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Fig. 3 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 3. Anterior dorsal vertebrae of juvenile Plateosaurus cf. trossingensis Fraas, 1913 skeleton MSF 15.8B. from the Norian of Frick, Switzerland. A. Centrum of?dorsal vertebra 1, MSF 15.8.2003, in left lateral view. B. Dorsal vertebra 2, MSF 15.8.908 (neural arch) and MSF 15.8.978 (centrum), in left lateral (B1), dorsal (B2), ventral (B3), anterior (B4), and posterior (B5) views. C. Dorsal vertebra 3, MSF 15.8.2004 (neural arch) and MSF 15.8.2005 (centrum), in left lateral (C1), dorsal (C2), ventral (C3), anterior (C4), and posterior (C5) views. D. Dorsal vertebra 4, MSF 15.8.477, in left lateral (D1), dorsal (D2), ventral (D3), anterior (D4), and posterior (D5) views. E. Dorsal vertebra 5, MSF 15.8.2006, in left lateral (E1), dorsal (E2), ventral (E3), anterior (E4), and posterior (E5) views. Centra are only depicted in lateral view. Scale bars 10 mm.
Fig. 13 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 13. Comparative plot of zygapophyseal lengths of Plateosaurus neural arches. Note size difference between large juvenile (MSF 15.8B.) and adult neural arches described by Hofmann and Sander (2014).
Fig. 12 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 12. Pes of juvenile Plateosaurus cf. trossingensis Fraas, 1913 skeleton MSF 15.8B. from the Norian of Frick, Switzerland. A. Left pes, MSF 15.8.2019, in dorsal (A1) and medial (A2) views. B. Distal tarsal III or IV, MSF 15.8.823, in distal view. C. Right metatarsal V, MSF 15.8.826, in dorsal anterior) view.
Fig. 5 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 5. Sacral and caudal vertebrae of juvenile Plateosaurus cf. trossingensis Fraas, 1913 skeleton MSF 15.8B. from the Norian of Frick, Switzerland. A. Sacral neural arch, MSF 15.8.558, in left lateral (A1), dorsal (A2), ventral (A3), anterior (A4), and posterior (A5) views. B. Anterior caudal neural arch, MSF 15.8.889, in left lateral view. C. Mid-caudal neural arch, MSF 15.8.972, in left lateral (C1), anterior (C2), and posterior (C3) views. D. Mid-caudal neural arch, MSF 15.8.476, in left lateral view (note fused transverse process). E. Distal caudal vertebra, MSF 15.8.371 (note closed neurocentral suture), in left lateral view. F. Proximal caudal centrum, MSF 15.8.2008, in lateral view. G. Proximal caudal centrum, MSF 15.8.488, in lateral (G1) and ventral (G2) views. H. Proximal caudal centrum, MSF 15.8.975, in lateral view. I. Mid-caudal centrum, MSF 15.8.1058, in lateral view. Scale bars 10 mm.
Fig. 2 in Postcranial osteology of the first early-stage juvenile skeleton of Plateosaurus trossingensis from the Norian of Frick, Switzerland
Fig. 2. Cervical vertebrae of juvenile Plateosaurus cf. trossingensis Fraas, 1913 skeleton MSF 15.8B. from the Norian of Frick, Switzerland. A. Cervical vertebra 2 (axis), MSF 15.8.2001, in left lateral (A1), dorsal (A2), anterior (A3), posterior (A4), and ventral (A5) views. B. Cervical vertebra 3, MSF 15.8.669 (neural arch) and MSF 15.8.936 (centrum), in left lateral (B1), dorsal (B2), anterior (B3), posterior (B4), and ventral (B5) views, C. Cervical vertebra 4, MSF 15.8.1032 (neural arch) and MSF 15.8.979 (centrum), in left lateral (C1), dorsal (C2), anterior (C3), posterior (C4), and ventral (C5) views. D. Cervical vertebra 6, MSF 15.8.2002 (neural arch) and MSF 15.8.592 (centrum), in left lateral (D1), dorsal (D2), ventral (D3), anterior (D4), and posterior (D5) views. E. Cervical vertebra 9, MSF 15.8.671 (neural arch) and MSF 15.8.905 (centrum), in left lateral (E1), dorsal (E2), ventral (E3), anterior (E4), and posterior (E5) views. F. Cervical vertebra 1 (atlas), MSF 15.8.2000, in?anterior view. Centra are omitted in ventral view to show neural arch. Scale bars 10 mm.
