Continental Pleistocene Climatic Variations from Speleothem Age and Isotopic Data

Astronomy and Astrophysics – Astronomy

Scientific paper

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Scientific paper

Speleothems from continental North American caves have been dated by means of the 230Th/234U method. Oxygen isotopic variations in the dated samples and phases of speleothem deposition can be interpreted in terms of climatic change. A glacial chronology constructed from the age and isotopic data lends support to the astronomical theory of climatic change.

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