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Main Authors: Antonioli, Fabrizio, Lo Presti, Valeria, Rovere, Alessio, Ferranti, Luigi, Anzidei, Marco, Furlani, Stefano, Mastronuzzi, Giuseppe, Orru, Paolo E, Scicchitano, Giovanni, Sannino, Gianmaria, Spampinato, Cecilia R, Pagliarulo, Rossella, Deiana, Giacomo, de Sabata, Eleonora, Sansò, Paolo, Vacchi, Matteo, Vecchio, Antonio
Format: Dataset Open Access
Language:en
Published: PANGAEA 2015
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.846652
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author Antonioli, Fabrizio
Lo Presti, Valeria
Rovere, Alessio
Ferranti, Luigi
Anzidei, Marco
Furlani, Stefano
Mastronuzzi, Giuseppe
Orru, Paolo E
Scicchitano, Giovanni
Sannino, Gianmaria
Spampinato, Cecilia R
Pagliarulo, Rossella
Deiana, Giacomo
de Sabata, Eleonora
Sansò, Paolo
Vacchi, Matteo
Vecchio, Antonio
author_facet Antonioli, Fabrizio
Lo Presti, Valeria
Rovere, Alessio
Ferranti, Luigi
Anzidei, Marco
Furlani, Stefano
Mastronuzzi, Giuseppe
Orru, Paolo E
Scicchitano, Giovanni
Sannino, Gianmaria
Spampinato, Cecilia R
Pagliarulo, Rossella
Deiana, Giacomo
de Sabata, Eleonora
Sansò, Paolo
Vacchi, Matteo
Vecchio, Antonio
collection Datos científicos de ciencias marinas y ambientales
contents Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology. Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development. Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_846652
institution PANGAEA
language en
publishDate 2015
publisher PANGAEA
record_format pangaea
spellingShingle A comprehensive analysis of tidal notches in the Mediterranean Sea
Antonioli, Fabrizio
Lo Presti, Valeria
Rovere, Alessio
Ferranti, Luigi
Anzidei, Marco
Furlani, Stefano
Mastronuzzi, Giuseppe
Orru, Paolo E
Scicchitano, Giovanni
Sannino, Gianmaria
Spampinato, Cecilia R
Pagliarulo, Rossella
Deiana, Giacomo
de Sabata, Eleonora
Sansò, Paolo
Vacchi, Matteo
Vecchio, Antonio

Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology. Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development. Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.
title A comprehensive analysis of tidal notches in the Mediterranean Sea
topic
url https://doi.org/10.1594/PANGAEA.846652