Yukon's mastodon history

December 1, 2014

American mastodons made 'vacation home' of warm Arctic 125,000 years ago

New radiocarbon dates on mastodon fossils found in Alaska and Yukon suggest local extinction long before human colonization

Press release from the American Museum of Natural History

Existing age estimates of American mastodon fossils indicate that they lived in the Arctic and Subarctic when the area was covered by ice caps. But this chronology conflicts with what scientists know about the massive animals’ preferred habitat: forests and wetlands filled with heaps of leafy food. In a paper published today in the Proceedings of the National Academy of Sciences, an international team of researchers report new radiocarbon dates that suggest that the Arctic and Subarctic were only temporary “vacation homes” for mastodons when the climate was warm. The new findings also indicate that mastodons suffered local extinction several tens of millennia before either human colonization or the onset of climate changes at the end of the ice age about 10,000 years ago, when they were among 70 species of mammals to disappear in North America.

A mammoth skull (foreground) and mastodon skeleton (background) on display at the Yukon Arts Centre in 2014 as part of the Ice Age Mammals exhibition. Photo © Government of Yukon

“Scientists have been trying to piece together information on these extinctions for decades,” said Ross MacPhee, a curator in the Department of Mammalogy at the American Museum of Natural History and a co-author on the paper. “Was is the result of over-hunting by early people in North America? Was it the rapid global warming at the end of the ice age? Did all of these big mammals go out in one dramatic die-off, or were they paced over time and due to a complex set of factors?”

Over the course of the late Pleistocene, between about 10,000 and 125,000 years ago, the American mastodon (Mammut americanum) became widespread, occupying many parts of continental North America, as well as peripheral locations like the tropics of Honduras and the Arctic coast of Alaska. Mastodons were browsing specialists, relying on woody plants and preferentially inhabiting coniferous or mixed woodlands with lowland swamps.

“Mastodon teeth were effective at stripping and crushing twigs, leaves, and stems from shrubs and trees. So it would seem unlikely that they were able to survive in the ice-covered regions of Alaska and Yukon during the last full-glacial period, as previous fossil dating has suggested,” said Grant Zazula, a paleontologist in the Yukon Palaeontology Program and lead author on the new work.


Temperature profile for last 140,000 years (as measured by oxygen isotope proxy data), vegetation and mastodon presence as determined from new radiocarbon dating approaches.

The research team used two different types of precise radiocarbon dating on a collection of 36 fossil teeth and bones of American mastodons from Alaska and Yukon, the region known as eastern Beringia. The dating methods, performed at Oxford University and the University of California, Irvine, are designed to only target material from bone collagen, not accompanying “slop” like preparation varnish and glues that were used many years ago to strengthen the specimens.

All of the fossils were found to be older than previously thought, with most surpassing 50,000 years, the effective limit of radiocarbon dating. When taking mastodon habitat preferences and other ecological and geological information into account, the results indicate that mastodons probably only lived in the Arctic and Subarctic for a limited time around 125,000 years ago, when forests and wetlands were established and the temperatures were as warm as they are today.

“The residency of mastodons in the north did not last long,” Zazula said. “The return to cold, dry glacial conditions along with the advance of continental glaciers around 75,000 years ago effectively wiped out their habitats. Mastodons disappeared from Beringia, and their populations became displaced to areas much further to the south, where they ultimately suffered complete extinction about 10,000 years ago.”

The work has a range of implications. Researchers know that giant ground sloths, American camels, and giant beavers made the migration as well, but they are still investigating what other groups of animals might have done this. The work also implies that humans had nothing to do with the extrication of mastodons in the north.

“We’re not saying that humans were uninvolved in the megafauna’s last stand 11,000 years ago. But by that time, whatever the mastodon population was down to, their range had shrunken mostly to the Great Lakes region,” MacPhee said. “That’s a very different scenario from saying the human depredations caused universal loss of mastodons across their entire range within the space of a few hundred years, which is the conventional view.”

Other authors on the paper include Jessica Metcalfe, University of British Columbia; Alberto Reyes, University of Alberta; Fiona Brock and Shweta Nalawade-Chavan, Oxford Radiocarbon Accelerator Unit; Patrick Drukenmiller, University of Alaska Museum and University of Alaska Fairbanks; Pamela Groves, Daniel Mann, and Michael Kunz, University of Alaska Fairbanks; C. Richard Harington, Canadian Museum of Nature; Gregory Hodgins, University of Arizona, Tucson; Fred Longstaffe, University of Western Ontario, London; H. Gregory McDonald, U.S. National Parks Service; and John Southon, University of California, Irvine.

Funding for this work was provided by the Bureau of Land Management Arctic Field Office. The Vuntut Gwitchin First Nation of Old Crow and the Yukon placer gold mining community provided support and assistance with the collection of ice age fossils from Yukon.

Reference: American mastodon extirpation in the Arctic and Subarctic predates human colonization and terminal Pleistocene climate change. GD Zazula, RDE MacPhee, JZ Metcalfe, AV Reyes, F Brock, PS Druckenmiller, P Groves, CR Harington, GWL Hodgins, ML Kunz, FJ Longstaffe, DH Mann, HG McDonald, S Nalawade-Chavan, and JR Southon 2014. Proceedings of the National Academy of Science USA.

Contact: Grant Zazula - Grant.Zazula@gov.yk.ca