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Fig. 19 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 19. Athyridide brachiopods from the Silurian–Devonian boundary beds at Dnistrove (Podolia, Ukraine). A–C. Dayia bohemica Bouček, 1941; three shells, ZPAL Bp. 56/200 (A), ZPAL Bp. 56/201 (B), and ZPAL Bp. 56/202 (C), in dorsal (A1, B1, C1), ventral (A2, B2, C2), lateral (A3, B3, C3), posterior (A4, B4, C4), and anterior (A5, B5, C5) views. D–F, J. Dnestrina gutta Nikiforova and Modzalevskaya, 1968. D, E. Two shells, ZPAL Bp. 56/208 (D) and ZPAL Bp. 56/209 (E), in dorsal (D1, E1), ventral (D2, E2), lateral (D3, E3), posterior (D4, E4), and anterior (D5, E5) views. F. Interior view of slightly damaged ventral valve, ZPAL Bp. 56/210. J. Shell ZPAL Bp. 56/207b in dorsal exterior view. G, H. Pseudoprotathyris infantilis (Kozłowski, 1929); two shells, ZPAL Bp. 56/176 (G) and ZPAL Bp. 56/177 (H), in dorsal (G1, H1), ventral (G2, H2), lateral (G3, H3), posterior (G4, H4), and anterior (G5, H5) views. I. Camarium sp.; shell ZPAL Bp. 56/29 in dorsal (I1), ventral (I2), lateral (I3), posterior (I4), and anterior (I5) views. Beds −24 (A–C), −21 (D–F, J), −4 (G, H), and 47–48 (I). Scale bars 2 mm.
Fig. 9 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 9. Scatter diagram of shell width, thickness, and length of tongue to shell length ratios in Clorinda pseudolinguifera Kozłowski, 1929. Dnistrove, beds 47–48.
Fig. 5 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 5. Strophomenide Plectodonta (Plectodonta) mariae pantherae subsp. nov. (A–J, M–O) and chonetoid Chlupacina sp. (K, L) from the Silurian–Devonian boundary beds at Dnistrove (Podolia, Ukraine). A. Holotype ZPAL Bp. 56/99 in dorsal (A1), ventral (A2), lateral (A3), posterior (A4), and anterior (A5) views, and ventral view of an uncoated shell (A6) to show colour pattern. B. Complete shell ZPAL Bp. 56/108 in dorsal (B1), ventral (B2), lateral (B3), posterior (B4), and anterior (B5) views. C, F, G, I. Four specimens, ZPAL Bp. 56/102 (C), ZPAL Bp. 56/93 (F), ZPAL Bp. 56/103 (G), and ZPAL Bp. 56/104 (I), in ventral exterior view. D. Ventral valve ZPAL Bp. 56/94 in exterior (D1; same as Baliński 2010: fig. 1C2), lateral (D2), and posterior (D3) views. E. Slightly incomplete ventral valve ZPAL Bp. 56/106 in interior view. H, J, N. Three dorsal valves, ZPAL Bp. 56/107 (H), ZPAL Bp. 56/98 (J), and ZPAL Bp. 56/95 (N), in exterior view (N, same as Baliński 2010: fig. 1D2). M. Interior of dorsal valve ZPAL Bp. 56/105 in general (M1) and oblique lateral (M2) views. O. Ventral valve ZPAL Bp. 56/91 in external view showing well preserved ornamentation; two other small shells in dorsal view visible near upper left and lower right corner of the photograph. P. Large ventral valve ZPAL Bp. 56/101 in exterior view. K, L. Chlupacina sp. K. Shell ZPAL Bp. 56/151 in ventral exterior view. L. Slightly damaged shell ZPAL Bp. 56/152 in ventral view. Beds 47–48.
Fig. 18 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 18. Transverse serial sections through shell of Camarium sp. Numbers refer to distance in mm from ventral umbo. ZPAL Bp. 56/71a. Dnistrove, beds 47–48.
