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1,777 results for “Mongolia”
Fig. 14 in Amphicticeps and Amphicynodon (Arctoidea, Carnivora) from Hsanda Gol Formation, Central Mongolia and Phylogeny of Basal Arctoids with Comments on Zoogeography
Fig. 14. Stereophotos of a cast of PIN 475–3016 (holotype of Cynodictis mongoliensis Janovskaja, 1970). A, occlusal view of upper teeth and B, occlusal view of lower teeth. Scales 5 10 mm.
Fig. 5 in Amphicticeps and Amphicynodon (Arctoidea, Carnivora) from Hsanda Gol Formation, Central Mongolia and Phylogeny of Basal Arctoids with Comments on Zoogeography
Fig. 5. Ventrolateral view of the right side of the basicranium of Amphicticeps shackelfordi, AMNH 19010, holotype. The region near the postglenoid process is reconstructed from that of the left side. cfn, canal for facial nerve; cica, canal for internal carotid artery; er, epitympanic recess; fc, fenestra cochleae (fenestra rotunda); fo, foramen ovale; fs, fossa for stapedius muscle; ftt, fossa for tensor tympani muscle; fv, fenestra vestibuli (fenestra ovalis); Gf, Glaserian fissure; ips, inferior petrosal sinus; mlf, middle lacerate foramen; mp, mastoid process; pf, promontory foramen; pgf, postglenoid foramen; plf, posterior lacerate foramen; pp, paroccipital process; pr, promontorium; sf, suprameatal fossa.
Fig. 13 in Amphicticeps and Amphicynodon (Arctoidea, Carnivora) from Hsanda Gol Formation, Central Mongolia and Phylogeny of Basal Arctoids with Comments on Zoogeography
Fig. 13. Teeth and lower jaw of Amphicynodon teilhardi. A, lateral view of upper teeth, PST 17/ 34; B, occlusal view of upper teeth, PIN 475–1388; C, occlusal view of upper teeth, PST 17/34, stereophotos; D, occlusal view of lower teeth, AMNH 19007, holotype, stereophotos; E, lingual, and F, labial views of lower jaw, AMNH 19007, holotype. All, except E and F, are photographs of a polyester cast. Scales 5 10 mm.
Data for: Repeatability of the 20th Century Earthquake Cluster in Mongolia: Paleoseismology along the Tsetserleg Fault (Mongolia)
<p>This dataset is associated to the article "Repeatability of the 20<sup>th</sup> Century Earthquake Cluster in Mongolia: Paleoseismology along the Tsetserleg Fault (Mongolia)" submitted to Journal of Geophysical Research: Solid Earth.</p> <p>It includes the following:</p> <ul> <li>Dataset S1 includes the output of the horizontal offset measurements performed with the LaDiCaOz Matlab GUI.</li> <li>Dataset S2 includes the drone DEMs.</li> </ul>
Text-fig. 2. Aptian to Albian Cerebropollenites taxa, all scale bars in LM and SEM overview images 10 µm, scale bars in SEM detailed images 2 µm. a–c: Cerebropollenites thiergartii from St. Pölten (Austria), a – LM image, equatorial view, b – SEM equatorial overview with visible, less sculptured leptoma, c – detail of echinate verrucae; d–f: Cerebropollenites thiergartii from Khovil basin (Mongolia), d – LM image polar view with well visible thin-walled leptoma, e – SEM of proximal polar view with faintly sculptures leptoma, f – SEM detailed view of transition from leptoma to normal sexine sculpturing; g–i: Cerebropollenites macroverrucosus from Khovil basin (Mongolia), g – LM image of oblique equatorial view, h – SEM of oblique equatorial view with concave leptoma, i – SEM detail of the rugulate to verrucate sexine and smaller sculpturing in leptoma area. in The Occurrence Of Pollen Of Sciadopityaceae Luerss. Through Time
Text-fig. 2. Aptian to Albian Cerebropollenites taxa, all scale bars in LM and SEM overview images 10 µm, scale bars in SEM detailed images 2 µm. a–c: Cerebropollenites thiergartii from St. Pölten (Austria), a – LM image, equatorial view, b – SEM equatorial overview with visible, less sculptured leptoma, c – detail of echinate verrucae; d–f: Cerebropollenites thiergartii from Khovil basin (Mongolia), d – LM image polar view with well visible thin-walled leptoma, e – SEM of proximal polar view with faintly sculptures leptoma, f – SEM detailed view of transition from leptoma to normal sexine sculpturing; g–i: Cerebropollenites macroverrucosus from Khovil basin (Mongolia), g – LM image of oblique equatorial view, h – SEM of oblique equatorial view with concave leptoma, i – SEM detail of the rugulate to verrucate sexine and smaller sculpturing in leptoma area.
