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76 results for “Emilia-Romagna”
Modelling NBSs for coastal erosion and marine flooding: the Emilia-Romagna case studies
<p>The study was conducted in the context of the OPEn-air laboRAtories for Nature baseD solUtions to Manage environmental risks (OPERANDUM) project which is an H2020 project which aims at providing tools and methodologies for the assessment of NBS efficiency around the world. Two NBs were tested via modelling simulations on the Bellocchio Beach at Lido di Spina (Italy) located in the northern part of the Emilia-Romagna coast (northern Adriatic Sea): an artificial dune built with natural materials and a marine seagrass meadow.</p> <p>The artificial dune is an engineered structure that will mimic the functioning of natural dunes. Its aims are reducing both natural dune erosion and flooding in adjacent coastal lowlands. It consists of a barrier between the sea and land, in a similar way to a seawall. Unlike the latter, the NBS are ‘dynamic’, i.e. the dune/beach system interacts a great deal and is constantly undergoing small adjustments in response to changes in wind and wave climate or sea level. Its construction involves the placement of sediment from dredged sources on the beach and it will be reinforced with a structure composed of biodegradable material. Different typologies of experimental solutions are foreseen.</p> <p>The second NBS consists of an alongshore seagrass belt located in front of the coastal area. It was investigated as a potential mechanism for wave amplitude reduction. Among the few species that can live in the northern Adriatic Sea, Zostera Marina was chosen due to its ability to live in a marine environment influenced by freshwaters. A more detailed description can be found in (Pillai et al., 2021).</p> <p>The numerical model chain, specifically developed for the study, consists of an Ocean Circulation model, so-called SHYFEM (Umgiesser et al., 2004), a wave model, so-called WWIII (Alves and Ardhuin, 2016), and a morphological model, so-called XBeach (Roelvink et al., 2009). Ten years of XBeach simulations have been executed to simulate the morphological impacts on the coastal strip for the present (2010-19) and future climate (2040-49). For each 10 years period, four scenarios were simulated: the baseline scenario without NBS (baseline_run), the scenario with the dune (dune_run), the scenario with the seagrass effect (seagrass_run) and the scenario with the two NBS integration (dune_seagrass_run).XBeach was forced with sea level and wave time series predicted by the SHYFEM and WWIII models respectively.</p> <p>The model domain consists in a curvilinear structured grid of about 3.2 km (longshore) x 2.8 km (cross-shore) covering the coastal stretch of Bellocchio beach at Lido di Spina (Italy) and extends seaward up to about 10 m depth.</p> <p>The performance of the NBSs and their impact on coastal erosion and marine flooding were investigated. For both present and future scenarios (201-2019 and 2040-2049), the reduction in wave intensity obtained with the seagrass provided greater benefits in terms of erosion mitigation and flood reduction. The analysis highlighted the limited scale of the dune intervention, in particular under present conditions, highlighting that the longer the artificial dune implemented, the larger the beach and dune area protected. For the future scenarios, the results are still significant and even small projects are expected to help in mitigating coastal erosion and marine flooding.</p> <p>For long-period simulations, no relevant improvements in reducing beach erosion was observed when the artificial dune was combined with the seagrass meadows with respect to the seagrass effects only. Instead, a dominant increase in sea levels will probably highlight the dune functions in hindering the marine ingression into the lagoon area behind and the consequent sediment redistribution.</p> <p>This dataset consists of XBeach model results, mainly:</p> <ul> <li>Morphological evolution of the coastal bottom at Bellocchio beach (Lido di Spina, Italy) in terms of initial and final bed levels, for the current (201-2019) and the future (2040-2049) scenarios. Results are available for the four NBS scenarios described above (and detailed in the Presentation.pdf)</li> <li>Maximum flood depth, defined as the non-simultaneous maximum water depth on the beach domain of Bellocchio (Lido di Spina, Italy) for the current (201-2019) and the future (2040-2049) scenarios. Results are available for the four NBS scenarios described above (and detailed in the Presentation.pdf) </li> <li>Erosion-deposition maps for the current (201-2019) and the future (2040-2049) scenarios. Results are available for the four NBS scenarios described above (and detailed in the Presentation.pdf).</li> </ul>
Emilia-Romagna coastal area NBS (OAL ITALY) for storm surge mitigation
<p>Within the framework of the OPEn-air laboRAtories for Nature baseD solUtions to Manage environmental risks (OPERANDUM) project, the seagrass NBS is presented within a simulation design methodology consisting of the comparison between validated wave numerical simulations for the present/ future climate, and modified wave simulations with marine seagrass. Ten years of WWIII simulations have been executed to generate the wave climatology, particularly over the Emilia-Romagna coastal strip for the present (2010-19) and future climate (2040-49) using MedCordex winds (based on RCP8.5). The WWIII model was modified to include a modified bottom dissipation stress due to submerged vegetation, thereby incorporating the NBS4 as a potential mechanism for wave amplitude reduction. The seagrass species <em>‘Zostera marina’</em> was chosen in this study and an along-shore seagrass belt was first inserted in WWIII and sensitivity experiments were carried out