Fine tuning the radiometrically derived geomagnetic polarity time scale (GPTS) for 0-10 Ma

Astronomy and Astrophysics – Astronomy

Scientific paper

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Argon Isotopes, Geochronology, Geomagnetism, Magnetic Poles, Ocean Bottom, Paleomagnetism, Polarity, Radiometers, Reversing, Stratigraphy

Scientific paper

New Ar-40/Ar-39 step-heating ages for geomagnetic field reversals at 3.2 and 4.5 Ma, along with previous data at approximately 1, 2, 10 and 16 Ma, are used to derive a geomagnetic polarity time scale for 0-10 Ma. These ages for chron boundaries are fitted to the relative widths of the polarity intervals on the ocean floor, using a cubic spline technique. The interpolated ages of chrons for 0-6 Ma are in good agreement with the astronomical time scale and differ considerably from earlier attempts, based, in part, on K-Ar dates. Significant differences between the interpolated ages and the astronomical time scale are noted for the onset of the Olduvai and Reunion (sub)chrons; there is better agreement if Ar-40/Ar-39 data obtained from direct dating of these chrons is utilized. This time scale is estimated to be accurate to +/- 1% for 0-6 Ma; for 6-10 Ma, the lack of a tie-point limits the accuracy to about +/- 2%.

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