Evidence of ancient hibernation Antarctica

Hibneration-like torpor in a 250 million year old mammalian predecessor may have served as a key adaptation in occupying polar environments and surviving the largest mass extinction the earth has experienced to date.

Like Comment
Read the paper

Antarctica is famous for its snow- and ice-covered landscape that makes it one of the most extreme environments on earth today. Below the snow and ice, however, are rocks that preserve fossil plants and animals that document a much more habitable environment with bodies of running water and forests. One of these environments include an important assemblage from the Early Triassic (~250 million years ago). Although these plants and animals lived in an ecosystem much warmer than what is found there today, Antarctica has remained at a high, polar latitude throughout the history of life on the continent subjecting its inhabitants to strong sunlight seasonality. 

A large fossil burrow from the Early Triassic Fremouw Formation of Antarctica. (photo credits: M. Whitney)

As a PhD student at the University of Washington, I studied how animals, specifically a mammalian predecessor called Lystrosaurus, adapted to this unique environment and how those adaptations can tell us something about their biology as well as the role polar regions play during recovery from mass extinctions as was the case during the Early Triassic. Using the tree-ring like structure preserved in the tusks of these charismatic beasts (and by charismatic I mean short stubby bodies, a beak like a turtle, and no teeth except for a pair of tusks; see illustration below!), I was able to study times of normal growth and times of stressed growth and compare our polar Antarctic sample to a non-polar sample of Lystrosaurus tusks from South Africa.

The tree ring-like growth structures preserved in the ever-growing tusks of Lystrosaurus. (photo credit: M. Whitney)

An important part of this project was a field season during the austral summer of 2017-2018 in the Transantarctic Mountains. We spent nearly two months in Antarctica, most of which were camped out at the confluence of the Shackleton and McGregor Glaciers, commuting in helicopters (a.k.a. Helicopter-Ubers) each day to our field sites in the surrounding mountains. Our team consisted of vertebrate paleontologists and geologists and we worked closely with an amazing group of camp staff, pilots and other science teams we shared a camp with.

Home sweet home! Our tents looking out on the Shackleton Glacier. Several of our field sites were in the mountains seen here. (photo credits: C. Sidor)

Upon our return from the ice, I began making thin sections of Lystrosaurus tusks and measuring the growth marks preserved in those tusks. In comparison to our non-polar sample, we found evidence of stress that appears most similar to hibernation patterns in some modern-day animals. These findings have some interesting implications in understanding the biology and ecology of Lystrosaurus and the evolution of warm-bloodedness, but my hope is this is just the first study of its kind. The Triassic assemblage of Antarctic fossils contains early reptiles, other mammalian predecessors, and amphibians. Presumably these other animals would have also adapted to the extreme sunlight seasonality and likely did so in different ways. Continued study of the physiological adaptations of this assemblage can help us understand the ways in which Antarctica, and high latitudes in general, have served as havens from the global warming events associated with one of the deadliest mass extinctions the earth has seen to date. 

Life restoration of a hibernating Lystrosaurus. (illustration by Crystal Shin)

Our amazing field team from left to right: Christian Sidor, Roger Smith, Akiko Shinya, Peter Mackovicky, Julia McIntosh, Nathan Smith, Hank Woolley, Peter Braddock, Megan Whitney. (photo credits: C. Sidor)

Megan Whitney

Postdoctoral Researcher, Museum of Comparative Zoology

No comments yet.