to assess the effects of different types of seagrass landscape designs in the Bellocchio beach. Simulation experiments with and without seagrass (NBS4) were carried out for the present and future climates. Based on the present and future climate simulations, it is noted that the seagrass landscaping is an important aspect in the numerical modelling of vegetation. A combination of broken vegetation stripes and clusters were seen to be effective in reduction of wave energy at the coast in comparison to other landscape designs. The wave height comparisons in the Bellocchio beach, with and without vegetation showed a considerable reduction in wave heights specifically in the higher ranges for both the present and future climates. There exists a strong seasonality in the attenuation rates along the coastal belt with higher attenuations during winter and comparatively lower in summer. In comparison to the present climate, a slightly increased rate of mean attenuation is expected in the future scenarios. Overall, the Zostera Marina seagrass applied for the Emilia-Romagna coastal belt was found to be efficient in reduction of wave energy (> 50%). The limitation being that the experiments were done with rigid seagrass and in the future, we look for advanced parameterization using flexible seagrass.</p> <p>This dataset contains wave model outputs for the OAL-ITALY, mainly:</p> <ul> <li>Bathymetry of the model domain, Spatial maps of mean significant wave height (Hs in m) for present (2010-19) and future climate (2040-49), Seagrass belt position in the Bellocchio beach, Time-series comparison of Hs, with & without vegetation, and Wave attenuation maps.</li> </ul> <ul> <li>Selected locations (station map) for the time series in the Emilia-Romagna coastal belt during the period 2010-19, and 2040-49 (8 stations), Selected locations (station map) in the Emilia-Romagna coastal belt for the time series comparison (with and without vegetation) during the period 2010-19, and 2040-49 (5 stations).</li> </ul> <ul> <li>WW3 time series of wave parameters (wave height, peak period, & direction) for 8 stations in the Emilia-Romagna coastal belt (2010-19, present climate).</li> <li>WW3 time series of significant wave height (Hs in metres) with and without vegetation for 5 stations in the Emilia-Romagna coastal belt (2010-19, present climate).</li> <li>WW3 time series of wave parameters (wave height, peak period, & direction) for 8 stations in the Emilia-Romagna coastal belt (2040-49, future climate).</li> <li>WW3 time series of significant wave height (Hs in metres) with and without vegetation for 5 stations in the Emilia-Romagna coastal belt (2040-49, future climate).</li> </ul>
Data/ codes used in the the Natural Hazards and Earth System Sciences (NHESS) publication titled "Wind-Wave Characteristics and extremes along the Emilia-Romagna coast" by Pranavam Ayyappan Pillai et al. (2022)
<p>The archive contains datasets and codes used in the manuscript titled "Wind-Wave Characteristics and extremes along the Emilia-Romagna coast", and published in the journal <em>Natural Hazards and Earth System Sciences</em> (<em>NHESS</em>) by Pranavam Ayyappan Pillai et al., 2022.</p> <p>Pranavam Ayyappan Pillai, U., Pinardi, N., Federico, I., Causio, S., Trotta, F., Unguendoli, S., and Valentini, A.: Wind-Wave Characteristics and extremes along the Emilia-Romagna coast, Nat. Hazards Earth Syst. Sci. Discuss. https://doi.org/10.5194/nhess-2022-103, 2022.</p>
INFO-CSO (PSR Emilia-Romagna) - Indagine sull'intenzione d'uso dell'App
<p>Dati del questionario agli ortofrutticoltori per valutare l'intenzione d'uso dell'App</p> <p>Dati Progetto: </p> <p>INFO-CSO Informazione fruibile per lo sviluppo del sistema ortofrutticolo Regionale dell'Emilia Romagna</p> <p><a href="http://agricoltura.regione.emilia-romagna.it/psr-2014-2020/temi/tipi-di-operazioni/16-1-01-gruppi-operativi-del-partenariato-europeo-per-la-produttivita-e-la-sostenibilita-dellagricoltura/bandi-e-documenti-utili/Bando-2018/bando-goi-2018">Deliberazione di Giunta regionale nr. 2144 del 10 dicembre 2018 </a></p> <p><strong>Focus Area: </strong>3.A - Migliorare la competitività dei produttori primari integrandoli meglio nella filiera agroalimentare attraverso i regimi di qualità, la creazione di un valore aggiunto per i prodotti agricoli, la promozione dei prodotti nei mercati locali, le filiere corte, le associazioni e organizzazioni di produttori e le organizzazioni interprofessionali</p> <p><strong>Tipo di Operazione: 16.1.01 </strong> - Gruppi Operativi del PEI per la produttività e la sostenibilità dell'Agricoltura</p> <p><br> <strong>Id domanda: 5116697</strong><br> <strong>Finanziamento ricevuto</strong><strong>: </strong><strong>€ 31.522,22</strong></p> <p><br> <strong>Obiettivi e Finalità: </strong></p> <p>Supportare le imprese della regione Emilia-Romagna ad intraprendere un vero e proprio percorso di ammodernamento e crescita, mettendo a disposizione con modalità di accesso rapido ed in formato facilmente fruibile, dati ed informazioni sulla produzione e sul mercato dei principali prodotti ortofrutticoli al fine di rendere più competitive le aziende, consentendo loro di fare programmazione, e di mettere a punto strategie produttive, organizzative e commerciali più efficaci ed in linea con le esigenze del mercato e dei consumatori. Il servizio online proposto intende mette in contatto i produttori, gli operatori della filiera e gli acquirenti nella catena del valore dei prodotti ortofrutticoli freschi, offrendo loro visibilità e trasparenza. L'accesso ai dati in tempo reale potrà supportare tutti gli attori della filiera, consentendo loro di risparmiare tempo, rafforzare le relazioni, essere meglio informati e migliorare i processi decisionali.