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FIG. 6 in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
FIG. 6. — Plastral remains of Testudo (Testudo) cf.kalksburgensis: A-D', from Mokrá-Quarry localities;A-F, Pal.1351A (left epiplastron);A, C, visceral;B, D, ventral;E, F, left lateral; G-I, Pal. 1354 (entoplatron); G, visceral; H, I, ventral; J-L, Pal. 1353 (entoplatron); J, visceral; K, L, ventral; M, N, Pal. 1352 (entoplatron); M, visceral; N, ventral; O-R, Pal. 1351B (hyoplastron);O, P, visceral;Q, R, ventral;S-V, Pal. 1355 (hyoplastron);S, T, visceral;U, V, ventral;W-Z, Pal.1356 (hypoplastron);W, X, visceral;Y, Z, ven- tral;A'-D', Pal. 1360 (xiphiplastron); A', B', visceral; C', D', ventral; E'-H', Pal. 1361 (xiphiplastron);E', F', visceral;G', H', ventral views; I', reconstruction of plastron. Thick lines correspond to scute sulci, dotted lines denote plate sutures, and oblique lines indicate missing plate portions. Abbreviations: Ab, abdominal; An, anal; ent, ento- plastron; epi, epiplastron; hyo, hyoplastron; hyp, hypoplastron; Fe, femoral; Gu, gular; Hu, humeral; Pe, pectoral; xi, xiphiplastron. Scale bars: A-H', 1 cm; I', 2.5 cm.
FIG. 1 in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
FIG. 1. — Approximate geographical position of Mokrá-Quarry (A). Schematic geological map of the Czech Republic (B). Position of the five Mokrá-Quarry localities that have yielded fossil turtle remains (B, C).
FIG. 3 in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
FIG. 3. — Plastral remains of Ptychogaster (Ptychogaster) sp. from Mokrá-Quarry localities: A-F, Pal. 1315 (hypoplastron); A, B, visceral; C, D, ventral; E, F, left lateral; G-L, Pal. 1316 (hypoplastron); G, H, visceral; I, J, ventral; K, L, right lateral; M-R, Pal. 1317 (hypoplastron); M, N, visceral; O, P, ventral; Q, R, right lateral; S-V, Pal. 1318 (xiphiplastron); S, T, visceral; U, V, ventral views; W, reconstruction of plastron. Thick lines indicate to scute sulci, dotted lines denote plate sutures, dashed lines denote completely ligamentous kinesis (between hypoplastra and peripherals and the hinge between hyoplastron and hypoplastron), and oblique lines indicate missing plate portions. Abbreviations: Ab, abdominal; An, anal; ent, entoplastron; epi, epiplastron; hyo, hyoplastron; hyp, hypoplastron; Fe, femoral; Gu, gular; Hu, humeral; Pe, pectoral; xi, xiphiplastron. Scale bars: 1 cm.
nal; E', F', internal, G'-J', Pal. 1341 (peripheral 8); G', H', external; I', J', internal; K'-N', Pal. 1343 (peripheral 9); K', L', external; M', N', internal; O'-R', Pal. 1345 (peripheral 10); O', P', external; Q', R', internal; S'-V', Pal. 1348 (peripheral 11); S', T', external; U', V', internal views; W', reconstruction of carapace Thick lines correspond to scute sulci, dotted lines denote plate sutures, and oblique lines indicate missing plate portions. Abbreviations: Ce, cervical; co, costal; Ma, marginal; ne, neural; nu, nuchal; per, peripheral; Pl, pleural; py, pygal; sp, suprapygal; Spr, supracaudal; Ve, vertebral. Scale bars: A-V', 1 cm; W', 2.5 cm. in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
nal; E', F', internal, G'-J', Pal. 1341 (peripheral 8); G', H', external; I', J', internal; K'-N', Pal. 1343 (peripheral 9); K', L', external; M', N', internal; O'-R', Pal. 1345 (peripheral 10); O', P', external; Q', R', internal; S'-V', Pal. 1348 (peripheral 11); S', T', external; U', V', internal views; W', reconstruction of carapace Thick lines correspond to scute sulci, dotted lines denote plate sutures, and oblique lines indicate missing plate portions. Abbreviations: Ce, cervical; co, costal; Ma, marginal; ne, neural; nu, nuchal; per, peripheral; Pl, pleural; py, pygal; sp, suprapygal; Spr, supracaudal; Ve, vertebral. Scale bars: A-V', 1 cm; W', 2.5 cm.
