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279 results for “Mediterranean region”
Figs 52–56 in The genusBolbelasmus in the western and southern regions of the Mediterranean Basin (Coleoptera: Geotrupidae: Bolboceratinae)
Figs 52–56. Lectoptype and labels of Bolbelasmus vaulogeri (Abeille de Perrin, 1898), male, deposited in MNHN. 52 – habitus in dorsal aspect, 53 – same but frontal aspect, 54 – same but lateral aspect, 55 – labels of lectotype, 56 – labels of paralectotype No1.
Figs 45–51 in The genusBolbelasmus in the western and southern regions of the Mediterranean Basin (Coleoptera: Geotrupidae: Bolboceratinae)
Figs 45–51. Types and labels of Bolbelasmus bocchus (Erichson, 1841), deposited in MNHB. 45 – male habitus in dorsal aspect (lectotype); 46 – male habitus in frontal aspect (lectotype); 47 – male habitus in lateral aspect (lectotype); 48 – female habitus in dorsal aspect (paralectotype); 49 – labels of lectotypes; 50 – labels of paralectotype No. 1; 51 – labels of paralectotype No. 2.
Figs 33–44 in The genusBolbelasmus in the western and southern regions of the Mediterranean Basin (Coleoptera: Geotrupidae: Bolboceratinae)
Figs 33–44. Head in dorsal aspect, 33–38 – ♂♂; 39–44 – ♀♀. 33 – Bolbelasmus bocchus (Erichson, 1841) (Morocco: Azrou, Foret de Cedres, NMPC); 34 – B. brancoi Hillert & Král sp. nov. (holotype); 35 – B. gallicus (Mulsant, 1842) (France: Bouches-du-Rhône, Barbentane, DJCP); 36 – B. howdeni Hillert & Král sp. nov. (holotype); 37 – B. nikolajevi Hillert, Arnone, Král & Massa sp. nov. (holotype); 38 – B. vaulogeri (Abeille de Perrin, 1898) (Tunisia: Cap Bon peninsula, 6 km W of El Hawariah, DKCP); 39 – B. bocchus (Morocco: Gaada de Debdou plateau., E of Rchida, DKCP); 40 – B. brancoi (allotype); 41 – B. gallicus (Spain: Andalusia, Aljaraque vill. env., JSCP); 42 – B. howdeni (allotype); 43 – B. nikolajevi (allotype); 44 – B. vaulogeri (Tunisia: Cap Bon peninsula, 6 km W of El Hawariah, DKCP).
Figs 9-21 in New species and additional records of Geostiba from the Eastern Mediterranean region and from Middle Asia (Coleoptera: Staphylinidae: Aleocharinae)
Figs 9-21: Geostiba kirghisica nov.sp. (9) and G. sultanica nov.sp. (10-21): (9, 21) spermatheca; (10) male habitus; (11) male forebody; (12) head in lateral view; (13-14) male tergites VII-VIII in dorsal and in lateral view; (15) male sternite VIII; (16-18) median lobe of aedeagus in lateral and in ventral view; (19) apical lobe of paramere; (20) female sternite VIII. Scale bars: 10: 1.0 mm; 11: 0.5 mm; 12-15, 20: 0.2 mm; 9, 16-19: 0.1 mm; 21: 0.05 mm.
Figs 1-8 in New species and additional records of Geostiba from the Eastern Mediterranean region and from Middle Asia (Coleoptera: Staphylinidae: Aleocharinae)
Figs 1-8: Geostiba kirghisica nov.sp.: (1) forebody (holotype); (2) head in lateral view; (3) posterior portion of male tergite VII; (4) male tergite VIII; (5) female sternite VIII; (6-7) median lobe of aedeagus in lateral and in ventral view; (8) apical lobe of paramere. Scale bars: 1: 0.5 mm; 2-5: 0.2 mm; 6-8: 0.1 mm.
Figs 1-8 in On the genus Sunius Stephens, 1829 of Turkey. V. A new micropterous species from central southern Anatolia, with additional records from the western Mediterranean region (Coleoptera: Staphylinidae: Paederinae)
Figs 1-8. Details of Sunius tauricus sp. n. (1) Habitus. (2) Forebody. (3) Male abdominal sternite VII. (4) Male abdominal sternite VIII. (5-6) Aedeagus, lateral view. (7-8) Aedeagus, ventral view. Scale bars: 0.5 mm (1-2); 0.1 mm (3-8).
