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153 results for “Tuscany”
Dataset and framework for the Open Potential Ecological Network of Tuscany
<p>This repository contains the main output of the related research, specifically: two Open Potential Ecological Networks (OPEN) of Tuscany in the Cytoscape format: "tuscany_potential_directed.cys" and "tuscany_potential_undirected.cys".</p> <p>Please see the "annotations.txt" file to more detailed explanation regarding the content in this repository.</p>
SERENA EJPSoil Soil loss by water erosion of Tuscany (Italy)
<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> <p>One of the objective of SERENA project was to develop methods to calculate and map soil-based ecosystem services and soil threats. The present data was prepared according to the methodology of the SERENA Soil erosion and soil erosion control cookbook. Soil loss was used as an indicator for soil erosion (ST). The map of soil loss by water erosion (soil threat) was based on the RUSLE model. For Italy, the cookbook was applied in the Tuscany region. <br> <br>To create the soil loss map we used:</p> <ul> <li>for R-factor, not freely available database of meteorological parameters spatialized at 250 m (minimum and maximum daily air temperature; cumulate daily precipitation) over Tuscany region (period 1990–2022, Lamma Consortium) and a local linear equation between R and mean annual precipitation (P);</li> <li>for C -factor, Regional Land use map 1:10.000 (2018, freely available at: https://www502.regione.toscana.it/geoscopio/usocoperturasuolo.html) and ESDAC method (https://doi.org/10.1016/j.landusepol.2015.05.021) ; </li> <li>for K-factor, sand, silt, clay, and O.C. (%) maps (built from 4.000 soil profiles, following FAO’s methodology in GSP-GSOC map, Lamma Consortium), and Torri et al. (1997) function;</li> <li>for LS-factor, DEM 10 m of Tuscany, (freely available at https://www502.regione.toscana.it/geoscopio/cartoteca.html99) and Desmet & Govers (1996) SAGA tool (applied at 10 m and upscaled);</li> <li>for P-factor, not freely available database 1:10.00 of terraced areas (Lamma Consortium, 2020) (for terraced areas a multiplication factor of 0.5 was considered, based on expert evaluation)</li> </ul> <p>Maps was delivered in the GeoTIFF format in the resolution of 100m. <br>Delivered data will be validated by stakeholders from Italy (scientist) in October, 2024.</p>
SERENA EJPSoil Soil erosion control in Tuscany (Italy)
<div> <p><span><span>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.</span></span></p> <p><span><span>One of the </span><span>objective</span><span> of SERENA project was to develop methods to calculate and map soil-based ecosystem services and soil threats. The present data was prepared according to the </span><span>methodology</span><span> of the SERENA Soil erosion and soil erosion control cookbook</span><span>. </span><span>Soil loss was used as an indicator for soil erosion (ST). T</span><span>he map of soil mass not eroded was based on the RUSLE model. </span><span>Soil erosion control was calculated as the difference between potential and actual soil erosion (SES, ecosystem service of soil erosion protection, i.e. soil eroded mass </span><span>retained</span><span> by vegetation, Mg/ha/y)</span><span>. For Italy, the cookbook was applied in the Tuscany region. </span></span><span> </span></p> </div> <div> <p><span><span>To create the soil loss map we used:</span></span><span> </span></p> </div> <div> <ul> <li><span><span>for R-factor, not freely available database of meteorological parameters spatialized at 250 m (minimum and maximum daily air temperature; cumulate daily precipitation) over Tuscany region (period 1990–2022, Lamma </span><span>Consortium) and</span><span> a local linear equation between R and mean annual precipitation (P);</span></span> </li> <li><span>for C -factor, Regional Land use map 1:10.000 (2018, freely available at: </span><span>https://www502.regione.toscana.it/geoscopio/usocoperturasuolo.html</span><span>) and ESDAC method (</span><span>https://doi.org/10.1016/j.landusepol.2015.05.021</span><span>) ;</span> <span> </span></li> <li><span>for K-factor, sand, silt, clay, and O.C. (%) maps (built from 4.000 soil profiles, following FAO’s </span><span>methodology</span><span> in GSP-GSOC map, Lamma Consortium), and Torri et al. (1997) function;</span><span> </span></li> <li><span>for LS-factor, DEM 10 m of Tuscany, (freely available at </span><span>https://www502.regione.toscana.it/geoscopio/cartoteca.html99</span><span>) and