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Fig. 14 in Brachiopod fauna from uppermost Visean (Mississippian) mud mounds in Derbyshire, UK
Fig. 14. Rhynchonellida and Spiriferida from the Brigantian (uppermost Visean) of Ricklow Quarry, near Monyash (localities RCC-, RCK-; Fig. 3) and Wensley Dale, near Matlock (locality WI1; Fig. 2), Derbyshire, UK. A–G. Pleuropugnoides pleurodon (Phillips, 1836). A. MPUM12011 (RCC49-22) in dorsal (A1) and anterior (A2) views. B. MPUM12013 (RCK15-4) in ventral (B1) and dorsal (B2) views. C. MPUM12017 (RCK15B-3) in ventral (C1), dorsal (C2), and anterior (C3) views. D. MPUM12015 (RCK15-19) in ventral (D1) and dorsal (D2) view. E. MPUM12014 (RCK15-15) in lateral (E1), ventral (E2), and posterior (E3) views. F. MPUM12012 (RCC73-9) in lateral (F1), ventral (F2), posterior (F3), and anterior (F4) views. G. MPUM12016 RCK15-29) in ventral (G1), dorsal (G2), and anterior (G3) views. H–L. Propriopugnus pugnus (Martin, 1809). H. MPUM12021 (RCC2-55) in dorsal view.. MPUM12022 (RCC3-7) in dorsal (I1) and anterior (I2) views. J. MPUM12024 (RCC73-22b) in ventral (J1) and anterior (J2) views. K. MPUM12026 RCC60-4d) dorsal valve in dorsal view. L. MPUM12028 (WI1-33) in dorsal view. M.?Fusella sp., MPUM12037 (RCC128-5) ventral valve in ventral view. N, O. Martiniinae gen. et sp. indet. N. MPUM12065 (RCC2-58a) ventral valve in ventral view. O. MPUM12066 (WI1-32) ventral valve in ventral view. P–S. Angiospirifer bisulcatus (Sowerby, 1825). P. MPUM12032 (WI1-12a) in ventral view. Q. MPUM12035 (WI1-11) ventral valve in ventral view. R. MPUM12031 (WI1-10) in lateral (R1), dorsal (R2), ventral (R3), anterior (R4), and posterior (R5) views. S. MPUM12033 (WI1-30) in lateral (S1), dorsal S2), ventral (S3), anterior (S4), and posterior (S5) views. T–V. Latibrachythyris cf. crassa (De Koninck, 1843). T. MPUM12039 (RCC1-34a) ventral valve in ventral view. U. MPUM12038 (RCC1-21) ventral valve in ventral view. V. MPUM12041 (RCC54-17a) ventral valve in ventral (V1) and posterior (V2) views. Scale bars 10 mm.
Fig. 14 in Mollusks from Miocene hydrocarbon-seep deposits in the Ilocos-Central Luzon Basin, Luzon Island, Philippines
Fig. 14. The vesicomyid bivalve Archivesica? sp. 2 from Upper Miocene seep deposits of the Amlang Formation in Pangasinan province, Luzon, Philippines. A. NRM Mo 192676, large articulated specimen, view on LV showing interior posterior ridge (A1), dorsal view showing moderate inflation and lunule (A2). B. NRM Mo 192678, articulated specimen, view on LV showing general outline. C. NRM Mo 192677, isolated RV, view on hinge.
Fig. 14 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages
Fig. 14. Dendrogram showing clustering of substrates sharing similar taxa of tube-dwelling polychaetes from the Polish Basin.
Fig. 14 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy
Fig. 14. Prostyliferid gastropods Prostylifer paludinaris (Münster, 1841) from Lago Antorno (A–C) and Misurina Landslide (D), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 13680, relatively large specimen with preserved protoconch and inner lip, in apertural view (A1); A2, close up showing umbilical chink and arched inner lip; A3, apex with mammilated protoconch having spiral crests, in lateral view. B. PZO 12823, juvenile specimen with protoconch having spiral crests, in apertural view. C. PZO 12824, juvenile specimen with protoconch having spiral crests; C1, larval shell ending at sinusigera, in apertural view; C2, close up of whorl of larval shell. D. PZO 12699, juvenile specimen with mammilated protoconch having spiral crests, in lateral view (D1); D2, early whorls, larval shell ending at sinusigera, in lateral view.