Fig. 4 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 4. Strophomenide brachiopods from the Silurian–Devonian boundary beds at Dnistrove (Podolia, Ukraine). A–J, L. Leptaena (Leptaena) aff. altera Rybnikova, 1966. A, B. Two nearly complete shells, ZPAL Bp. 56/42 (A) and ZPAL Bp. 56/43 (B), in dorsal (A1, B1), ventral (A2, B2), lateral (A3, B3), posterior (A4, B4), and anterior (A5, B5) views. C. Shell ZPAL Bp. 56/46 in ventral view (C1) and enlargement showing the pedicle tube (C2). D. Enlargement of the posterior region of the ventral valve ZPAL Bp. 56/32d showing interarea, delthyrium, and well preserved teeth. E–G. Enlargement of the posterior region of three shells, ZPAL Bp. 56/32c (E), ZPAL Bp. 56/32b (F), and ZPAL Bp. 56/32a (G); ventral valves uppermost. H. Almost complete shell ZPAL Bp. 56/45 in ventral view. I. Enlargement of the interior of ventral valve ZPAL Bp. 56/32e. J. Ventral valve ZPAL Bp. 56/44 with partially shown interior in general (J1) and enlarged (J2) views. L. Interior of incomplete dorsal valve ZPAL Bp. 56/32f. K, N–O. Cymostrophia (Protocymostrophia) costatula (Barrande, 1847). K. Incomplete shell ZPAL Bp. 56/18 in dorsal (A1) and ventral (A2) views. N. Interior of dorsal valve ZPAL Bp. 56/21. O. Interior of an incomplete ventral valve ZPAL Bp. 56/19. P. Exterior of an incomplete ventral valve ZPAL Bp. 56/20. M.?Mesodouvillina sp.; exterior of ventral valve ZPAL Bp. 56/53. Beds 47–48 (A–L, N–P), 102 (M). Scale bars 2 mm.
Fig. 13 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 13. Transverse serial sections through shell of Oglu senilis Havlíček, 1987. A. ZPAL Bp. 56/88. B. ZPAL Bp. 56/89. Numbers refer to distance in mm from ventral umbo. Dnistrove, beds 47–48.
Fig. 16 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 16. Scatter diagrams of shell width (A) and shell thickness (B) to shell length ratios in Sepatrypa (Septatrypa) secreta Kozłowski, 1929. Dnistrove, beds 47–48.
Fig. 11 in The brachiopod succession through the Silurian-Devonian boundary beds at Dnistrove, Podolia, Ukraine
Fig. 11. Transverse serial sections through three shells of Sphaerirhynchia gibbosa (Nikiforova, 1954). A. ZPAL Bp. 56/64−3. B. ZPAL Bp. 56/64−2. C. ZPAL Bp. 56/64−1. Numbers refer to distance in mm from ventral umbo. Dnistrove, beds 47–48.
Fig. 10. Mimosphinctes rudicostatus Bogoslovsky, 1980, PIMUZ 28595, bed 48 in Devonian pearls and ammonoid-endoparasite co-evolution
Fig. 10. Mimosphinctes rudicostatus Bogoslovsky, 1980, PIMUZ 28595, bed 48, Polygnathus inversus Zone, Dzhaus−beds, early Emsian, Khodzha− Kurgan Gorge, Zerashan Range, Uzbekistan. This individual had suffered from a deep fracture, which had caused an irritation of the mantle. This had the formation of a spiral trace as a consequence.
Field data used in "A field-based estimation of the variability of particle entrainment in coarse-bed rivers"
<p>This file is a companion file to "A field-based estimation of the variability of particle entrainment in coarse-bed rivers ", co-authored by Daniel Vázquez-Tarrío, Estrella Carrero-Carralero, Raúl López, Fanny Ville, Damià Vericat and Ramon J. Batalla .</p> <p>This is a paper published in the <em>Journal of Geophysical Research: Earth Surface</em>, 129 (10) (https://doi.org/10.1029/2024JF007695).</p> <p>This Excel file contains all the raw data used in this research.</p>
Fig. 7 in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 7. Non−chondrichthyan ichthyoliths from the Frasnian–Famennian boundary beds. A. Acanthodian scale, ZPALP.IV/313, from Płucki, sample P−1, Pa. linguiformis Zone, lateral view, × 90. B–E. Specimens from Dębnik, sample 13, Early Pa. triangularis Zone. B. Acanthodian scale, IGPUW/Ps/4/14, basal view, × 80. C. Sarcopterygian Strunius rolandi, parasymphysial tooth, IGPUW/Ps/4/15, lateral view, × 40. D. Actinopterygian scale, IGPUW/Ps/4/16, × 60. E. Osteichthyan jaw fragment, IGPUW/Ps/4/17, × 60. All SEM micrographs.
