SCIENCE WEST ARCHAEOLOGY/PALEONTOLGY
Study confirms Bering land bridge flooded later than previously believed
July 31, 1996
A new study confirms the Bering land bridge that carried ancient wanderers from Asia into North America was not inundated by rising seas
until about 11,000 years ago, according to a University of Colorado at
Boulder researcher.
The study also shows the Bering land bridge vegetation at the time
consisted primarily of tundra plants and shrubs and was unsuitable for
long-term habitation by large grazing mammals, said CU-Boulder researcher
Scott Elias. Because of the abundance of mammoth and other large animal
fossils from adjacent areas, researchers had thought the environment of the
land bridge was an arid grassland similar to the steppe region of northern
Asia today, said Elias.
A paper by Elias and Susan Short of CU-Boulder's Institute of
Arctic and Alpine Research, C. Hans Nelson of the U.S. Geological Survey in
Menlo Park, Calif., and Hilary Birks of the Botanical Institute in Bergen,
Norway, was published in the July 4 issue of Nature. The newest dates for
the inundation of the land bridge corroborate radiocarbon dates calculated
by Elias and colleagues in 1992 using seafloor sediment cores.
The Bering land bridge surfaced during Earth's ice ages when sea
level in the Bering Sea and Chukchi Sea dropped by 300 feet or more due to
a buildup of glacial ice. During the most recent ice age that ended about
10,000 years ago, the land bridge covered 580,000 square miles -- an area
roughly twice the size of Texas, Elias said.
Elias and his colleagues analyzed 20 ocean-core samples obtained by U.S. Geological Survey researchers from the shallows of the Bering and
Chukchi seas for the study. Taken in the 1970s and 1980s and stored at a
USGS facility in Menlo Park, the cores contain layers of organic peat and
silt that harbor plant, pollen and insect fossils ranging from about 4,000
years old to roughly 50,000 years old.
"The exciting thing here is that we were able to sample an ancient
landscape that no longer exists," said Elias. "We don't have to guess any
more as to what the Bering land bridge was like back then."
Plant seeds and stems and insect body parts were radiocarbon dated using an accelerator mass spectrometer at the University of Arizona that
accelerates carbon atoms at near the speed of light. The instrument
allowed researchers to count the ratio of carbon 14 atoms to carbon 12
atoms from the samples and arrive at the estimated dates for the most
recent inundation of the land bridge.
"This study indicates that early people were free to move across
the land bridge until about 10,500 years ago, right up to the beginning of
the Holocene Period," said Elias. Several Paleo Indian sites in the Nenana
Valley of central Alaska that date to about 12,000 years ago are considered
the earliest reliable dates for the human occupation of North America,
Elias said.
These new data confirm that the people who spread from Beringia to North America about 14,000 years ago came from a stock able to gain a
livelihood from the meager resources of tundra, or perhaps from the sea
coast," wrote Paul Colinvaux in an accompanying News and Views article in
the July 4 issue of Nature. Colinvaux is a researcher at the Smithsonian
Tropical Research Institute in Panama.
Although mammoth, horse and bison fossils unearthed in northern
Alaska near the ancient land bridge had indicated it may once have
supported a large number of grazing mammals, the new study shows the
animals probably migrated through the area rather than living there. "This
new evidence tells us the big mammals probably did not linger on the land
bridge," said Elias.
Pollen samples from the peat cores dating from 14,000 years ago to 11,000 years ago match pollen from modern Alaskan tundra, which is
characterized by clumps of sedges, low-lying willows, dwarf birch shrubs
and grasses, he said.
The previous dates for the inundation of the land bridge -- about
14,400 years ago -- came from a 25-year-old radiocarbon sample that now
appears to have been contaminated with coal deposits washed into the Bering
and Chukchi seas, he said.
The study also indicates summer temperatures on the land bridge were about 8 to 11 degrees F warmer 11,000 years ago than they are today, said Elias. Since virtually no evolution has occurred in beetles over the past
700,000 years, scientists can compare today's beetles -- which are
sensitive indicators of climate change -- with fossil beetles from ancient
sites to reliably estimate past temperatures.
Courtesy of the University of Colorado
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