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A census of 83 Infralittoral Prograding Wedges (IPWs) was carried out in the Central-Eastern Tyrrhenian Sea, to learn more about their morpho-bathymetric variability and test their reliability as environmental indicators of current sea level. With this aim, a database recording for each wedge the main morphometric indices, the effective fetch and the significant height of the storm waves– here used as proxies for sea state forcing to which they are exposed- and the ground elevation in the backshore - here used as a numerical descriptor of coastal morphology and energy of the relief- was realized (Campania Region IPWs Database). The statistical analysis on the entire IPWs dataset explored the relationship between the environmental and morphometric variables while the Principal Component Analysis grouped the variables into two clusters, governed by sea state forcing and energy of relief in the backshore, respectively. The multi-regression analysis highlighted a significant correlation of IPWs depth with effective fetch and extreme significant wave height and a moderate correlation with the ground elevation in the backshore. The outcomes that emerged from the observational law on present-day IPWs were then applied to relict IPWs, currently lying on the continental shelf and at the shelf margin, with the aim of establishing their original depth of formation. This procedure aims to solve the non-trivial issue, namely that concerning the reliability of paleo-IPWs as proxies for past sea levels. Thus, a simplified equation based only on the use of geographical variables is proposed here to roughly establish the original depth (with errors of few metres) of paleo-IPWs, whose geographical exposure is known and the effective fetch computable. Although the applicability of this method suffers from spatial and temporal restrictions, due to the girth of the original dataset, it provides a first analytical procedure for gauging the original depth of formation of paleo-IPWs which, over the last decade, have been increasingly used as environmental indicators of past sea levels. This study highlights the relationship between the depth of these sedimentary coastal bodies and sea storm wave climate at a regional scale and provides clues for the use of their past counterparts as morphological proxies of past sea level stands. Further developments of this study would use a wider dataset so as to extend the observational law on present-day IPWs to a Mediterranean scale and strengthen the applicability of the method to a spatially broader set of paleo-IPWs.

This article reports on the dataset gathered following the census of 83 present-day Infralittoral Prograding Wedges (IPWs), surveyed on the inner continental shelf of the Central-Eastern Tyrrhenian Sea. The purpose of the census was to explore their bathymetric range and assess the observational laws governing this variability. The ensued dataset (Campania Region IPW Dataset, CRID) includes geographic, topographic and morpho-bathymetric indices, descriptive of each IPW and more, the exposure of each IPW to wave forcing (Geographical fetch, Effective fetch and extreme significant wave height, HS). In this work, histograms contribute to describe all the variables and highlight the dominant features of each IPW. Location maps univocally links the geographic position of each IPW to the appropriate attribute record in the dataset. Further, thematic maps illustrate eight wave fields obtained by offshore-to-nearshore transformation by as many sea states scenarios with 200-year return period. Such wave fields are used as sources for significant wave height representing wave conditions over each IPW. This dataset could be implemented with new measures at a broader scale, by following analogue procedures for measurements, to enlarge the observational scale on IPWs and improve the numerical models which might eventually derive by the analysis of this dataset.

A fronte di un'intensa e profonda attività di ricerca, in ambito petrologico, vulcanologico, geochimico e geodinamico, in relazione all'evoluzione e alle caratteristiche del vulcanismo nell'area mediterranea, poco sforzo è stato speso per un'adeguata comprensione dei processi idrotermali che interessano aree estremamente complesse, dal punto di vista geologico, come quella del mar Tirreno meridionale. In quest'area insistono sistemi di bacini di retroarco e sistemi di roll back in corrispondenza di noti seamounts (Marsili, Palinuro, Vavilov), nonché attività magmatica tipica di arco di isole (in corrispondenza del gruppo delle Eolie) con magmatismo assai diverso in evoluzione verso un sistema calcalino alto in potassio. Al fine di individuare potenziali flussi idrotermali in suddetta zona, è stata instaurata una collaborazione tra i ricercatori del nostro Istituto ( IAMC-CNR di Napoli), e dell'Osservatorio Vesuviano (INGV) di Napoli, con il gruppo di ricercatori del NOAA di Seattle e del GNS neozelandese, considerati leader nel campo delle ricerche di plumes idrotermali in aree geodinamicamente attive del pianeta (Arco delle Marianne, Arco Egeo, area di Tonga, etc.). È stata, quindi, pianificata una campagna oceanografica focalizzata su un survey sistematico delle attività idrotermali potenzialmente presenti nell'area meridionale del mar Tirreno.