File:Suhongtu site - Sinornithomimus quarry.png
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Summary
| Description |
English: 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. |
| Date | |
| Source | (2008). "Mud-Trapped Herd Captures Evidence of Distinctive Dinosaur Sociality". Acta Palaeontologica Polonica 53 (4): 567–578. DOI:10.4202/app.2008.0402. ISSN 0567-7920. |
| Author | David J. Varricchio, Paul C. Sereno, Zhao Xi-jin, Tan Lin Jeffrey A. Wilson & Gabrielle H. Lyon |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 05:28, 21 August 2020 | | 1,147 × 758 (496 KB) | PaleoNeolitic | {{Information |description ={{en|1=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−diagr... |
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