Ancient plant life recovered in recent Arctic Ocean sampling cores shows that at the time of the last major global warming, humidity, precipitation levels and salinity of the ocean water altered drastically, along with the elevated temperatures and levels of greenhouse gases, according to a report in the August 10 issue of Nature.
The Arctic Ocean drilling expedition in 2004 allowed scientists to directly measure samples of biological and geological material from the beginning of the Palaeocene/Eocene thermal maximum (PETM), a period of rapid, extreme global warming about 55 million years ago. It has given researchers a direct resource of measurable information on global warming -- from a time when the overall global temperature was higher and more uniform from the subtropics to the arctic.
"Analysis of carbon and hydrogen isotopes in the recovered fossil plants told us a lot about the way water is transported in the atmosphere and its effect on the climate," said Mark Pagani, professor of geology and geophysics at Yale and principal author of the study. "The isotope traces we measured indicated that a large-scale alteration in the water cycle occurred and that future alterations may leave us poorly equipped to predict our water supply."
"Without being hysteric, it is important to realize that the impact of global warming is not just about searing hot summers -- it is about water as a resource. It is about when and where it rains and how much we have to drink," said Pagani. "This is a red flag"
Pagani and his collaborators show that water and atmospheric water vapor are a major indicator of the "greenhouse" changes. Rather than just looking at changes in ocean water -- that can be influenced by many factors -- the researchers measured carbon and hydrogen isotopes in the fossil plants and reconstructed the pattern of precipitation and characteristics of the ancient arctic water.
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http://www.sciencedaily.com/releases/2006/08/060812085938.htm