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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Antonioli, Fabrizio; Lo Presti, Valeria; Rovere, Alessio; Ferranti, Luigi; Anzidei, Marco; Furlani, Stefano; Mastronuzzi, Giuseppe; Orru, Paolo E; Scicchitano, Giovanni; Sannino, Gianmaria; Spampinato, Cecilia R; Pagliarulo, Rossella; Deiana, Giacomo; de Sabata, Eleonora; Sansò, Paolo; Vacchi, Matteo; Vecchio, Antonio (2015): Tidal notches in Mediterranean Sea: a comprehensive analysis. Quaternary Science Reviews, 119, 66-84, https://doi.org/10.1016/j.quascirev.2015.03.016
    Publication Date: 2023-01-21
    Description: Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology. Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development. Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-01-21
    Keywords: Erosion rate; Lithology/composition/facies; Location; Reference/source
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
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  • 3
    Publication Date: 2023-04-13
    Keywords: Badisco; Badisco_notch_64; Badisco_notch_65; Badisco_notch_66; Balzi_Rossi_Ventimiglia_notch_3; Balzi Rossi Ventimiglia; Biddiriscottai; Biddiriscottai_notch_8; Bottom depth of biological rim; Buggerru; Buggerru_notch_21; Buggerru_notch_22; Cala_Domestica_notch_19; Cala_Domestica_notch_20; Cala_Fuili_notch_9; Cala_Mosca_notch_11; Cala_Mosca_notch_12; Cala Domestica; Cala Fuili; Cala Mosca; Calamosche; Calamosche_notch_48; Capo_Caccia_notch_5; Capo Caccia; Capri; Capri_notch_27; Cefalu; Cefalu_notch_40; Cefalu_notch_41; Ciolo; Ciolo_notch_62; Circeo; Circeo_notch_25; Colonia_de_Sant_Jordie_Palma_notch_1; Colonia de Sant Jordie Palma; Comino; Comino_notch_51; Comment; Depth of cliff toe; Direction; Dubrovnik; Dubrovnik_notch_71; ELEVATION; Event label; Favignana_Cala_rossa_notch_30; Favignana Cala rossa; Gaeta; Gaeta_notch_26; Gavathas; Gavathas_notch_73; Giovinazzo; Giovinazzo_notch_69; Gozo; Gozo_eroded_mushroom_notch_50; Gozo_notch_49; Gozo eroded mushroom; Lampedusa; Lampedusa_Cala_Calandra_notch_53; Lampedusa_notch_54; Lampedusa_notch_55; Lampedusa Cala Calandra; Latitude of event; Levanzo; Levanzo_harbour_notch_32; Levanzo_notch_31; Levanzo harbour; Lithology/composition/facies; Location; Longitude of event; Macari; Macari_notch_34; Malta; Malta_notch_52; Marettimo_Castello_notch_29; Marettimo_harbour_notch_28; Marettimo Castello; Marettimo harbour; Marina_di_Pulsano_notch_56; Marina di Pulsano; Marseille_Fausse_Monnaie_notch_2; Marseille Fausse Monnaie; Marzamemi; Marzamemi_notch_47; Masua; Masua_notch_13; Masua_notch_14; Masua_notch_15; Mongerbino; Mongerbino_notch_39; Montenegro; Montenegro_notch_72; MULT; Multiple investigations; Noli_Malpasso_notch_4; Noli Malpasso; Notch depth; Notch width; Palermo_harbour_notch_38; Palermo_Mondello_notch_37; Palermo harbour; Palermo Mondello; Pan_di_zucchero_notch_16; Pan_di_zucchero_notch_17; Pan_di_zucchero_notch_18; Pan di zucchero; Polignano_Modugno_notch_67; Polignano_San_Vito_notch_68; Polignano Modugno; Polignano San Vito; Porto_Conte_notch_6; Porto_Conte_notch_7; Porto Conte; Range; San_Vito_Castelluzzo_notch_33; Santa_Maria_di_Leuca_notch_60; Santa_Maria_di_Leuca_notch_61; Santa Maria di Leuca; San Vito Castelluzzo; Scopello; Scopello_notch_36; Sella_del_Diavolo_notch_10; Sella del Diavolo; Serra_Cicora_notch_58; Serra_Cicora_notch_59; Serra Cicora; Siracusa; Siracusa_notch_42; Siracusa_notch_43; Siracusa_notch_44; Siracusa_notch_45; Siracusa_notch_46; Site; Species; Talamone; Talamone_notch_24; Tharros; Tharros_notch_23; Thickness; Torre_Colimena_notch_57; Torre Colimena; Tremiti; Tremiti_notch_70; Type; Uncertainty; Variation bottom depth of biological rim; Variation of notch width; Waves energy, flux; Width; Zingaro; Zingaro_notch_35; Zinzulusa; Zinzulusa_notch_63
    Type: Dataset
    Format: text/tab-separated-values, 1569 data points
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  • 4
    Publication Date: 2020-06-03
