Abstract
New palaeomagnetic data from the proposed Plio-Pleistocene boundary stratotype section (Vrica section, southern Italy) are presented here in order to improve the correlation of these sediments to the magnetic polarity time scale. If the interpretation preferred here is correct, the boundary falls above the Olduvai normal subchron at approximately 1.6 Myr.
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Tauxe, L., Opdyke, N., Pasini, G. et al. Age of the Plio-Pleistocene boundary in the Vrica section, southern Italy. Nature 304, 125–129 (1983). https://doi.org/10.1038/304125a0
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DOI: https://doi.org/10.1038/304125a0
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