Find research datasets worth reusing

opencc-by-4.0Oct 2014View details →

Text-fig. 3. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Chodba naděje in Za Hájovnou Cave (Moravia, the Czech Republic). a – gnawed lumbar vertebra with a bite mark on the body head; b – fragment of pelvis with a bite mark; c – femur head with a bite mark; d – Mc II dext. with a pathological phenomenon on the metapodial proximal part (tuberosity/exostosis?). in Basic Population And Taphonomic Analysis Of Bear Assemblages From Za Hájovnou Cave (Moravia, The Czech Republic): A Fossil Record From 1987-2007

Text-fig. 3. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Chodba naděje in Za Hájovnou Cave (Moravia, the Czech Republic). a – gnawed lumbar vertebra with a bite mark on the body head; b – fragment of pelvis with a bite mark; c – femur head with a bite mark; d – Mc II dext. with a pathological phenomenon on the metapodial proximal part (tuberosity/exostosis?).

opencc-by-4.0Nov 2011View details →

Text-fig. 1. A. Preserved part of Kučlín specimen No. Pa 24 (foto B. Ekrt); B. For comparison, a corresponding part of a Paleogene ungulate of the genus Phenacodus (Gregory 1951, modified). Abbreviations: il – ilium, Lu – lumbar vertebrae, Th – thoracic vertebrae. in Mammal Discovery In Kučlín Diatomite

Text-fig. 1. A. Preserved part of Kučlín specimen No. Pa 24 (foto B. Ekrt); B. For comparison, a corresponding part of a Paleogene ungulate of the genus Phenacodus (Gregory 1951, modified). Abbreviations: il – ilium, Lu – lumbar vertebrae, Th – thoracic vertebrae.

Text-fig. 10. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 26. Lateral plates on undersurface of arm segment in Hunsrück Slate articulated specimen. Short thin groove spines on ventral edge of lateral arm plates protect undersurface of vertebra and partially cover ambulacral groove. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)

Text-fig. 10. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 26. Lateral plates on undersurface of arm segment in Hunsrück Slate articulated specimen. Short thin groove spines on ventral edge of lateral arm plates protect undersurface of vertebra and partially cover ambulacral groove.

Text-fig. 11. Eospondylus cf. primigenius (STÜRTZ) "Prastav" quarry at Praha-Holyně, Třebotov Limestone, Lower Devonian, Dalejan, NM L 36905, x 65. Overlay of proximal and distal articulations. Upper photo is proximal surface with distal bird-like articulation knobs superposed in ink. Lower photo is distal surface with proximal articulation knobs superposed in ink. The architecture of articulation surfaces is both zygospondylous and auluroid. This architecture occurs also in vertebrae of Furcaster and indicates that families Eospondylidae and Furcasteridae are closely related. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)

Text-fig. 11. Eospondylus cf. primigenius (STÜRTZ) "Prastav" quarry at Praha-Holyně, Třebotov Limestone, Lower Devonian, Dalejan, NM L 36905, x 65. Overlay of proximal and distal articulations. Upper photo is proximal surface with distal bird-like articulation knobs superposed in ink. Lower photo is distal surface with proximal articulation knobs superposed in ink. The architecture of articulation surfaces is both zygospondylous and auluroid. This architecture occurs also in vertebrae of Furcaster and indicates that families Eospondylidae and Furcasteridae are closely related.

Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)

Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra.

Text-fig. 6. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 12.5. Undersurface of arm segments in Hunsrück Slate articulated specimen. A few lateral plates are displaced and expose details of vertebrae. The canal for radial water vessel is in center of zygosphene knob and zygotreme pit, like spout and funnel. At distal outer edges of vertebrae is cupola for tube feet. There are no under arm plates. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)

Text-fig. 6. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, NM S 4766, x 12.5. Undersurface of arm segments in Hunsrück Slate articulated specimen. A few lateral plates are displaced and expose details of vertebrae. The canal for radial water vessel is in center of zygosphene knob and zygotreme pit, like spout and funnel. At distal outer edges of vertebrae is cupola for tube feet. There are no under arm plates.

Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass]. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)

Text-fig. 2. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate,, NM S 4764, x 3. Specimen with ventral arm coiling. The specimen is on its dorsum in slate with all five rays curled ventrally inward toward mouth area on underside of disk. Barely visible are tips of two jaws; slightly exposed are proximal parts of rays in oral view extending outward from disk. The location of abrupt ventral bending of rays is indicated by emergence from slate of five rays in aboral view that point inward toward buried disk. Based on ventral bending of rays and intimate association with crinoids Eospondylus has been interpreted as stratigraphic first occurrence of Order Euryalida, which contains epizoic gorgonocephalid and euryalid basket-stars of modern oceans. This status is rejected using new evidence from isolated vertebrae. [Photo by Alexander Glass].