Fig. 14 in New insights into the origin and relationships of blastoid echinoderms
Fig. 14. Subterminal branching in the ambulacra of the callocystitid Callocystites fresti Paul, 2015a (SM A.85652), Wenlock (Silurian), Indiana, USA. Open arrow points to the place where the next lateral branch of the radial water vessel would have taken place, but the tip of the radial water vessel was at the top of the brachiole (Br) that arose from the final facet (solid arrow). Thus, branching of the radial water vessel in brachiole-bearing echinoderms was always subterminal. Modified from Paul and Hotchkiss 2020: fig. 7.
Fig. 14 in Research history, taphonomy, and age structure of a mass accumulation of the ornithopod dinosaur Dysalotosaurus lettowvorbecki from the Upper Jurassic of Tanzania
Fig. 14. Examples of states of bone preservation of ornithopod dinosaur Dysalotosaurus lettowvorbecki Pompeckj, 1920, from Kimmeridgian, Late Jurassic of Tendaguru, Tanzania. A. Several tibiae originally labelled with low Ig numbers showing multiple breaks perpendicular to their long axis. B. Isolated shaft of the left femur GPIT/RE/3446 in medial view with its proximal and distal ends broken off but with excellent preservation of the bone surface and of the delicate 4th trochanter. C. The right ilium GPIT/RE/6544 with the usual broken off preacetabular process and net-like surface cracks on the otherwise well-preserved lateral bone surface. D. Dorsal vertebra GPIT/RE/5462 of a juvenile individual in anterior view with plastic deformation of the left diapophysis. The deformation of this side is visible in two additional, potentially associated dorsal vertebrae. E. Unlabeled right humerus from the SMNS collections with well-preserved articular ends but with a distorted and compressed midshaft. F. Excellent preservation of the right calcaneum GPIT/RE/5808 in lateral view. G. The left jugal MB.R.1333 in lateral view with numerous diagenetic cracks which were resealed in situ by calcite. H. Right quadrate MB.R.3478 in lateral view with its cotylar head and upper part of the anterolateral wing broken off and slightly displaced forward whereas the surface of the bone and its delicate processes are generally well preserved. Scale bars 10 mm.
Fig. 14. A in Morphology and relationships of the enigmatic stenothecoid pan-brachiopod Stenothecoides-new data from the middle Cambrian Burgess Shale Formation
Fig. 14. A. Hypothesized morphogenetic pathway for derivation of the bivalved stenothecoid scleritome from a multisclerite, tubular, organocalcitic, eccentrothecimorph ancestor via a hypothetical organocalcitic tannuolinid. Eccentrothecimorph slightly modified from Skovsted et al. (2011: text-fig. 17). Tannuolinid modified from Skovsted et al. (2014). B. A possible cladogram that assumes an organocalcitic scleritome is primitive for the Pan-Brachiopoda. In this view, organophosphatic mineralogy evolved independently several times and the Stenothecoida evolved a bivalved scleritome independently of the Brachiopoda + Micrina clade.
Fig. 14 in Evidence of external gametophores in puzzling Late Triassic-Early Jurassic dasycladalean green algae
Fig. 14. Dasycladalean alga Chinianella ellenbergeri (Lebouché and Lemoine in Granier and Deloffre, 1994) Granier, Masse, and Berthou, 1994, emend. nov., upper Sinemurian (Lotharingian), Canders, 2.4 km E of Fontcaude (S France). LM-DiSTAR/BA.577.b, n. 045 (lost specimen), oblique section showing the presence of reproductive structures (see arrows).
Fig. 14. The provannid gastropod Provanna antiqua Squires, 1995 in Mollusks and a crustacean from early Oligocene methane-seep deposits in the Talara Basin, northern Peru
Fig. 14. The provannid gastropod Provanna antiqua Squires, 1995, from early Oligocene seep deposits at Cerro La Salina (block 1, A, F; block 4, H; block 6, B, C, D, G; block 8, E), Talara Basin, northern Peru. A. NRM Mo187044, specimen with distinctive axial and spiral sculpture, in abapertural view. B. NRM Mo187045, specimen with distinctive sculpture and showing the basal groove, in apertural view. C. NRM Mo187046, specimen with weak axial sculpture in the upper whorl, in apertural view. D. NRM Mo187047, fragmentary specimen with mainly spiral sculpture, in apertural view. E. NRM Mo187048, nearly smooth specimen showing slightly sinuous growth lines, in apertural view. F. NRM Mo187049, specimen with small shoulder and sculpture mainly in upper part of whorls, in apertural view. G. NRM Mo187050, specimen with faint axial and spiral sculpture, in apertural view. H. NRM Mo187051, two specimens with small shoulder and sculpture mainly in upper part of whorls..