Fig. 8 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 8. Two conical fossils regarded as palaeoscolecid fragments from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. A. NRM X11556 in latero-abapical (A1) and latero-apical (A2) views, with a close-up on button-shaped elements (A3). B. NRM X11556 in latero-apical (B1, B2) views, with a close-up on button-shaped elements (B3).
Fig. 6 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 6. Fibrous structures observed on elevations on the dorsal sides of palaeoscolecid Floraconformis egiinensis gen. et sp. nov., plate from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. these structures are only visible when the outer hyaline layer is absent. A. NRM X11499. B. NRM X11497.
Fig. 7 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 7. Unusual plates of palaeoscolecid Floraconformis egiinensis gen. et sp. nov. from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. A. NRM X11467; two merged plates. B. NRM X11524; second and third-generation elevations are not elongated toward the margin but parallel to it. C. NRM X11510; absence of the usual larger central elevation.
Fig. 5 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 5. Palaeoscolecid Floraconformis egiinensisgen. et sp. nov., plates (in ventral view) from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. A. NRM X11516; note the fingerprint-like ornamentation on this plate. B. NRM X11522. C. NRM X11498. D. NRM X11518. E. NRM X11501.
Fig. 4 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 4. Palaeoscolecid Floraconformis egiinensis gen. et sp. nov., plates (in dorsal view) from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. A. NRM X11465. B. NRM X11493. C. NRM X11502. D. NRM X11492. E. NRM X11489. F. NRM X11497. G. NRM X11495. H. NRM X11521. I. NRM X11508. J. NRM X11505 in general (J1) and close-up (J2) views; the dashed line in J2 represents the second large elevation delimited from the brim mentioned in the diagnosis. K. NRM X11500. L. NRM X11513. M. NRM X11499. N. NRM X11490. O. NRM X11496. P. MNRM X11491. Q. NRM X11523. R. NRM X11463.
Fig. 3 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 3. Palaeoscolecid Floraconformis egiinensis gen. et sp. nov., plate from Khuhtolgoi section, northern Mongolia, Cambrian Stage 3. Holotype NRM X11462 in dorsal (A1) and dorso-lateral (A2) views. The white arrow shows the small gap present on few plates, at the bound between inner and outer sides. The black arrow shows small tubercles that are present on the brim, when the outer hyaline layer is preserved.
Fig. 2 in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 2. Schematic drawing of palaeoscolecid Floraconformis egiinensis gen. et sp. nov. plate showing the terminology used, based on specimen NRM X11497; outer (A1) and inner (A2) side.
Fig. 1. A in New palaeoscolecid plates from the Cambrian Stage 3 of northern Mongolia
Fig. 1. A. Map of Mongolia showing location of the studied section. B. Precise location of the section Khuhtolgoi.
Fig. 2 in A Lujiatun-like dinosaurian assemblage from the Jehol Biota of Ningcheng, Inner Mongolia, Northeast China
Fig. 2. Fossils found in the Xidayingzi site from the Early Cretaceous Ningcheng Basin, Inner Mongolia. A. Sinovenator-like troodontid dinosaur (SDUST-V1062), the left pes is exposed in medial view. B. Ceratopsian dinosaur Psittacosaurus sp. (PMOL-AD00163), the maxilary teeth are loosely arranged and exposed in lateral view. C. Neornithischian dinosaur Jeholosaurus sp. (SDUST-V1063), the scapulocoracoid, humerus, ulna, and radius in lateral view. D. Euhelopus-like sauropod (SDUST-V1064), digital image of the tooth crown in medial view. E. Indeterminated lizard (PMOLAR00268), digital image of the fragmentary mandible in lingual view. F. Symmetrodont-like mammal (PMOL-AM00036), digital image of the mandible in lingual view.
Fig. 1 in A Lujiatun-like dinosaurian assemblage from the Jehol Biota of Ningcheng, Inner Mongolia, Northeast China
Fig. 1. Map of the Inner Mongolia, Liaoning and Hebei (A) showing location of the Xidayingzi site and the outcrops of the Lujiatun Unit of the Yixian Formation of the Jehol Biota in Beipiao, western Liaoning Province, China. Stratigraphic column (B) and corresponding photographic image (C) of the Early Cretaceous Xidayingzi site.
