High Arctic camel

The High Arctic camel, from the mid-Pliocene epoch, is a fossil camel related to the fossil genus Paracamelus from which modern camels arose. It is also related to the extinct Ice Age Yukon giant camel. Collagen-containing fossils were found in 2006 near Strathcona Fiord on Ellesmere Island in Nunavut, Canada. The High Arctic camel lived at least 3.4 million years ago during a warmer period in a boreal-type forest environment.

The remains of the High Arctic camel were discovered over several field seasons (2006-2010) in the Strathcona Fiord area of Ellesmere Island, in the Canadian Arctic Archipelago, at about 78°N latitude. About 30 fragments were collected from the Fyles Leaf Bed site and assembled, forming part of a right tibia. The presence of a fibular notch at the distal end of the bone suggests the bone was from an artiodactyl hooved mammal (e.g. cows, deer, camels). Size estimates are consistent with camels, as they were the largest artiodactyls in North America at the time. This is the first evidence of camels in the High Arctic and a new taxon for the mammal assemblage of the Pliocene High Arctic.

Collagen fingerprinting showed the fragmentary fossil remains were from camel and involved comparison of the ancient collagen with that of 37 modern mammal species, as well as the Pleistocene-Aged giant Yukon camel (tentatively referred to the genus Paracamelus). The High Arctic camel was most similar to the one-humped Dromedary camel and the Yukon giant camel.

The estimated age of the camel fossil was obtained using a terrestrial cosmogenic nuclide (TCN) burial dating technique, which was applied to quartz sand containing the fossils. These deposits are at least 3.4 million years old and equivalent in age to the mammal fossil record in the nearby Beaver Pond fossil site. The deposits hosting the camel remains correlate to the Beaufort Formation, which was emplaced prior the onset of extensive North American glaciation at ~2.6 Ma.

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