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Fig. 1 in Systematic relationships of the blind phacopine trilobite Trimerocephalus, with a new species from Causses-et-Veyran, Montagne Noire
Fig. 1. Location map of the old quarry of Concours−le−Haut at Causses−et−Veyran, in Montagne Noire, southern of the France.
Fig. 6 in Systematic relationships of the blind phacopine trilobite Trimerocephalus, with a new species from Causses-et-Veyran, Montagne Noire
Fig. 6. Trimerocephalus (Trifoliops) nigritus subgen. et sp. nov. Concours−le−Haut, Causses−et−Veyran, Montagne Noire, Famennian, Upper Devonian. Samples housed in the collection USTL/CC of the Laboratory of Paleontology of Montpellier (France). Photographs of calcareous shells. A. Cephalon, USTL/CC018, in dorsal (A1), frontal (A2), lateral (A3), and ventral (A4) views; × 3. B. Cephalon, USTL/CC019, in dorsal (B1) and lateral (B2) views; × 5. C. Cephalon, USTL/CC020, in dorsal (C1), ventral (C2), and lateral (C3) views; × 5. D. Cephalon, USTL/CC021, in dorsal (D1) and lateral (D2) views; × 10. E. Cephalon, USTL/CC022, in ventral view, × 5. F. Cephalon, USTL/CC023, in ventral view, × 5. G. Pygidium, USTL/CC024, in frontal (G1) and dorsal (G2) views; × 7. H. Pygidium, USTL/CC025, in dorsal (H1) and frontal (H2) views; × 5.
Fig. 1. A. Eodelphis browni Matthew, 1916 in Stagodontid marsupials from the Late Cretaceous of Canada and their systematic and functional implications
Fig. 1. A. Eodelphis browni Matthew, 1916, incomplete left maxilla, TMP 85.53.3, from the Dinosaur Park Formation, Judithian Land Mammal Age (late Campanian), Dinosaur Provincial Park, Alberta, containing P1–2, M1 in occlusal (A1) and labial (A2) views. B. Eodelphis cutleri (Smith Woodward, 1916), incomplete right maxilla, UALVP 7031, from the Dinosaur Park Formation, Judithian Land Mammal Age (late Campanian), mouth of Sand Creek, Dinosaur Provincial Park, Alberta, containing M1 (broken), M2–3 in occlusal view; arrow shows posterior alveolus of P3. C. Didelphodon coyi Fox and Naylor, 1986, incomplete right dentary, TMP 91.161.1, from the Horseshoe Canyon Formation, Edmontonian Land Mammal Age (early Maastrichtian), Paintearth Creek, Alberta, containing i2–3 (broken), c (broken), p1–3, m1–2, m3–4 (broken) in labial (C1), lingual (C2), and lingually oblique (C3) views. A1 and B stereophoto pairs. Scale bar 5 mm.
Fig. 2 in Stagodontid marsupials from the Late Cretaceous of Canada and their systematic and functional implications
Fig. 2. Didelphodon coyi Fox and Naylor, 1986 from the Horseshoe Canyon Formation, Edmontonian Land Mammal Age (early Maastrichtian). A. TMP 91.161.1, Paintearth Creek, Alberta, incomplete right dentary, containing 12−3 (broken), c (broken), p1–3, m1–2, m3–4 (broken) in occlusal (A1) and anterior (A2) views. B. TMP 90.12.29, Michichi Creek (type locality), Alberta, incomplete left dentary, containing p3 (broken) in occlusal (B1) and labial (B2) views. A1 and B1 stereophoto pairs. Scale bars 5 mm.
Fig. 2 in A new brittle star from the early Carboniferous of Poland and its implications on Paleozoic modern-type ophiuroid systematics
Fig. 2. Ophiurin brittle star Aganaster jagiellonicus sp. nov. from the upper Tournaisian to lower Visean (lower Carboniferous) Mazurowe Doły Formation, Rudawa Group of Czatkowice quarry, Dębnik Massif, southern Poland; MZUJ T/0282, holotype. A. General view of the specimen, exposing the ventral side (also illustrated by O'Hara et al. 2014). B. Oral skeleton. C. Detail of the oral skeleton; photograph (C1), interpretative drawing (C2). D. Detail of basal arm segments; photograph (D1), interpretative drawing (D2).
Fig. 1 in A new brittle star from the early Carboniferous of Poland and its implications on Paleozoic modern-type ophiuroid systematics
Fig. 1. Geographical position of the investigated specimen (map after Salata 2013, with modifications).
Fig. 3 in A new brittle star from the early Carboniferous of Poland and its implications on Paleozoic modern-type ophiuroid systematics
Fig. 3. Ophiurin brittle star Aganaster jagiellonicus sp. nov. from the upper Tournaisian to lower Visean (lower Carboniferous) Mazurowe Doły Formation, Rudawa Group of Czatkowice quarry, Dębnik Massif, southern Poland; MZUJ T/0282, holotype. Detail of ventral side (A); median arm segments, showing the transition from between-plate tentacle pores to within-plate tentacle pores (B); median arm segments in ventro-lateral view (C); proximal arm segments in dorso-lateral view (D).
