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Paleomagnetism and radiochemical age estimates for Late Brunhes polarity episodes
Authors:Charles R Denham  Robert F Anderson  Michael P Bacon
Institution:1. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Mass 02543USA;2. Department of Chemistry, Woods Hole Oceanographic Institution, Woods Hole, Mass 02543USA
Abstract:Several reversed polarity magnetozones occur within deep-sea sediment core CH57-8 from the Greater Antilles Outer Ridge, within sediment of latest Pleistocene/Late Brunhes age. The uppermost reversed interval spanning 31 data points coincides with the X faunal zone of the Last Interglacial Period. Radiochemical dating of cores CH57-8 and KN25-4 has shown that all the reversed polarity magnetozones are significantly younger than the Brunhes/Matuyama boundary at 0.7 m.y. B.P. A variation of the excess230Th method was used, in which210Po and238U were the actual radionuclides measured. In a third core from the Mid-Atlantic Ridge, our210Po results were similar to those which others obtained earlier by direct230Th measurements.
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