Fig. 14 in Sieve-type normal pore canals in Jurassic ostracods: A review with description of a new genus
Fig. 14. Cytherid ostracod Minyocythere maculosa (Bate, 1963) from Everthorpe Quarry, South Cave, UK, Basement Beds, Bajocian (A, B) and Borehole Rodewald WA12, 395 m (C, D), 390 m (E), NW Germany, Witchellia laeviuscula Zone (Braun Jura γ), Lower Bajocian. A. Topotype, SMF Xe 23744, male left valve in external view (A1), macro sieve-type pore canals (StPC-M) (A2), micro sieve-type normal pore canals (StPC-m) (A3), and simple pore (A4). B. Topotype, SMF Xe 23745, female right valve in internal view (B1), muscle scars (B2), hinge (B3). C. SMF Xe 23746, male left valve in external view (C1), StPC-M (C2, C3), StPC-m (C4). D. SMF Xe 23747, female right valve in external (D1) and internal (D3) views, simple pore (D2), StPC-M (D4), StPC-m (D5), hinge, posterior part (D6), muscle scars (D7). E. SMF Xe 23748, interior of StPC-M (E1), fragment of a left valve in internal view (E2).
Fig. 14 in Mollusks from Pliocene and Pleistocene seep deposits in Leyte, Philippines
Fig. 14. The lucinid bivalve Lucinoma canudai sp. nov. from the Pleistocene Cambantug Point seep deposit, Leyte, Philippines. A. Holotype NMP-2167, large, articulated specimen with attached, filled burrow; outer surfaces of right (A1) and left (A2) valves; dorsal side (A3). B. Paratype NMNS PM 28157, small specimen showing ligament nymph of left valve. C. Paratype NMNS PM 28158, small specimen with remnants of two cardinal teeth in the left valve.
Fig. 14 in Evolution and identity of synapsid carpal bones
Fig. 14. Interpretation of the cartilaginous anlagen of the embryological carpus of different mammals by different authors. Whenever the radiale, ulnare or lunate have been interpreted previously as homologues of a centrale, the details are given in brackets following the abbreviations in the figures. A. Microcebus myoxinus Peters, 1852, 10.2 mm neck-rump length (from Schmidt-Ehrenberg 1942: 61, fig. 10, courtesy of Revue Suisse de Zoologie). B. Tarsius spectrumgurskyae Shekelle, Groves, Maryanto, and Mittermeier, 2017, 20.5 mm body length, (from Holmgren 1952: 80, fig. 93, reproduced with permission of Acta Zoologica, © The Royal Swedish Academy of Sciences, all rights reserved). C. Talpa europaea Linnaeus, 1758, 15 mm body length (from Kindahl 1942b: 270, fig. 4, courtesy of Sächsisches Staatsarchiv, Staatsarchiv Leipzig). D. Ovis aries Linnaeus, 1758, 38 mm body length, three-dimensional reconstruction of the left carpus in dorsal aspect (from Slabý 1967: pl. 6: 30). Abbreviations: ce, centrale; d, distal; di, distal carpal; int, intermedium; lu, lunate; na, naviculare; p, prepollex; p/s, prepollex/sesamoid; pis, pisiform; pr, proximal; ra, radius; rl, radiale; ul, ulna; ur, ulnare.
