Lodolo Emanuele, Nannini Paolo, Baradello Luca, Ben-Avraham Zvi
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy.
Soprintendenza Archeologia Belle Arti e Paesaggio per le Province di Siena, Grosseto e Arezzo, Italy.
Heliyon. 2023 Mar 15;9(3):e14575. doi: 10.1016/j.heliyon.2023.e14575. eCollection 2023 Mar.
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.
潘泰莱里亚韦基亚浅滩是西西里海峡西北部一个水下钙质砂质浅滩。该浅滩与其他一些形态高地(其中一些起源于火山)一起,点缀着浅海探险高原,该高原自末次盛冰期以来一直高于海平面,至少持续到9000年前。冰盖融化导致海平面上升,逐渐淹没了高原,使这些高地孤立起来,形成了一个广阔的群岛,直到该地区最终被淹没。高分辨率多波束测深测绘显示,潘泰莱里亚韦基亚浅滩有一条820米长的直线型海脊连接浅滩的两个主要浅滩,还有一条82米长的海脊,在距离其南端100米处垂直于820米的海脊。820米海脊的顶部位于水深35米处,底部约在42米处,向海一侧有相当均匀的16°-22°坡度。82米的海脊平均宽度约为7米,比周围海底高出约1米。水下照片记录显示,820米海脊的整个向海一侧由并列的石块组成,最大的石块尺寸约为3×4米,其中一些呈长方形,而上部由水平排列的石块组成,下部由嵌入沉积物中的近垂直石块组成。岩石学分析表明,构成820米海脊向海一侧的石块可归类为晚更新世的砾屑灰岩,而82米的海脊由托尔托纳阶的生物碎屑砂屑灰岩组成。一系列穿过这两条海脊的高分辨率地震剖面以及从水下视频获得的海底复合拼图,提供了这两个独特且在许多方面神秘的构造的全面全景。所描述的构造以及它们所处的古地理背景并不排除它们是表明潘泰莱里亚韦基亚浅滩曾有古代临时或永久人类存在的人工制品的可能性。