Fig. 6. Protacrodus vetustus Jaekel, 1921. A in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 6. Protacrodus vetustus Jaekel, 1921. A. Tooth−whorl composed of three teeth, right side incomplete, IGPUW/Ps/1/222, sample Md−I/1, Late Pa. triangularis Zone, occlusal view, × 30. B–D. Large, almost completely preserved tooth, IGPUW/Ps/4/13, sample Ko−SF, Pa. linguiformis Zone, oblique lingual, oblique labial and lingual views, × 17. All SEM micrographs.
Fig. 5 in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 5. Chondrichthyan microremains from Płucki. A, B. Branchial denticles?, IGPUW/Ps/4/10 and IGPUW/Ps/4/11, sample KWK3. C. Stethacanthus resistens sp. nov. tooth, IGPUW/Ps/4/12, sample KWK4, basal−labial view. All × 60. All SEM micrographs.
Fig. 4 in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 4. Chondrichthyan microremains from Dębnik, sample Dz−13, Early Pa. triangularis Zone. A, B. "Ctenacanth−type" scales, IGPUW/Ps/4/4 and IGPUW/Ps/4/5. C–I. Stethacanthus resistens sp. nov. teeth. C, D. Problematic tricuspid tooth, IGPUW/Ps/4/6, labial and occlusal views. E. IGPUW/Ps/4/7, basal view. F. IGPUW/Ps/4/8, occlusal view. G–I. IGPUW/Ps/4/9, occlusal, lingual and labial views respectively. All × 80. All SEM micrographs.
Fig. 3 in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 3. Stethacanthus resistens sp. nov., large tooth, IGPUW/Ps/4/3 from Kowala, sample Ko−SF, Pa. linguiformis Zone, basal (A) and labial (B) views, × 20. All SEM micrographs.
Fig. 2 in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 2. Stethacanthus resistens sp. nov. A, B. IGPUW/Ps/1/215 from Miedzianka, sample M−EZ, Late Pa. triangularis Zone, lingual and occlusal views, × 40. C–F. Holotype, ZPALP.IV/216 from Płucki, sample P−1, Pa. linguiformis Zone, occlusal, labial, lateral and lingual views, × 60. G. IGPUW/Ps/4/1 from Płucki, sample KWK3, Early Pa. triangularis Zone, lingual view, × 40. H. IGPUW/Ps/4/2 from Kowala, sample Kx−12, labial−basal view, × 27. I, J. IGPUW/Ps/1/216 and IGPUW/Ps/1/217 from Psie Górki, sample PG−T, Pa. linguiformis Zone, lingual and basal views, × 32 and × 40 respectively. All SEM micrographs.
Fig. 1. A in Chondrichthyan fauna of the Frasnian-Famennian boundary beds in Poland
Fig. 1. A. Position of the study area (marked with asterisk) against a palaeogeographic reconstruction of the Late Devonian (after Scotese and McKerrow 1990, modified). B. Location of the Holy Cross Mountains (H) and Dębnik area (D) against a contour of Poland. C. Position of sections which yielded latest Frasnian–early Famennian chondrichthyan remains against a geological sketch map of western and central Holy Cross Mountains. J, Jabłonna; K, Kadzielnia; Kw, Kowala; Ł+Pł, Łagów and Płucki; Md, Miedzianka; P, Psie Górki; W, Wietrznia.
