Ancient Coastal Changes Due to Ground Movements and Human Interventions in the Roman Portus Julius (Pozzuoli Gulf, Italy): Results from Photogrammetric and Direct Surveys

被引:31
作者
Aucelli, Pietro P. C. [1 ]
Mattei, Gaia [1 ]
Caporizzo, Claudia [1 ]
Cinque, Aldo [2 ]
Troisi, Salvatore [1 ]
Peluso, Francesco [1 ]
Stefanile, Michele [3 ]
Pappone, Gerardo [1 ]
机构
[1] Univ Napoli Parthenope, Dipartimento Sci & Tecnol, Ctr Direzionale Is C4, Naples 80121, Italy
[2] Univ Napoli Federico II, Dipartimento Sci Terra Ambiente & Risorse, Largo San Marcellino 10, Naples 80138, Italy
[3] Univ Napoli Orientale, Dipartimento Asia Africa & Mediterraneo, Piazza S Domenico Maggiore 12, Naples 80134, Italy
关键词
coastal changes; vertical ground movements; geoarchaeology; 3D model; relative sea level changes; Campi Flegrei; SEA-LEVEL CHANGES; ERUPTION CAMPI-FLEGREI; NEAPOLITAN YELLOW TUFF; LANDSCAPE EVOLUTION; SORRENTO PENINSULA; MEDITERRANEAN SEA; TYRRHENIAN SEA; HOLOCENE; CALDERA; NAPLES;
D O I
10.3390/w12030658
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This research aims to evaluate the amount of vertical ground movements during Roman times inside the archaeological area of Portus Julius (Gulf of Pozzuoli) using high-precision surveys on the most reliable archaeological sea-level markers. Measuring the submersion of ancient floors, structural elements belonging to a former fish tank, and several roman pilae, two different relative sea levels (RSLs), related to the beginning and the end of the first century BCE, respectively, -4.7/-5.20 m and -3.10 m MSL (mean sea level), were detected. A photogrammetric survey was carried out in order to produce a 3D model of the fish tank. The results in terms of the RSL variations have enabled us to reconstruct a morpho-evolution of the ancient coastal sector during the last 2.1 kyBP. At the beginning of the first century BCE, the area was characterized by a sheltered gulf with numerous maritime villae located along the coast. In 37 BCE, the construction of the military harbour of Portus Julius strongly modified the paleogeography of the sector, which was also affected by a prevailing subsidence at least until the end of the first century BCE (year 12 BCE), when the port was converted into a commercial hub.
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页数:24
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