from SCUBA video-transects performed at two depths (3 and 7 m) in May and November 2021 (before and after the tourist season, respectively), and species inventories were refined through qualitative sampling. A total of 118 taxa were recorded. Benthic cover was consistently high (98-99%) across caves, depths, sectors, and periods. Assemblages were dominated by encrusting sciaphilic Rhodophyta and Porifera, and showed clear spatial gradients both horizontally and vertically. Recreational boating pressure was high, with >5000 boat transits and approximately 77,000 passengers recorded in summer 2021. Despite this intensity, no detectable short-term changes in benthic composition were detected at the community level. Large excursion boatsquick visits, regulated, and professionally operatedhad minimal impact, whereas small, rented motorboats, with longer and less controlled visits, represent a potential risk. These findings provide the first integrated ecological and geomorphological baseline for Tremiti semi-submerged caves and support targeted management of recreational boating within MPAs.
  • PublicationOpen Access
    Cliff-top boulder deposits as geomorphological markers of Last Interglacial extreme wave events in the Mediterranean: evidence from south-eastern Sicily
    (Elsevier Science Limited:Oxford Fulfillment Center, PO Box 800, Kidlington Oxford OX5 1DX United Kingdom:011 44 1865 843000, 011 44 1865 843699, EMAIL: asianfo@elsevier.com, tcb@elsevier.co.UK, INTERNET: http://www.elsevier.com, http://www.elsevier.com/locate/shpsa/, Fax: 011 44 1865 843010, 2026-04-30) ; ; ; ; ;
    Nandasena, N
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    Cliff-top boulder deposits represent one of the most extreme and debated geomorphological expressions of highenergy coastal processes, as their emplacement requires sustained overtopping of cliffs during coastal flooding. Occurring several metres above mean sea level and well beyond the reach of ordinary wave run-up, cliff-top boulder deposits are particularly sensitive indicators of extreme wave events. In this study, we investigate clifftop boulder deposits atop a 10-m-high cliff in southeastern Sicily by integrating geomorphological observations with hydrodynamic modelling for both present and Last Interglacial forcing conditions. Hydrodynamic modelling was used to simulate extreme wave events that can cause coastal flooding and wave flow under tropical-like cyclone and tsunami scenarios. To evaluate the geomorphological effects of these extreme wave events, we modelled and compared the current scenarios under the present-day sea level, and Last Interglacial scenarios, which in contrast, incorporate elevated relative sea level and intensified hurricane and tsunami forcings to evaluate wave flow needed for cliff-top deposit emplacement. The results reflect a scenario with a Last Interglacial post-highstand regressive phase, highlighting the role of sea-level-controlled boundary conditions in enabling extreme coastal flooding and inland boulder transport. Our results indicate that Mediterranean cliff-top boulder deposits reflect the effectiveness of extreme waves acting under specific boundary conditions, rather than the absolute magnitude of the waves themselves, with relative sea level exerting a first-order control on coastal impact.
  • PublicationOpen Access
    Seasonal ground deformation at subglacial Katla Volcano, Iceland: observations and models
    (Lausann : Frontiers Media S.A., 2013-, 2026-01-20)
    O'hara, Catherine
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    Magnússon, Eyjólfur
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    Albino, Fabien
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    Liebsch, Jonas
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    Gestsson, Bessi
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    Changes at the surface of a volcanic edifice, such as snow or hydrological loading, ice cap melting, and flank destabilization, can cause significant surface deformation. Understanding the contribution of surface processes to ground deformation is therefore important for monitoring the state of the underlying volcanic system. The Katla Volcano in Iceland lies under Mýrdalsjökull, the fourth largest glacier in Iceland, and undergoes the largest seasonal deformation of all Icelandic volcanoes: up to 4 cm horizontally and 3 cm vertically at the Austmannsbunga (AUST) Global Navigation Satellite System (GNSS) station. The last confirmed eruption of Katla occurred in 1918. Since then, episodes of elevated seismicity and jökulhlaups (sudden glacial outburst floods) have been recorded at the volcano, the most noticeable in 1955, 1999, 2011, and 2024. During the 2024 jökulhlaup, horizontal displacement of up to 7 cm was recorded at AUST. In this work, elastic three-dimensional finite element method models were implemented to quantify surface deformation from seasonal load changes. The models include realistic bedrock topography and ice unloading based on recent data collected at Mýrdalsjökull. A deformation model considering only seasonal snow unloading can reproduce within uncertainty the observed GNSS vertical surface displacements. It can also explain the horizontal signals at GNSS stations located outside the glacier, although not at GNSS stations located on nunataks inside Mýrdalsjökull. An additional deformation source must be considered to explain the residual cm-scale horizontal displacement at these stations. We model the residual signal using a thermo-poro-elastic cylindrical source. The best-fit source is a cylinder located at the surface that produces cm-scale horizontal deformation with limited vertical deformation. The shallow source depth derived from the inversion and the surface deformation recorded at AUST during the jökulhlaup series in 2024 and 2025 suggests that seasonal deformation is not strictly related to magmatic activity. We infer that changes within the hydrologic system of the glacier are responsible for most of the horizontal deformation at Katla.