Fig. 2 in A new species of the "condylarth" Hyopsodus from the middle Eocene of the Erlian Basin, Inner Mongolia, China, and its biostratigraphic implications
Fig. 2. Temporal distributions of species of Hyopsodus and Asiohyopsodus from North America and Eurasia based on Archibald (1998) and Tong and Wang (2006). The left column shows the correlation between NALMAs and ALMAs modified from Speijer et al. (2020) and Wang et al. (2019b). The numbers below the vertical bars indicate the range or the mean value for lower molar m2 length in millimeters. Numbers with an asterisk mean that the measurement is taken from a single specimen. The traditional Wasatchian, Bridgerian, and Uintan species of Hyopsodus are discriminated by different grey shading. Abbreviations: A., Asiohyopsodus; ALMA, Asian Land Mammal Age; Clarkfork., Clarkforkian; H., Hyopsodus; NALMA, North American Land Mammal Age.
Fig. 1 in A new species of the "condylarth" Hyopsodus from the middle Eocene of the Erlian Basin, Inner Mongolia, China, and its biostratigraphic implications
Fig. 1. The middle Eocene "condylarth" mammal Hyopsodus arshantensis sp. nov. (A) and Hyopsodus sp. (B) from the Arshanto Formation of the Erlian Basin, Inner Mongolia, China. A. IVPP V 28282 from Chaganboerhe, m1–m2 in occlusal (A1), buccal (A2), and lingual (A3) views; mandible in buccal view (A4). B. IVPP V 28283 from Huheboerhe, mandible in buccal view (B1); m2 and m3 root in occlusal (B2), buccal (B3), and lingual (B4) views.
Fig. 4 in A new species of the "condylarth" Hyopsodus from the middle Eocene of the Erlian Basin, Inner Mongolia, China, and its biostratigraphic implications
Fig. 4. Mandible fragments and teeth for several species of "condylarth" mammal Hyopsodus previously reported from China utilizing µ-CT scanning A, B) and SEM images (C). A. Hyopsodus turpanensis Zhai, 1978 (IVPP V 4355) from the early Eocene Shisanjianfang Formation, Turpan Basin, Xinjiang, China. The left mandible with p2–p3 root, p4 talonid and m1–m3 in occlusal (A1, A2), lingual (A3), and buccal (A4) views, horizontal (A5) and longitudinal (A6) sections. B. Hyopsodus fangxianensis Huang, 1985 (IVPP V 12005) from the early Eocene Youping Formation, Fangxian, Hubei, China. The right mandible with m1–m3 in occlusal (B1), buccal (B2), and lingual (B3) views; cross section at the level of m2 trigonid (B4). C. Hyopsodus huashigouensis Tong, 1989 (IVPP V 7921) from the middle Eocene Üqbulak Formation, Junggar Basin, Xinjiang, China. The right m2 in occlusal (C1), lingual (C2), and buccal (C3) views.
Fig. 3 in A new species of the "condylarth" Hyopsodus from the middle Eocene of the Erlian Basin, Inner Mongolia, China, and its biostratigraphic implications
Fig. 3. Scatter plots of lower molar m1–m2 width (W) versus length (L), and size proportions of Hyopsodus and Asiohyopsodus. m1 (A) and m2 (B) width versus length, and regression lines for width as a function of length in species of Hyopsodus and Asiohyopsodus. Size proportions of m2 versus m1 (C) and m3 versus m2 (D), and regression lines for tooth size as a function of its preceding tooth size in species of Hyopsodus and Asiohyopsodus. Black symbols and lines, Wasatchian, blue symbols and lines, Bridgerian, red symbols represents the middle Eocene Hyopsodus from China, and the green symbols represent the Uintan Hyopsodus from North America. Abbreviation: H., Hyopsodus. (Raw data: SOM, the Supplementary Online Material available at http://app.pan.pl/SOM/app66-Bai_etal_SOM.pdf).
Fig. 3 in A new genus of lance lacewings from the Middle Jurassic of Inner Mongolia, China
Fig. 3. Female lance lacewing Vetosmylus maculosus gen. et sp. nov. (paratype, CNU−NEU−NN2019003P/C) from Aalenian–Bajocian boundary (Middle Jurassic) of Jiulongshan Formation of Daohugou, China (A) and extant Parosmylus tibetanus Yang, 1988 (B). A. Photographs of part part (A1) and counterpart (A2); terminalia in lateral view, a combination of photos of part and counterpart under dry condition (A3) and line drawing (A4), sternite 8 and gonapophysis 9 cannot be clearly observed. B. Line drawing of terminalia in lateral view.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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