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Fig. 6 in New bioerosion traces in rhynchosaur bones from the Upper Triassic of Brazil and the oldest occurrence of the ichnogenera Osteocallis and Amphifaoichnus
Fig. 6. Clusters of grooves on bone fragments of the rhynchosaurid archosauromorph Hyperodapedon mariensis (Tupi Caldas, 1933) from Buriol Site, Brazil, Hyperodapedon AZ, Carnian. A. UFRGS-PV-1581-T #20, arcuate and paired grooves, similar to feeding traces of Osteocallis mandibulus Roberts et al., 2007, but without forming a trail. B. UFRGS-PV-1581-T #22, densely concentrated grooves, giving the bone surface an etched appearence. C. UFRGS-PV-1581-T #5, straight and arcuate grooves closely associated to an incipient Osteocallis mandibulus (arrow). D. UFRGS-PV-1581-T #26, straight and arcuate grooves and some isolated grooves. E. UFRGS-PV-1581-T #6, dentary fragment; E1, two clusters of grooves; E2, schematic drawing. F. UFRGS-PV-1581-T #17; F1, subparallel grooves; F2, subparallel grooves associated to a subcircular cluster of grooves (arrow).
Fig. 6 in Morphological disparity of early ammonoids: A geometric morphometric approach to investigate conch geometry
Fig. 6. Evolution of the morphospace occupation through the seven intervals constituting the Early and Middle Devonian, showing the distribution of ammonoid superfamilies; based on the analysis of the whorl profiles (on each diagram, the horizontal axis corresponds to PC1 and the vertical axis to PC2). See Fig. 2 for interval labels.
Fig. 6. Tettigarctinae occurrences through time. 1 in First North American occurrence of hairy cicadas discovered in the Cenomanian (Late Cretaceous) of Labrador, Canada
Fig. 6. Tettigarctinae occurrences through time. 1, Liassocicada antecedens Bode, 1953 from Early Jurassic Posidonia Shale Formation, Germany drawing from Nel et al. 1998); 2, Kisylia psylloides Martynov, 1937 from Early Jurassic Kisyl-Kiya, Kyrgyzstan; 3, Protabanus chaoyangensis Hong, 1982 from the Callovian/Oxfordian (Middle/Late Jurassic) Jiulongshan Formation, China; 4, Sunotettigarcta (represented by drawing of Sunotettigarcta kudryashevae Shcherbakov, 2009) from Late Jurassic Karatau, Kazakhstan; 5, Tettagalma striata Menon, 2005 from the Aptian (Early Cretaceous) Crato Formation, Brazil; 6, Magrebarcta africana Nel, Zarbout, Barale, and Philippe, 1998 from the Aptian (Early Cretaceous) Duriet Formation, Tunisia; 7, Cretotettigarcta burmensis Fu, Cai, and Huang, 2019 from the Cenomanian (Late Cretaceous) Hukawng Valley, Myanmar; 8, Maculaferrum blaisi gen. et sp. nov. (holotype RMIP 2018.18.24) from the Cenomanian (Late Cretaceous) Redmond Formation, Labrador, Canada; 9, Eotettigarcta scotica Zeuner, 1944 from the Palaeocene Isle of Mull, UK (only known from a partial hind wing); 10, Meuniera haupti Piton, 1936 from the Palaeocene Menat quarry, France; 11, Paratettigarcta zealandica Kaulfuss and Moulds, 2005 from the Miocene Hindon Maar, New Zealand; 12, Tettigarcta crinita Distant, 1883 from southern Victoria, Australia (extant). The classification of Liassocicada ignota Brodie, 1845 within Cicadoprosbolinae introduces uncertainty about the affinities of L. antecedens to Tettigarctinae (Shcherbakov 2009). Drawings not to scale; 1, 4, 6, 7, 9–11, mirrored to facilitate comparison with Maculaferrum. Fossil occurrences retrieved from the Paleobiology Database (Czaplewski 2019). Palaeogeographical maps from Scotese (2001).