Fig. 7 in Osteology of the dorsal vertebrae of the giant titanosaurian sauropod dinosaur Dreadnoughtus schrani from the Late Cretaceous of Argentina

Fig. 7. Partial neural arch of titanosaurian sauropod Dreadnoughtus schrani Lacovara, Lamanna, Ibiricu, Poole, Schroeter, Ullmann, Voegele, Boles, Carter, Fowler, Egerton, Moyer, Coughenour, Schein, Harris, Martínez, and Novas, 2014 (MPM-PV 1156?-7), from Santa Cruz Province, Argentina; middle–late Campanian to early Maastrichtian; in left lateral (A) and posterior (B) views.

Fig. 3 in Osteology of the dorsal vertebrae of the giant titanosaurian sauropod dinosaur Dreadnoughtus schrani from the Late Cretaceous of Argentina

Fig. 3. Nearly complete dorsal vertebrae of titanosaurian sauropod Dreadnoughtus schrani Lacovara, Lamanna, Ibiricu, Poole, Schroeter, Ullmann, Voegele, Boles, Carter, Fowler, Egerton, Moyer, Coughenour, Schein, Harris, Martínez, and Novas, 2014, from Santa Cruz Province, Argentina; middle–late Campanian to early Maastrichtian; in posterior view. A. MPM-PV 1156?-4, estimated as the ~4th dorsal vertebra. B. MPM-PV 1156?-5, ~5th. C. MPM-PV 1156-6, ~6th. D. MPM-PV 1156?-8, ~7th. E. MPM-PV 1156?-9, ~8th. F. MPM-PV 1156?-10, ~9th. G. MPM-PV 1156-11, ~10th. Dashed lines indicate fractured neural arch laminae. Colours indicate neural arch fossae.

Fig. 2 in Osteology of the dorsal vertebrae of the giant titanosaurian sauropod dinosaur Dreadnoughtus schrani from the Late Cretaceous of Argentina

Fig. 2. Nearly complete dorsal vertebrae of titanosaurian sauropod Dreadnoughtus schrani Lacovara, Lamanna, Ibiricu, Poole, Schroeter, Ullmann, Voegele, Boles, Carter, Fowler, Egerton, Moyer, Coughenour, Schein, Harris, Martínez, and Novas, 2014, from Santa Cruz Province, Argentina; middle–late Campanian to early Maastrichtian; in anterior view. A. MPM-PV 1156?-4, estimated as the ~4th dorsal vertebra. B. MPM-PV 1156?-5, ~5th. C. MPM-PV 1156-6, ~6th. D. MPM-PV 1156?-8, ~7th. E. MPM-PV 1156?-9, ~8th. F. MPM-PV 1156?-10, ~9th. G. MPM-PV 1156-11, ~10th. Colours indicate neural arch fossae.

Fig. 1 in Osteology of the dorsal vertebrae of the giant titanosaurian sauropod dinosaur Dreadnoughtus schrani from the Late Cretaceous of Argentina

Fig. 1. Nearly complete dorsal vertebrae of titanosaurian sauropod Dreadnoughtus schrani Lacovara, Lamanna, Ibiricu, Poole, Schroeter, Ullmann, Voegele, Boles, Carter, Fowler, Egerton, Moyer, Coughenour, Schein, Harris, Martínez, and Novas, 2014, from Santa Cruz Province, Argentina; middle–late Campanian to early Maastrichtian; in left lateral view. A. MPM-PV 1156?-4, estimated as the ~4th dorsal vertebra. B. MPM-PV 1156?-5, ~5th. C. MPM-PV 1156-6, ~6th. D. MPM-PV 1156?-8, ~7th. E. MPM-PV 1156?-9, ~8th. F. MPM-PV 1156?-10, ~9th. G. MPM-PV 1156-11, ~10th. Dashed lines indicate fractured neural arch laminae. Colours indicate neural arch fossae.

opencc-by-4.0Jan 2018View details →

Fig. 4. Morphological comparisons between Lower and Middle Jurassic African sauropod middle cervical vertebrae. A in Sauropod dinosaur remains from a new Early Jurassic locality in the Central High Atlas of Morocco

Fig. 4. Morphological comparisons between Lower and Middle Jurassic African sauropod middle cervical vertebrae. A. Pulanesaura (BP/1/6199; McPhee et al. 2015: fig. 4). B. Jobaria tiguendis (MNN TIG F40-49; PDM personal observation 2013). C. Eusauropoda indet. (NHMUK PV R36834). D. Spinophorosaurus nigerensis (Remes et al. 2009: fig. 3A). Scale bars 100 mm.

Fig. 11. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 11. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 10 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 10. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 10. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 9 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 9. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 9. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 8 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 8. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 8. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 7 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 7. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 7. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 6 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 6. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 6. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 5 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 5. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 5. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 4 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.

Fig. 4. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 in The cervical vertebrae of the Late Cretaceous abelisaurid dinosaur Carnotaurus sastrei

Fig. 4. Abelisaurid dinoasaur Carnotaurus sastrei Bonaparte, 1985 (MACN-CH 894), Argentina, La Colonia Formation, Maastrichtian, Upper Cretaceous. Cervical 3 in anterior (A), posterior (B), left lateral (C), dorsal (D), and ventral (E) views.