</p> <p><strong>Risultati attesi</strong>:</p> <p>I risultati attesi sono relativi all’applicazione delle informazioni identificate alle scelte imprenditoriali dei produttori ortofrutticoli dell’Emilia Romagna. CSO, tramite i suoi soci, copre circa il 50%% della produzione ortofrutticola regionale. Una corretta gestione imprenditoriale, tramite l’utilizzo di informazioni strutturate, può portare ad un aumento delle marginalità sufficiente a garantire la redditività di tutti gli attori della filiera. Inoltre, il presente piano avrà tra le applicazioni, la realizzazione di uno studio LCA che consentirà di dare agli agricoltori indicazioni sulle migliori tecnologie per la gestione ambientale, le quali se applicate, statisticamente consentono di ridurre il peso ambientale delle scelte agronomiche. Lo studio relativo alle certificazioni sociali ed etiche, consentirà di fornire un altro strumento per le scelte imprenditoriali, in quanto fornirà informazioni circa la percezione dei consumatori di tali certificazioni (GLOBALGAP-GASP, SA 8000).</p> <p> <strong>Referente scientifico: </strong>Canavari Maurizio</p>
Inventory of landslides triggered by heavy rainfall in the Emilia-Romagna region (Italy) in May 2023
<p>The dataset contains 49103 landslides, that were manually mapped by visual inspection of pre- and post-event satellite images in an area of 8981 km2. Such images are acquired by PlanetScope satellites (<a href="https://www.planet.com/">https://www.planet.com/</a>) and are provided under an academic license; 3-m resolution multiband tiles are used.</p> <p>Pre-event imagery refers to the Monthly Global Basemap products provided by Planet, the April 2023 Basemap was used. Post-event images were acquired between 22 May and beginning of June 2023. The cloud-free image closer to the event was used and multi-temporal frames were checked in selected areas (e.g., due to the presence of shadows or unclear images). Images are accessed through the Planet QGIS Plugin.</p> <p>This dataset supersedes version 1, since it represents its update; major changes include:</p> <ul> <li>mapping over a wider area (8981 vs 5764 km2);</li> <li>check on the landslides mapped in version 1 located on flat slopes (lower than 5°); removal of polygons associated with river erosion and not due to gravity movements</li> </ul> <p> </p> <p>NOTES ON VERSION 1</p> <p>landslides were manually mapped at a scale of 1:5.000 by a single operator in a time interval of 5 weeks following the rainfall event; the inventory (version 1.0) was completed on 28 June 2023. Please note that data did not undergo any kind of validation.</p> <p>Data are provided in shapefile format (coordinate system WGS84 UTM 32N) and in kml format.</p> <p>The main dataset is the “Emilia landslides” shp/kml file; the “area” shapefile refers to the investigated area; the “riverbank and agricultural fields” files include polygons that were mapped but refer either to river courses having high discharge in the post-event images, or to color changes probably due to farming activities or the evolution of agricultural fields. The “riverbank and agricultural fields” elements should not refer to slope movements, and usage of these data is not recommended, unless a validation is made.</p>
SERENA EJP Soil: Green House Gas Regulation Application Emilia-Romagna, Italy (Summer)
<p>The internal EJP SOIL project SERENA contributed to the evaluation of soil multifunctionality aiming at providing assessment tools for land planning and soil policies at different scales. By co-working with relevant stakeholders, the project provided co-developed indicators and associated cookbooks to assess and map them, to report both on soil degradation, soil-based ecosystem services and their bundles, under actual conditions and for climate and land-use changes, at the regional, national, and European scales.</p>
Monitoring NBS for coastal erosion and marine flooding: the Emilia-Romagna case study
<p>The study was conducted in the context of the OPERANDUM project which is an H2020 project which aims at providing tools and methodologies for the assessment of NBS efficiency around the world. As NBS will be tested an artificial dune built with natural materials. </p> <p>The artificial dune is an engineered structure that will mimic the functioning of natural dunes. Its aims are reducing both natural dune erosion and flooding in adjacent coastal lowlands. It consists of a barrier between the sea and land, in a similar way to a seawall. Unlike the latter, the NBS are ‘dynamic’, i.e. the dune/beach system interacts a great deal and is constantly undergoing small adjustments in response to changes in wind and wave climate or sea level. Its construction involves the placement of sediment from dredged sources on the beach and it will be reinforced with a structure composed of biodegradable material. Different typologies of experimental solutions are foreseen.</p> <p>The Bellocchio Beach at Lido di Spina (Italy) was initially chosen for the study, however the Volano beach was selected as the new study area because of the strong erosion caused by an intense storm event in December 2020 at Bellocchio. The dune was built on the Volano beach and monitoring surveys were carried out on this new site. </p> <p>A morphological monitoring aimed to assess the beach evolution and the performance of the NBS were performed. Monitoring of morphology evolution of shoreline and inland area provide information about impact of the NBS on coastal erosion. Furthermore, the changes in the form of the work give information about the resistance of the NBS to wave attacks. Sedimentological campaigns have been planned in order to provide information regarding the texture of the sediments present in the area detected and possibly highlight changes after the construction of the dune.