Fig. 1 - A in The Norian Worthenia-like gastropods (Main Dolomite, Upper Triassic): reclassification of the specimens housed at the "Antonio Stoppani" Natural Museum, Italy
Fig. 1 - A) Wortheniella pygmaea (Stoppani) AS 41/43, lateral view, showing the pattern of the growth lines, which curve backwards above and below the nodose adapical carina (corresponding to the selenizone). Songavazzo (BG), Norian, Main Dolomite. B) Wortheniella pygmaea (Stoppani) AS 41/43, latero-basal view, showing the very conspicuous threads on the base. C) Wortheniella pygmaea (Stoppani) AS 41/43, apical view of the early whorls of the spire. D) Wortheniella pygmaea (Stoppani) AS 41/43, lateral view of the early whorls of the spire. E) Wortheniella pygmaea (Stoppani) AS 41/43a, lateral view. F) Wortheniella pygmaea (Stoppani) AS 41/43a, latero-basal view, showing the region of the umbilicus, which is largely occupied by a columellar lip.
Fig. 3 in Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece
Fig. 3 Diplopora obliqusipora nov. sp. (Holotype). The magnification from Fig. 5c shows the relics of metaspondyle arrangement of the tufts (large arrows, also the cross sections of the laterals at the base of the thallus indicate the metaspondyle arrangement of the laterals). Small arrows indicate the tufts arising from the common base. The thin wall around the axial cavity is clearly recognizable.
Fig. 4 a in Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece
Fig. 4 a to n Probolocupsis sarmeikensis nov. sp. from the reef carbonates near the town of Sarmeika, Peloponnes, Greece. a Cross section exhibiting the narrow axial cavity and the thick thallus wall. Laterals appear as white points in section through them. G058, x10. b Cross section through two poorly preserved specimens. G058, x8. c Oblique longitudinal section through an incomplete? specimen exhibits the laterals, which are oriented perpendicular to the axial cavity. G05C, x16. d Cross section of a specimen exhibiting the partly recrystallized laterals of the thallus. G05A, x16. e Cross section through an apparently poorly preserved specimen. Laterals appear as white points in section through them. G058, x16. f Cross section through an incomplete specimen. G050, x8. g Sections through a complete and an incomplete specimen. Laterals appear as white points around the incomplete specimen. G05B, x16. h Cross sections through two specimens. G05C, x12. i Cross section through a relatively well preserved specimen. G05C, x16. j Oblique section similar to Fig. i. G05C, x10. k Cross section exhibiting the pores (arrows) in the laterals. G05B, x16. l Longitudinal section through the holotype (for magnification see Fig. 2) and cross sections through two paratypes. G05C, x6. m Cross section through a recrystallized specimen. Arrows indicate the pores within the laterals. G05B, x16. n Cross section through a strongly recrystallized specimen causing the disappearance of the axial cavity. G025, x16.
Fig. 5 in Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece
Fig. 5 Diplopora obliguspora nov. sp. (a to d) and Probolocuspis tenuiparia nov. sp. (e to l) from the Norian-Rhaetian reef carbonates of Sarmeika, Peloponnes, Greece. a Specimen exhibits the thin wall around the axial cavity and the spine-like extended laterals. Thin section G1, x32. b Similar section as Fig. a showing the common base of oblique orientation of individual laterals. Thin section G89, x12. c (Holotype). Longitudinal section exhibiting the metaspondyle arrangement of the laterals, tuft of laterals and the thin wall around the axial cavity (for more information see Fig. 3). Thin section G75, x8. d Two cross sections exhibiting the spine-like extended individual laterals. G12, x20. e Cross sections through several specimens with thin thallus wall. Thin section G012, x20. f Sections through three specimens with relatively thick thallus wall but the individual laterals are recognizable. Thin section G08a, x25. g Oblique to longitudinal section. Thin section G08a, x20. h Holotype. The oblique section shows the individual laterals at the base. Thin section G08a, x20. i Sections through four specimens showing the laterals in part. Thin section G08a, x20. j Sections similar to Fig. i. Thin section G08a, x20. k Cross sections clearly showing the spine-like extended laterals. Thin section G08a, x40. l Similar to k. Thin section G40/1, x12.
Fig. 2 in Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece
Fig. 2 Probolocupsis sarmeikensis nov. sp. (Holotype). The magnification from Fig. 4l shows the spine-like extended individual laterals (some of the internal pores: see arrows). Laterals are perpendicular to the thallus axis.
