2020
DOI: 10.3390/oceans1020007
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The Footprints of the Wreckage of the Italian Royal Navy Battleship Leonardo Da Vinci on the Mar Piccolo Sea-Bottom (Taranto, Southern Italy)

Abstract: Over the last two decades, the scientific interest for marine geophysical surveys has shown a huge increase, mostly for multidisciplinary applicability on different studies, from historical heritage to environmental remediation. One of the main research fields carried out through marine geophysical surveys is the study of the wreckage footprints connected to the seabed perturbation. In 2018, a strategic project planned by the Italian National Government Commissioner for the remediation in the Taranto area (Sou… Show more

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Cited by 6 publications
(5 citation statements)
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“…We conclude that limited environmental information and assessments for the offshore marine areas restricts the possibilities of using quantitative attribute levels. Information from geophysical and sedimentological surveys (see Madricardo et al 2019 [73]; De Giosa et al 2019 [74]; Scardino et al 2020 [75]) and more detailed assessment of the ES supply, using the field data, are relevant for solving these limitations.…”
Section: Discussionmentioning
confidence: 99%
“…We conclude that limited environmental information and assessments for the offshore marine areas restricts the possibilities of using quantitative attribute levels. Information from geophysical and sedimentological surveys (see Madricardo et al 2019 [73]; De Giosa et al 2019 [74]; Scardino et al 2020 [75]) and more detailed assessment of the ES supply, using the field data, are relevant for solving these limitations.…”
Section: Discussionmentioning
confidence: 99%
“…This condition, which characterizes mostly the southwestern sector (Figure 7b,c), is mainly due to the Sn and Hg concentrations. The presence of concentrations exceeding both site-specific and lower CSC values can be related to local phenomena of mixing of the most superficial, unconsolidated soft sediments [61], due mostly to the maritime activities carried out in the basin, whose impacts are also evident from the analysis of the morpho-bathymetric data [42,62,63] To define the thickness and the main geometries of the Holocene sedimentary units, the sub-bottom profiles were accurately interpreted. In particular, SBP data (Figure 8) allowed to highlight the presence of a reflector parallel to the seabed, which can be interpreted as the lower limit of the most recent, coarser, non-stratified, and less consistent sediments.…”
Section: Resultsmentioning
confidence: 99%
“…The potential 3D extent of the contamination can be reconstructed by the interpretation of SBP data, from which the seismic facies limits and the internal reflectors can be recognized allowing the correlation between specific lithology and corresponding lithofacies 89 . Similarly, the exploitation of morpho-acoustic datasets (SSS and MBES data) for the identification and mapping of traces and large litter items on the seafloor highlights the remarkable usefulness of marine surveys for the integrated characterization of marine environments 5 , 60 , 111 . This latter aspect allows to state that the efforts required for performing high-resolution marine morpho-acoustic data can be exploited for a dual purpose and therefore, such kind of data have a high suitability in supporting the geo-environmental characterization of coastal sites 17 .…”
Section: Discussionmentioning
confidence: 99%