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FIGURE 6. Cystodictya formosa Moore, 1929 in Stenolaemate bryozoans from the Graham Formation, Pennsylvanian (Virgilian) at Lost Creek Lake, Texas, USA
FIGURE 6. Cystodictya formosa Moore, 1929 (A–B): A – deep tangential section showing autozooecial chambers with hemisepta and vesicular skeleton (XCI 27); B – branch transverse section showing mesotheca, autozooecial chambers and vesicles (XCI 23c). Goniocladia grahamensis Moore, 1929 (C–E): branch fragment showing the shape of fenestrule, ridges on branches and autozooecial apertures with lunaria (XCI 100). Dyscritella felixi n. sp. (F–H): F – colony encrusting a brachiopod spine (holotype XCI 101); G – colony surface showing autozooecial apertures, exilazooecia, and acanthostyles; H – tangential thin section showing autozooecial apertures, exilazooecia, and acanthostyles (paratype XCI 86).
Figure 6 in Hermann Karsten (1817-1908): a German naturalist in the Neotropics and the significance of his paleovertebrate collection
Figure 6. "Ground sloth" and glyptodont specimens. (a–k) Tardigrada indet. (a–h) Centra thoracic vertebrae ((a–b) MB.Ma. 17154; (c–d) MB.Ma. 17153; (e–f) MB.Ma. 17156; (g–h) MB.Ma. 17155); (i–k) centra of caudal vertebra (MB.Ma. 33543)], (l–r) Right hemimandible and two upper molariforms of Glyptotherium cf. G. cylindricum (MB.Ma. 33532), and (s–z) Glyptodontidae indet. [(s–t) osteoderm (MB.Ma. 33533-1); (u–z) four carpal–metacarpal elements of indet. laterality (MB.Ma. 33533-2-6). Scale bar equals 2 cm.
Figure 6. Ebertichthys ettlingensis n. gen. et n in New remarkable Late Jurassic teleosts from southern Germany: Ascalaboidae n. fam., its content, morphology, and phylogenetic relationships
Figure 6. Ebertichthys ettlingensis n. gen. et n. sp. Details of certain abdominal vertebrae and pectoral fin. (a) Anterior abdominal region and pectoral girdle and fin (holotype JME ETT 108). (b) Enlargement of a few abdominal vertebrae illustrating details of the epineural processes (holotype JME ETT 108). (c) Details of pectoral fin and radials (JME ETT 132a). Abbreviations: cl, cleithrum; cor, coracoid; d.ra, distal radials; epin.p, epineural process; na, neural arch; ns, neural spine; paph, parapophyses; pcl1–3, postcleithrum 1–3; pec.f, pectoral fin; pec.ra, proximal radials supporting pectoral rays; pel.p, pelvic plate; ptt, posttemporal; ri, ribs; sc, anterior field of cycloid scales; sca, scapula; scl, supracleithrum; sn, supraneurals; vc, abdominal vertebral centra; 1st. pec, first pectoral ray.
Figure 6 in New information on the cranial and postcranial anatomy of the early synapsid Ianthodon schultzei (Sphenacomorpha: Sphenacodontia), and its evolutionary significance
Figure 6. Ianthodon schultzei cranial and skeletal reconstruction. Three-dimensional arrangement and projections based on a wax maquette. Skull in dorsal, ventral and lateral view; mandible in lateral and medial view.
