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Fig. 3 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 3. Photograph and interpretive drawing of GMV-2158 after complete preparation. The two slabs shown in figure 2 were glued and then prepared from one side. Abbreviations: alm, alular metacarpal; co, coracoid; cmm, claw of major manual digit; cv, caudal vertebrae; cve, cervical vertebrae; f, frontal; fem, femur; fib, fibula; fur, furcula; gas, gastralia; hum, humerus; hyo, hyoid; isc, ischium; ili, ilium; j, jugal; loj, lower jaw; mam, major metacarpal; mim, minor metacarpal; mtI–IV, metatarsals I–IV; o, orbit; p, parietal; pmx, premaxilla; pub, pubis; r, ribs; rad, radius; sc, scapula; st, sternum; syn, synsacrum; tib, tibia; tv, thoracic vertebrae; uln, ulna; vr, ventral ribs; (l) or (r), left or right element.

Fig. 7 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 7. Photograph and interpretive drawing of GMV-2156. This slab, the counterpart of which is shown in figure 6, was used as the holotype of Lingyuangornis parvus by Ji and Ji (1999) (drawing after Ji and Ji, 1999). Abbreviations as in figures 3 and 5.

Fig. 2 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 2. Slab (A) and counterslab (B) of GMV-2158 prior to preparation. C. Details of the feather impressions preserved on the slab.

Fig. 1 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 1. Map of Liaoning Province (Northeastern China) showing the Early Cretaceous localities of GMV-2158 (Jianshangou) and NIGP-130723/GMV-2156 and GMV-2159 (Dawangzhangzi).

Fig. 18 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 18. Photograph and interpretive drawing of the tarsus of GMV-2158. Abbreviations: asp, ascending process of astragalus; ast, astragalus; cal, calcaneum; dts, distal tarsal. Other abbreviations as in figure 3.

Fig. 17 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 17. Photograph and interpretive drawing of the carpus and manus of GMV-2159. Abbreviations as in figure 15.

Fig. 12 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 12. Photograph and interpretive drawing of the caudal series and pelvis of GMV-2158. Abbreviations: vc1–8, caudal vertebrae 1–8; idp, ischiadic proximal dorsal process; ifa, iliac articular facet of ischium; pfa, pubic articular facet of ischium; ptr, posterior trochanter. Other abbreviations as in figure 3.

Fig. 20 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 20. Comparisons of the carpus of a nonavian theropod (Deinonychus antirhopus), Archaeopteryx lithographica, GMV-2158, the enantiornithine Longipteryx chaoyangensis, and the embryo of a modern bird (Gallus gallus). Abbreviations as in figure 15.

Fig. 19 in Juvenile Birds from the Early Cretaceous of China: Implications for Enantiornithine Ontogeny

Fig. 19. Interpretive drawings of the pes of GMV-2158 and GMV-2159. Abbreviations as in figures 3 and 5.

Fig. 6 in New Stratigraphic Data from the Erlian Basin: Implications for the Division, Correlation, and Definition of Paleogene Lithological Units in Nei Mongol (Inner Mongolia)

Fig. 6. Sketch profiles from (above) Camp Margetts and (below) 7 miles southwest (235°) of Camp Margetts (Granger, 1930).

Fig. 4 in New Stratigraphic Data from the Erlian Basin: Implications for the Division, Correlation, and Definition of Paleogene Lithological Units in Nei Mongol (Inner Mongolia)

Fig. 4. Above, The Arshanto Formaiton (middle beds) and Irdin Manha Formation (upper beds) at the Nuhetingboerhe locality; the arrow points to the upper hiatus between the two formatitons. Below, Close-up view of the upper hiatus showing the lithology and erosional surface.

Fig. 3 in New Stratigraphic Data from the Erlian Basin: Implications for the Division, Correlation, and Definition of Paleogene Lithological Units in Nei Mongol (Inner Mongolia)

Fig. 3. Above, Beds at the transition of the Nomogen (lower) and Arshanto (upper) at the Huheboerhe locality. Below, Close-up view of the lower hiatus showing the lithology and erosional surface between the Nomogen and Arshanto fomarions.

Fig. 2 in New Stratigraphic Data from the Erlian Basin: Implications for the Division, Correlation, and Definition of Paleogene Lithological Units in Nei Mongol (Inner Mongolia)

Fig. 2. Above, Paleogene outcrops at the Nuhetingboerhe locality. The arrow points to the lower hiatus between the Nomogen (lower) and Arshanto (upper) formations; Below, Close-up view of the lower hiatus showing the lithology and erosional surface.

