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Fig. 14 in Palaeobiogeographic and evolutionary meaning of an early Late Tournaisian ammonoid fauna from the Tafilalt of Morocco
Fig. 14. Whorl width/ conch diameter and umbilical width/ conch diameter ratios of Irinoceras minutum sp. nov.
Fig. 14 in The lanternflies from Andaman and Nicobar: one new Pyrops species, new records and illustrated key to the species (Hemiptera: Fulgoromorpha: Fulgoridae)
Fig. 14. Pyrops rogersi (Distant, 1906), male genitalia. A, pygofer, anal tube and gonostylus, left lateral view. B, pygofer and gonostyli, posteroventral view. C, anal tube and pygofer, dorsal view. An: anal tube; G: gonostylus; Py: pygofer.
Fig. 14 in The new stick insect genus Medauromorpha gen. nov. with one new species from Vietnam and notes on Medauroidea Zompro, 2000 (Phasmida: Phasmatidae: Clitumninae)
Fig. 14. Medauromorpha regina (Brunner von Wattenwyl, 1907) comb. nov., captive reared (B. Kneubühler) from Tay Yen Tu N.R. (photographs by B. Kneubühler). A–G, ♂. A, lateral view. B, dorsal view. C, ventral view with typical black marking. D, head and pronotum, lateral view. E, terminalia, dorsal view. F, terminalia, lateral view. G, terminalia, ventral view. — H–Q, ♀. H, lateral view. I, dorsal view. J, dorsal view K, lateral view. L, ventral view with typical black marking. M, lobes on metafemora. N, head and pronotum, lateral view. O, terminalia, dorsal view. P, terminalia, lateral view. Q. terminalia, ventral view. — R–T, ♀ nymph. R, dorsal view. S, dorsal view. T, head and thorax, dorsal view.
Fig. 14 in Two new stick insect genera from Vietnam, Nuichua gen. nov. and Pterohirasea gen. nov. with two new species (Phasmida: Diapheromeridae: Necrosciinae)
Fig. 14. Pterohirasea nigrolineata sp. nov., wild specimens and habitat in Bach Ma N.P. (photographs A–G by J. Constant, H by H.T. Pham). A–C, ♂, 12.VII.2011. D–F, ♀, 17.VII.2011. G, subadult nymph, 12.VII.2011. H, habitat in Bach Ma N.P, 12.VII.2011.
Fig. 14 in New Species, Combinations, and Records of Jumping Spiders in the Galápagos Islands (Araneae: Salticidae)
Fig. 14. Nycerella vestita comb. nov. Male: A. palp ventral, B. palp dorsal, C. palp retrolateral, D. face, E. dorsal. Female: F. dorsal, G. ventral, H. epigyne dorsal cleared, I. epigyne ventral cleared, J. epigyne ventral.
Fig. 14 in Polydictya lanternflies of the Indochinese region: Six new species and identification key (Hemiptera: Fulgoromorpha: Fulgoridae)
Fig. 14. Polydictya thompsoni sp. nov., A–B, in nature, Thailand, Kaeng Krachan N.P., 10.XI.2017. B, trophobiotic interaction with Camponotus sp. (Formicidae) (photographs © P. Thompson).
Figure 14 in Tokorhabditis tauri n. sp. and T. atripennis n. sp. (Rhabditida: Rhabditidae), isolated from Onthophagus dung beetles (Coleoptera: Scarabaeidae) from the Eastern USA and Japan
Figure 14: Scanning electron micrograph of the male tail of TOKOrhabditiS atripenniS n. sp. Genital papillae are labeled with the prefix "P"; suffix "d" indicates papillae that open dorsally or laterally.
Fig. 14. Helcionellid mollusc Mellopegma uslonicum Parkhaev, 2004 in An early Cambrian fauna of skeletal fossils from the Emyaksin Formation, northern Siberia
Fig. 14. Helcionellid mollusc Mellopegma uslonicum Parkhaev, 2004 internal moulds from lower Cambrian Emyaksin Formation, Bol'shaya Kuonamka River, Anabar Uplift, Siberia; sample B-247 (A), sample 7/70 (B–D). A. SMNH Mo 167672; lateral (A1), sub-apical (A2), and upper (A3) views. B. SMNH Mo 167671; sub-apical (B1), lateral (B2), and upper (B3) views. C. SMNH Mo 160410; lateral (C1), upper (C2), and sub-apical (C3) views. D. SMNH Mo 167612; lateral view. Scale bar 600 μm, except D, 300 μm.