Figure 6 in High-resolution stratigraphy of the Changhsingian (Late Permian) successions of NW Iran and the Transcaucasus based on lithological features, conodonts and ammonoids
Figure 6. Characteristic Changhsingian conodonts from the Julfa region (scale bars equal to 100 µm); all specimens stored in the collection of the Ferdowsi University, Mashhad. (A) Clarkina orientalis (Barskov and Koroleva, 1970); FUM#1J192.1; upper Julfa beds (Vedioceras beds), Ali Bashi 1 section. (B) Clarkina subcarinata Sweet, 1973; FUM#4J142.8; Zal Member (Ali Bashi Formation), Ali Bashi 4 section. (C) Clarkina changxingensis Wang and Wang, 1981; FUM#4J153.1; Zal Member (Ali Bashi Formation), Ali Bashi 4 section. (D) Clarkina bachmanni Kozur, 2004; FUM#AJ185.23; Paratirolites Limestone (Ali Bashi Formation), Aras Valley section. (E) Clarkina nodosa Kozur, 2004; FUM#G249.16; Paratirolites Limestone (Ali Bashi Formation), Ali Bashi M section. (F) Clarkina yini Mei, 1998; FUM#AJ192.4; Paratirolites Limestone (Ali Bashi Formation), Aras Valley section. (G) Clarkina abadehensis Kozur, 2004; FUM#1J248.9; Paratirolites Limestone (Ali Bashi Formation), Ali Bashi 1 section. (H) Clarkina hauschkei Kozur, 2004, FUM#1J249D.9; Paratirolites Limestone (Ali Bashi Formation), Ali Bashi 1 section. (I) Hindeodus eurypyge Nicoll, Metcalfe and Wang, 2002, FUM#1J255.7 (cusp broken); Zal Member (Ali Bashi Formation), Ali Bashi 1 section. (J) Hindeodus typicalis Sweet, 1970, FUM#G233.5; Paratirolites Limestone (Ali Bashi Formation), Ali Bashi M section. (K) Hindeodus typicalis Sweet, 1970, FUM#4J200.56; Paratirolites Limestone (Ali Bashi Formation), Ali Bashi 4 section. (L) Hindeodus julfensis Sweet, 1973, FUM#1J198.4; Zal Member (Ali Bashi Formation), Ali Bashi 4 section. (M) Hindeodus praeparvus Kozur, 1996, FUM#G274.6 (cusp broken); Aras Member (Elikah Formation), Ali Bashi M section. (N) Hindeodus changxingensis Wang, 1995, FUM#4J201.6 (cusp broken); Aras Member (Elikah Formation), Ali Bashi 4 section. (O) Merrillina ultima Kozur, 2004, FUM#AJ204.13; Aras Member (Elikah Formation), Aras Valley section. (P) Hindeodus parvus Kozur and Pjatakova, 1976, FUM#4J213.1; Elikah Formation; Ali Bashi 4 section.
FIGURE 6 in A new species of Characidium (Characiformes: Crenuchidae) from the Chapada dos Veadeiros, Goiás, Brazil
FIGURE 6 | Underwater photography of Characidium kalunga in the rio Preto, at the Parque Nacional da Chapada dos Veadeiros, Goiás, Brazil (not collected).
FIGURE 6 in Deep-sea anglerfishes (Lophiiformes: Ceratioidei) from off northeastern Brazil, with remarks on the ceratioids reported from the Brazilian Exclusive Economic Zone
FIGURE 6 | Species of the Gigantactinidae reported in this study: A. Gigantactis watermani, NPM 4424, 170 mm SL; B. Rhynchactis sp., NPM 4425, 113 mm SL. Scale bars = 10 mm.
FIGURE 6 in Two new species of Knodus (Characidae: Stevardiinae) from the upper rio Tocantins basin, with evidence of ontogenetic meristic changes
FIGURE 6 | Knodus obolus, holotype, NUP 22667, 46.4 mm SL, ribeirão Dois Irmãos, tributary to the rio do Peixe, tributary to the rio das Almas, tributary to the rio Maranhão, tributary to the rio Tocantins, Municipality of Pirenópolis, Goiás State, Brazil.
FIGURE 6 in Description of three new species of Eigenmannia (Gymnotiformes: Sternopygidae) from the rio Mearim and rio Parnaíba basins, Northeastern Brazil
FIGURE 6 | Eigenmannia robsoni, MZUSP 125872, holotype, 139.3 mm LEA, rio Parnaíba, Muricí dos Portelas, Piauí, 03°18'24.8"S 42°05'36.2"W. A. lateral view of head, B. lateral view of body.
FIGURE 6 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 6. Fossil turtle shell fragment (DMNH 2013-07-0563) with putative shell disease.. Photograph (A) shown in external view. Frames on the photograph and highlight specific areas with shell disease as both direct µCT data (B, D) and heatmapped slices illustrating bone density changes (C, E). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Specific patches of shell disease are indicated with purple arrows. Scale bar in A equals 2 cm. Scale bars in B and D equal 5 mm.
