Tham khảo Dinosauromorpha

  1. ↑ Langer, M. C.; Nesbitt, S. J.; Bittencourt, J. S.; Irmis, R. B. (2013). “Non-dinosaurian Dinosauromorpha”. Geological Society, London, Special Publications. doi:10.1144/SP379.9.
  2. ↑ Brusatte, S.L.; Niedźwiedzki, G.; Butler, R.J. (2010). “Footprints pull origin and diversification of dinosaur stem lineage deep into Early Triassic”. Proceedings of the Royal Society B. 278 (1708): 1107–1113. doi:10.1098/rspb.2010.1746. PMC 3049033. PMID 20926435.
  3. ↑ Saltopus, a dinosauriform from the Upper Triassic of Scotland. Michael J. Benton and Alick D. Walker. Earth and Environmental Science Transactions of the Royal Society of Edinburgh / Volume 101 / Special Issue 3-4, pp 285 - 299 Royal Society of Edinburgh 2011 Published online: ngày 17 tháng 5 năm 2011 doi:10.1017/S1755691011020081
  4. ↑ Baron, M.G., Norman, D.B., and Barrett, P.M. (2017). A new hypothesis of dinosaur relationships and early dinosaur evolution. Nature, 543: 501–506. doi:10.1038/nature21700
  5. ↑ Irmis, Randall B.; Nesbitt, Sterling J.; Padian, Kevin; Smith, Nathan D.; Turner, Alan H.; Woody, Daniel; Downs, Alex (2007). “A Late Triassic dinosauromorph assemblage from New Mexico and the rise of dinosaurs”. Science. 317 (5836): 358–361. doi:10.1126/science.1143325. PMID 17641198.
  6. ↑ Nesbitt, Sterling J.; Irmis, Randall B.; Parker, William G.; Smith, Nathan D.; Turner, Alan H.; Rowe, Timothy (2009). “Hindlimb osteology and distribution of basal dinosauromorphs from the Late Triassic of North America”. Journal of Vertebrate Paleontology. 29 (2): 498–516. doi:10.1671/039.029.0218.
  7. ↑ Ferigolo, J.; Langer, M.C. (2006). “A Late Triassic dinosauriform from south Brazil and the origin of the ornithischian predentary bone”. Historical Biology. 19 (1): 1–11. doi:10.1080/08912960600845767.
  8. ↑ Nesbitt, Sterling J.; Irmis, Randall B.; Parker, William G. (2007). “A critical re-evaluation of the Late Triassic dinosaur taxa of North America”. Journal of Systematic Palaeontology. 5 (2): 209–243. doi:10.1017/S1477201907002040.