Fig. 14 in The Hirnantian (Late Ordovician) brachiopod fauna of the East Baltic: Taxonomy of the key species
Fig. 14. Trigonorhynchiid brachiopod Plectothyrella crassicostis (Dalman, 1828) from the Kuldiga Formation of the Porkuni Regional Stage, Hirnantian ( Upper Ordovician), East Baltic, western Latvia. A. Ventral valve, LDM G 328-15, Blīdene-5, depth 816.6 m, exterior view (A1), interior view (A2) and the detail of the posterior part of the same (A3). B. Incomplete dorsal valve, GIT 542-16, Riekstini-15, 854.8 m, dorsal interior (B1), posterior (B2), and posteriorly tilted (B3) views of cruralium. C. Ventral valve, LDM G 328-149, Mežmali-16, depth 914.9 m, view of pedicle opening. D. Shell, LDM G 328-135, Ēdole-61, 848.1 m, lateral (D1) and dorsal (D2) views. E. Shells, GIT 542-3/1–3, Adze-6, 838.5 m, posterior views of shells in live position and →
Fig. 14 in A re-evaluation of goniopholidid crocodylomorph material from Central Asia: Biogeographic and phylogenetic implications
Fig. 14. Strict consensus of 34 trees. Length = 2219, CI = 0.2881, RI – 0.7500. 100 taxa are included. Goniopholididae are monophyletic, with Calsoyasuchus the most basal form. Goniopholis forms a paraphyletic group with respect to Anteophthalmosuchus. Sunosuchus is polyphyletic, spread among several groups including Eutretauranosuchus, Kansajsuchus, and the European goniopholidids. All European goniopholidids form a monophyletic group to the exclusion of the Asian and North American forms. Tomistoma and Gavialis cluster together to the exclusion of Alligator.
Fig. 14 in Cenomanian-Campanian (Late Cretaceous) mid-palaeolatitude sharks of Cretalamna appendiculata type
Fig. 14. Otodontid shark Cretalamna hattini sp. nov., holotype, LACM 128126; anteriormost preserved centrum equals one (designations follow Shimada 2007), latest Santonian or earliest Campanian (Late Cretaceous); upper Smoky Hill Chalk, Niobrara Formation, Logan County, Kansas, USA. A. Partial vertebral column and left palatoquadrate. B. Centra 17–21 in dorsal view. C. Centra 25–31 in lateral view. D. Detail of centra 9–13 viewed in various angles. Abbreviation: v, vertebral centrum.
Fig. 14 in Late Viséan pelagic chondrichthyans from northern Europe
Fig. 14. Chondrichthyan teeth from the upper Viséan of Todowa Grząba, north of Ostrówka Quarry, Gałęzice Region, Holy Cross Mountains, Poland. A. Euselachii indet. 2, MWGUW/Ps/11/21, in lateral (A1), labial (A2), lingual (A3), and oral (A4) views. B. Euselachii indet. 1, MWGUW/Ps/11/22, in labial (B1) and lingual (B2) views. C. Bransonella nebraskensis (Johnson, 1984), ZPAL P.IV/215, in lateral (C1) and labial/aboral (C2) views. D. Orodont-like crushing tooth, ZPAL P.IV/233, in oral/lingual view. E. Denaea sp., large tooth, MWGUW/Ps/11/23, in labial view.
