Pregled bibliografske jedinice broj: 449393
Relative Sea-Level Change during the Late Holocene on the Island of Vis (Croatia) - Issa Harbour Archaeological Site
Relative Sea-Level Change during the Late Holocene on the Island of Vis (Croatia) - Issa Harbour Archaeological Site // Geodinamica acta, 23 (2010), 5-6; 209-223 doi:10.3166/ga.23.209-223 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 449393 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Relative Sea-Level Change during the Late Holocene on the Island of Vis (Croatia) - Issa Harbour Archaeological Site
Autori
Faivre, Sanja ; Bakran-Petricioli, Tatjana ; Horvatinčić, Nada
Izvornik
Geodinamica acta (0985-3111) 23
(2010), 5-6;
209-223
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
sea-level change ; submerged Issa harbour ; tidal notch ; coralline algae ; Adriatic Sea
Sažetak
The 2.4 ka shoreline evolution on the Island of Vis has been investigated. It represents a particularly interesting area for this kind of investigation due to the existence of the submerged archaeological remains, the antique port of Issa, as well as to the existence of geomorphological and biological sea-level markers. The actual depths of the different parts of the submerged quay have been mapped and measured with respect to the present mean sea-level, applying corrections for tide and atmospheric pressure values at the time of the surveys. The functional heights related to the sea level at the time of construction have also been taken into account. These data were further compared with predictions derived from a glacio-hydro-isostatic model associated with the Last Glacial cycle. During the investigation of the coast, tidal notches and algal rims were found. They were mapped, measured and correlated with results of the submerged port remains, as well as with other available data along the Croatian coast. Our results demonstrate a 199±25 cm sea-level change during 2.4 ka on the Island of Vis. Taking into account the total relative sea-level change, an average rate of around ~0.83 mm/yr is derived. If the isostatic-eustatic component is separated, a tectonic subsidence rate ranges between 0.17 and of 0.3 mm/yr depending on the predicted model used. Compared to the Northern Adriatic area, the Island of Vis shows a much smaller component of tectonic subsidence.
Izvorni jezik
Engleski
Znanstvena područja
Biologija, Geografija
POVEZANOST RADA
Projekti:
098-0982709-2741 - Prirodni radioizotopi u istraživanju krških ekosustava i datiranju (Horvatinčić, Nada, MZOS ) ( CroRIS)
119-0362975-1226 - Istraživanje ugroženih staništa morem preplavljenog krša u obalnom moru Hrvatske (Bakran-Petricioli, Tatjana, MZOS ) ( CroRIS)
119-1191306-1305 - Geomorfološka i geoekološka istraživanja krša RH (Faivre, Sanja, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus