The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography

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The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography

Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically vary...

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Bibliographic Details
Main Authors:	Rovere, A., Raymo, M., Mitrovica, J., Hearty, P., O'Leary, Mick, Inglis, J.
Format:	Journal Article
Published:	Elsevier Science BV 2014
Subjects:	isostasy dynamic topography Mid-Pliocene sea level southeast coast USA Australia Republic of South Africa
Online Access:	http://hdl.handle.net/20.500.11937/49117

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