Morphology of the submerged Ferdinandea Island, the ‘Neverland’ of the Sicily Channel (central Mediterranean Sea)

ABSTRACT We present the bathy-morphological map at a scale of 1: 50,000 of the area around the submerged Ferdinandea Island, the ‘Neverland’ of the Sicily Channel (central Mediterranean Sea). We investigate an area of 100 km2, between 10 and 350 m, which is part of a triangular morphological high, 360 km2 wide, representing the SE-wards prolongation of the Adventure Bank. The study is based on the morphometric analysis based on high resolution multibeam, and sub-bottom CHIRP profiles collected in 2015. The area around the remains of Ferdinandea Island is morphologically shaped by the interplay between volcanic, tectonic, fluid seepage, and oceanographic processes. Since the study area is considered a hot spot of biodiversity affected by maritime traffic (especially in Ferdinandea Channel) and hosting communication pipelines, this map provides insights both for habitat mapping purposes and preliminary marine geohazard assessment due to the occurrence of historically active submarine volcanoes, pockmarks, and mass transport deposits.

[1]  C. Faccenna,et al.  Shear‐Velocity Structure and Dynamics Beneath the Sicily Channel and Surrounding Regions of the Central Mediterranean Inferred From Seismic Surface Waves , 2022, Geochemistry, Geophysics, Geosystems.

[2]  A. Sulli,et al.  Seismic stratigraphy of the north-westernmost area of the Malta Plateau (Sicily Channel): The Middle Pleistocene-Holocene sedimentation in a tidally influenced shelf , 2022, Marine Geology.

[3]  A. Sulli,et al.  First Evidence of Contourite Drifts in the North-Western Sicilian Active Continental Margin (Southern Tyrrhenian Sea) , 2021, Journal of Marine Science and Engineering.

[4]  T. Romeo,et al.  Species and habitats of conservation interest in the Ecologically and Biologically Significant Area of the Strait of Sicily: a contribution towards the creation of a Specially Protected Areas of Mediterranean Importance , 2021, Mediterranean Marine Science.

[5]  A. Micallef,et al.  Depositional mechanism of the upper Pliocene-Pleistocene shelf-slope system of the western Malta Plateau (Sicily Channel) , 2021 .

[6]  C. Romagnoli,et al.  Evaluating the distribution of priority benthic habitats through a remotely operated vehicle to support conservation measures off Linosa Island (Sicily Channel, Mediterranean Sea) , 2021 .

[7]  M. Agate,et al.  Growth and geomorphic evolution of the Ustica volcanic complex at the Africa-Europe plate margin (Tyrrhenian Sea) , 2020 .

[8]  S. Mazzola,et al.  Spawning ecology of the European anchovy (Engraulis encrasicolus) in the Strait of Sicily: Linking variations of zooplankton prey, fish density, growth, and reproduction in an upwelling system , 2020 .

[9]  M. Coltelli,et al.  The Graham Volcanic Field Offshore Southwestern Sicily (Italy) Revealed by High-Resolution Seafloor Mapping and ROV Images , 2019, Front. Earth Sci..

[10]  A. Micallef,et al.  Active degassing across the Maltese Islands (Mediterranean Sea) and implications for its neotectonics , 2019, Marine and Petroleum Geology.

[11]  R. Cas,et al.  Why Deep-Water Eruptions Are So Different From Subaerial Eruptions , 2018, Front. Earth Sci..

[12]  A. Micallef,et al.  Evidence of active fluid seepage (AFS) in the southern region of the central Mediterranean Sea , 2018, Measurement.

[13]  A. Micallef,et al.  The Graham Bank (Sicily Channel, central Mediterranean Sea): Seafloor signatures of volcanic and tectonic controls , 2018, Geomorphology.

[14]  T. Romeo,et al.  Mediterranean banks in EBSA area: Hotspots of biodiversity under threat. , 2017, Marine environmental research.

[15]  T. Romeo,et al.  Fish Distribution and Habitat Complexity on Banks of the Strait of Sicily (Central Mediterranean Sea) from Remotely-Operated Vehicle (ROV) Explorations , 2016, PloS one.

[16]  D. Patanè,et al.  Exploring the submarine Graham Bank in the Sicily Channel , 2016 .

[17]  A. M. Conte,et al.  The 1891 submarine eruption offshore Pantelleria Island (Sicily Channel, Italy): Identification of the vent and characterization of products and eruptive style , 2014 .

[18]  R. Geletti,et al.  Magnetic signature of the Sicily Channel volcanism , 2012, Marine Geophysical Research.

[19]  I. Fontana,et al.  Distribution and spatial structure of pelagic fish schools in relation to the nature of the seabed in the Sicily Straits (Central Mediterranean) , 2009 .

[20]  G. Alvarado,et al.  Morphometry and evolution of arc volcanoes , 2009 .

[21]  Luigi Tortorici,et al.  Relationships between magmatism and tectonics in a continental rift: The Pantelleria Island region (Sicily Channel, Italy) , 2008 .

[22]  P. Galea Seismic history of the Maltese islands and considerations on seismic risk , 2007 .

[23]  F. Chiocci,et al.  The Ischia debris avalanche: first clear submarine evidence in the Mediterranean of a volcanic island prehistorical collapse , 2006 .

[24]  Massimo Pompilio,et al.  Petrology and Geochemistry of Submarine Volcanism in the Sicily Channel Rift , 2006, The Journal of Geology.

[25]  James V. Gardner,et al.  The significance of pockmarks to understanding fluid flow processes and geohazards , 2002 .

[26]  A. Robinson,et al.  Features of dominant mesoscale variability, circulation patterns and dynamics in the Strait of Sicily , 2001 .

[27]  A. Felpeto,et al.  Submarine volcanism surrounding Tenerife, Canary Islands: implications for tectonic controls, and oceanic shield forming processes , 2000 .

[28]  J. Osler,et al.  A High Resolution Seismic Sequence Analysis of the Malta Plateau , 1999 .

[29]  C. Millot Circulation in the Western Mediterranean Sea , 1999 .

[30]  G. Serri,et al.  The Strait of Sicily continental rift systems: Physiography and petrochemistry of the submarine volcanic centres , 1989 .

[31]  J. Woodside,et al.  Geologic structure and neotectonics of the North African Continental Margin south of Sicily , 1985 .

[32]  T. Levesque,et al.  Campaign Resource Allocations Under the Electoral College , 1975, American Political Science Review.

[33]  H. S. Washington Submarine eruptions of 1831 and 1891 near Pantelleria , 1909 .

[34]  M. Kervyn,et al.  Systematic morphometric characterization of volcanic edifices using digital elevation models , 2012 .

[35]  G. Corti,et al.  Coexisting geodynamic processes in the Sicily Channel , 2006 .

[36]  Javier Delgado,et al.  Hydrographic phenomena influencing early life stages of the Sicilian Channel anchovy , 2002 .

[37]  S. Swift,et al.  Gas venting and late Quaternary sedimentation in the Persian (Arabian) Gulf , 1996 .

[38]  Jeffrey P. Ellis,et al.  Pockmarks of the Northwestern Arabian Gulf , 1986 .