FIGURE 6 in Redescription of soft tissue preservation in the holotype of Scaphognathus crassirostris (Goldfuss, 1831) using reflectance transformation imaging
FIGURE 6. Close-ups of RTIViewer snapshots of the region ventral to the zeugopodial bones of the right wing on the main slab, taken under different lighting conditions, but all processed using the specular enhancement mode (except for 6A and 6H). Scale bar for all illustrations equals 10 mm, except for 6G and 6H (one millimetre). Markings for various pycnofibre types used throughout this Figure: Type 2 (bifurcated; yellow circle), Type 3 (trident-like; orange circle), Type 5 (tuft, red circle), and Type 6 (symmetrical "feather", green circle). The path of individual pycnofibre impressions, and the path of individual side branches of single impressions are illustrated by red markings (either by straight lines or by curved arcs as in 6D, 6E, and 6H). 6A, 6C. Overview of the area with the pycnofibres ventral to the zeugopodial bones of the right wing (upper left corner of both images) and the phalanges of the right wing finger (near the right image margin) under normal light (6A) as well as under the specular enhancement mode (6C). 6B. Schematic sketch of Figure 6C, showing the appearance of the pycnofibre impressions under normal light. 6D-6E. Closeups of 6C. Note the parallel to subparallel alignment of several pycnofibre impressions (red vertical lines in 6D and 6E) and the easily detected caudally curved side branches of the Type 4 pycnofibre (red rectangle in 6F). The complex structure with several putative side branches at the right image margin between Type 2 and 3 pycnofibres (red arrow) is more likely to represent an arrangement of overlapping impressions of individual pycnofibres. 6F. Sketch of the RTI images 6D and 6E. 6G. Detailed close-up of the Type 2 pycnofibre, outlined by red markings. 6H. Detailed close-up of the Type 5 pycnofibre. The longest branch in the middle has a distinctive bifurcation (red circle).
FIGURE 6 in Phylogeny of iguanodontian dinosaurs and the evolution of quadrupedality
FIGURE 6. Parsimony (left) and Bayesian (right) trees plotted together. Strict consensus of 84 MPTs after pruning Oryctodromeus, Atlascopscosaurus, Planicoxa, Cumnoria, Cedrorestes, and NHMUK R28860. Jackknife values above 20 (with 10% chance of character removal) are shown above and to the left of their respective nodes. Bremer supports above one are shown below and to the left of their respective nodes, and bolded. CI=0.272, RI=0.634. Maximum clade credibility tree produced by Bayesian analysis showing posterior probabilities below and to the right of their respective node.
FIGURE 6 in Taxon-specific variability of leaf traits in three long-ranging fossil-species of the Paleogene and Neogene: Responses to climate?
FIGURE 6. Site-specific data for lamina centroid and leaf length-to-width ratio (LWR) plotted for each taxon. 6A: Lamina centroid for Platanus neptuni. 6B: LWR for P. neptuni. 6C: Lamina centroid for Eotrigonobalanus furcinervis. 6D: LWR for E. furcinervis. 6E: Lamina centroid for Daphnogene cinnamomifolia. 6F: LWR for D. cinnamomifolia. The boxes span the 50% interquartile. The horizontal lines within the boxes indicate the median values. The "whiskers" mark the highest and lowest values. Outliers located at a distance of up to 1.5 times the quartile span outside the whiskers are drawn as asterisks, and extreme outliers are drawn as circles. Different minuscule letters indicate statistically significant differences among sites. Colors indicate deposit type. Colors indicate deposit type. Green: fluviatile. Red: volcanic. Blue: marine. Lines delimit age groups. LE: Late Eocene. EO: Early Oligocene. LO: Late Oligocene. EM: Early Miocene. For site numbers and dating see Table 1.
FIGURE 6 in Evaluating the ecology of Spinosaurus: Shoreline generalist or aquatic pursuit specialist?
FIGURE 6. Suggested head positions of Spinosaurus relative to water. A) when dipping the snout in the water to forage while leaving the naris above the waterline as per the wading model. Head angle of 45 degrees based on Schade et al. (2020) for Irritator. B) while lying submerged, keep the naris and orbit clear of the water while minimising the amount of head that is exposed as per Arden et al. (2019), C) fully submerged as if coming up for air and trying to expose only the nares to breathe. Scale bar equals 1 m.