Desmet & </span><span>Govers</span><span> (1996) SAGA tool (applied at 10 m and upscaled);</span><span> </span></li> <li><span>for P-factor, not freely available database 1:10.00 of terraced areas (Lamma Consortium, 2020) (for terraced areas a multiplication factor </span><span>of 0.5</span><span> was considered, based on expert evaluation)</span><span> </span></li> <li><span>for P-factor, not freely available database 1:10.00 of terraced areas (Lamma Consortium, 2020) (for terraced areas a multiplication factor </span><span>of 0.5</span><span> was considered, based on expert evaluation)</span><span> </span></li> </ul> </div> <div> <p><span><span>Maps was delivered in the </span><span>GeoTIFF</span><span> format in the resolution of 100m. </span></span><span> </span></p> </div> <div> <p><span><span>Delivered data will be </span><span>validated</span><span> by stakeholders from Italy (scientist) in </span><span>October,</span><span> 2024.</span></span><span> </span></p> </div>
Territorial land use data relative to Pesa Basin ( Tuscany) and its recent changes ( 2016- 2007)
<p>Data and elaborations are provided by IBIMET CNR , Accademia Georgofili and <a href="http://www.cbmv.it/">Consorzio di Bonifica 3 Medio Valdarno. </a></p>
Dataset for: "Last century changes in annual precipitation in a Mediterranean area and their spatial variability. Insights from northern Tuscany (Italy)"
<p>The version 1.0 contains the supporting data for the work (still under submission) "Last century changes in annual precipitation in a Mediterranean area and their spatial variability. Insights from northern Tuscany (Italy)".</p> <p>The following files are here available (all file are georeferenced in EPSG: 3003):</p> <p>- AVG_Rainfall_1990-2019.tif -> Raster map of the mean annual precipitation for the northern Tuscany, Italy. It encompasses the portion of the Tuscany region northern of the cities of Livorno - Florence. The interpolation was validated via a leave one out cross-validation procedure.</p> <p>- D3-1_Area2_ApuanAlps.tif -> Raster map of the differences in mean annual precipitation between the two 3-decades periods 1921 to 1950 and 1990 to 2019 for the Apuan Alps mountain ridge (Tuscany, Italy).</p> <p>- D3-2_Area2_ApuanAlps.tif -> Raster map of the differences in mean annual precipitation between the two 3-decades periods 1951 to 1980 and 1990 to 2019 for the Apuan Alps mountain ridge (Tuscany, Italy).</p> <p>- DeltaSHP_Points_AVG_Annual_Rainfall.zip -> Shape file of the raingauges locations with the mean annual precipitation values of the period 1990 to 2019.</p> <p>- RaingaugesSHP_Points_AVG_Annual_Rainfall_1990-2019.zip -> Shape file of the raingauges locations with the following information: differences in the mean annual precipitation values between the two 3-decades periods 1951 to 1980 and 1990 to 2019 (named D3-2); p values of the t-test for significance of the differences between the mean annual precipitation ofthe two 3-decades periods 1951 to 1980 and 1990 to 2019; difference in the mean annual precipitation values between the two 3-decades periods 1921 to 1950 and 1990 to 2019 (named D3-1); p values of the t-test for significance of the differences between the mean annual precipitation ofthe two 3-decades periods 1921 to 1950 and 1990 to 2019.</p>
FIG. 18. — Alloschizidium labronicum n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 18. — Alloschizidium labronicum n. sp., from Maroccone, ♀ paratype: A, adult specimen, lateral view; B, dorsal scale-seta; C, cephalon, frontal view; D, cepha- lon, dorsal view; E, epimeron of pereonite 1, dorsal view; F, telson and uropods, dorsal view; G, antennula; H, antenna. Scale bar: A, 1 mm.
FIG. 16. — Trogleluma pilosa n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 16. — Trogleluma pilosa n. sp., from Poggio Capalbiaccio, ♀ paratype: A, left mandible; B, right mandible; C, maxillula; D, maxilla; E, maxilliped; F, left uropod.
FIG. 15. — Trogleluma pilosa n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 15. — Trogleluma pilosa n. sp., from Poggio Capalbiaccio, ♀ paratype: A, adult specimen, lateral view; B, dorsal scale-seta; C, cephalon, frontal view; D, cephalon, dorsal view; E, epimeron of pereonite 1, dorsal view; F, telson and uropods, dorsal view; G, antennula; H, antenna. Scale bar: A, 1 mm.
FIG. 13. — Parachizidium ferrarai n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 13. — Parachizidium ferrarai n. sp., from Gorgona, ♂ paratype: A, left mandible; B, right mandible; C, maxillula; D, maxilla; E, maxilliped; F, uropod.