Fig. 1 in Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece
Fig. 1 Geographic position of the Norian-Rhaetian reef locality north of the town of Sarmeika, Peloponnes, Greece.
Fig. 9 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 9. Traversodontidae indet. (cf. Exaeretodon sp.) from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul Brazil; MCN-PV 10205, isolated left lower incisor 1 in lingual (A) and distal (B) views.
Fig. 8. A in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 8. A. Probainognathian cynodonts from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio grande do Sul, Brazil; isolated left lower postcanine tooth (MCN-PV 10204) originally interpreted as belonging to Riograndia, in labial (A1) and lingual (A2) views. B, C. Riograndia guaibensis Bonaparte, Ferigolo, and Ribeiro, 2001 from the Riograndia Assemblage Zone, Linha São Luiz site, Late Triassic Caturrita Formation, Faxinal do Soturno, Rio grande do Sul, Brazil; anterior postcanines of UFRGS-PV-833-T in lingual view (B) and UFRGS-PV-1319-T in labial view (C). D, E. Riograndia guaibensis from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio grande do Sul, Brazil, originally referred to Brasilitherium riograndensis; isolated right lower postcanines of MCN-PV 10102 (D) and MCN-PV 10103 (E), in labial (D1, E1) and lingual (D2, E2) views. F. Brasilodon quadrangularis Bonaparte, Martinelli, Schultz, and Rubert, 2003 from the Riograndia Assemblage Zone, Late Triassic Caturrita Formation, Faxinal do Soturno, Rio grande do Sul, Brazil, UFRGS-PV-603-T (inverted), detail of middle and posterior left lower postcanines, in labial (F1) and lingual (F2) views. Abbreviations: 4o, fourth cusp; 8o, eighth cusp; a–d, names of lower cusps; (e), cusp e; g, lower cusp g; cr, constriction; pc1, pc4, postcanine tooth 1 and 4.
Fig. 2 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 2. Right ectopterygoid of a sauropodomorph from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul, Brazil; MCN PV 10049 in dorsal (A) and ventral (B) views. Arrows point to cranial.
Fig. 7 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 7. Distal end of metatarsal I of a sauropodomorph from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul, Brazil; MCN PV 10049 in cranial (A), lateral (B), caudal (C), mediodistal (D), and distal (E) views.
Fig. 5 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 5. Left femur of a sauropodomorph from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul, Brazil; MCN PV10008 in medial (A), cranial (B), lateral (C), and caudal (D) views. The head fragment in articulation with the rest of the bone in craniolateral (E) and caudomedial (F) views. Abbreviation: M., muscle.
Fig. 10 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 10. Strict consensus tree of 2052 MPTs found in the analysis of the data matrix of Bronzati et al. (2018), showing the phylogenetic relationships of MCN PV sauropodomorph among Triassic sauropodomorphs and other dinosauromorphs.
Fig. 3 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 3. Cervical vertebra of a sauropodomorph from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul, Brazil; MCN PV 10027 in dorsal (A), caudal (B), right lateral (C), ventral (D), cranial (E), and left lateral (F) views. The zoomed area in A shows the epipophyseal-prezygapophyseal lamina. Arrows point to cranial.
Fig. 4 in New sauropodomorph and cynodont remains from the Late Triassic Sacisaurus site in southern Brazil and its stratigraphic position in the Norian Caturrita Formation
Fig. 4. Right ilium of a sauropodomorph from Sacisaurus site, Late Triassic Caturrita Formation, Agudo, Rio Grande do Sul, Brazil; MCN PV10026 in lateral (A), medial (B), dorsal (C), and ventrocaudal (D) views. Arrows point to cranial.
Fig. 5 in A new genus of Norian involutinid foraminifers: Its morphological, biostratigraphic, and evolutionary significance
Fig. 5. Involutinid foraminifer Aulosina oberhauseri (Koehn−Zaninetti and Brönnimann, 1968), Black Marble Quarry (upper Carnian?–lower–middle? Norian). A, B. Tangential sections, MHNG 2011−1−440w (A) and MHNG 2011−1−341c (B). Note the absence of transversely sectioned inner−pillars. C–F. Lamellae interfingering in the umbilical region (white arrowheads). C. MHNG 2011−1−440x, sub−axial; centred section. D. MHNG 2011−1−391a, thin +
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