FIGURE 6. CMM-V-10108, a in A Miocene cetacean vertebra showing a partially healed longitudinal shear-compression fracture, possibly the result of domoic acid toxicity or failed predation
FIGURE 6. CMM-V-10108, a second Miocene pathological cetacean vertebra (also shown in Figure 5) associated with the one shown in Figures 2-4. A. CT-scan image towards the anterior end of the vertebra. B. CT-scan image at about the midpoint in the length of the vertebra showing the thickness of the periosteal reactive bone.
FIGURE 6 in New Neogene anourosoricin shrews from northern Asia
FIGURE 6. Teeth and bones of Paranourosorex seletiensis Storch and Zazhigin, 1996 (A, B), Crusafontina sp. 1, (C), Crusafontina sp. 2 (D) and Paranourosorex intermedius sp. nov. (E). A, GIN 951/1000 (holotype) from SLT/1A, left hemimandible fragment (cut image) with m1 and m2 in occlusal view (A2, magnified m2); B, GIN 951/1001 (paratype) from SLT/1A, left P4 in occlusal view; C, GIN 640/1004 from PVL/1A, left M1 in occlusal view; D, GIN 951/1003 SLT/ 1A, left P4 in occlusal view; E, GIN 948/1051 (holotype) from NST/1A, right dentary fragment with m1 and m2 (E1, occlusal view; E2, lateral view E3, medial view;). Scale bars equal 1 mm.
FIGURE 6. A in Distinguishing between three modern Ellobius species (Rodentia, Mammalia) and identification of fossil Ellobius from Kaldar Cave (Iran) using geometric morphometric analyses of the first lower molar
FIGURE 6. A) First two PCs from the Principal component analysis performed on the size and shape including the reference collection and Kaldar Cave material. B) Boxplot of the total length of Ellobius from the extant reference collections and Kaldar Cave.
FIGURE 6 in Patagonia's diverse but homogeneous early Paleocene forests: Angiosperm leaves from the Danian Salamanca and Peñas Coloradas formations, San Jorge Basin, Chubut, Argentina
FIGURE 6. Morphotype SA002. A, MPEF-Pb-2021 (exemplar, see also Figure 6F); B, MPEF-Pb-4007; C, MPEF-Pb-4010 (white arrow, asymmetric base), note insect damage (black arrow, DT26; also see Donovan et al., 2018 figure 9.16); D, MPEF-Pb-9004; E, digital overlay drawing (DOD) of leaf venation in Figure 6C (arrow, swollen petiole base; see also Figure 31F); F, DOD of leaf venation of specimen in Figure 6.A (exemplar); G, apex in MPEF-Pb-9005; H, tooth detail of specimen in Figure 6.A; I, DOD of tooth venation of specimen in Figure 6H; J, camera lucida drawing (CLD) of MPEF-Pb-9006; K, medial tooth venation of specimen in Figure 6J; L, basal tooth venation of specimen in Figure 6J; M, CLD of leaf venation of specimen in Figure 6D (arrow, chevroned epimedial tertiaries); N, tooth venation of specimen in Figure 6M. Single-color scale bars equal 10 mm; grid scales equal one millimeter (per rectangle).
FIGURE 6. SHSU 1-235 in First fossil manatees in Texas, USA: Trichechus manatus bakerorum from Pleistocene beach deposits along the Gulf of Mexico
FIGURE 6. SHSU 1-235, mandibular symphysis with partial left dentary ramus in dorsal (A), ventral (B), and anterior (C) views. The shallow dorsoventral depth and low, rounded ventrally projecting boss (arrow) are diagnostic features of the extinct morphotype Trichechus manatus bakerorum. Scale bar equals 2 cm.
FIGURE 6 in Geometric morphometric analysis of Protoconites minor from the Cambrian (Terreneuvian) Yanjiahe Formation in Three Gorges, South China
FIGURE 6. Protoconites minor morphospace generated by the Relative Warp (RW) analysis using mirrored specimens. 1. plot for RW 1–2; 2. plot for RW 1–3. All thin-plate splines correspond to points (indicated as a line) within the morphospace in RW 1–2 and RW 1–3 planes, respectively.
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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.