Fig. 1. A in Crustacean microcoprolites from the Upper Jurassic- Lower Cretaceous of the Neuquén Basin, Argentina: Systematics and biostratigraphic implications
Fig. 1. A. Location map of the Neuquén Basin with study localities and a stratigraphic chart of the Mendoza Group. 1, Tres Esquinas; 2, Loncoche creek; 3–4, Bardas Blancas; 5, Rahue creek; 6, Yeso creek; 7, Cara Cura range. B. Microcoprolites distribution in the Vaca Muerta Formation. Ammonite Zonation according to Aguirre−Urreta et al. (2008) and Riccardi (2008).
Fig. 8 in New Lower Kimmeridgian ataxioceratin ammonite from the eastern Iberian Chain, Spain: Systematic, biogeographic, and biostratigraphic relevance
Fig. 8. Ataxioceratin ammonite Geyericeras aragoniense sp. nov. [M] from the Lower Kimmeridgian Ataxioceras lothari Biozone, A. lothari Subzone, G. aragoniense biohorizon in the eastern Iberian Chain. Paratype UGR MPR.36.20; Guadalope River section at the Villarluengo area, in right (A) and left (B) side views. Arrows indicate the beginning of the body chamber. Scale for shell size reference.
Fig. 7 in New Lower Kimmeridgian ataxioceratin ammonite from the eastern Iberian Chain, Spain: Systematic, biogeographic, and biostratigraphic relevance
Fig. 7. Ataxioceratin ammonite Geyericeras aragoniense sp. nov. [m] from the Lower Kimmeridgian Ataxioceras lothari Biozone, A. lothari Subzone, G. aragoniense biohorizon in the eastern Iberian Chain, Spain. A. Holotype UGR MLG.23.20; Reservoir of Calanda section in the Calanda area, in left (A1) and right (A2) side views. B. Paratype UGR MPC.29.8; Morrón section at the Calanda area, in right side view. C. Paratype UGR MPC.28.15; Morrón section at the Calanda area, in left side view. D. Paratype UGR MPC.28.73; Morrón section at the Calanda area, in right side view. Arrows indicate the beginning of the body chamber. Scale for shell size reference.
Fig. 1 in New Lower Kimmeridgian ataxioceratin ammonite from the eastern Iberian Chain, Spain: Systematic, biogeographic, and biostratigraphic relevance
Fig. 1. Location (C), palaeogeography (B), and studied sections (A) with indication of Geyericeras records together with others ataxioceratins relevant for biostratigraphic correlation. Sections labeling as follows: Villarluengo [MPR], Berge−Molinos [MBV, MVP], Alcorisa−Gallipuén [MTG], and Calanda [MLG, MPC] areas. FAD and LAD for First and Last Appearance Data, respectively.
Fig. 2 in Crustacean microcoprolites from the Upper Jurassic- Lower Cretaceous of the Neuquén Basin, Argentina: Systematics and biostratigraphic implications
Fig. 2. Transversal section of crustacean microcoprolites from the Vaca Muerta Formation. A. Palaxius azulensis Kietzmann isp. nov. (CPBA−N° 20675, early Valanginian, Rahue creek). B. Palaxius caracuraensis Kietzmann isp. nov. (CPBA−N° 20689, late Tithonian, Cara Cura range). C. Helicerina? isp. A aff. Helicerina siciliana Senowbari−Daryan, Schäfer, and Catalano, 1979 (CPBA−N° 20675, early Valanginian, Rahue creek). D. Helicerina isp. B (CPBA−N° 20675, early Valanginian, Rahue creek).
Fig. 3 in Crustacean microcoprolites from the Upper Jurassic- Lower Cretaceous of the Neuquén Basin, Argentina: Systematics and biostratigraphic implications
Fig. 3. Schematic diagrams of the different ichnospecies of Palaxius and Helicerina mentioned in this work (Modified from Blau and Grün (2000), not to scale). A. Palaxius ichnospecies with 4 canals: Palaxius caucaensis (A1), P. kumaensis (A2), P. salataensis (A3), P. tetraochetarius (A4), P. osaensis (A5), and P. azulensis Kietzmann isp. nov (A6). B. Palaxius ichnospecies with 10 canals: Palaxius colombiensis (B1), P. decaochetarius (B2), P. habanensis (B3), P. decemlunulatus (B4), P. decemporatus (B5), and P. caracuraensis Kietzmann isp. nov. (B6). C. Helicerina ichnospecies with simple canals: Helicerina siciliana (C1), H. alata (C2), H. spinosa (C3), H. keuperiana (C4), and Helicerina isp. A aff. H. siciliana (C5). D. Helicerina isp. with multiple canals: Helicerina ruttei (D1), H. kainachensis (D2), H. kalakyra (D3), and Helicerina isp. B (D4).