FIG. 10. — Typhlarmadillidium occidentale n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 10. — Typhlarmadillidium occidentale n. sp., from Grotta del Cane di Uliveto, Monte Pisano, ♂ paratype: A, left mandible; B, right mandible; C, maxillula; D, maxilla; E, maxilliped; F, right uropod.
FIG. 8. — Moserius talamonensis n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 8. — Moserius talamonensis n. sp., from Grotta Gianninoni, Uccellina, ♂ paratype: A, pereopod 1; B, pereopod 7; C, genital papilla; D, pleopod 1; E, pleopod 2; F, pleopod 3 exopod; G, pleopod 4 exopod; H, pleopod 5 exopod.
FIG. 6. — Moserius gruberae n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 6. — Moserius gruberae n. sp., from Grotta del Cane di Uliveto, Monte Pisano, ♂ paratype: A, pereopod 1; B, pereopod 2; C, genital papilla; D, pleopod 1; E, pleopod 2; F, pleopod 3 exopod; G, pleopod 4 exopod; H, pleopod 5 exopod.
FIG. 21. — A, Leucocyphoniscus pisanus n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 21. — A, Leucocyphoniscus pisanus n. sp., ♀ paratype from Buca delle Fate di Cima Sugheretta, Monte Pisano; B, Moserius gruberae n. sp., ♀ paratype from Grotta del Cane di Uliveto, Monte Pisano; C, Moserius talamonensis n. sp., ♀ paratype from Grotta Gianninoni, Uccellina; D, Typhlarmadillidium occidentale n. sp., ♀ paratype from Grotta del Cane, Monte Pisano; E, Paraschizidium ferrarai n. sp., ♀ paratype, from Gorgona; F, Trogleluma pilosa n. sp., ♀ paratype from Poggio Capalbiaccio; G, Alloschizidium labronicum n. sp., ♀ paratype from Maroccone. Scale bars: A-D, F, G, 1 mm; E, 0.5 mm.
FIG. 3. — Leucocyphoniscus pisanus n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 3. — Leucocyphoniscus pisanus n. sp., from Buca delle Fate di Cima Sugheretta, Monte Pisano, ♂ paratype: A, pereopod 1; B, pereopod 7; C, genital papilla; D, pleopod 1; E, pleopod 2; F, pleopod 3 exopod; G, pleopod 4 exopod; H, pleopod 5 exopod.
FIG. 5. — Moserius gruberae n in New species of subterranean and endogean terrestrial isopods (Crustacea, Oniscidea) from Tuscany (central Italy)
FIG. 5. — Moserius gruberae n. sp., from Grotta del Cane di Uliveto, Monte Pisano, ♂ paratype: A, left mandible; B, right mandible; C, maxillula; D, maxilla; E, maxilliped; F, left uropod.
Maps of topsoil (0-30 cm) properties of Tuscany (Italy)
<p><span>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.</span></p> <p><span>The topsoil (0-30 cm) properties maps are prepared to evaluate soil ecosystem services in SERENA/EJP-Soil and for applying SOC loss Cookbook and SOIL Loss Cookbook. In particular Soil Organic Carbon content map was directly considered as an application of SOC loss Cookbook (DOI: </span><a href="https://doi.org/10.5281/zenodo.13951265"><span>10.5281/zenodo.13951265 </span></a><span>Version 3).</span></p> <p><span>They are based on Tuscany Region soil database available at Geoscopio (https://www502.regione.toscana.it/geoscopio/pedologia.html) and on point soil data not freely available (Lamma Consortium). More information and requests to: </span><a href="mailto:info@lamma.toscana.it"><span>info@lamma.toscana.it</span></a><span>.</span></p> <p><span>In accordance with the methodology reported in the Soil Organic Carbon Mapping Cookbook (Yigini et al., 2018), the following soil properties were mapped for all Tuscany Region:</span></p> <ul> <li><span>soil organic carbon content (dag/kg),</span></li> <li><span>soil organic carbon stock (t/ha),</span></li> <li><span>textural fractions (sand, silt and clay, USDA limits, dag/kg),</span></li> <li>rock fragments (vol/vol),</li> <li>pH in water,</li> <li>bulk density (g/cm3).</li> </ul> <p><span>They were obtained through Digital Soil Mapping (DSM) approach, based on correlations with numerous environmental factors and using Random Forest algorithm.</span></p> <p><span>All the maps have a 100 m spatial resolution.</span></p>
Fig. 2 in Salix ×marchettii (Salicaceae), a new nothospecies from the Apuan Alps (Northern Tuscany, Central Italy)
Fig. 2. – Salix ×marchettii M. Merli & F. Mart. A. Mixed indumentum on young twig: silky and matted hairs. B. Connate filaments.
