The McCoy Brook Formation rests on the North Mountain Basalt, one of the volcanic flows associated with the Triassic–Jurassic boundary in the Newark Supergroup. The base of the McCoy Brook Formation is probably within 100,000 to 200,000 years of the boundary.[1]
Scots Bay Member
This thin unit (9 m) of lacustrine sediments is preserved in six small synclinal outcrops around Scots Bay on the west side of the Blomidon Peninsula. Originally named as the Scots Bay Formation, it is now correlated with the lowermost part of the McCoy Brook Formation, where it is referred to as the Scots Bay Member.[2][3]
Although long assigned to Ammosaurus, the material actually represents a new genus and species;[6] found in fluvio-lacustrine sandstone and mudstone, and basalt agglomerate[1]
^ abcdefghijklmnopqrstuvwxyzaaabacadaeafagahaiajakalShubin, N. H.; Olsen, P. E.; Sues, H.-D. (1994). "Early Jurassic small tetrapods from the McCoy Brook Formation of Nova Scotia, Canada". In Fraser, N. C.; and Sues, H. D., editors (ed.). In the Shadow of the Dinosaurs. Cambridge, United Kingdom: Cambridge University Press. pp. 242–250. ISBN0-521-45899-4. {{cite book}}: |editor= has generic name (help)CS1 maint: multiple names: editors list (link)
^ abcdefSues, H.-D.; Shubin, N. H.; Olsen, P. E. (1994). "A new sphenodontian (Lepidosauria: Rhynchocephalia) from the McCoy Brook Formation (Lower Jurassic) of Nova Scotia, Canada". Journal of Vertebrate Paleontology. 14 (3): 327–340. doi:10.1080/02724634.1994.10011563.
^ abcdeSues, H.-D.; Shubin, N. H.; Olsen, P. E.; Amaral, W. W. (1996). "On the cranial structure of a new protosuchid (Archosauria: Crocodyliformes) from the McCoy Brook Formation (Lower Jurassic) of Nova Scotia, Canada". Journal of Vertebrate Paleontology. 16 (1): 34–41. doi:10.1080/02724634.1996.10011281.
^ abcFedak, T. J. (2007). Description and evolutionary significance of the sauropodomorph dinosaurs from the early Jurassic (Hettangian) McCoy Brook Formation. Ph.D. dissertation. Halifax, Nova Scotia: Dalhousie University.