Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand

Abstract Relic coastal landforms (fossil corals, cemented intertidal deposits, or erosive features carved onto rock coasts) serve as sea‐level index points (SLIPs), that are widely used to reconstruct past sea‐level changes. Traditional SLIP‐based sea‐level reconstructions face challenges in capturi...

Full description

Saved in:
Bibliographic Details
Main Authors: N. Georgiou, P. Stocchi, E. Casella, A. Rovere
Format: Article
Language:English
Published: Wiley 2024-03-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL106829
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849321810453069824
author N. Georgiou
P. Stocchi
E. Casella
A. Rovere
author_facet N. Georgiou
P. Stocchi
E. Casella
A. Rovere
author_sort N. Georgiou
collection DOAJ
description Abstract Relic coastal landforms (fossil corals, cemented intertidal deposits, or erosive features carved onto rock coasts) serve as sea‐level index points (SLIPs), that are widely used to reconstruct past sea‐level changes. Traditional SLIP‐based sea‐level reconstructions face challenges in capturing continuous sea‐level variability and dating erosional SLIPs, such as tidal notches. Here, we propose a novel approach to such challenges. We use a numerical model of cliff erosion embedded within a Monte Carlo simulation to investigate the most likely sea‐level scenarios responsible for shaping one of the best‐preserved tidal notches of Last Interglacial age in Sardinia, Italy. Results align with Glacial Isostatic Adjustment model predictions, indicating that synchronized or out‐of‐sync ice‐volume shifts in Antarctic and Greenland ice sheets can reproduce the notch morphology, with sea level confidently peaking at 6 m and only under a higher than present erosion regime. This new approach yields insight into sea‐level trends during the Last Interglacial.
format Article
id doaj-art-e7e1ae2dae3f4868b1c162c2f5acc13c
institution Kabale University
issn 0094-8276
1944-8007
language English
publishDate 2024-03-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-e7e1ae2dae3f4868b1c162c2f5acc13c2025-08-20T03:49:37ZengWileyGeophysical Research Letters0094-82761944-80072024-03-01516n/an/a10.1029/2023GL106829Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High StandN. Georgiou0P. Stocchi1E. Casella2A. Rovere3Ca’ Foscari University of Venice Department of Environmental Sciences Informatics and Statistics Mestre (VE) ItalyDipartimento di Scienze Pure e Applicate (DiSPeA) Università degli Studi di Urbino “Carlo Bo” Urbino ItalyCa’ Foscari University of Venice Department of Environmental Sciences Informatics and Statistics Mestre (VE) ItalyCa’ Foscari University of Venice Department of Environmental Sciences Informatics and Statistics Mestre (VE) ItalyAbstract Relic coastal landforms (fossil corals, cemented intertidal deposits, or erosive features carved onto rock coasts) serve as sea‐level index points (SLIPs), that are widely used to reconstruct past sea‐level changes. Traditional SLIP‐based sea‐level reconstructions face challenges in capturing continuous sea‐level variability and dating erosional SLIPs, such as tidal notches. Here, we propose a novel approach to such challenges. We use a numerical model of cliff erosion embedded within a Monte Carlo simulation to investigate the most likely sea‐level scenarios responsible for shaping one of the best‐preserved tidal notches of Last Interglacial age in Sardinia, Italy. Results align with Glacial Isostatic Adjustment model predictions, indicating that synchronized or out‐of‐sync ice‐volume shifts in Antarctic and Greenland ice sheets can reproduce the notch morphology, with sea level confidently peaking at 6 m and only under a higher than present erosion regime. This new approach yields insight into sea‐level trends during the Last Interglacial.https://doi.org/10.1029/2023GL106829tidal notchcliff erosion numerical modelLast Interglacial MIS 5esea level changegeomorphologyMonte Carlo
spellingShingle N. Georgiou
P. Stocchi
E. Casella
A. Rovere
Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
Geophysical Research Letters
tidal notch
cliff erosion numerical model
Last Interglacial MIS 5e
sea level change
geomorphology
Monte Carlo
title Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
title_full Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
title_fullStr Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
title_full_unstemmed Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
title_short Decoding the Interplay Between Tidal Notch Geometry and Sea‐Level Variability During the Last Interglacial (Marine Isotope Stage 5e) High Stand
title_sort decoding the interplay between tidal notch geometry and sea level variability during the last interglacial marine isotope stage 5e high stand
topic tidal notch
cliff erosion numerical model
Last Interglacial MIS 5e
sea level change
geomorphology
Monte Carlo
url https://doi.org/10.1029/2023GL106829
work_keys_str_mv AT ngeorgiou decodingtheinterplaybetweentidalnotchgeometryandsealevelvariabilityduringthelastinterglacialmarineisotopestage5ehighstand
AT pstocchi decodingtheinterplaybetweentidalnotchgeometryandsealevelvariabilityduringthelastinterglacialmarineisotopestage5ehighstand
AT ecasella decodingtheinterplaybetweentidalnotchgeometryandsealevelvariabilityduringthelastinterglacialmarineisotopestage5ehighstand
AT arovere decodingtheinterplaybetweentidalnotchgeometryandsealevelvariabilityduringthelastinterglacialmarineisotopestage5ehighstand