Fig. 3 in Molecular phylogenetics and systematics of two enteric helminth parasites (Baylisascaris laevis and Diandrya vancouverensis) in the Vancouver Island marmot (Marmota vancouverensis)
Fig. 3. Bayesian consensus phylogram based on Baylisascaris and outgroup alignments of concatenated nuclear sequences (28S, ITS, and ard1) from GenBank and this study (B. laevis). Branch labels represent Bayesian posterior probabilities. Branch lengths are scaled to expected number of substitutions per site. Abbreviations refer to sampling sites (AK = Alaska, ID = Idaho, CT = Connecticut; IL = Illinois; CA = California; WV = West Virginia; ALB = Alberta). See also Table 1.
Fig. 2 in Molecular phylogenetics and systematics of two enteric helminth parasites (Baylisascaris laevis and Diandrya vancouverensis) in the Vancouver Island marmot (Marmota vancouverensis)
Fig. 2. Bayesian consensus phylogram based on Baylisascaris and outgroup alignments of concatenated mitochondrial sequences (12S, cox1, and cox2) from GenBank and this study (B. laevis). Branch labels represent Bayesian posterior probabilities. Branch lengths are scaled to expected number of substitutions per site. Abbreviations refer to sampling sites (AK = Alaska, ID = Idaho, CT = Connecticut; IL = Illinois; CA = California; WV = West Virginia; ALB = Alberta). See also Table 1.
Fig. 1 in Molecular phylogenetics and systematics of two enteric helminth parasites (Baylisascaris laevis and Diandrya vancouverensis) in the Vancouver Island marmot (Marmota vancouverensis)
Fig. 1. Known geographic distributions of Baylisascaris laevis and Diandrya composita in North America.
Fig. 4 in Molecular phylogenetics and systematics of two enteric helminth parasites (Baylisascaris laevis and Diandrya vancouverensis) in the Vancouver Island marmot (Marmota vancouverensis)
Fig. 4. Bayesian consensus phylogram based on Baylisascaris and outgroup alignments of concatenated mitochondrial (12S, cox1, and cox2) and nuclear sequences (28S, ITS, and ard1) from GenBank and this study (B. laevis). Branch labels represent Bayesian posterior probabilities. Branch lengths are scaled to expected number of substitutions per site. Abbreviations refer to sampling sites (AK = Alaska, ID = Idaho, CT = Connecticut; IL = Illinois; CA = California; WV = West Virginia; ALB = Alberta). See also Table 1.
Fig. 1 in Sarcoptic mange in wild ungulates in the European Alps - A systematic review
Fig. 1. Map of the European Alps and sarcoptic mange outbreaks in wild ungulates reported in the literature (n = 27). Host species is indicated with colour, the number of reported animals is indicated with size, and the time period is indicated by opacity. Grey area: alpine regions. Thin black lines: administrative boundaries. Thick black lines: country borders. The names of the countries are given. (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)
Domain-Driven Design in Microservices-Based Systems Development: A Systematic Literature Review and Thematic Analysis [Dataset]
<p>This repository contains all artifacts related to the study: Domain-Driven Design in Microservices-Based Systems Development: A Systematic Literature Review and Thematic Analysis</p>
FIGURE 5 in Ataxioceras (Ataxioceras) lopeztichae Cantú-Chapa, 1991: Updating the systematic and palaeobiogeographic interpretation
FIGURE 5. Adapertural structures in microconchiate Schneidia, Ataxioceras and Parataxioceras drafted from different authors as indicated: 1 - Schneidia lussasense Atrops (= Ataxioceras [Atax.] subinvolutum [Siemiradzki] in Geyer, 1961, pl 10, fig. 6). 2 - Schneidia lussasense (= Atax. [Schn.] lussasense in Atrops, 1982, pl. 21, fig. 6). 3 - Schneidia lopeztichai (=Atax. [Atax.] lopeztichae in Cantú-Chapa, 1991, fig. 2). 4 - Atax. lothari (Oppel) morphotype lothari Oppel [m] (Moliner, 2009, fig. 2.5 d). 5 - Atax. (Parataxioceras) hyppolytense (Atrops, 1982, pl. 7, fig. 7). 6 - Atax. (Paratax.) hyppolytense (Atrops, 1982, pl. 8, fig. 6). 7 - Atax. (Paratax.) lothari lothari (Oppel) (Atrops, 1982, pl. 42, fig.4). 8 - Atax. (Paratax.) pseudolothari (Geyer, 1961, pl. 16, fig. 6). 9 - Atax. (Paratax.) evolutum (Atrops, 1982, pl.4, fig. 5). 10 - Atax. (Paratax.) planulatum (Quenstedt) (Geyer, 1961, pl. 14, fig. 2). 11 - Atax. (Paratax.) planulatum (Quenstedt) (Atrops, 1982, pl. 43, fig. 6). 12 - Atax. (Paratax.) oppeli (Geyer, 1961, pl. 16, fig. 5). 13 - Atax. (Paratax.) oppeli (Geyer, 1961, pl. 14, fig. 2). 14 - Atax. (Paratax.) pseudoeffrenatum Wegele (Geyer, 1961, pl. 16, fig. 1).
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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.