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Storer, John E., Bryant, Harold N. (1993) Biostratigraphy of the Cypress Hills Formation (Eocene to Miocene), Saskatchewan: equid types (Mammalia: Perissodactyla) and associated faunal assemblages. Journal of Paleontology, 67 (4) 660-669 doi:10.1017/s0022336000024987

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Reference TypeJournal (article/letter/editorial)
TitleBiostratigraphy of the Cypress Hills Formation (Eocene to Miocene), Saskatchewan: equid types (Mammalia: Perissodactyla) and associated faunal assemblages
JournalJournal of Paleontology
AuthorsStorer, John E.Author
Bryant, Harold N.Author
Year1993 (July)Volume67
Issue4
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000024987Search in ResearchGate
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Mindat Ref. ID415989Long-form Identifiermindat:1:5:415989:0
GUID0
Full ReferenceStorer, John E., Bryant, Harold N. (1993) Biostratigraphy of the Cypress Hills Formation (Eocene to Miocene), Saskatchewan: equid types (Mammalia: Perissodactyla) and associated faunal assemblages. Journal of Paleontology, 67 (4) 660-669 doi:10.1017/s0022336000024987
Plain TextStorer, John E., Bryant, Harold N. (1993) Biostratigraphy of the Cypress Hills Formation (Eocene to Miocene), Saskatchewan: equid types (Mammalia: Perissodactyla) and associated faunal assemblages. Journal of Paleontology, 67 (4) 660-669 doi:10.1017/s0022336000024987
In(1993, July) Journal of Paleontology Vol. 67 (4) Cambridge University Press (CUP)
Abstract/NotesAmong the equid species named from the Cypress Hills Formation (Eocene to Miocene) of Saskatchewan, Mesohippus westoni and M. propinquus are documented from the early Chadronian Calf Creek local fauna, and M. westoni is also known from the earlier Southfork local fauna and from other Chadronian and Orellan deposits of western North America. Teeth possibly referable to Miohippus assiniboiensis are found in association with Whitneyan or early Arikareean assemblages. Miohippus grandis, not M. assiniboiensis, is the correct reference for larger Chadronian equids from Calf Creek and other local faunas. Archaeohippus stenolophus (new combination) is preserved in latest Arikareean or early Hemingfordian beds of the Cypress Hills, and occurs in faunal assemblages that show strong resemblances to the Runningwater assemblage of Nebraska.


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