    Description: Boulders are frequently dislodged from rock platforms, transported and deposited along coastal zones by high- magnitude storm waves or tsunamis. Their size and shape are often controlled by the thickness of bedding planes as well as by high-angle to bedding fracture network. We investigate these processes along two coastal areas of Favignana Island by integrating geological data for 81 boulders, 49 rupture surfaces (called sockets) and fracture orientation and spacing with four radiocarbon dates, numerical hydrodynamic analysis, and hindcast numerical simulation data. Boulders are scattered along the carbonate platform as isolated blocks or in small groups, which form, as a whole, a discontinuous berm. Underwater surveys also highlight free boulders with sharp edges and sockets carved out in the rock platform. Boulders are composed of ruditic- to arenitic-size clastic carbonates. Their size ranges from 0.6 to 3.7 m, 0.55 to 2.4 m, and 0.2 to 1 m on the major (A), medium (B), and minor (C) axes, respectively. The highest value of mass estimation is 12.5 t. Almost all of boulders and sockets are char- acterized by a tabular or bladed shape. The comparisons between a) the fractures spacing and the length of A- and B-axes, and b) the frequency peaks of C-axis with the recurrent thickness of beds measured along the coastal zone demonstrate the litho-structural control in the size and shape of joint-bounded boulders. These comparisons, to- gether with the similarity between the shapes of the boulders and those of the sockets as well as between the lithology of boulders and the areas surrounding the sockets, suggest that blocks originate by detachment from the platform edge. Thus, the most common pre-transport setting is the joint-bounded scenario. Hydrodynamic equations estimate that the storm wave heights necessary to initiate the transport of blocks diverge from ~2 m to ~8 m for joint-bounded boulders and from few tens of centimeters up to ~11 m for submerged boulders. The comparison between the wave heights at the breaking point of the coastal zones with the results of hydro- dynamic equations shows that waves approaching the coastline are able to transport all surveyed boulders. Our data suggest that boulders have been transported by several storm events, even in very recent times.
    Description: Published
    Description: 191-209
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 2TR. Ricostruzione e modellazione della struttura crostale
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2019-04-02
    Description: Submerged caves represent potential archives of speleothems with continental and marine biogenic layers. In turn, these can be used to reconstruct relative sea-level changes. This study presents new data on the tectonic behaviour of the island of Malta during the Holocene. These data were obtained from a speleothem sampled, during an underwater survey, at a depth of −14.5 m, inside a recently discovered submerged cave. Since the cave was mainly formed in a subaerial karst environment, the presence of a speleothem with serpulids growing on its continental layers permitted the reconstruction of the chronology for drowning of the cave. The radiocarbon dates obtained from the penultimate and last continental layers of the speleothem, before a serpulid encrustation, were compared with synthetic aperture radar (SAR) and global positioning system (GPS) data, together with published sedimentological and archaeological data. The radiocarbon analyses provided an average age of 7.6 ka BP that perfectly aligns with the Lambeck’s model of Holocene sea level. Morevoer, long-term data agree with published archeological and sedimentological data as well as with SAR interpherometric and GPS trends on a decadal scale. We conclude that the Maltese islands were tectonically stable during the Holocene, and this tectonic behaviour still persists nowadays. On the contrary, new informations on older deposits, such as MIS5e (Maritime Isotope Stage, corresponding to 125 ka ago) were not found in the study area, confirming the lack of older Quaternary marine deposits in these islands.
