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Late Pliocene–Pleistocene Stratigraphy in Deep Sea Cores from the South-central North Atlantic

A Corrigendum to this article was published on 21 October 1967

Abstract

PALAEOMAGNETIC studies of deep sea cores have shown that the history of geomagnetic polarity reversal is recorded in sea floor sediments1–8. The local extinction of certain species of Radiolaria can be related to palaeomagnetic polarity reversals1,4,8, and specifically there is an association of the Brunhes–Matuyama polarity reversal at 0.7 × 106 yr ago with the ψ/X radiolaria boundary4,8. Another such extinction has been suggested4,9; occurring within the Olduvai Normal polarity event about 2 × 106 yr ago, approximates the Plio/Pleistocene chronostratigraphic boundary defined by Ericson10,11 for oceanic sediments. Although this chronostratigraphic age assignment may be correct, the relationship of the geomagnetic polarity time scale to the biostratigraphic units used to define Plio/Pleistocene geological history has not been demonstrated. This results primarily from the lack of appropriate palaeontological criteria in deep sea cores which can be correlated with the standard (type) sections of the Pliocene/Pleistocene of Italy.

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BERGGREN, W., PHILLIPS, J., BERTELS, A. et al. Late Pliocene–Pleistocene Stratigraphy in Deep Sea Cores from the South-central North Atlantic. Nature 216, 253–255 (1967). https://doi.org/10.1038/216253a0

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