FIG. 5 in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
FIG. 5. — Carapace remains of Testudo (Testudo) cf. kalksburgensis from Mokrá-Quarry localities: A-D, Pal. 1320 (nuchal); A, B, dorsal; C, D, visceral; E, Pal. 1322 (neural 4) in dorsal; F, Pal. 1323 (neural 6) in dorsal; G, Pal. 1350 (neural 7) in dorsal; H-J, Pal. 1325 (pygal); H, external; I, J, internal; K, L, Pal. 1326 (costal 1) in dorsal; M, N, Pal. 1329 (costal 2) in dorsal; O, P, Pal. 1330 (costal 3) in dorsal; Q, R, Pal. 1331 (costal 6) in dorsal; S-V, Pal. 1333 (peripheral 1); S, T, external; U, V, internal; W-Z, Pal. 1334 (peripheral 2); W, X, external; Y, Z, internal; A', B', Pal. 1338 (peripheral 5) in external; C'-F', Pal. 1340 (peripheral 7); C', D', exter-
sal; W, visceral; X-Z, Pal. 1308 (costal 5); X, Y, dorsal; Z, visceral; A'-C', Pal. 1309 (costal 6); A', B', dorsal; C', visceral; D'-F', Pal. 1310 (costal 8); D', E', dorsal; F', visceral; G'-J', Pal. 1312 (peripheral 1); G', H', dorsal; I', J', visceral; K'-N', Pal. 1313 (peripheral 7); K', L', dorsal; M', N', visceral; O'-R', Pal. 1314 (peripheral 8); O', P', dorsal; Q', R', visceral views; S', reconstruction of carapace. Thick lines indicate to scute sulci, dotted lines sutures and oblique lines denote missing plate portions. Abbreviations: Ce, cervical; co, costal; Ma, marginal; ne, neural; nu, nuchal; per, peripheral; Pl, pleural; py, pygal; sp, suprapygal; Ve, vertebral. Scale bars: 1 cm. in Fossil turtles from the early Miocene localities of Mokrá-Quarry (Burdigalian, MN4), South Moravian Region, Czech Republic
sal; W, visceral; X-Z, Pal. 1308 (costal 5); X, Y, dorsal; Z, visceral; A'-C', Pal. 1309 (costal 6); A', B', dorsal; C', visceral; D'-F', Pal. 1310 (costal 8); D', E', dorsal; F', visceral; G'-J', Pal. 1312 (peripheral 1); G', H', dorsal; I', J', visceral; K'-N', Pal. 1313 (peripheral 7); K', L', dorsal; M', N', visceral; O'-R', Pal. 1314 (peripheral 8); O', P', dorsal; Q', R', visceral views; S', reconstruction of carapace. Thick lines indicate to scute sulci, dotted lines sutures and oblique lines denote missing plate portions. Abbreviations: Ce, cervical; co, costal; Ma, marginal; ne, neural; nu, nuchal; per, peripheral; Pl, pleural; py, pygal; sp, suprapygal; Ve, vertebral. Scale bars: 1 cm.
Fig. 1. A in Terrestrial Vertebrates Of Post-Quarrying Sites In The Donbas Region Of Ukraine
Fig. 1. A digital elevation model (DEM): exemplified for the Amvrosievka quarry site (legend: meters above sea level).
Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor. in The Late Oligocene Macroflora Of Zsámbék, Central Hungary
Text-fig. 2. Moderately dipping Oligocene layers of the Mány Member in the eastern part of the Strázsa Hill quarry, SW of Zsámbék. The claymarl and siltstone layers cover sandstone and conglomerate. The arrow indicates the position of fossiliferous layers. Photo: László Fodor.
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils. in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils.
Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile. in Evidence For Wildfires During Deposition Of The Late Miocene Diatomites Of The Konservat-Lagerstätte Lake Saint-Bauzile (Ardèche, France) - Preliminary Results
Text-fig. 1. a: Map of France showing geographic position of Saint-Bauzile (source: http://d-maps.com/m/europa/france/france/ france09.gif). b: Overview of the active diatomite quarry at the Montagne d'Andance, photograph taken in 2017. c: SEM image of a frustule of pennate diatom (cf. Navicula sp.) from Saint-Bauzile. d) SEM image of frustules forming a colony of centric diatoms (cf. Diatoma sp.) from Saint-Bauzile.
Fig. 1. Geological map and the abandoned Ogrodzieniec quarry. A in Morphological variations and geographic distribution of the rare Middle Jurassic ammonite Oecoptychius refractus
Fig. 1. Geological map and the abandoned Ogrodzieniec quarry. A. Map showing the studied localities in Poland, western France, and Kachchh (western India). B. Map of France showing the position of St.-Laon and Montreuil-Bellay. C. Map of India showing the position of Kachchh. D. Map of Poland showing the the position of Ogrodzieniec. E. Detailed location of Ogrodzieniec quarry (modified after Jain and Mazur 2021). F. Geological map of the Polish Jura Chain showing the location of the studied Ogrodzieniec quarry. G. Aerial view of the Ogrodzieniec quarry; arrow marks the location of the studied section. H. Exposure of the studied section.
Fig. 2 in Redescription of the type specimens for the Late Jurassic rhynchocephalian Opisthias rarus and a new specimen of Theretairus antiquus from Quarry 9, Morrison Formation, Wyoming, USA
Fig. 2. Teeth of rhynchocephalians Opisthias sp. (A–D) and Theretairus antiquus Simpson, 1926 (E) from Quarry 9, Como Bluff, Wyoming, USA, Upper Jurassic. A. USNM 6126, right dentary fragment with a relatively complete coronoid process in labial view. B. USNM 26080, fragment of palatine in?lingual view with four teeth attached. C. USNM 508532, rock matrix with fragments of right maxilla in lingual view (C1), close-up detail (C2), maxillary teeth (C3). D. USNM 7767 and USNM 26086, fragments of a right dentary, in lingual (D1), labial (D2), and occlusal (D3) views, close-up detail of the four distalmost additional teeth (D3), close-up detail of the four distalmost additional teeth in labial (D4) and lingual (D5) views. E. USNM 26088, anterior fragment of a left dentary, in labial (E1), lingual (E2), and occlusal (E3) views.
Fig. 1 in Redescription of the type specimens for the Late Jurassic rhynchocephalian Opisthias rarus and a new specimen of Theretairus antiquus from Quarry 9, Morrison Formation, Wyoming, USA
Fig. 1. Teeth in the type specimens of the rhynchocephalian Opisthias rarus Gilmore, 1909, Quarry 9, Como Bluff, Wyoming, USA, Upper Jurassic. A. USNM 2860 (holotype), nearly complete left dentary, in labial (A1, A4), lingual (A2, A5), and occlusal (A3, A6) views. B. USNM 2858 (paratype), partial left dentary, in labial (B1, B4), lingual (B2, B5), and occlusal (B3, B6) views. C. Fragment of rock matrix belonging to the holotype. D. Holotype when it is superimposed to the rock matrix.
Fig. 5 in Biostratigraphy (Calcareous Nannofossils And Molluscs) Of The Pannonian Deposits From Transylvania, Romania (Guşteriţa Quarry - Sibiu)
Fig. 5 The molluscs species of the Guşteriţa quarry. Scale bar 1cm. a Congeria banatica R. Hoernes, 1875; b Congeria banatica - monospecific assemblage; c Lymnocardium cf. promultistriatum Jekelius, 1944; d-e Paradacna lenzi (R. Hoernes, 1874); f Paradacna syrmiense (R. Hoernes, 1874); g-h Gyraulus tenuistriatus (Gorjanović-Kramberger, 1899); i Gyraulus ponticus (Lörenthey, 1893); j-k Undulotheca halavatsi Gorjanović-Kramberger, 1901.