    Description: Published
    Description: 1588-1597
    Description: 5A. Ricerche polari e paleoclima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2022-03-07
    Description: Areas of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthropic activities. We analyzed light detection and ranging (LiDAR) and Copernicus Earth observation data. The aim of this research is to provide estimates and detailed maps (in three coastal plain of Sardinia (Italy) and in the Pontina Plain (southern Latium, Italy) of: (i) the past marine transgression occurred during MIS 5.5 highstand 119 kyrss BP; (ii) the coastline regression occurred during the last glacial maximum MIS 2 (21.5 krs cal BP); and (iii) the potential marine submersion for 2100 and 2300. The objective of this multidisciplinary study is to provide maps of sea level rise future scenarios using the IPCC RCP 8.5 2019 projections and glacio-hydro-isostatic movements for the above selected coastal zones (considered tectonically stable), which are the locations of touristic resorts, railways and heritage sites. We estimated a potential loss of land for the above areas of between about 146 km2 (IPCC 2019-RCP8.5 scenario) and 637 km2 along a coastline length of about 268 km.
    Description: Published
    Description: 2597
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Keywords: central Mediterranean coastal plains; past (MIS 5.5) and future sea level at 2100 and 2300; Sardinia; Pontina Plain ; sea level
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
    Publication Date: 2022-03-07
    Description: Coastal dynamics are the result of several processes controlling the balance between sediment input and output over time. The beach system is not always able to maintain a neutral coastal balance due to natural and anthropogenic causes. We present an integrated marine geology, geomorphological and sea-level rise analysis in the coastal sector between Torre delle Ciavole and Capo Calavà (North-Eastern Sicily, Italy).This sector is characterized by high uplift rates and frequent seismicity (mainly generated by the very active Vulcano-Tindari Fault System), promoting the development of mass-wasting processes in the coastal and offshore sectors. A main erosive feature observed in the area is the head of the Gioiosa Marea submarine canyon, located at some meters of depth, few hundred meters far the coastline. The main morphological features of the canyon were reconstructed through the analysis of high-resolution multibeam data, indicating that the canyon is active, as also testified by the comparison of time-lapse aerial photos. Due to this active setting, the study area is exposed to multiple geohazards, among which we deal with: (1) retrogressive instability at the head of the Gioiosa Marea submarine canyon, (2) coastal erosion favored by the downlope funnelling of littoral drift at the canyon head, (3) flooding scenario at 2100 using the IPCC (Intergovernmental Panel on Climate Change) and Rahmstorf sea-level projections. The consequences associated with these geohazards are amplified by the strong anthropization pressures occurring along in this sector. Our results provide key insights regarding the future scenarios of this coastal sector, revealing the effects of the retrogressive activity associated with the canyon head on the coastal strip. We also present the first management tool for the application of forecasting studies by local administrations.
