Sinornithomimus
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Sinornithomimus (2).jpg
Författare/Upphovsman: Carpenter, Kenneth, Licens: CC BY-SA 4.0
Sinornithomimus specimen
Författare/Upphovsman: Carpenter, Kenneth, Licens: CC BY-SA 4.0
Sinornithomimus specimen
Sinornithomimus Scale.svg
Size comparison of two specimens of the Chinese ornithomimid theropod Sinornithomimus dongi. Based on Kobayashi & Lü, 2003. Human silhouette 180 cm from File:Silhouette of man standing and facing forward.svg.
Size comparison of two specimens of the Chinese ornithomimid theropod Sinornithomimus dongi. Based on Kobayashi & Lü, 2003. Human silhouette 180 cm from File:Silhouette of man standing and facing forward.svg.
Sinornithomimus skeletal.jpg
Författare/Upphovsman: Yoshitsugu Kobayashi & Jun−Chang Lü, Licens: CC BY 4.0
Reconstructed skeletons of Sinornithomimus dongi gen. et sp. nov. (subadult, IVPP−V11797−10; juvenile, IVPP−V11797−11). Scale bar 30 cm
Författare/Upphovsman: Yoshitsugu Kobayashi & Jun−Chang Lü, Licens: CC BY 4.0
Reconstructed skeletons of Sinornithomimus dongi gen. et sp. nov. (subadult, IVPP−V11797−10; juvenile, IVPP−V11797−11). Scale bar 30 cm
Suhongtu site - Sinornithomimus quarry.png
Författare/Upphovsman: David J. Varricchio, Paul C. Sereno, Zhao Xi-jin, Tan Lin Jeffrey A. Wilson & Gabrielle H. Lyon, Licens: CC BY 4.0
Suhongtu site, partial quarry map, locality map, and orientation data. A. Map of the central and northern portions of site showing the position of 12 of 13 skeletons. Skeletons 3 and 4 enlarged in Fig. 3. B. Fossil locality (41°17’ 10”N, 103°52’38”E) located 90 km northwest of Bayan Mod, InnerMongolia, China. C. Rose−diagram showing trends for skeletons (black, numbers denote skeleton count) and ripples (white). D. Mirror rose−diagram of elongated, isolated elements (n=13). Trends of skeletons have a strong, non−random (p<0.002) alignment to southeast. Flow direction of ripples is roughly perpendicular to that of elongate elements.
Författare/Upphovsman: David J. Varricchio, Paul C. Sereno, Zhao Xi-jin, Tan Lin Jeffrey A. Wilson & Gabrielle H. Lyon, Licens: CC BY 4.0
Suhongtu site, partial quarry map, locality map, and orientation data. A. Map of the central and northern portions of site showing the position of 12 of 13 skeletons. Skeletons 3 and 4 enlarged in Fig. 3. B. Fossil locality (41°17’ 10”N, 103°52’38”E) located 90 km northwest of Bayan Mod, InnerMongolia, China. C. Rose−diagram showing trends for skeletons (black, numbers denote skeleton count) and ripples (white). D. Mirror rose−diagram of elongated, isolated elements (n=13). Trends of skeletons have a strong, non−random (p<0.002) alignment to southeast. Flow direction of ripples is roughly perpendicular to that of elongate elements.