Non-susceptible landslide areas in Italy and in the Mediterranean region
<p>We used landslide information for 13 study areas in Italy and morphometric information obtained from the 3-arcseconds shuttle radar topography mission digital elevation model (SRTM DEM) to determine areas where landslide susceptibility is expected to be negligible in Italy and in the landmasses surrounding the Mediterranean Sea. The morphometric information consisted of the local terrain slope which was computed in a square 3 × 3-cell moving window, and in the regional relative relief computed in a circular 15 × 15-cell moving window. We tested three different models to classify the "non-susceptible" landslide areas, including a linear model (LNR), a quantile linear model (QLR), and a quantile, non-linear model (QNL). We tested the performance of the three models using independent landslide information presented by the Italian Landslide Inventory (<em>Inventario Fenomeni Franosi in Italia</em> – IFFI). Best results were obtained using the QNL model. The corresponding zonation of non-susceptible landslide areas was intersected in a geographic information system (GIS) with geographical census data for Italy. The result determined that 57.5% of the population of Italy (in 2001) was located in areas where landslide susceptibility is expected to be negligible. We applied the QNL model to the landmasses surrounding the Mediterranean Sea, and we tested the synoptic non-susceptibility zonation using independent landslide information for three study areas in Spain. Results showed that the QNL model was capable of determining where landslide susceptibility is expected to be negligible in the validation areas in Spain. We expect our results to be applicable in similar study areas, facilitating the identification of non-susceptible landslide areas, at the synoptic scale.</p>
MESMAR v1: A new regional coupled climate model for downscaling, predictability, and data assimilation studies in the Mediterranean region. Article data
<p>Regional coupled and Earth System models are fundamental numerical tools for climate investigations, downscaling of predictions and projections, process-oriented understanding of regional extreme events, and many more applications. Here we introduce a newly developed coupled regional modeling framework for the Mediterranean region, called MESMAR (Mediterranean Earth System model at ISMAR) version 1, which is composed of the WRF atmospheric model, the NEMO oceanic 15 model, and the HD hydrological discharge model, coupled via the OASIS coupler. The model is implemented at moderate resolution (about 1/12° for the ocean and river routing, while twice coarser for the atmosphere) for long-term investigations.</p> <p>The gzipped tarball contains data files contained in the manuscript associated with the MESMARv1 description and submitted to Geoscientific Model Developments:</p> <p>MESMAR v1: A new regional coupled climate model for downscaling, predictability, and data assimilation studies in the Mediterranean region</p> <p>by Andrea Storto, Yassmin Hesham Essa, Vincenzo de Toma, Alessandro Anav, Gianmaria Sannino,<br> Rosalia Santoleri, Chunxue Yang</p>
FIG. 15 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 15. — Scutocyclopora dentata (López de la Cuadra & García-Gómez, 1991) n. comb.: A, one non-ovicellate and three ovicellate zooids; B, two non-ovicellate zooids with high, indented peristome; C, E, ovicellate zooid with nodular frontal shield and endooecium and orifice edged by a vizor on the ovicell and a collar with pseudo-spines; D, non-ovicellate zooid with indented collar, orifice with internal arch ending in step-shaped condyles, and small marginal pores; F, young stage of a colony with ancestrula. Origin of specimens: A, Italy, Campania, Palinuro Cape, Scaletta Cave, 47 m; B, E, France, Port-Cros, Bagaud Cave, 5 m; C, France, Provence, Trémies cave, 6 m; D, F, Italy, Sicily, off Avola, 100 m. Scale bars: A, C, 200 µm; B, D, E, 100 µm; F, 300 µm.
FIG. 13 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 13. — Hemicyclopora sp. 2: A, colony on a fragment of coral skeleton; B, same colony, zooids showing a typical profile with a great distal thickness, a terminal orifice, a vertical distal wall, and a terminal, highly recumbent ovicell; C, frontal view of non-ovicellate and ovicellate zooids. Origin: Asturias, Thalassa X301; MNHN-IB-2017-1559. Scale bars: A, 1 mm; B, C, 400 µm.