    Description: Published
    Description: 2
    Description: 3A. Geofisica marina e osservazioni multiparametriche a fondo mare
    Description: JCR Journal
    Keywords: Submarine canyon · Sicily continental margin · Uplift rate · Coastal erosion · Relative sea-level projections · Coastal flooding ; Geohazard assessment
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2021-10-07
    Description: This paper re-apprises the scant elephant remains belonging to a dwarf Palaeoloxodon of uncertain taxonomy collected during the 1980s from a cave on Favignana Island (Aegadian Archipelago, western Sicily). The elephant was recently 14C-dated to the Last Glacial Maximum (20,350–19,840 cal. BP), indicating that the Favignana elephant is likely the most recent insular endemic Palaeoloxodon species thus far reported from the Western Mediterranean. Dimensionally the remains are smaller than the late Middle- Late Pleistocene P. ex gr. P. mnaidriensis from Puntali Cave (Palermo), and similar in size to the P. ex gr. P. mnaidriensis individual from San Teodoro Cave (Messina) post-dating a flowstone U-Th dated to ca. 32 ka. Accordingly, the possibility that relict populations of Palaeoloxodon persisted on Sicily longer than previously believed remains an intriguing possibility. None the less, the available data do not clearly indicate whether or not the small dimensions and recent age of the Favignana elephant may reflect a Late Pleistocene colonisation of Favignana Island by small P. ex gr. P.mnaidriensis. Our palaeogeographic reconstruction of the Aegadian Islands does however demonstrate that Favignana was connected to Sicily during most of the Late Pleistocene, allowing elephants to disperse freely between Sicily and Favignana during the Last Glacial (MIS 4-MIS2).
    Description: Published
    Description: 2116-2134
    Description: 4A. Oceanografia e clima
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2022-02-18
    Description: The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to have been tectonically stable since the last interglacial (Marine Isotope Stage 5.5 [MIS 5.5]), because related sea level markers fit well with sea level rise models. The analysis of visual observations and punctual measurements highlighted that, with respect to the total length of surveyed coast, the occurrence of tidal notches, shore platforms, and other indicators accounts for 85% of the modern coastline, and only 1% of the MIS 5.5 equivalent. Therefore, only 1% of the surveyed coast showed the presence of fossil markers of paleo sea levels above the datum. This significant difference is mainly attributable to erosion processes that did not allow the preservation of the geomorphic evidence of past sea level stands. In the end, our research method showed that the feasibility of applying such markers to define long-term tectonic behaviour is much higher in areas where pre-modern indicators have not been erased, such as at sites with hard bedrock previously covered by post-MIS 5.5 continental deposits, e.g., Sardinia, the Egadi Islands, Ansedonia, Gaeta, and Circeo. In general, the chances of finding such preserved indicators are very low.
    Description: Published
    Description: 2127
    Description: 4A. Oceanografia e clima
    Description: 7A. Geofisica per il monitoraggio ambientale
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2021-11-08
    Description: The coastal areas of the central Mediterranean Sea are sensitive to climate change and the consequent relative sea level rise. Both phenomena may affect densely urbanized and populated areas, causing severe damages. Our maps show the land-marine flooding projections as effects of the expected relative sea level rise for four Italian coastal plains using (i) IPCC AR5 estimations, based on the IPCC RCP 8.5 emission scenarios and (ii) the Rahmstorf 2007 model. Isostatic and tectonic data were added to the global projections to estimate the relative sea changes expected along the coastline by 2100, as well as sea-flooding. The northern Adriatic map shows the study area, extending for about 5500 km2, and is presented at a scale of 1:300,000 with two inset maps at a scale of 1:150,000. The Oristano coastal plain is about 125 km2; the map scale is at 1:60,000 with an inset map scale at 1:33,000. The Cagliari coastal study area extends for 61 km2; the map scale is at 1:60,000 with two inset maps at 1:30,000. The Taranto area extends for 4.2 km2 and is represented at a scale map of 1:30,000, while the three inset maps are at a scale of 1:10,000.
    Description: Published
    Description: 961 – 967
    Description: 3SR. AMBIENTE - Servizi e ricerca per la Società
    Description: JCR Journal
    Keywords: Relative sea level rise, Italian coastal plains, IPCC and Rahmstorf projections, flooding maps, 2100 scenarios
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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