</p> <p>Three monitoring campaigns were carried out before, immediately after and six months later the construction of the dune (January, May and October 2022). All data were analysed to assess local coastal dynamics and NBS evolution. </p> <p>The monitoring consisted of: </p> <ul> <li> <p>topographic and bathymetric surveys (GNSS and multibeam/singlebeam echosounder) to generate DTMs of the entire area (10 m cell size); </p> </li> <li> <p>aerial photogrammetric surveys by UAV for the production of orthophotos and high resolutions DTMs of the emerged beach (1m cell size) and of the dune area (0.2 m cell size); </p> </li> <li> <p>sediment sampling and grain size analysis. </p> </li> </ul> <p>Surveys show that morphological and sedimentological changes are determined mostly by anthropic actions to the beach and seabed maintenance (artificial winter banks and Sacca di Goro channel). </p> <p>Regarding the dune area no significant changes in morphology were observed due to the limited period between the surveys. Appreciable signals were detected, such as the natural recolonization by pioneer plant species and the slight sand accumulation on the dune foot.</p> <p>This dataset consists of data related to monitoring activities. </p>
Rapid mapping inventories of landslides triggered by heavy rainfall in the Emilia-Romagna region (Italy) during May 2023
<p>The dataset contains the spatial explicit inventories of landslides triggered by heavy rainfall in the Emilia-Romagna region (Italy) during May 2023. Hybrid pixel-based and object-based image analysis approach was used to generate the rapid mapping products. The fully automated supervised procedure relies on change detection analysis, based on quantitative variation of vegetation cover in pre-event and post-event remote sensing imagery. Two separate inventories were generated using:<br>- Copernicus Sentinel-2 MSI satellite imagery<br>- PlanetScope SuperDove satellite imagery</p> <p>The dataset is a spatial representation vector polygons representing potential landslides, distributed in GeoPackage format, complemented with confidence measure. It contains modified Copernicus Sentinel data, available at no cost from Copernicus Open Access Hub. Use of PlanetScope images is under license: ©Planet Labs PBC, CC BY-NC-SA 2.0.</p>
Extreme Total Water Level values for different possible combinations along the Southern Veneto, Emilia-Romagna and Northern Marche coastlines
<p><strong>Description:</strong> This data set is the result of the calculation of the extreme values of different Total Water Level combinations, including a range of components (Mean Sea Level, Tide, Residual, wave setup, wave runup). A total of 8 possible combinations:</p> <table> <tbody> <tr> <td> <p><strong>TWL Acronyms</strong></p> </td> <td> <p><strong>Used component</strong></p> </td> </tr> <tr> <td> <p>dCUE</p> </td> <td> <p>MSL (base) + Tide (Highs) + Residual + Estimated nearshore components (setup and runup)</p> </td> </tr> <tr> <td> <p>dCUU</p> </td> <td> <p>MSL (base) + Tide (Highs) + Residual + Univariated nearshore components (setup and runup)</p> </td> </tr> <tr> <td> <p>dTU</p> </td> <td> <p>TWL dynamic [MSL (base) + Tide (Highs) + Residual + Univariated nearshore components (setup and runup)]</p> <p>Based on Sanuy et al. (2020)</p> </td> </tr> <tr> <td> <p>dWUU</p> </td> <td> <p>Water Level [MSL (base) + Tide (Highs) + Residual] + Univariated nearshore components (setup and runup)</p> </td> </tr> <tr> <td> <p>sCUE</p> </td> <td> <p>MSL (base) + Tide (Highs) + Residual + Estimated Setup</p> </td> </tr> <tr> <td> <p>sCUU</p> </td> <td> <p>MSL (base) + Tide (Highs) + Residual + Univariated Setup</p> </td> </tr> <tr> <td> <p>sTU</p> </td> <td> <p>TWL static[ MSL (base) + Tide (Highs) + Residual + Univariated setup]</p> <p>Based on Sanuy et al. (2020)</p> </td> </tr> <tr> <td> <p>sWUU</p> </td> <td> <p>Water Level [ MSL (base) + Tide (Highs) + Residual] + Univariated Setup</p> </td> </tr> </tbody> </table> <div> </div> <div>The database has 3 representative extreme values for each type of frequency of event occurrence (High, Medium, Low).</div> <p>Each coastal point has the data using 3 slopes: 0.02, 0.03, 0.04. The points have a 0.025º (~2.5 km) distance between each other and 20 m depth.</p> <p><strong>Data location</strong>: The points with the data are located along the Italian coast of Regions: Veneto, Emilia-Romagna and Marche. Using the reference system WGS 84 / UTM zone 32N (EPSG:32632).</p> <p><strong>Fundings:</strong> The creation of this dataset was supported by the Autorità di Bacino Distrettuale del Fiume Po in the framework of the project “Approfondimento tecnico-scientifico sui quadri conoscitivi in ambito costiero”, coordinator Prof. P. Ciavola, University of Ferrara.</p> <p><strong>Disclaimer:</strong> Regardless of whether the data is quality-controlled or not, the authors do not accept any responsibility for the correctness and/or appropriate interpretation of the data. The correct and appropriate interpretation of the data must follow scientific rules and is always the exclusive responsibility of the users.</p>
Fig. 23 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 23 - Conchiglie di Fissuria sossoi n. sp., olotipo (A) e paratipi (B-C). A-B) sorgente sulla riva destra del Torrente Stura, sulla sterrata per Casa Brusona (Masone, Alessandria), M. Bodon leg. 15/01/1995 (coll. MZUF GC/45293, GC/45294); C) permeazioni sul greto del T. Vezzulla, in riva sinistra, 500 m a monte della confluenza con il Torrente Stura (Masone, Alesssandria), M. Bodon leg. 01/05/1994 (coll. MZUF GC/45295). / Shells of Fissuria sossoi n. sp., holotype (A) and paratypes (B-C). A-B) spring on the right bank of the Stura stream, on the track to Casa Brusona (Masone, Alessandria), M. Bodon leg. 15/01/1995 (MZUF GC/45293, GC/45294); C) small springs on the riverbed of the Vezzulla stream, on the left bank, 500 m upstream the confluence of the Stura stream (Masone, Alesssandria), M. Bodon leg. 01/05/1994 (MZUF GC/45295).