FIG. 10 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 10. — Distal part of ovicellate and non-ovicellate zooids, and ancestrulae, all at the same scale: A-C, Hemicyclopora neatonensis n. sp.; D-F, H. hexaspinae n. sp.; G- I, Escharella similis Ramalho, Rodríguez-Aporta & Gofas, 2022. Drawings from SEM pictures and examination under stereomicroscope. Origin: A-C, Sicily; D-F, Provence; G-I, Alboran Sea. Scale bar: 200 µm.
FIG. 12. — Hemicyclopora hexaspinae n in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 12. — Hemicyclopora hexaspinae n. sp.: A, ancestrula, note the large size of the cryptocyst; B, ancestrula and daughter zooids; C, autozooid with a tubule budded from a distolateral pore-chamber; D, ancestrula with three successive daughter zooids, the third one with a basal tubular part budded by the ancestrula; E, same ancestrula and zooids, sketch from stereomicroscopic examination: darkening by Mn-Fe oxides increasing from the youngest zooid to the ancestrula attesting to the very slow growth in confined dark caves. Origin: A, C-E, Provence, 3PP Cave; B, Ustica Island, Apollo Bank. Scale bars: A, 50 µm; B, 300 µm; C-E, 100 µm.
FIG. 9 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 9. — "Hemicyclopora" pytheasi n. sp.: A, colony with many ovicells and its ancestrula; another ancestrula with a single daughter zooid, both marked (a); B, ovicellate zooids with converging oral spines; C, ovicellate and non-ovicellate zooids, with a small zooid regenerated inside a broken cystid; D, distal part of two ovicellate zooids and an interzooidal porous kenozooid; E, juvenile colony with ancestrula; F, distal part of a non-ovicellate zooid, orifice with typically convex proximal edge; G, inner side of an orifice showing the lyrula-like suboral umbo and three basal pores of spines (partly visible on the right side). Origin: Atlantic, Armorican margin; Biaçores Stn 259; A, B, paratype PMC-B33.5.52021; C, D, F, G, paratype MNHN-IB-2017-775; E, paratype MNHN-IB-2017-777. Scale bars: A, 1 mm; B, C, E, 200 µm; D, 100 µm; F, G, 50 µm.
FIG. 6. — Hemicyclopora celtica n in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 6. — Hemicyclopora celtica n. sp.: A, colony with clustered ovicells; B, small portion of a colony, note the occurrence of six, seven or eight spines in nonovicellate zooids, and 6 spines in ovicellate zooids; C, non-ovicellate and ovicellate zooids, all with six spines, ovicells associated with a distal autozooid; D, nonovicellate zooids with small marginal pores, subterminal orifice edged by six spines, prominent condyles and markedly convex proximal edge; E, F, non-ovicellate and ovicellate zooids, note the granular frontal shield with tiny marginal pores, the terminal orifice of the non-ovicellate zooid with eight prominent basal parts of spines, and ovicells with endooecium formed by the distal autozooid; G, H, frontal view of two orifices, with eight spines and a moderately convex proximal edge (G) and six spines and a triangular proximal edge (H); I, inner side of an orifice with smooth surface and basal pores of spines. Origin: Armorican Margin, A, C, D, Thalassa Z398, paratype PMC.B35.2021; B, E-I, Thalassa Z435, paratype MNHN-IB-2017-780. Scale bars: A, 1 mm; B, 400 µm; C, 200 µm; D-F, G-I, 100 µm.
FIG. 5 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 5. — Hemicyclopora discrepans (Jullien in Jullien & Calvet, 1903): A, colony with ovicellate zooids bearing six, seven, or eight oral spines; B, non-ovicellate zooid with eight spines, primary orifice with internal arch and protruding condyles, and granular frontal shield; C, three ovicellate zooids with six spines and ovicells inserted between the base of distal autozooids; D, zooids with long, curved spines, large porous area lateral to orifice and ovicells attached to distal maternal wall, one under construction; E, orifice with triangular, down-curved condyles, concave proximal edge with a narrow rim of gymnocyst; F, lateral view of the distal part of an ovicellate zooid with eight spines, large marginal pores and the ovicell with the basal kenozooid; G, two zooids, one ovicellate, both with eight spines, frontal shield and endooecium with pointed granules. Origin: A, B, F, G, Alboran Sea, Balgim DW132, 170 m; C, D, E, Atlantic, Gorringe Bank, Seamount 1 DW5, 180 m. Scales bars: A, 400 µm; B, F, 100 µm; C, D, G, 200 µm; E, 50 µm.