Dataset of measurements of the soil CO2 flux and soil brightness temperature at Le Biancane (geothermal field of Larderello-Travale, Tuscany, Italy) in the May-June 2021 period.
<p>Dataset of measurements of the soil CO<sub>2</sub> flux and soil brightness temperature at Le Biancane (geothermal field of Larderello-Travale, Tuscany, Italy) in the period May-June 2021. The dataset is structured as follows:</p> <p>Column A is the progressive number of the point (#);</p> <p>Column B is the Longitude of the point, datum WGS 1984;</p> <p>Column C is the Latitude of the point, datum WGS 1984;</p> <p>Column D is the Universal Transverse Mercator (UTM) Longitude coordinate, datum WGS 1984, zone 32N;</p> <p>Column E is the Universal Transverse Mercator (UTM) Latitude coordinate, datum WGS 1984, zone 32N;</p> <p>Column F is the soil brightness temperature, in °C;</p> <p>Column G is the soil CO<sub>2</sub> flux in grams of CO<sub>2</sub> per square meter, per day (g m<sup>-2</sup> day<sup>-1</sup>)</p>
Dataset of structural measurements at Le Biancane (geothermal field of Larderello-Travale, Tuscany, Italy) in the May-June 2021 period.
<p>The dataset contains measurements of fractures and bedding at Le Biancane (geothermal field of Larderello-Travale, Tuscany, Italy) in the period May-June 2021. The term fractures in this dataset indicate a break in a rock where the orthogonal opening is predominant; when clear lateral displacement by shearing is observed, then we adopt the term fault accordingly to the definition by National Research Council (1996). The topological analysis has been conducted using the methods described by Sanderson and Nixon (2015; 2018). This dataset consists of two text files described below.</p> <p><strong>structural-dataset.txt:</strong></p> <p>this file contains the measured fractures and bedding planes, it is structured as follow:</p> <p>Column A is the Longitude of the point, datum WGS 1984;</p> <p>Column B is the Latitude of the point, datum WGS 1984;</p> <p>Column C is the dip direction of the measured structure;</p> <p>Column D is the dip of the measured structure;</p> <p>Column E is the type of the measured structure (fracture, fault, bedding)</p> <p> </p> <p><strong>topological-analysis.txt:</strong></p> <p>this file contains the measurement done for the topological analysis on nine sites at Le Biancane area, it is structured as follow:</p> <p>Column A is the code of the site;</p> <p>Column B is the Longitude of the point, datum WGS 1984;</p> <p>Column C is the Latitude of the point, datum WGS 1984;</p> <p>Column D is the number of nodes I (NI);</p> <p>Column E is the number of nodes Y (NY);</p> <p>Column F is the number of nodes X (NX);</p> <p>Column G is the percent of nodes I (%NI);</p> <p>Column H is the percent of nodes Y (%NY);</p> <p>Column I is the percent of nodes X (%NX);</p> <p>Column J is the probability of connection of nodes I-I (PII’);</p> <p>Column K is the probability of connection of nodes I-C (PIC’);</p> <p>Column L is the probability of connection of nodes C-C (PCC’);</p> <p>Column M is the radius in meter (r) of the circle used for the topological analysis;</p> <p>Column N is the value of the parameter CL;</p> <p>Column O is the value of the parameter CB;</p> <p>Column P is the area (m^2) of the circle;</p> <p>Column Q is the fracture intensity;</p> <p> </p> <p> </p> <p> </p>
Figs. 7–14 in A new species of Heteraphorura Bagnall, 1948 (Collembola, Poduromorpha, Onychiuridae) from Apennine Mountains (Tuscany, Italy).
Figs. 7–14.- Heteraphorura steineri sp. nov. 7.- Chaetotaxy of central part of Abd. sternum IV, male ventral organ, remnant of furca. 8.- Chaetotaxy of central part of Abd. sternum IV, female, remnant of furca. 9.- Dorsal pso on Th. II. 10.- Dorsal pso on Abd. V. 11.- Dorsal pso on Abd. II. 12.- Maxillary palp. 13.- Distal part of leg I. 14.- Distal part of leg III. Scales¡ 0.05 mm.
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