Fig. 14 in The appendicular skeleton of Neuquensaurus, a Late Cretaceous saltasaurine sauropod from Patagonia, Argentina
Fig. 14. The saltasaurine sauropod Neuquensaurus, from the Anacleto Formation (Upper Cretaceous), Patagonia, Argentina. Metatarsals. A. Right metatarsal I of Neuquensaurus robustus (Huene, 1929) nomen dubium (MLP−CS 1179) in anterior (A1), posterior (A2), lateral (A3), medial (A4), proximal, anterior towards top (A5), and distal, anterior towards top (A6) views. B. Left metatarsal II of N. robustus nomen dubium (MLP−CS 1183) in anterior (B1), posterior (B2), lateral (B3), medial (B4), proximal, anterior towards top (B5), and distal, anterior towards top (B6) views. C. Left? metatarsal III of Neuquensaurus australis (Lydekker, 1893) (MLP−CS 1191) in anterior (C1), posterior (C2), medial (C3), lateral (C4), proximal, anterior towards top (C5), and distal, anterior towards top (C6) views. D. Right? metatarsal IV? of N. australis (MLP−CS 1193) in anterior (D1), posterior (D2), lateral (D3), medial (D4), proximal, anterior towards top (D5). E. Left metatarsal V of N. australis (MLP−CS 1180) in medial (E1), lateral (E2), and proximal, anterior towards top (E3). F. Pedal phalanx in anterior (F1), posterior (F2), lateral (F3), medial (F4), proximal, anterior towards top (F5), and distal, anterior towards top (F6) views. G. Pedal phalanx in anterior (G1), posterior (G2), lateral? (G3), medial? (G4), proximal, anterior towards top (G5), and distal, anterior towards top (G6) views.
Fig. 14 in The soft-tissue attachment scars in Late Jurassic ammonites from Central Russia
Fig. 14. Reconstruction of two Late Volgian ammonites from Craspeditidae family, Kachpurites fulgens (Trautschold, 1861) (A), Garniericeras catenulatum (Fischer, 1830) (B). Ten arms are shown because Nautilus and representatives of Coleoidea exhibit five arm pairs in embryos, it can be a base number of arms in Cephalopoda (Kröger et al. 2011). Two long tentacles are very speculative. However, such tentacles for external-shelled cephalopods could be very useful for catching pray which is at a distance; since rapid jumping forward could be difficult for these mollusks. The large hyponome was shown because of the presence of a funnel-locking apparatus and hyponomic retractors, and also due to the shape of aperture edges with lateral apertural sinuses and the presence of a large round opening between lappets in some ammonites (Westermann 1990: fig. 2). The eyes were drawn similar to coleoid eyes because Ammonoidea and Coleoidea were sister taxons (Jacobs and Landman 1993). The dark transverse bands on the shells correspond to the most common ammonites' color pattern (Keupp 2000). The presence of such a color pattern in the Craspeditidae family is confirmed by findings of shells with transverse dark bands (AAM unpublished material). This picture, drawn by Andrey Atuchin, was based on the sketch of the author of this article.
Fig. 14 in The oldest and youngest records of afrosoricid placentals from the Fayum Depression of northern Egypt
Fig. 14. Implied ghost lineages and maximum likelihood reconstructions of M2 metacone size (treated as an ordered character with four states), given one of the topologies (Fig. 12A) recovered by parsimony analysis of morphological data. Here the topology is plotted against time, with major divergences among clades with extant representatives based on the molecular estimates of Douady et al. (2003) for Macroscelidea, Poux et al. (2008) for Tenrecoidea, and Gilbert et al. (2006) for the origin of crown Chrysochloroidea. The depth of the Potamogale–Micropotamogale divergence has not been estimated using molecular data, and is here arbitrarily placed at half the time depth of Potamogalidae. An origin of crown Afrotheria at ~80 Ma is supported by various studies (e.g., Springer et al. 2003). Although parsimony reconstructs metacone loss as homologous in tenrecs and golden moles, note that when branch lengths are taken into account for maximum likelihood reconstructions ("MLR", computed in Mesquite v. 2.72; Maddison and Maddison 2005), the common ancestors of crown Afrosoricida and crown Tenrecoidea are reconstructed as having had a reduced but distinct M2 metacone, the former with high proportional likelihood (0.779). These data, combined with the numerous zalambdomorph Paleogene ghost lineages that are required by the parsimony−based topology, arguably call into question the likelihood of the topology itself.