Fig. 20 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 20 - Conchiglie di Fissuria varicosa n. sp., olotipo (A) e paratipi (B-L). A) risorgive nell'alveo del Torrente Borbera, 1 km ca. a monte di Vignole Borbera, al centro dell'alveo e in riva sinistra (Vignole Borbera, Alessandria), M. Bodon leg. 09/06/1991 (coll. MZUF GC/46036). B, G) risorgive nell'alveo del Torrente Borbera, in riva sinistra, 300 m ca. a monte della briglia a valle di Variano Inferiore (Vignole Borbera, Alessandria), M. Bodon leg. 20/02/1994 (coll. MZUF GC/46032); C) risorgive nell'alveo del Torrente Borbera, in riva destra, 300 m ca. a monte della briglia a valle di Variano Inferiore (Borghetto di Borbera, Alessandria), M. Bodon leg. 23/01/1994 (coll. MZUF GC/46034); D) risorgiva nell'alveo del Torrente Arda, in riva destra, in loc. La Colombara (Lugagnano Val d'Arda, Piacenza), M. Bodon, E. Bodon & S. Cianfanelli leg. 11/05/2014 (coll. MZUF GC/46037); E-F) risorgive nell'alveo del Torrente Borbera, in riva destra, 100 m a monte della briglia a valle di Variano Inferiore (Borghetto di Borbera, Alessandria), M. Bodon leg. 23/01/1994 (coll. MZUF GC/46031); H) risorgiva nell'alveo del Torrente Arda, in riva destra, 200 m a valle della loc. La Colombara (Lugagnano Val d'Arda, Piacenza), M. Bodon, E. Bodon & S. Cianfanelli leg. 11/05/2014 (coll. MZUF GC/46038); I) risorgiva nell'alveo del Torrente Borbera, in riva destra, al ponte di Variano (Borghetto di Borbera, Alessandria), M. Bodon leg. 22/08/1992 (coll. MZUF GC/45033); J-L) sorgente nella piana presso l'alveo del Torrente Spinti, in riva sinistra, di fronte a Costa Castagnighe (Grondona, Alessandria), M. Bodon leg. 20/07/1997 (coll. MZUF GC/46030). / Shells of Fissuria varicosa n. sp., holotype (A) and paratypes (B-L). A) alluvial springs in the riverbed of the Borbera stream, about 1 km upstream of Vignole Borbera, on the centre of the riverbed and on left bank (Vignole Borbera, Alessandria), M. Bodon leg. 09/06/1991 (MZUF GC/46036). B, G) alluvial springs in the riverbed of the Borbera stream, on left bank, about 300 m upstream of the dike downstream of Variano Inferiore (Vignole Borbera, Alessandria), M. Bodon leg. 20/02/1994 (MZUF GC/46032); C) alluvial springs in the riverbed of the Borbera stream, on right bank, about 300 m upstream of the dike, downstream of Variano Inferiore (Borghetto di Borbera, Alessandria), M. Bodon leg. 23/01/1994 (MZUF GC/46034); D) alluvial spring in the riverbed of the Arda stream, on right bank, in locality La Colombara (Lugagnano Val d'Arda, Piacenza), M. Bodon, E. Bodon & S. Cianfanelli leg. 11/05/2014 (MZUF GC/46037); E-F) alluvial springs in the riverbed of the Borbera stream, on the right bank, 100 m upstream the dike downstream of Variano Inferiore (Borghetto di Borbera, Alessandria), M. Bodon leg. 23/01/1994 (MZUF GC/46031); H) alluvial spring in the riverbed of the Arda stream, on right bank, 200 m down-nstream the locality La Colombara (Lugagnano Val d'Arda, Piacenza), M. Bodon, E. Bodon & S. Cianfanelli leg. 11/05/2014 (MZUF GC/46038); I) alluvial spring in the riverbed of the Borbera stream, on the right bank, at the bridge of Variano (Borghetto di Borbera, Alessandria), M. Bodon leg. 22/08/1992 (MZUF GC/45033); J-L) spring in the plain near the riverbed of the Spinti stream, on left bank, in front of Costa Castagnighe (Grondona, Alessandria), M. Bodon leg. 20/07/1997 (MZUF GC/46030).
Fig. 28 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 28 - Frequenza degli Idrobiidi campionati nelle posature dei bacini campionati (A), espressi come numero medio di conchiglie - 1 kg di detrito, e frequenza delle conchiglie (B) o degli esemplari viventi (C) nelle risorgive dei rispettivi bacini, espressi come percentuale di presenza di ciascuna specie sul totale dei campionamenti effettuati. / Frequency of the Hydrobiids collected in the alluvial debris of the examined basins (A), valued as mean number of shells - 1 kg of debris, and frequency of the shells (B) or living specimens (C) in the alluvial springs of the respective basins, expressed as percentage presence of each species on all samples.
Fig. 17 - Opercolo e caratteri anatomici Fissuria globosa n in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 17 - Opercolo e caratteri anatomici Fissuria globosa n. sp. A-B) stomaco, intestino, apparato genitale (pene escluso) e organi palleali di due maschi; C) stomaco, intestino e organi palleali di un altro maschio; D) opercolo visto dal lato esterno (a sinistra) e di profilo (a destra). Esemplari raccolti nella risorgente del Rio d'Assereto, Pratogrande, 500 m ca. a monte della confluenza nel Torrente Scrivia (Montoggio, Genova), M. Bodon leg. 04/08/1996 (coll. MZUF GC/47090) (A); risorgive nell'alveo del Torrente Tidone, in riva destra, 50-100 m a valle del ponte della strada per Ronchi (Nibbiano, Piacenza), M. Bodon & E. Bodon leg. 28/05/2011 (coll. MZUF GC/47088) (B); galleria filtrante di Pozzo Leone (Busalla, Genova), M. Bodon & S. Gaiter leg. 29/01/1983 (coll. MZUF GC/41622) (C); risorgive nell'alveo del Torrente Borbera, in sponda destra, 800 m a monte di Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (coll. MZUF GC/47092) (D). / Operculum and anatomical details of Fissuria globosa n. sp. A-B) stomach, intestine, reproductive apparatus (penis excluded) and pallial organs of two males; C) stomach, intestine and pallial organs of another male; D) outer side (left) and profile (right) of operculum. Specimens collected in the water resurgence of the Assereto brook, Pratogrande, about 500 m upstream the confluence in the Scrivia stream (Montoggio, Genova), M. Bodon leg. 04/08/1996 (MZUF GC/47090) (A); alluvial springs in the riverbed of the Tidone stream, on right bank, 50-100 m downstream of the bridge of the road to Ronchi (Nibbiano, Piacenza), M. Bodon & E. Bodon leg. 28/05/2011 (MZUF GC/47088) (B); filter tunnel of Leone well (Busalla, Genova), M. Bodon & S. Gaiter leg. 29/01/1983 (MZUF GC/41622) (C); alluvial springs in the riverbed of the Borbera stream, on the right bank, 800 m upstream of Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (MZUF GC/47092) (D).
