Beavers, once abundant and widespread in the Northern Hemisphere, helped to forge the ground underneath many Americans’ feet.
The team behind a new study, published in the January 2012 issue of Geology, used ground-penetrating radar to detect buried beaver dams -- revealing how beaver activity up to thousands of years ago affected sedimentation and left its lasting mark within North America's ground.
“Ecologists have estimated that, prior to the arrival of Europeans in North America, anywhere from 60 to 400 million beavers inhabited the continent, with a geographic range estimated at 15 million square kilometers,” co-author Ellen Wohl told Discovery News.
“Beavers were present from the arctic tundra to the deserts of northern Mexico, so they would have been in every U.S. state but Hawaii,” added Wohl, a professor in the Warner College of Natural Resources at Colorado State University.
For the study, Wohl and colleagues Natalie Kramer and Dennis Harry used both ground-penetrating radar and near-surface seismic refraction to detect beaver-induced sedimentation.
Both methods put energy, radar and seismic waves, into the ground. The researchers then recorded the times required for the energy’s return, using spatial differences in these travel times to infer the presence of contrasts in the subsurface. These, in turn, can reveal buried beaver dams that may have no surface expression.
The scientists focused their work at a site appropriately called Beaver Meadows in Colorado’s Rocky Mountain National Park. As of 1976, no beavers were present in the area, but earlier surveys documented the presence of numerous beaver lodges. The beaver dam sedimentation detected by the scientists dated from 180 to 4,300 years ago, with even older remains possible.
The study determined that beavers contributed 30-50 percent of post-glacial sediments in the target area.
“I think it very likely that our results are not unique to the Beaver Meadows study site, but also apply to other regions with relatively low rates of sediment yield to valley bottoms,” Wohl said.
She explained that beaver dams interrupt the flow of a stream, creating a backwater effect of reduced velocity. Sediment deposits in the backwater zone of the beaver pond, with this material remaining “in storage” until river erosion may mobilize it and carry it downstream.
The process is beneficial to humans, she continued, because “wet meadows associated with beaver dams have higher habitat and species diversity for plants, insects and other invertebrates, amphibians, reptiles, birds and mammals -- pretty much all forms of life.”
Beaver ponds additionally help to remove carbon and nitrogen from water. When carbon combines with chlorine -- used in many water treatment facilities -- it can result in cancer-causing chemicals, she said, so beavers can help to keep drinking water safe.
Jill Baron, co-director of the John Wesley Powell Center for Earth System Analysis and Synthesis at the U.S. Geological Survey, believes that studies like this latest one, which show the widespread and long-standing effects of beaver activity, are important.
“Not only do beavers make wetlands, but they also alter the appearance and function of rivers for a very long time,” Baron said.
“What beavers do is create environments for storing carbon and processing nitrogen,” Baron said. The latter, in particular, provides a “very important ecosystem service, because reactive nitrogen flowing down rivers is what causes eutrophication, hypoxia and dead zones in many of the world’s estuaries (such as at Chesapeake Bay and the Gulf of Mexico),” she said.
Due to intense beaver hunting, habitat destruction, pollution and other problems, the beaver population has plummeted by the millions in recent decades. Since beavers can impact human activities, their presence in areas remains controversial. Conservation groups such as Worth a Dam in Martinez, California, however, work hard to maintain beaver dams through responsible stewardship and to educate the public about the many benefits associated with beavers.