Fig. 1. A in New Stratigraphic Data from the Erlian Basin: Implications for the Division, Correlation, and Definition of Paleogene Lithological Units in Nei Mongol (Inner Mongolia)

Fig. 1. A. Localities (black dots) of the Erlian Basin, Nei Mongol (Inner Mongolia). The shaded area indicates the location of the Nuhetingboerhe-Huheboerhe area (NHA). B. Topographic map of NHA. The black bars indicate positions of measured sections at the Daoteyin Obo, Nuhetingboerhe, Wulanboerhe (Huheboerhe of Meng et al., 2004), and Huheboerhe.

Text-fig. 3. Two re-determined gastropod species from the travertine of Gánovce-Hrádok Neanderthal site in collections of the Podtatranské Museum in Poprad. a) Helix pomatia (P-14283); b) Cepaea vindobonensis (P-14288). Scale bars 50 mm. in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 3. Two re-determined gastropod species from the travertine of Gánovce-Hrádok Neanderthal site in collections of the Podtatranské Museum in Poprad. a) Helix pomatia (P-14283); b) Cepaea vindobonensis (P-14288). Scale bars 50 mm.

Text-fig. 2. Floral record from the travertine of Gánovce-Hrádok Neanderthal site. a–c) Salix L.; d–f) Quercus L.; g) Fraxinus excelsior L.; h) Pinus L.; i) Poaceae, stem of cf. Poa sp.; j) Betula L.; k) Salix rosmarinifolia L., leaf detail; l) Salix rosmarinifolia L. All scale bars (except "g") are 20 mm, for "g" 50 mm. in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 2. Floral record from the travertine of Gánovce-Hrádok Neanderthal site. a–c) Salix L.; d–f) Quercus L.; g) Fraxinus excelsior L.; h) Pinus L.; i) Poaceae, stem of cf. Poa sp.; j) Betula L.; k) Salix rosmarinifolia L., leaf detail; l) Salix rosmarinifolia L. All scale bars (except "g") are 20 mm, for "g" 50 mm.

Text-fig. 1. Location of Gánovce-Hrádok Neanderthal site in northern Slovakia and the rest of the travertine mound (map source: https://commons.wikimedia.org and Google Earth; 2017). in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 1. Location of Gánovce-Hrádok Neanderthal site in northern Slovakia and the rest of the travertine mound (map source: https://commons.wikimedia.org and Google Earth; 2017).

Text-fig. 4. Non-mammalian record from travertine of Gánovce-Hrádok Neanderthal site. a) Emys orbicularis s. l. (NM-Rv 21001), internal core of shell in dorsal view; b) Vipera berus (P-14297), partly articulated skeleton in dorsal view; c–e) Aves gen. et sp. (c: NM-Rv 21002a, d: NM-Rv 21002b; e: P-14292), feather impressions in travertine. All scale bars (except "b") are 50 mm, for "b" 10 mm. in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 4. Non-mammalian record from travertine of Gánovce-Hrádok Neanderthal site. a) Emys orbicularis s. l. (NM-Rv 21001), internal core of shell in dorsal view; b) Vipera berus (P-14297), partly articulated skeleton in dorsal view; c–e) Aves gen. et sp. (c: NM-Rv 21002a, d: NM-Rv 21002b; e: P-14292), feather impressions in travertine. All scale bars (except "b") are 50 mm, for "b" 10 mm.

Text-fig. 6. Fossil endocasts of large mammals from Gánovce-Hrádok Neanderthal site. a) Equidae gen. et sp. indet. (NM-Rv 21008); b) Equidae gen. et sp. indet. (NM-Rv 21007); c) Equidae gen. et sp. indet. (NM-Rv 21006); d) Bovidae gen. et sp. indet. (NM-Rv 21009); e) Ursus ex gr. spelaeus (NM R-604); f) Ursus ex gr. spelaeus (NM-Rv 21010); lateral and dorsal (except for f: ventral) views; lateral view for d and f are inverted. in Revised Floral And Faunal Assemblages From Late Pleistocene Deposits Of The Gánovce-Hrádok Neanderthal Site -Biostratigraphic And Palaeoecological Implications

Text-fig. 6. Fossil endocasts of large mammals from Gánovce-Hrádok Neanderthal site. a) Equidae gen. et sp. indet. (NM-Rv 21008); b) Equidae gen. et sp. indet. (NM-Rv 21007); c) Equidae gen. et sp. indet. (NM-Rv 21006); d) Bovidae gen. et sp. indet. (NM-Rv 21009); e) Ursus ex gr. spelaeus (NM R-604); f) Ursus ex gr. spelaeus (NM-Rv 21010); lateral and dorsal (except for f: ventral) views; lateral view for d and f are inverted.