Fig. 14 in A taxonomic and phylogenetic review of the anhanguerid pterosaur group Coloborhynchinae and the new clade Tropeognathinae
Fig. 14. Histogram showing the distribution of the species and specimens attributed to Anhnagueridae during the Cretaceous. Each bar of the histogram represents the number of diverse species found in each labelled site, whilst the geometric figures identified the species within the three anhangerid clades: Coloborhynchinae, Anhanguerinae, and Tropeognathinae. Drawing by BH. Abbreviations: Al, Albian; Ap, Aptian; Ba, Barrenian Be, Berriasian; Ca, Campanian; Ce, Cenomanian; Co, Coniacian; Ha, Hauterivian; Ma, Maastrichtian; Sa, Santonian; Tu, Turonian; Va, Valangian.
Fig. 14 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 14. Skeletal reconstruction of MSF 15.8B., preserved elements highlighted in white, grey elements restored following adult Plateosaurus skeletons SMNS 13200 (von Huene 1926) and GPIT 1 (Mallison 2010a, b).
Figure 14 in A revised faunal list and geological setting for Bullock Creek, a Camfieldian site from the Northern Territory of Australia
Figure 14. Occlusal stereopair of?dasyurid dentary and isolated teeth. a, b, NTMAG P9215-4, right?dasyurid dentary containing p2-m2; c, d, NTMAG P9215-6,?dasyurid left lower molar; e, f, NTMAG P8663-4,?dasyurid right lower molar. Scale bar = 2 mm.
Figure 14 in Description of new cranial material of Propalorchestes (Marsupialia: Palorchestidae) from the Middle Miocene Camfield Beds, Northern Territory, Australia
Figure 14. Dental measurements for Propalorchestes check teeth plotted with those of smaller Palorchestes: a, length upper cheek teeth; b, anteriorloph width upper cheek teeth; c. lower cheek teeth; d, anteriorloph width lower cheek teeth; data points that represent measures for successive teeth of the same tooth row are connected by a line; data points that represent measures for non-successive teeth of the same tooth row are connected by a dashed line; Data and sources provided in Table 2.
Figure 14. Molpadia violacea Studer, 1876 photos and SEM ossicle images. a in Sea cucumbers of the Kerguelen Plateau, with descriptions of new genus and species (Echinodermata: Holothuroidea)
Figure 14. Molpadia violacea Studer, 1876 photos and SEM ossicle images. a, left lateral view of holotype (oral end left) (ZMB 2070) (bottom left insert with photo of tentacles); b, right lateral view of HIMI specimen of Molpadia violacea (NMV F165737) (insert with drawing of radial (left) and inter-radial plates of the calcareous ring); c, d, SEM images of fusiform rod ossicles from HIMI specimen of Molpadia violacea (NMV F165737); c, from mid-body wall (insert with drawings of table disc and spire); d, from caudal body wall.
Figures 10–14 in Oogenesis in Phragmatopoma (Polychaeta: Sabellariidae): Evidence for morphological distinction among geographically remote populations
Figures 10–14. Ultrastructure in Phragmatopoma caudata of the SW Atlantic. Proliferative Phase. Figures 10 and 11 Oogonia (Oo) and oocytes (Oc) connected via cellular prolongations (white arrow) to the endothelium of the intersegmental blood vessel (Bv). Note that the contact of ovary basal lamina is quite electron dense (black arrow). Desmosomes (D) form the oocyte-oocyte junction (Figure 10, 1,150X; Figure 11, 2,050X). M = mitochondria; Ch = chromosome. Figure 12 Oogonia with mitotic chromosomes (Ch) and oocytes in prophase with finely granular chromatin and chromosomes united by synaptonemal complexes (arrows) (2,400X). Figure 13 Synaptonemal complex (33,600X). N = nucleus. Figure 14 Narrow cytoplasm in oogonia (Oo) androunded nucleus. Oocyte (Oc) with wide cytoplasm and adhesion via desmosomes (D) (2,050X).
Figure 14 in The phyllophorid sea cucumbers of southern Australia (Echinodermata: Holothuroidea: Dendrochirotida: Phyllophoridae)
Figure 14. SEM images of ossicles from holotype of Massinium melanieae O'Loughlin sp. nov. (NMV F174897). Regular tables from peri-oral body wall (top left); mid-body tube foot endplate (top right); large irregular table from anal region (central right); thin rods from tentacle branches (bottom right).
Figure 14 in A review of Australian fossil penguins (Aves: Sphenisciformes)
Figure 14.?Pseudaptenodytes minor holotype partial right humerus, NMV P26669: A, dorsal view; B, ventral view.
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