Cargando…

Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)

The Pantelleria Vecchia Bank is a submerged calcareous-arenitic shoal in the NW sector of the Sicilian Channel. Together with other morphological heights, some of which are volcanic in origin, this shoal punctuates the shallow Adventure Plateau, which was above sea level from the Last Glacial Maximu...

Descripción completa

Detalles Bibliográficos
Autores principales: Lodolo, Emanuele, Nannini, Paolo, Baradello, Luca, Ben-Avraham, Zvi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10031469/
https://www.ncbi.nlm.nih.gov/pubmed/36967956
http://dx.doi.org/10.1016/j.heliyon.2023.e14575
_version_ 1784910614242525184
author Lodolo, Emanuele
Nannini, Paolo
Baradello, Luca
Ben-Avraham, Zvi
author_facet Lodolo, Emanuele
Nannini, Paolo
Baradello, Luca
Ben-Avraham, Zvi
author_sort Lodolo, Emanuele
collection PubMed
description The Pantelleria Vecchia Bank is a submerged calcareous-arenitic shoal in the NW sector of the Sicilian Channel. Together with other morphological heights, some of which are volcanic in origin, this shoal punctuates the shallow Adventure Plateau, which was above sea level from the Last Glacial Maximum until at least 9000 years ago. The rise in sea level caused by the melting of the ice caps gradually flooded the plateau, isolating the heights and creating a broad archipelago until the area was finally submerged. High-resolution Multibeam bathymetric mapping shows that the Pantelleria Vecchia Bank has an 820 m long rectilinear ridge connecting the two main shoals of the bank, and an 82 m long ridge perpendicular to the 820 m ridge 100 m from its southern end. The top of the 820 m ridge lies in a water depth of 35 m, its base in about 42 m, and the seaward side has a fairly uniform slope of 16°–22°. The 82 m ridge has an average width of ∼7 m and rises ∼1 m above the surrounding seafloor. Underwater photographs document that the entire seaward side of the 820 m ridge consists of juxtaposed blocks, the largest measuring about 3 × 4 m, some of which are rectangular in shape, while the upper part consists of horizontally arranged blocks and the lower part of sub-vertical blocks embedded in the sediments. Petrographic analyses show that the blocks forming the seaward side of the 820 m ridge can be classified as late Pleistocene calcirudites, while the 82 m ridge consists of bioclastic calcarenites of Tortonian age. A series of high-resolution seismic profiles crossing both ridges and composite mosaics of the seafloor obtained from underwater videos provide a comprehensive panorama of these two peculiar and in many ways enigmatic structures. The structures described and the palaeogeographical context in which they are embedded do not exclude the possibility that they are artefacts indicating an ancient temporary or permanent human presence in the Pantelleria Vecchia Bank.
format Online
Article
Text
id pubmed-10031469
institution National Center for Biotechnology Information
language English
publishDate 2023
publisher Elsevier
record_format MEDLINE/PubMed
spelling pubmed-100314692023-03-23 Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel) Lodolo, Emanuele Nannini, Paolo Baradello, Luca Ben-Avraham, Zvi Heliyon Research Article The Pantelleria Vecchia Bank is a submerged calcareous-arenitic shoal in the NW sector of the Sicilian Channel. Together with other morphological heights, some of which are volcanic in origin, this shoal punctuates the shallow Adventure Plateau, which was above sea level from the Last Glacial Maximum until at least 9000 years ago. The rise in sea level caused by the melting of the ice caps gradually flooded the plateau, isolating the heights and creating a broad archipelago until the area was finally submerged. High-resolution Multibeam bathymetric mapping shows that the Pantelleria Vecchia Bank has an 820 m long rectilinear ridge connecting the two main shoals of the bank, and an 82 m long ridge perpendicular to the 820 m ridge 100 m from its southern end. The top of the 820 m ridge lies in a water depth of 35 m, its base in about 42 m, and the seaward side has a fairly uniform slope of 16°–22°. The 82 m ridge has an average width of ∼7 m and rises ∼1 m above the surrounding seafloor. Underwater photographs document that the entire seaward side of the 820 m ridge consists of juxtaposed blocks, the largest measuring about 3 × 4 m, some of which are rectangular in shape, while the upper part consists of horizontally arranged blocks and the lower part of sub-vertical blocks embedded in the sediments. Petrographic analyses show that the blocks forming the seaward side of the 820 m ridge can be classified as late Pleistocene calcirudites, while the 82 m ridge consists of bioclastic calcarenites of Tortonian age. A series of high-resolution seismic profiles crossing both ridges and composite mosaics of the seafloor obtained from underwater videos provide a comprehensive panorama of these two peculiar and in many ways enigmatic structures. The structures described and the palaeogeographical context in which they are embedded do not exclude the possibility that they are artefacts indicating an ancient temporary or permanent human presence in the Pantelleria Vecchia Bank. Elsevier 2023-03-15 /pmc/articles/PMC10031469/ /pubmed/36967956 http://dx.doi.org/10.1016/j.heliyon.2023.e14575 Text en © 2023 The Authors. Published by Elsevier Ltd. https://creativecommons.org/licenses/by-nc-nd/4.0/This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
spellingShingle Research Article
Lodolo, Emanuele
Nannini, Paolo
Baradello, Luca
Ben-Avraham, Zvi
Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title_full Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title_fullStr Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title_full_unstemmed Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title_short Two enigmatic ridges in the Pantelleria Vecchia Bank (NW Sicilian Channel)
title_sort two enigmatic ridges in the pantelleria vecchia bank (nw sicilian channel)
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10031469/
https://www.ncbi.nlm.nih.gov/pubmed/36967956
http://dx.doi.org/10.1016/j.heliyon.2023.e14575
work_keys_str_mv AT lodoloemanuele twoenigmaticridgesinthepantelleriavecchiabanknwsicilianchannel
AT nanninipaolo twoenigmaticridgesinthepantelleriavecchiabanknwsicilianchannel
AT baradelloluca twoenigmaticridgesinthepantelleriavecchiabanknwsicilianchannel
AT benavrahamzvi twoenigmaticridgesinthepantelleriavecchiabanknwsicilianchannel