  • PublicationOpen Access
    From Waste to Value: A Data-Driven Framework for Sustainable Raw Materials Substitution in the Ceramic Industry
    With increasing geopolitical risks, environmental pressures, and regulatory demands, the sustainable sourcing of raw materials has become a global priority for achieving the United Nations Sustainable Development Goals (SDGs), particularly SDG 9 (Industry, Innovation and Infrastructure), SDG 12 (Responsible Consumption and Production), and SDG 13 (Climate Action). This study presents a data-driven framework for assessing the substitution of imported primary raw materials with secondary resources derived from mining waste, using the Italian ceramic industry as a testbed. Through a combined approach integrating material characterization, life cycle assessment, and supply chain analytics, we evaluate the technical, environmental, and resilience performance of substituting Turkish albite with feldspathic waste from Calabrian quarries. Results show that hybrid logistics configurations (truck and ship) for domestic by-products can outperform imported materials in terms of greenhouse gas emissions, supply chain resilience, and strategic autonomy while supporting circular economy principles. The framework provides replicable analytical tools to support evidence-based sourcing decisions in resource-intensive sectors, helping companies and policymakers align operational practices with sustainability goals. Implications for circular value creation, climate mitigation, and industrial policy are discussed.
  • PublicationOpen Access
    Deciphering carbon dioxide signals in urban environments: integrated stable isotope and concentration monitoring for evaluating the impact of human activities on the atmospheric composition
    Urban environments function as major hotspots for anthropogenic greenhouse gas emissions, yet quantifying the contribution of specific sources is still a challenge due to the complex interplay between emissions, meteorology, and biospheric activity. Continuous high-frequency monitoring of atmospheric CO 2 concentration and stable isotope composition provides critical insight into the sources and processes governing urban carbon dynamics. In this study, airborne CO 2 concentration, δ 13 C-CO 2 , and δ 18 O-CO 2 were measured at 5-min intervals at the ACO-Pa1 station in Palermo (Italy) from November 2023 to September 2025, together with a comprehensive set of meteorological variables. The dataset reveals that CO 2 concentrations exceeded the global atmospheric background by approximately 4.5%. Probability plot analysis showed four distinct CO 2 populations, highlighting urban CO 2 enhancement and revealing some pollution episodes. Carbon isotope data show systematic 13 C-depletion during elevated CO 2 conditions, and Keeling plot analysis shows that fossil fuel and natural gas combustion represent the dominant forcing sources, with episodic contributions from landfill gas under specific atmospheric conditions. Principal component analysis demonstrated that while δ 13 C-CO 2 and CO 2 concentration are strongly coupled to anthropogenic emissions and seasonal house-heating demands (explaining 30.5% of the dataset variance), the δ 18 O-CO 2 signal behaves as a rather independent tracer linked to biospheric exchange and hydrological processes in the urban area of Palermo. Seasonal patterns are marked by higher CO 2 concentrations and stronger 13 C-depletion during fall and winter, which is consistent with enhanced residential heating and reduced biospheric uptake, while the spring-summer periods show lower concentrations and isotopic signature driven by photosynthetic carbon fixation. Oxygen isotope variability displays a pronounced seasonal cycle that is partly decoupled from δ 13 C-CO 2 , reflecting biosphere-atmosphere oxygen exchange. These results prove that integrated monitoring of the concentration and stable isotopes is a powerful