Fig. 6. A in The giant pliosaurid that wasn't-revising the marine reptiles from the Kimmeridgian, Upper Jurassic, of Krzyżanowice, Poland
Fig. 6. A. Approximate position of the identifiable fragments of the thalassochelydian turtle Craspedochelys? sp., MZ VIII Vr-71, within the shell, in dorsal (A1) and ventral (A2) views (schematic reconstruction of Craspedochelys spp. based on Anquetin et al. 2014, 2017, and TS personal observations, modified to fit the observed morphologies). Numbers represent the elements illustrated in the text: 1, Fig. 2; 2, Fig. 3A; 3, Fig. 3B; 4, Fig. 4A; 5, Fig. 4B; 6, Fig. 4D. Fragments likely belonging to the same individual are indicated by the same colour. B–E. Anterior edges of the carapace of Plesiochelys etalloni (Pictet and Humbert, 1857), NMS 8514/NMS 118 (B) and NMS 8727/NMS 116 (C), Craspedochelys jaccardi (Pictet, 1860), NMS 101 (D), and Craspedochelys picteti (Rütimeyer, 1873), NMS 9149/NMS 608 (E); all from the Kimmeridgian of Solothurn, Switzerland. The numbers indicate marginal scutes. Note the anteriorly protruding first marginal of Plesiochelys etalloni (B, C) and straight anterior edge in Craspedochelys spp. (D, E).
Fig. 6 in The oldest post-Paleozoic (Ladinian, Triassic) brachiopods from the Betic Range, SE Spain
Fig. 6. Paleogeographical map of the Ladinian times (modified after Pérez-López and Pérez-Valera 2007), showing the distribution of taxa highly related to, or common with the brachiopod fauna inhabiting the Middle Triassic peri-Iberian platforms system. Color of arrows and taxa symbolizes the inferred paleobiogeographical affinities. ACP, Apennine Carbonate Platform; AM, Armorican Massif; BM: Bohemian Massif; CM, Central Massif; EM, Ebro Massif; MM, Meso-Mediterranean Massif; Mi, Misunithyris; Me, Menathyris; Mz, Mentzelia; Co, Coenothyris. Occurrences mainly based on Schmidt (1935), Siblík (1972, 1988, 2001), Popiel-Barczyk and Senkowiczowa (1989), Dagys (1993), Török (1993), Kaim (1997), Torti and Angiolini (1997), Pálfy (2003), Feldman (2005, 2013), Ruban (2010), Escudero-Mozo et al. (2015), among others (see text for details). Dotted line shows palaeogeographic position of the currently emerged land.
Fig. 6 in A late Paleocene fauna from shallow-water chemosynthesis-based ecosystems, Spitsbergen, Svalbard
Fig. 6. Solemyid bivalve Solemya sp. from the upper Paleocene, Basilika Formation, Zachariassendalen, Spitsbergen, Svalbard. A. NRM-PZ Mo 183945, shell (LV), internal mold (RV), left (A1) and right (A2) valve, dorsal view of both valves (A3), ventral view (A4). B. NRM-PZ Mo 183946, internal mold, butterflied specimen in dorsal view (LV, left valve; RV, right valve).