Fig. 15 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 15 - Protoconca (A, C, E) e teleoconca, sul terzo giro (B, D, F) di Fissuria globosa n. sp. (A, B), di Fissuria varicosa n. sp. (C-D) e di Fissuria sossoi n. sp (E-F). A-B) galleria filtrante di Pozzo Leone (Busalla, Genova), M. Bodon & S. Gaiter leg. 28/08/1982 (coll. MZUF GC/44544, supporto SEM MZ/252_3). C-D) risorgive nell'alveo del Torrente Borbera, in sponda destra, 800 m a monte di Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (coll. MZUF GC/44541, supporto SEM MZ/252_6). E-F) Torrente Vezzulla alla confluenza del Torrente Stura (Masone, GE). M. Bodon leg. 11/09/1993 (coll. MZUF GC/45292, supporto SEM MZ/252_8). / Protoconch (A, C, E) and teleoconch, on the third whorl (B, D, F) of Fissuria globosa n. sp. (A, B), Fissuria varicosa n. sp. (C-D) and Fissuria sossoi n. sp (E-F). A-B) filter tunnel of the Leone well (Busalla, Genova), M. Bodon & S. Gaiter leg. 28/08/1982 (MZUF GC/44544, SEM stub MZ/252_3). C-D) allu-alluvial springs in the riverbed of the Borbera stream, on the right bank, 800 m upstream of Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (MZUF GC/44541, SEM stub MZ/252_6). E-F) the Vez-Vezzulla stream at the confluence with the Stura stream (Masone, GE). M. Bodon leg. 11/09/1993 (MZUF GC/45292, SEM stub MZ/252_8).
Fig. 13 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 13 - Esempi di specie simpatriche e di altre specie raccolte nei bacini in esame. Conchiglie di Alzoniella isoensis n. sp. (A, C) e di Alzoniella ligustica (Giusti & Bodon, 1981) (B, D) delle sorgenti sul muro sotto la strada sulla riva destra del T. Secca, a valle della briglia sotto la confluenza del Rio Cassine con il Rio Valleregia, n° 230 in Appendice (A, B) e delle sorgenti sulla riva sinistra del Rio Ciae, poco a monte del secondo affluente di sinistra a monte di C. Carre, n° 238 in Appendice (C, D), nel bacino del T. Polcevera. Alzoniella finalina Giusti & Bodon, 1984 (E) e Fissuria sossoi n. sp. (F) delle sorgenti sulla riva destra del T. Stura, sulla sterrata per C. Brusona, n° 150 in Appendice, nel bacino del Torrente Stura di Ovada. Fissuria cf. sossoi n. sp. (G) della sorgente sulla riva destra del T. Visone, 250 m a monte di C. Musotto, alla stretta, nell'alveo (Grognardo, AL), 220 m s.l.m., MQ6041, nel sottobacino del Torrente Visone. Alzoniella sp. (H) con conchiglia a spira breve, dall'aspetto quasi valvatiforme, della sorgente Coppi, 400 m a sud di C. Albergo del Piano, sotto la strada (Ovada, AL), 220 m s.l.m., MQ7339, nel bacino del Torrente Stura di Ovada. Pezzolia sp. 3 (I) e Islamia piristoma Bodon & Cianfanelli, 2012, (J) della fonte a Pallavicino, lungo la strada, 100 m a sud della chiesa (Cantalupo Ligure, AL), 715 m s.l.m., NQ0753, nel sottobacino del T. Borbera. Altre specie inedite citate per i bacini piemontesi ed emiliani: Alzoniella sp. 3 (K) della sorgente sulla riva destra di un ruscello sulla mulattiera presso Case Insoldini (Pallare, SV), 440 m s.l.m., MQ4009, nel bacino del F. Bormida di Spigno e Alzoniella sp. 4 (L) della sorgente Gaminoi, poco sopra la strada tra Mulino Egola e Pellegrino Parmense (S. Pellegrino Parmense, PR), 395 m s.l.m., NQ7154, nel bacino del F. Taro, sottobacino T. Stirone. Materiale in collezione MZUF, GC/62244 (A), GC/64422 (B), GC/59194 (C), GC/64424 (D), GC/64425 (E), GC/45293 (F), GC/64426 (G), GC/64427 (I), GC/64428 (J), GC/64429 (K), GC/21286 (L). / Examples of sympatric species and other species collected in the investigated basins. Shells of Alzoniella isoensis n. sp. (A, C) and Alzoniella ligustica (Giusti & Bodon, 1981) (B, D) from the springs on the wall below the road on the right bank of the Secca stream, downstream the dike, downstream the confluence of the Rio Cassine with the Rio Valleregia, n° 230 in Appendix (A, B) and from the springs on the left bank of the Rio Ciae, a little upstream of the second left tributary upstream C. Carre, n° 238 in Appendix (C, D), in the basin of Polcevera stream. Alzoniella finalina Giusti & Bodon, 1984 (E) and Fissuria sossoi n. sp. (F) from the springs on the right bank of the Stura stream, on the track to Casa Brusona, n° 150 in Appendix, in the basin of the Stura di Ovada stream. Fissuria cf. sossoi n. sp. (G) from the spring on the right bank of the Visone stream, 250 m upstream C. Musotto, in the riverbed at the narrow sides (Grognardo, AL), 220 m a.s.l., MQ6041, in the sub-basin of the Visone stream. Alzoniella sp. (H) with short spire, almost valvatiform in appearance, from the Coppi spring, 400 m south of C. Albergo del Piano, below the road (Ovada, AL), 220 m a.s.l., MQ7339, in the basin of the Stura di Ovada stream. Pezzolia sp. 3 (I) and Islamia piristoma Bodon & Cianfanelli, 2012, (J) from the fountain at Pallavicino, along the road, 100 m south of the church (Cantalupo Ligure, AL), 715 m a.s.l., NQ0753, in the sub-basin of the Borbera stream. Other undescribed species from Piedmont and Emilia basins: Alzoniella sp. 3 (K) from the spring on the right bank of a brook on the track near Case Insoldini (Pallare, SV), 440 m a.s.l., MQ4009, in the basin of the Bormida di Spigno river and Alzoniella sp. 4 (L) from the Gaminoi spring, a little upper the road between Mulino Egola and Pellegrino Parmense (S. Pellegrino Parmense, PR), 395 m a.s.l., NQ7154, in the basin of the Taro river, sub-basin of the Stirone stream. Specimens in MZUF collection, GC/62244 (A), GC/64422 (B), GC/59194 (C), GC/64424 (D), GC/64425 (E), GC/45293 (F), GC/64426 (G), GC/64427 (I), GC/64428 (J), GC/64429 (K), GC/21286 (L).