Fig. 14 in Ecophenotypic plasticity versus evolutionary trends-morphological variability in Upper Jurassic bivalve shells from Portugal
Fig. 14. Lithostratigraphy plot of Eomiodon securiformis. A. Lithostratigraphically arranged groups are displayed as convex hulls. Calculated artificial shell outlines for full number coordinate pairs are plotted to illustrate the morphospace. M, mean artificial shell outline. B. 95% confidence ellipses of group means and corresponding calculated shell outlines for group means are plotted. Numbers in squared brackets refer to Fig. 2.
Fig. 14 in Mammalian distal humeri from the Late Cretaceous of Uzbekistan
Fig. 14. Left distal humerus of zhelestid group 4 (URBAC 03−126, Bissekty Formation, Upper Cretaceous: Turonian, Kyzylkum Desert, Uzbekistan), in anterior (A), distal (B), and posterior (C) views.
Fig. 14 in Devonian pearls and ammonoid-endoparasite co-evolution
Fig. 14. Relation between the estimated amount of pits per half whorl and the ratio between pit size and phragmocone diameter.
Fig. 14 in Silicified Mississippian brachiopods from Muhua, southern China: Rhynchonellides, athyridides, spiriferides, spiriferinides, and terebratulides
Fig. 14. Athyridoid brachiopod Actinoconchus sp. from the Tornaisian Muhua Formation, southern China. A. Complete shell, PKUM02−0436, in dorsal (A1), ventral (A2), lateral (A3), and anterior (A4) views. B. Shell, PKUM02−0437, in dorsal (B1), ventral (B2), and anterior (B3) views. C. Ventral valve, PKUM02−0438, viewed from exterior (C1), and interior (C2). D. Dorsal valve, PKUM02−0439, in exterior (D1), interior (D2), and lateral (D3) views, and enlargement of the external lamellose ornamentation (D4). E. Incomplete ventral valve, PKUM02−0440, viewed internally (E1) and enlargement showing dental plates and muscle scars (E2). F. Umbonal region of a broken shell, PKUM02−0441, showing dental plates and cardinalia (dorsal valve below). G. Exterior of ventral valve, PKUM02−0442, showing well preserved long growth lamellae. All from sample MH1.
Fig. 14. A in Revision of the flexible crinoid genus Ammonicrinus and a new hypothesis on its life mode
Fig. 14. A. Schematic reconstruction of Ammonicrinus (strongly modified after Piotrowski 1977: 209, fig. 3) of a feeding Ammonicrinus within low−intensity current water. Alternating water pressure was possibly generated in the interior of the enrolled proximal stem by slow, bellow−like partial opening and closing (red arrows) of the base of the central mass; due to the synarthrial (bifacial) articulation of the ammonicrinid mesistele that developed two huge ligamentary facets (orange), separated by the fulcrum, bellow−like partial opening could possibly enabled by stiffening of the outer ligaments (see orange bars in A1); closing could be controlled by stiffening of the inner ligaments (see orange bars in A2). A1, suction during opening may result from low−pressure (P−) and create an ingesting water flow (blue arrow); A, ejection during closure (red arrow) resulted from overpressure (P+); to minimise faecal recycling, 2 the water ejection may have occurred laterally (blue arrows), feasibly at both lateral centres, which have "openings". B. Lobe−like enlarged appendages (framed in red) could possibly support the lateral water faecal−ejection (modified from Ubaghs 1952: pl. 1: 4). C. Reconstruction of a feeding "encased runner−type" of A. leunisseni sp. nov., attached to a tabulate coral (model); the spined specimen dwelled enrolled on the muddy seafloor; alternating water pressure was obviously generated in the interior of the enrolled proximal stem globe by non−muscular, probably MCT−controlled, slow, bellow−like partial opening and closing of the oblate sphere at its bottom (dashed arrow); suction during opening created an ingesting water flow (see arrow on the left), which was funnelled in a "canal", formed by the unspined interior of the columnals of the mesistele, whose U−shaped LCEE additionally formed a protection against immersive sediment; ejection during closure resulted from overpressure; to minimise faecal recycling, the water ejection occurred supposably laterally, feasibly at both lateral centres, which accordingly show "openings" (see arrows on the right). Not to scale.
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