Fig. 6 in Palaeobiology of orthothecide hyoliths from the Cambrian Manto Formation of Hebei Province, North China
Fig. 6. Opercula of cupithecid hyolith Cupitheca convexa sp. nov. preserved as internal or external moulds, which are prepared from natural casts, collected from the Manto Formation (Cambrian Stage 4/5) in the Zuojiawu section of Tangshan, China. A, B. Internal moulds of opercula, NIGPAS 166337 A) and NIGPAS 166342 (B); showing exteriors covered with concentric ribs, protoopercula (indicated by white arrows) and imprints of bilobate cardinal →
Fig. 6 in A new assessment of the Late Devonian antiarchan fish Bothriolepis leptocheira from South Timan (Russia) and the biotic crisis near the Frasnian-Famennian boundary
Fig. 6. Antiarchan fish Bothriolepis leptocheira jeremejevi (Rohon, 1900), Sosnogorsk locality, Sosnogorsk Formation, lowermost Famennian, postpineal A–C, E, G), nuchal (D–G, I, K–M), and paranuchal (H, J, L, M) plates of the head shield. A. IG KSC 155/54-2, disconnected from the Nu IG KSC 155/54-1, in dorsal (A1) and visceral (A2) views. B. IG KSC 155/146 in dorsal (B1) and visceral (B2) views. C. IG KSC 155/155 in dorsal (C1) and visceral C2) views. D. IG KSC 155/58 in dorsal view. E. Articulated plates IG KSC 155/118 in dorsal view. F. IG KSC 155/53 in dorsal (F1), visceral (F2), and posterior (F3) views. G. Articulated plates IG KSC 155/154 in dorsal (G1) and visceral (G2) views. H. IG KSC 155/55 in dorsal (H1) and visceral (H2) views. I. IG KSC 155/54-1 from the same individual as plate in A, in dorsal view. J. IG KSC 155/119 in dorsal view. K. IG KSC 155/56 in dorsal view. L. IG KSC 155/117 in visceral (L1) and dorsal (L2) views. M. IG KSC 155/125 in dorsal view.
Fig. 6 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 6. Construction of the prismatic reduced dorsal shell wall (median section, growth direction to the left, centrifugal). Ptychophylloceras cf. dacquei Joly, 1976, BSPG MAn-4516, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar. The dorsal shell wall consists of an outer wrinkle layer and dorsal inner prismatic layer. The dorsal inner prismatic layer becomes thinner towards the aperture (A, B) and vanishes completely (C). Abbreviations: dipl, dorsal inner prismatic layer; ipl, inner prismatic layer; ncl, nacreous layer; opl, outer prismatic layer; s, septum; wl, wrinkle layer.
Fig. 6 in A review of Neogene and Quaternary pikes of southeastern Europe and a new species from the early Pleistocene of Nogaisk, Ukraine
Fig. 6. Isolated elements assigned to a pike Esox spp. from Southeastern Europe; late Miocene (A–J), Pliocene (N–Q), and Pleistocene (K–M, R–T). A–G, I–T. Tooth, lateral view. A. NMNHU-P 41/3472, Palievo. B. NMNHU-P 33/561, Mykhailivka 2. C. NMNHU-P 29/1708, Popovo 3. D. NMNHU-P 29/1045, Verkhnya Krynitsya 2. E. NMNHU-P 41/4498, Egorovka 2. F. NMNHU-P 41/4329, Egorovka 1. G. NMNHU-P 38/1964, Novoukrainka 1. I. NMNHU-P 41/2466, Pontian Lectostratotype. J. NMNHU-P 41/2742, Vinogradovka 1. K. NMNHU-P 53/4395, Bol'shevik 2. L. NMNHU-P 29/380, Lysa Gora 1. M. NMNHU-P 53/4388, Semibalka 1. N. NMNHU-P 42/2458, Vinogradovka 2. O. NMNHU-P 53/4281, Obukhovka 2. P. NMNHU-P 53/4344, Zhevakhova Gora. Q. NMNHU-P 29/627, Verkhnya Krynitsya 1. R. NMNHU-P 42/2463, Kotlovina 2. S. NMNHU-P 53/4406, Medzhibozh. T. NMNHU-P 42/2472, Kotlovina 3. H. Left palatine (NMNHU-P 33/517), Andreevka, occlusal view. Scale bars: C, D, H–O, R, S, T, 5 mm; A, B, E, F, P, Q, 4 mm; G, 3 mm.
