On the Origin of Holocene Sea-Level Transgressions in Formerly Glaciated Regions
Samuel Chester,
Jacqueline Austermann,
William D'Andrea
et al.
Abstract:Over glacial cycles, the growing and shrinking of ice sheets has caused relative sea level (RSL) to differ from global mean sea level (GMSL) due to glacial isostatic adjustment (GIA), which depends on the viscoelastic properties of the solid Earth. During the last termination and through the Holocene, GIA-related isostatic uplift caused RSL to fall in regions formerly covered by ice sheets. Surrounding these uplifting regions is a narrow band of land where postglacial RSL fall was interrupted during the Holoce… Show more
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