speleothems are scattered over most continen-tal areas and provide exceptional chronology. They will allow investigation of spatially vari-able changes as climate fronts move across continental regions, and enable direct compar-ison of climate in distant regions, as recently demonstrated in a study...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.pdf |
Summary: | speleothems are scattered over most continen-tal areas and provide exceptional chronology. They will allow investigation of spatially vari-able changes as climate fronts move across continental regions, and enable direct compar-ison of climate in distant regions, as recently demonstrated in a study of rainfall in the south-ern and northern Tropics (9). For paleoclimate, the past two decades have been the age of the ice core. The next two may be the age of the speleothem. |
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