Fig. 10 - Opercolo e in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 10 - Opercolo e caratteri anatomici di Alzoniella isoensis n. sp. A) corpo di un maschio estratto dalla conchiglia e con la cavità palleale aperta; B) corpo di una femmina estratta dalla conchiglia e con la cavità palleale aperta; C) opercolo visto dal lato esterno (a sinistra), di profilo (al centro) e dal lato interno (a destra); D) stomaco, intestino, apparato genitale (pene escluso) e organi palleali di un maschio; E) intestino e organi palleali di un altro maschio; F) ovario presso l'apice del sacco viscerale di una femmina; G) pene di un maschio, in visione dorsale; H) pene di un altro maschio, in visione dorsale (a destra) e ventrale (a sinistra); I) ovidotto renale e palleale e organi palleali di una femmina, sotto raffigurata con il loop disteso; J) ovidotto renale e palleale di un'altra femmina, sotto raffigurata con il loop disteso; K) pene di un altro maschio, in visione dorsale (a sinistra) e ventrale (a destra); L-M) peni di altri due maschi, in visione dorsale. Esemplari raccolti nella galleria filtrante nel subalveo del Torrente Scrivia a Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015 (coll. MZUF GC/49421) (A-D, F, I, K), nella sorgente I Buxi, Isoverde (Campomorone, Genova), M. Bodon leg. 01/02/1981 (coll. MZUF GC/18374) (E, G-H, J), e nella sorgente sulla riva sinistra del Rio Ciae, Carrè (Serra Riccò, Genova), M. Bodon leg. 13/03/1994 (coll. MZUF GC/49421) (L-M). / Operculum and anatomical details of Alzoniella isoensis n. sp. A) body of a male with pallial cavity open; B) body of a female with pallial cavity open; C) outer side (left), profile (centre) and inner side (right) of operculum; D) stomach, intestine, reproductive apparatus (penis excluded) and pallial organs of a male; E) intestine and pallial organs of another male; F) ovary near the apex of visceral sac of a female; G) penis of a male, from dorsal side; H) penis of another male, from dorsal (left) and ventral (right) side; I) renal and pallial oviduct and pallial organs of a female, with the loop in natural position (upper) and the loop extended (lower); J) renal and pallial oviduct of another female, with the loop in natural position (upper) and the loop extended (lower); K) penis of another male, from dorsal (left) and ventral (right) side; L-M) penis of other two males, from dorsal side. Specimens collected in the filter tunnel in the riverbed of Scrivia stream at Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015 (MZUF GC/49421) (A-D, F, I, K), in the spring I Buxi, Isoverde (Campomorone, Genova), M. Bodon leg. 01/02/1981 (MZUF GC/18374) (E, G-H, J), and in the spring on the left bank of the Rio Ciae, Carrè (Serra Riccò, Genova), M. Bodon leg. 13/03/1994 (MZUF GC/49421) (L-M).
Fig. 9 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 9 - Esemplari viventi di Alzoniella isoensis n. sp. (A, C, E) e di Fissuria globosa n. sp. (B, D, F), provenienti dalla galleria filtrante nel subalveo del Torrente Scrivia a Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015. / Living specimens of Alzoniella isoensis n. sp. (A, C, E) and Fissuria globosa n. sp. (B, D, F), from the filter tunnel in the riverbed of the Scrivia stream at Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015.
