Millions of years ago, the American Southwest sat next to East Antarctica

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FITTING THE PIECES Rocks from the Transantarctic Mountains hint that about 800 million years ago East Antarctica sat next to Laurentia, a landmass that includes much of modern-day North America.Adapted from J. Meert, Univ. of Florida What a juxtaposition: About 800 million years ago, East
Antarctica, now one of the coldest regions on Earth, abutted what is now California’s Death Valley,
one of the hottest.
Both locales were part of an equatorial supercontinent
called Rodinia, says John Goodge, a geologist at the University of Minnesota
Duluth.
The motion of tectonic plates continually rearranges Earth’s
continents, sometimes cramming most or all of them into immense groupings
called supercontinents.
One of those assemblages, Rodinia, existed between 750
million and 800 million years ago. Debate has long raged about how today’s
landmasses were arranged then, says Goodge. The orientation of magnetic lines
locked into rocks that formed at the time — which often can be used to estimate
the location and orientation of ancient landmasses — are in many cases
contradictory, he notes.
In previous studies, various teams have argued that Australia, southern China,
or even Siberia lay along the southwestern edge of Laurentia, a landmass that
held most of what is now North America.
Now, geochemical analyses of rock samples taken from the
Transantarctic Mountains hint instead that portions of East Antarctica occupied
that spot, Goodge and his colleagues report in the July 11 Science. For one thing, the ratios of neodymium isotopes in the
ancient sediments in the Transantarctic
Mountains are the same as
those in what was then Laurentia, says Goodge. Also, the hafnium isotope ratios
in the 1.44-billion-year-old zircons found in East Antarctica match those of
the zircons found in the distinctive granites now found primarily in North America.
Finally, the researchers note, the ratios of various
isotopes and elements in a basketball-sized chunk of granite found in East Antarctica — a chunk ripped by a glacier from
bedrock now smothered by thick ice, the team speculates — match those of
granite found only in what was southwestern Laurentia, which today is the
American Southwest.
Found in: Earth
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