EUGENE, Ore. - (Feb. 12, 2018) - A fossilized trackway on public lands in Lake County, Oregon, may reveal clues about the ancient family dynamics of Columbian mammoths.
Recently excavated by a team from the University of Oregon Museum of Natural and Cultural History, the Bureau of Land Management and the University of Louisiana, the trackway includes 117 footprints thought to represent a number of adults as well as juvenile and infant mammoths.
Discovered by Museum of Natural and Cultural History paleontologist Greg Retallack during a 2014 class field trip on fossils at the UO, the Ice Age trackway is the focus of a new study appearing online ahead of print in the journal Palaeogeography, Palaeoclimatology, Palaeoecology.
Retallack returned to the site with the study's coauthors, including UO science librarian Dean Walton, in 2017. The team zeroed in on a 20-footprint track, dating to roughly 43,000 years ago, that exhibited some intriguing features.
"These prints were especially close together, and those on the right were more deeply impressed than those on the left-as if an adult mammoth had been limping," said Retallack, also a professor in the UO Department of Earth Sciences and the study's lead author.
But, as the study reveals, the limping animal wasn't alone: Two sets of smaller footprints appeared to be approaching and retreating from the limper's trackway.
"These juveniles may have been interacting with an injured adult female, returning to her repeatedly throughout the journey, possibly out of concern for her slow progress," Retallack said. "Such behavior has been observed with wounded adults in modern, matriarchal herds of African elephants."
The tracks were made in a layer of volcanic soil at Fossil Lake, a site first excavated by UO science professor Thomas Condon in 1876 and today administered by the Bureau of Land Management.
"America's public lands are some of the world's greatest outdoor laboratories. Localities such as this mammoth tracksite are unique parts of America's heritage and indicate that there are many special sites still to be discovered," said study co-author Brent Breithaupt, a paleontologist in the Wyoming State Office of the Bureau of Land Management.
Specimens from the 1876 Fossil Lake excavation-along with the rest of Condon's extensive assemblage of fossils and geologic specimens-were donated to UO in the early 1900s and form the core of the museum's Condon Fossil Collection, now under Retallack's direction and boasting upwards of 50,000 fossil specimens.
Last month a new state law went into effect, making the UO museum Oregon's default repository for fossils found on state lands. The museum is also a designated repository for artifacts and paleontological specimens collected from BLM-administered lands in Oregon, ensuring they are available to future generations for education and research.
As part of the 2017 study, Neffra Matthews of the BLM's National Operations Center in Denver, helped survey, map and document the trackway using photogrammetry, which helps scientists perform accurate measurements based on land-based or aerial photographs.
"There is a vast storehouse of natural history found on BLM-managed land, and it's exciting to work with researchers like Professor Retallack in capturing 3D data on fragile paleontological resources," she said.
Retallack said that trace fossils such as trackways can provide unique insights into natural history.
"Tracks sometimes tell more about ancient creatures than their bones, particularly when it comes to their behavior," he said. "It's amazing to see this kind of interaction preserved in the fossil record."
Elephants once roamed across much of North America. Woolly mammoths (Mammuthus primigenius) were common in Canada and Alaska. Columbian mammoths (Mammuthus columbi) occupied the region that became Washington state to South Dakota and south into Mexico. Most mammoths went extinct about 11,500 years ago, but some isolated Arctic island populations of woolly mammoth persisted until 4,000 years ago.
Co-authors on the paper with Breithaupt, Retallack, Walton and Matthews were James E. Martin of the University of Louisiana Geology Museum and Adrian P. Broz, a doctoral student in the UO Department of Earth Sciences who was among the students who found the site.
The excavation was funded by a Sandal Society grant from the UO's Museum of Natural and Cultural History and under a permit granted by the Bureau of Land Management.
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