Articles | Volume 12, issue 4
https://doi.org/10.5194/esurf-12-883-2024
https://doi.org/10.5194/esurf-12-883-2024
Research article
 | 
24 Jul 2024
Research article |  | 24 Jul 2024

Pliocene shorelines and the epeirogenic motion of continental margins: a target dataset for dynamic topography models

Andrew Hollyday, Maureen E. Raymo, Jacqueline Austermann, Fred Richards, Mark Hoggard, and Alessio Rovere

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Latest update: 18 Apr 2025
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Short summary
Sea level was significantly higher during the Pliocene epoch, around 3 million years ago. The present-day elevations of shorelines that formed in the past provide a data constraint on the extent of ice sheet melt and the global sea level response under warm Pliocene conditions. In this study, we identify 10 escarpments that formed from wave-cut erosion during Pliocene times and compare their elevations with model predictions of solid Earth deformation processes to estimate past sea level.
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