A northern pike caught at the mouth of the Kandik River. Photo by Ned Rozell.
Suspecting the pinky-size fragment of a toothy creature was thousands of years old, Wooller ran it up to the UA Museum of the North. There, experts could tell him whether the bone was fish or fowl.
Andres Lopez, curator of fishes, recognized the jawbone of a northern pike, a duck-billed, needle-toothed super predator among freshwater fishes.
“The chance of putting the 4-centimeter barrel of the coring head through a skull like this . . . I have never seen this before,” Wooller said.
The pike jawbone was not something Wooller imagined within a 20-foot-long plug of sediment he and his colleagues pulled from Quartz Lake a few winters ago. Much smaller things within the core — ancient birch and spruce seeds, shells of tiny clams and bits of charcoal — were the gold Wooller was mining. The carbon dates from those things told him the lake formed about 11,000 years ago.
Quartz Lake covers 1,500 acres about 10 miles north of Delta Junction. The lake is shallow, averaging less than 15 feet deep, and archaeologists have found recurring evidence of ancient Alaskans on old sand dunes rimming the lake. Quartz Lake is part of the Alaska State Park system and state workers stock it with rainbow trout, Arctic char and silver salmon. Northern pike lived in the lake until 1970, when state biologists killed them all with rotenone, a powder that interferes with fish respiration.
Working out of the cabin of Dave Klein, an emeritus wildlife ecologist at UAF and one of many private landowners on the lake, Wooller and his colleagues pulled up the core with some difficulty in March 2010. The core resulted in a paper in which researchers dated the lake and a time the nearby Tanana River flooded it about 3,000 years ago.
The northern pike jaw found 14 feet deep in the muck of Quartz Lake is 8,800 years old. DNA extracted from the jaw shows the pike is related to pike that now swim the fresh waters of Eastern Asia and North America.
The Quartz Lake pike tells researchers that pike were probably present 8,000 years ago in the entire Tanana River watershed downstream of Quartz Lake, waters that connect to the Yukon River. It also hints that during the height of the last Ice Age, when New York City was buried in ice but Interior Alaska was not, northern pike were probably darting through the fresh water bodies of the Bering Land Bridge.
Since the late 1970s, the University of Alaska Fairbanks’ Geophysical Institute has provided this column free in cooperation with the UAF research community. Ned Rozell is a science writer for the Geophysical Institute.