FIG. 11. — Hemicyclopora hexaspinae n in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 11. — Hemicyclopora hexaspinae n. sp.: A, ovicellate and non-ovicellate zooids at the edge of a small colony, with frontal shield bulged and granular; B, C, ovicellate zooids: terminal ovicells with six curved spines, attached to maternal distal wall and lying on a small kenozooid responsible for ovicell formation; D, colony edge with six ovicells: two fully grown and four under construction from a basal kenozooid; E, ovicellate zooid with thick bases of spines; F, orifice of non-ovicellate zooid: six basal parts of spines, concave proximal edge and prominent condyles; G, shape of the oral spines in a non-ovicellate zooid:. Origin: A, B, F, G, paratype MNHN-IB-2017-772, Provence, 3PP Cave; C, paratype MNHN-IB-2017-773, Provence, Cape Morgiou Cave; D, paratype PMC.B29.8.11.2020; Ustica Is., Apollo Bank; E, Atlantic, Balgim DR49. Scale bars: A, D, 300 µm; B, E, G, 100 µm; C, 200 µm; F, 50 µm.
FIG. 7 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 7. — Escharella similis Ramalho, Rodríguez-Aporta & Gofas, 2022: A, edge of colony with five ovicellate zooids; B, non-ovicellate zooids with eight oral spines and a triangular proximal umbo; C, orifice of non-ovicellate zooid showing the lyrula-like inner bump and the proximal peristomial umbo in vertical view; D, two zooids, one with a terminal ovicell associated to a tiny basal kenozooid and orifice with a lyrula-like bump; E, distal part of an ovicellate zooid with 8 spines, a triangular peristomial umbo, and the orifice of the ovicell in an upper position; F, orifice of a non-ovicellate zooid with a low inner protuberance and step-shaped condyles. Origin: A, B, C, E, F, Alboran Sea, Balgim DW132; D, Atlantic, Gulf of Cadiz, Balgim DR42. Scale bars: A, 400 µm; B, D, 200 µm; C, E, F, 100 µm.
FIG. 14 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 14. — Oral spines in a non-ovicellate zooid of Hemicyclopora polita (Norman, 1864): A, outside view of four spines with tall bases; B, inside view of the orifice area showing four pores corresponding to the opening of spines into the coelom and the distal part of the umbonuloid frontal shield. Ancestrula and early astogeny in the genera Hemicyclopora and Scutocyclopora n. gen.: C, H. polita, D, S. dentata n. comb, Origin: A-C, NE Atlantic, Armorican Margin, 1050 m, R/V Thalassa Z435; D, Ionian Sea, Sicily, off Avola, 100 m. Scale bars: A, B, 100 µm; C, D, 200 µm.
FIG. 4 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 4. — Hemicyclopora sp. 1: A, lateral view of ovicellate and non-ovicellate zooids with granular frontal shield, marginal pores and basal pore chambers, note the structure of the orifices and the ovicells with vizor, recumbent on a basal kenozooid; B, frontal view of an ovicellate zooid with typical features; C, ancestrula with 12 spines. Origin: Azores; Biaçores Stn 145-146; MNHN-IB-2017-1558. Scale bars: A, B, 200 µm; C, 100 µm.
FIG. 8 in On some "Hemicyclopora" Norman, 1894 and "Escharella" Gray, 1848 species (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region. Re-examination of their generic status and description of new species and a new genus
FIG. 8. — "Escharella" massiliana n. sp.: A, zooids of the colony edge with hummocky frontal shield and three terminal, recumbent ovicells; B, lateral view of an ovicellate zooid, note the small basal kenozooid and the large marginal pores; C, E, F, G, edge of the same colony as A, with different stages in the ovicell construction involving a small basal kenozooid, note the thickness of the proximal edge of the orifice; D, ancestrula and periancestrular zooids. Origin: A, C, E-G, Marseille, Planier canyon, holotype MNHN-IB-2017-774; B, D, Calvi, paratype PMC. B36. 5.5.2021. Scale bars: A, B, C, D, 200 µm; E, F, 50 µm; G, 100 µm.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.