Fig. 8 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 8 - Conchiglie di Alzoniella isoensis n. sp., olotipo (A) e paratipi (B-P). A-G) sorgente I Buxi, sulla riva destra del Rio d'Iso (Campomorone, Genova), M. Bodon leg. 08/11/1998 (coll. MZUF GC/59133, GC/59134); H) galleria filtrante di Pozzo Leone, dal subalveo del Torrente Scrivia a Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 29/01/1983 (coll. MZUF GC/45020); I) Torrente Scrivia sotto la briglia a valle del ponte Vittorio Veneto, presso Casella (Casella, Genova), M. Bodon leg. 27/05/1992 (coll. MZUF GC/45019); J) sorgente Cà Nei N° 3, loc. Luama, Fumeri (Mignanego, Genova), S. Gaiter leg. 18/08/1997(coll. MZUF GC/59135); K-L) galleria filtrante nel subalveo del Torrente Scrivia a Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015 (coll. MZUF GC/59130); M-O) sorgenti sulla riva sinistra del Rio Ciae, poco a monte del secondo affluente di sinistra a monte di C. Carre (Serra Riccò, Genova), M. Bodon leg. 13/03/1994 (coll. MZUF GC/59194); P-R) sorgente a Larvego, presso il rio, nel ramo SW, in riva sinistra (Campomorone, Genova), M. Bodon leg. 18/01/1981 (coll. MZUF GC/59132). / Shells of Alzoniella isoensis n. sp., holotype (A) and paratypes (B-P). A-G) spring I Buxi, on the right bank of Rio d'Iso (Campomorone, Genova), M. Bodon leg. 08/11/1998 (MZUF GC/59133, GC/59134); H) filter tunnel of the Leone well, in the riverbed of Scrivia stream at Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 29/01/1983 (MZUF GC/45020); I) the Scrivia stream under the dike, downstream of the bridge Vittorio Veneto, near Casella (Casella, Genova), M. Bodon leg. 27/05/1992 (MZUF GC/45019); J) spring Cà Nei N° 3, locality Luama, Fumeri (Mignanego, Genova), S. Gaiter leg. 18/08/1997(MZUF GC/59135); K-L) filter tunnel in the riverbed of Scrivia stream at Busalla (Busalla, Genova), M. Bodon & S. Gaiter leg. 22/07/2015 (MZUF GC/59130); M-O) springs on the left bank of the Rio Ciae, a little upstream of the second left tributary upstream C. Carre (Serra Riccò, Genova), M. Bodon leg. 13/03/1994 (MZUF GC/59194); P-R) spring at Larvego, near the Rio, on the SW branch, on the left bank (Campomorone, Genova), M. Bodon leg. 18/01/1981 (MZUF GC/59132).
Fig. 7 in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 7 - Reticolo idrografico del sottobacino del Torrente Scrivia, con i principali affluenti, i tratti soggetti a secca durante il periodo estivo, i tratti a canali intrecciati e i tratti con ampio greto alluvionale. Sono inoltre indicati i comuni e i confini di provincia, e, per l'area montuosa, le principali formazioni litologiche. Per ciascun tratto del reticolo, sotto al nome del corso d'acqua, è riportata la presenza delle nuove specie freatobie. / Hydrographic network of the sub-basin of the Scrivia stream, with the main tributaries, the dry tracts in summer times, the braided tracts and the tracts with large alluvial riverbed. Moreover, the municipalities and the provincial boundaries and, for the mountainous area, the main lithological formations, are showed. For each tract of the hydrographic network, the presence of the phreatic new species is reported under the name of the water course.
Fig. 18 - Caratteri anatomici Fissuria globosa n in Nuovi idrobiidi freatobi e stigobi dell'Appennino Settentrionale in Piemonte, Liguria ed Emilia-Romagna (Gastropoda: Caenogastropoda: Hydrobiidae)
Fig. 18 - Caratteri anatomici Fissuria globosa n. sp. A-C, E) ovidotto renale e palleale e organi palleali di quattro femmine, sotto con il loop disteso. D, F-H) ovidotto renale e palleale di altre quattro femmine, sotto con il loop disteso. Esemplari raccolti nelle risorgive nell'alveo del Torrente Curone, in sponda sinistra, alla base di uno scavo sul greto 150 m a valle del ponte per Musigliano, Ronco (Gremiasco, Alessandria), M. Bodon & E. Bodon leg. 23/09/2007 (coll. MZUF GC/47091) (A); risorgive nell'alveo del Torrente Tidone, in riva destra, 50-100 m a valle del ponte della strada per Ronchi (Nibbiano, Piacenza), M. Bodon & E. Bodon leg. 28/05/2011 (coll. MZUF GC/47088) (B, E); risorgive nell'alveo del Torrente Brevenna a valle della Madonna dell'Acqua (Valbrevenna, Genova), M. Bodon leg. 06/10/1985 (coll. MZUF GC/ 47087) (C); galleria filtrante di Pozzo Leone (Busalla, Genova), M. Bodon & S. Gaiter leg. 17/08/1982 (coll. MZUF GC/47086) (D); risorgive nell'alveo del Torrente Borbera, in sponda destra, 800 m a monte di Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (coll. MZUF GC/ 47092) (F); risorgente del Rio d'Assereto, Pratogrande, 500 m ca. a monte della confluenza nel Torrente Scrivia (Montoggio, Genova), M. Bodon leg. 04/08/1996 (coll. MZUF GC/ 47090) (G, H). / Anatomical details of Fissuria globosa n. sp. A-C, E) renal and pallial oviduct and pallial organs of four females, with the loop in natural position (upper) and the loop extended (lower). D, F-H) renal and pallial oviduct and pallial organs of other four females, with the loop in natural position (upper) and the loop extended (lower). Specimens collected in the alluvial springs in the riverbed of the Curone stream, on left bank, at the base of an excavation in the riverbed 150 m downstream of the bridge to Musigliano, Ronco (Gremiasco, Alessandria), M. Bodon & E. Bodon leg. 23/09/2007 (MZUF GC/47091) (A); alluvial springs in the riverbed of the Tidone stream, on right bank, 50-100 m downstream of the bridge of the road to Ronchi (Nibbiano, Piacenza), M. Bodon & E. Bodon leg. 28/05/2011 (MZUF GC/47088) (B, E); alluvial springs in the riverbed of the Brevenna stream downstream of Madonna dell'Acqua (Valbrevenna, Genova), M. Bodon leg. 06/10/1985 (MZUF GC/ 47087) (C); filter tunnel of the Leone well (Busalla, Genova), M. Bodon & S. Gaiter leg. 17/08/1982 (MZUF GC/47086) (D); alluvial springs in the riverbed of the Borbera stream, on the right bank, 800 m upstream of Vignole Borbera (Stazzano, AL), M. Bodon leg. 17/05/1992 (MZUF GC/ 47092) (F); water resurgence of the Assereto brook, Pratogrande, about 500 m upstream the confluence in the Scrivia stream (Montoggio, Genova), M. Bodon leg. 04/08/1996 (MZUF GC/ 47090) (G, H).
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