Details - The first Tertiary fossils of mammals, turtles, and fish from Canada's Yukon

The first Tertiary fossils of mammals, turtles, and fish from Canada's Yukon

Title

The first Tertiary fossils of mammals, turtles, and fish from Canada's Yukon

Title Variants

Alternative: First Tertiary fossils from Yukon

By

Eberle, Jaelyn, , author

Hutchison, J. Howard (John Howard), 1939- , author
Kennedy, Kristen, , author
Koenigswald, Wighart von , author
MacPhee, R. D. E. , author
Zazula, Grant D. , author

Type

Book

Material

Published material

Publication info

New York, NY, American Museum of Natural History, [2019]

Notes

Caption title.

"October 31, 2019."

Local PDF available in high- and low-resolution versions.

Despite over a century of prospecting and field research, fossil vertebrates are exceedingly rare in Paleogene and Neogene rocks in northern Canada's Yukon Territory. Here, we describe the first records of probable Neogene vertebrate fossils from the territory, including tooth fragments of a rhinocerotid, a partial calcaneum of an artiodactyl, shell fragments of the pond turtle Chrysemys s.l. and tortoise Hesperotestudo, and a fragment of a palatine of Esox (pike). Although the tooth fragments cannot be identified solely by traditional paleontological means, we use tooth enamel microstructure, and primarily the presence of vertical Hunter-Schreger bands, to refer them to the Rhinocerotidae. As the only known record of the Rhinocerotidae in North America's western Arctic, the tooth fragments from the Wolf Creek site support the hypothesis that the clade dispersed between Asia and North America across Beringia. The fossils are consistent with a Miocene age for the Wolf Creek site that is inferred from radiometric dates of the Miles Canyon basalt flows in the vicinity of the fossil locality. Further, the tortoise and pond turtle fossils indicate a mild climate in the Yukon at the time, consistent with the vegetation reconstructions of others that indicate a warmer, wetter world in the Miocene than today.