Fig. 6 in Morphology and histology of dorsal spines of the xenacanthid shark Orthacanthus platypternus from the Lower Permian of Texas, USA: Palaeobiological and palaeoenvironmental implications
Fig. 6. Cross-sections of dorsal spines (non-denticulated region) of Orthacanthus platypternus (Cope, 1884), Lower Permian, Craddock Bone Bed, Texas, USA. Comparison between the smallest, specimen HMNS-T1 (A), and the largest Orthacanthus dorsal spine sampled, specimen HMNS-J1 (B). Posterior sides of the spines are pointing to the top of the figure.
Fig. 6 in Globicephaline whales from the Mio-Pliocene Purisima Formation of central California, USA
Fig. 6. Plot of maximum width of external bony nares versus length of promontorium for 62 delphinidan specimens, representing 34 species. Solid line is a reduced major axis regression (for all Delphinida). Horizontal dotted line is the nares width for the Seacliff Beach skull (UCMP 219223) and the vertical dashed lines are the lengths of the promontoria in UCMP 219488 (black) and 219487 (gray). In order to maximize the measurement area occupied by the specimens we sampled, the labeled y axis does not pass through the origin, but instead x = 8.
Fig. 6 in Revision of the enigmatic insect family Anthracoptilidae enlightens the evolution of Palaeozoic stem-dictyopterans
Fig. 6. Forewing of anthracoptilid insect Westphaloptilus gallicus sp. nov. from Westphalian of Bruay-en-Artois, Department of North, France, holotype Bruay F.5 BR27–28.
Fig. 6 in Two New Species Of The Genus Eupyrgops Berg, 1898 (Coleoptera: Curculionidae: Celeuthetini) From The Luzon Island (Philippines)
Fig. 6. Genitalia of E. sabatiensis sp. nov. 1 – aedeagus in lateral view; 2 – male spicula; 3 – apex of aedeagus in dorsal view; 4, 6 – female spicula; 5, 7 - spermatheca.
Fig. 6 in New Species Of The Genus Pachyrhynchus Germar (Coleoptera, Curculionidae, Entiminae) From The Greater Mindanao Pleistocene Aggregate Island Complex (Philippines)
Fig. 6. Lateral view of habitus; A – P. absurdus; B – P. orientalis; C – P. occidentalis; D – P. neoabsurdus. All females.
Fig. 6 in Immediate Allelopathic Effect Of Two Invasive Heracleum Species On Acceptor-Germination
Fig. 6. CCU content accordingly ryegrass germination in leachates of H. sosnovskyi and H. mantegazzianum (p<0,05; mean±SE).
Fig. 6-10 in A Contribution To Knowledge Of Dermestidae (Coleoptera: Bostrichiformia) from the Philippines
Fig. 6-10. Anthrenus (Nathrenus) hrdlickai sp. nov.: 6- habitus, dorsal aspect; 7- antennae of male; 8- abdomen; 9- male genitalia; 10- 9th abdominal ventrite.
Figs 6–11 in A new species of Cerozodus and new records of Asilinae and Ommatiinae (Diptera: Asilidae) from Tocantins, Brazil
Figs 6–11. Cerozodus inesperatus sp. nov., male holotype: 6, antenna, lateral view; 7, wing, dorsal view; 8, scutellum, dorsal view; terminalia: 9, lateral view; 10, dorsal view; 11, ventral view.
Figs 5, 6 in Dimorfismo sexual emHepatus pudibundus (Crustacea, Decapoda, Brachyura)
Figs 5, 6. Hepatus pudibundus (Herbst, 1785). Dimorfismo sexual na forma: 5, prÓpodo direito; 6, prÓpodo esquerdo. DeformaÇões magnificadas uma vez.
Fig. 6 in Reproductive success of Trypoxylon (Trypargilum) lactitarse (Hymenoptera: Crabronidae) in a fragmented landscape
Fig. 6. Results of the Generalized Linear Mixed Model (GLMM) between the numbers of adults emerged from each nest and fragment size. No difference was foUnd between small and large fragments for sUrvival rate (z = 0.784, p = 0.433).
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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.