Older Peron
The Older Peron was the name for a period identified in 1961Holocene Epoch.[2][3] Modern understanding of the various factors involved in quantifying eustatic sea level, particularly processes relating to ocean siphoning and glacio-hydro-isostatic adjustment, claim that such previous instances of purported high-stands were not globally coherent, and do not constitute episodes of eustatic sea level higher than present.[4][5]
References
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- JSTOR 25735659.
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