The present Pliocene/Pleistocene boundary is at the top of the Olduvai normal subchron. Many data now favour the lowering of the Pliocene/Pleistocene boundary to the Gauss-Matuyama reversal. This affords an opportunity to give to the boundary a more global significance in keeping with recent evidence.
Towards the lowering of the Pliocene/Pleistocene boundary to the Gauss/Matuyama reversal / SUC J.-P.; A. BERTINI; LEROY S.; SUBALLYOVA D.. - In: QUATERNARY INTERNATIONAL. - ISSN 1040-6182. - STAMPA. - 40:(1997), pp. 37-42.
Towards the lowering of the Pliocene/Pleistocene boundary to the Gauss/Matuyama reversal
BERTINI, ADELE;
1997
Abstract
The present Pliocene/Pleistocene boundary is at the top of the Olduvai normal subchron. Many data now favour the lowering of the Pliocene/Pleistocene boundary to the Gauss-Matuyama reversal. This affords an opportunity to give to the boundary a more global significance in keeping with recent evidence.
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