Fig. 3 in Biostratigraphy (Calcareous Nannofossils And Molluscs) Of The Pannonian Deposits From Transylvania, Romania (Guşteriţa Quarry - Sibiu)
Fig. 3 Calcareous nannofossils from Guşteriţa quarry: a - f Isolithus semenenko Lyulieva, 1989; g - i Isolithus pavelici Ćorić & Vrsaljko; j, k Pontosphaera multipora (Kamptner, 1948 ex Deflandre in Deflandre & Fert, 1954) Roth, 1970; l Helicosphaera carteri (Wallich 1877) Kamptner, 1954; m Helicosphaera wallichii (Lohmann 1902) Okada & McIntyre, 1977; n, o Helicosphaera walbersdorfensis Müller, 1974; p Noelaerhabdus sp.; q Ascidian spicule; r, s Cyclicargolithus floridanus (Roth & Hay, in Hay et al., 1967) Bukry, 1971.; t Calcidiscus leptoporus (Murray & Blackman 1898) Loeblich & Tappan, 1978.
Fig. 4 in Biostratigraphy (Calcareous Nannofossils And Molluscs) Of The Pannonian Deposits From Transylvania, Romania (Guşteriţa Quarry - Sibiu)
Fig. 4 Calcareous nannofossils from Guşteriţa quarry: a Reticulofenestra pseudoumbilicus (Gartner, 1967) Gartner, 1969; b Coccolithus pelagicus (Wallich 1877) Schiller, 1930; c Calcidiscus leptoporus (Murray & Blackman 1898) Loeblich & Tappan, 1978; d Sphenolithus moriformis (Brönnimann & Stradner, 1960) Bramlette & Wilcoxon, 1967; e Sphenolithus heteromorphus Deflandre 1953; f. Rhabdosphaera pannonica Baldi-Beke, 1960; g Calciosolenia murrayi Gran, 1912 and Discoaster variabilis Martini and Bramlette, 1963; h Pannonian calcareous nannofossils assemblages with Isolithus pavelici and I. semenenko; Discoaster cf. variabilis.; i Candona sp. Baird, 1845 right valve; j Candona sp. Baird, 1845 right valve; k fragment of Candona sp.
FIGURE 12 in Pygocephalomorphan crustaceans further emphasise the similarities between the Carboniferous Piesberg quarry in Germany and the Mazon Creek Lagerstätte in North America
FIGURE 12. Time span of the species of Pygocephalomorpha during the Carboniferous of North America, the UK and continental Europe. Abbreviation: Ks, Kasimovian.
FIGURE 11 in Pygocephalomorphan crustaceans further emphasise the similarities between the Carboniferous Piesberg quarry in Germany and the Mazon Creek Lagerstätte in North America
FIGURE 11. Frequency plot of the distribution of ingroups of Eumalacostraca and of its sister-group Phyllocarida, during the Carboniferous (A) of North America, the UK and continental Europe, the Mississippian (B) and the Pennsylvanian (C).
FIGURE 10 in Pygocephalomorphan crustaceans further emphasise the similarities between the Carboniferous Piesberg quarry in Germany and the Mazon Creek Lagerstätte in North America
FIGURE 10. Restoration drawings of the pygocephalmorphan Anthracaris gracilis (Meek and Worthen, 1865) and Pygocephalus cooperi Huxley, 1857. (A–C) A. gracilis. (A) Dorsal aspect. (B) Ventral aspect of putative female, note the pouch on the last thorax segment. (C) Ventral aspect of putative male. (D–F) P. cooperi. (D) Dorsal aspect. (E) Ventral aspect of female with thorax sternites hidden by oostegites. (F) Putative male in ventral aspect.
FIGURE 8 in Pygocephalomorphan crustaceans further emphasise the similarities between the Carboniferous Piesberg quarry in Germany and the Mazon Creek Lagerstätte in North America
FIGURE 8. Restoration drawings of shields of pygocephalmorphans. (A) Specimen 1.587, (B) 1.228 and (C) Pal.590-2 of Anthracaris gracilis (Meek and Worthen, 1865) from the Carboniferous of Germany. (D) Anthracaris gracilis, based on Brooks (1962, pl. 32, fig. 2). (E) Pygocephalus cooperi Huxley, 1857, based on Schram (1979, fig. 39a). (F) Pygocephalus dubius (Prestwich, 1840), based on Schram (1979, fig. 39c).
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