Global sea-level rise and the disappearance of tidal notches

• Published in: Global and planetary change Vol. 92-93; pp. 248 - 256
• Main Authors: Evelpidou, N., Kampolis, I., Pirazzoli, P.A., Vassilopoulos, A.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-07-2012; Elsevier
• Subjects: biological erosion rate; Carbonates; Coasts; Fossils; Geography; Geomorphology; global isostatic adjustment; Greece; Humanities and Social Sciences; limestone dissolution; Marine; Notches; Reconstruction; sea-level indicators; Seismic phenomena; Submerged; tectonic movement; Greece; limestone dissolution; biological erosion rate; tectonic movement; sea-level indicators; global isostatic adjustment
• ISSN: 0921-8181; 1872-6364
• DOI: 10.1016/j.gloplacha.2012.05.013

The recent rise in global sea level is causing the disappearance of an important geomorphological sea-level indicator, the tidal notch.
Tidal notches have often been used in carbonate coasts for Quaternary and late Holocene sea-level reconstructions and estimation of tectonic movements, especially in uplifting areas. In this paper, we review the rates of tidal notch development, and examine the recent gradual depletion of this feature, during at least the last century, and its relation to the increasing rates of sea-level rise. Some examples of tidal notch development are provided with fossil submerged notches from Greece. Although tidal notches are no longer forming in the present-day mid-littoral zone, underwater marks on carbonate cliffs may still provide evidence of submerged tidal notches corresponding to former sea-level positions, or of recent vertical shoreline displacements of seismic origin.
► Tidal notches' recent depletion and recent global sea-level rise correlation. ► Eustatic trend/bioerosion rates drive to present tidal notches disappearance. ► Based on near-future predictions new tidal notches will not be developed.