Study Casts Doubt on Earlier Ice Caps Research
UK: August 23, 2007
LONDON - Pinhead-sized fossils buried deep under the ocean show that
glaciers did not coat the poles 41 million years ago, a new study shows,
disputing earlier research that suggested huge ice sheets covered the
Earth's extremities.
Any glaciers then -- a time when the planet was much warmer -- would only
have been in small areas in Antarctica's interior and not in the Northern
hemisphere, said Paul Wilson, from Britain's National Oceanography Centre,
who led the study.
Wilson's study contradicts research published in 2005 that suggested ice
sheets covered much of both polar regions, despite the higher temperatures.
He added that the fossils could provide clues to the future of climate
change.
"Essentially their idea (in the earlier study) was a mistake based on
inadequate data," he told Reuters of the previous study before his work
appeared in the journal Nature.
Using the world's only ship capable of executing the research operation,
Wilson's team drilled deep through sediment layers at the bottom of the
Atlantic Ocean near Surinam for the fossils of single-celled animals called
foraminifera. It then tested the chemistry of their tiny shells for signs of
ice formation.
"The hard thing is getting hold of sediment 40 million years old to generate
a record," he said.
In the period his team studied, the earth had about as much carbon dioxide
in the atmosphere as scientists predict may be present in 100 years, so the
findings also offer clues as to how rising greenhouse gas levels may affect
the planet, Wilson said.
"In order to understand where we are headed you need to go a lot farther
back in geologic history to encounter conditions we may face in the future,"
he said.
Greenhouse gases such as carbon dioxide are widely blamed for global
warming. Scientists say average temperatures will rise by between 2-6
degrees Celsius (about 4-11 F) by the end of the century, causing droughts,
floods and violent storms.
Story by Michael Kahn
REUTERS NEWS SERVICE
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