Fig. 1. A in Ostracods and fore-reef sedimentology of the Frasnian-Famennian boundary beds in Kielce (Holy Cross Mountains, Poland)
Fig. 1. A. General map of Poland with the location of the Holy Cross Mountains. B. Position of the Psie Górki section at a geological map of the Kielce area (modified after Szulczewski 1971).
Fig. 7. A, B in Ostracods and fore-reef sedimentology of the Frasnian-Famennian boundary beds in Kielce (Holy Cross Mountains, Poland)
Fig. 7. A, B. Microcheilinella frumentaria Lethiers and Casier, 1996. Right lateral and dorsal views of a carapace. PG18. IRScNB n° b3809, × 95. C. Microcheilinella cf. larionovae Polenova, 1955 sensu Lethiers and Casier (1996). Right lateral view of a carapace. PG16. IRScNB n° b3810, × 50. D, E. Microcheilinella sp. nov. A, aff. M. peculiaris Rozhdestvenskaja and Netchaeva in Rozhdestvenskaja (1972). Right lateral and dorsal views of a carapace. PG5. IRScNB n° b3811, × 60. F, G. Acratia evlanensis Egorov, 1953. Right lateral and dorsal views of a carapace. PG33. IRScNB n° b3812, × 70. H, I. Acratia nevadaensis Casier and Lethiers, 1997. H. Right lateral view of a carapace. PG15. IRScNB n° b3813, × 100. I. Dorsal view of a carapace. PG44. IRScNB n° b3814, × 100. J. Acratia gassanovae Egorov, 1953. Right lateral view of a carapace. PG15. IRScNB n° b3815, × 80. K. Acratia sp. A, aff. A. gassanovae Egorov, 1953. Right lateral view of a carapace. PG26. IRScNB n° b3816, × 100. L, M. Acratia cf. zadonica Egorov, 1953. Right lateral and dorsal views of a carapace. PG8. IRScNB n° b3817, × 60. N, O. Acratia cf. ljubzovi Schischkinskaja, 1964. Right lateral and dorsal views of a carapace. PG21. IRScNB n° b3818, × 80.
Fig. 3 in Ostracods and fore-reef sedimentology of the Frasnian-Famennian boundary beds in Kielce (Holy Cross Mountains, Poland)
Fig. 3. Upper Devonian (upper Frasnian to lower Famennian) calcareous beds of the Psie Górki section (Holy Cross Mountains, Poland). Microfacies. A. Microfacies 2b (or MF2b) consists of a fine−grained bioclastic and peloidal packstone. Abundant dasycladaceans algae (center of the picture), ostracods and foraminifers. Thin section PG7. B–D. Microfacies 4c (or MF4c) corresponds to a medium− to coarse grained crinoidal grainstone rich in subrounded microbreccias. The microbreccias are composed of algal mats with irregular thin fenestrae and a few peloids (center of D). The grains are well to poorly sorted and composed mainly of crinoids with few ostracods and molluscs. Micritized grains and peloids are present. Thin sections PG43 (B), PG39 (C) and PG35 (D). E. Microfacies 4a (or MF4a) consists of microconglomeratic floatstones with stromatoporoids fragments. The intraclasts are abundant and consist of subangular millimeter to centimeter−sized packstones and grainstones of microfacies 1 to 3. Thin section PG13. F. Microfacies 4b (or MF4b) is a coarse grainstone−rudstone with rare micritic oolites. The bioclasts are dominated by crinoids and brachiopods, rare dasycladaceans algae, ostracods and foraminifers. Intraclasts are present, and a few are encrusted by small tubular algae (Girvanella?). A small synsedimentary inverse fault is observed in the center of the picture. Graded bedding is present. The grainstone texture is episodically interrupted by thin stromatolitic mudstone laminae (white arrows). Thin section PG27. G, H. Foraminifers from Psie Górki: Eogeinitzina Lipina, 1950 (G) and Nanicella Henbest, 1935 (H). Thin section PG6. A,G, H, scale bars 250 µm; B–F, scale bars 1 cm.
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