Page 39 - Studia Universitatis Hereditati, vol 13(2) (2025)
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‘Multiproxy Assessment of Holocene      es. This narrow waterway, separating the islands
                   Relative Sea-Level Changes in the Western   of Lošinj and Cres, played a key role in maritime
                   Mediterranean: Sea-Level Variability and   trade routes linking Istria and Dalmatia. Geoar-
                   Improvements in the Definition of the   chaeological investigations in the Osor area in-
                   Isostatic Signal.’ Earth-Science Reviews   cluded geophysical surveys, sediment coring, and
                   155:172–97.                             detailed geochemical and grain-size analyses of
               Vinci, G., F. Vanzani, A. Fontana, and S.   sediment cores. Radiocarbon and optically stim-
                   Campana. 2024. ‘LiDAR Applications      ulated luminescence (OSL) dating were employed
                   in Archaeology: A Systematic Review.’   to establish a chronological framework. Integrated
                   Archaeological Prospection 32 (1): 81–101.   airborne laser scanning and multibeam sonar ba-
               Vlahović, I., J. Tišljar, I. Velić, and D. Matičec.   thymetric data provided detailed insights into the
                   2005. ‘Evolution of the Adriatic Carbonate   submerged geomorphology of the area surround-
                   Platform: Paleogeography, Main Events and   ing Osor.
                   Depositional Dynamics.’ Palaeogeography,    A 2.9 m-thick sediment succession (core     39
                   Palaeoclimatology, Palaeoecology 220 (3–4):   OSOR 2), recovered from Osor Bay, enabled the
                   333–60.                                 reconstruction of Holocene palaeoenvironmen-
                                                           tal changes driven by both natural processes in the
               Summary                                     wider region and anthropogenic activities in Osor.
               Sea-level variability during the Late Pleistocene   The OSOR 2 core did not yield unequivocal evi-
               and Holocene profoundly shaped the Mediterra-  dence of human intervention associated with the   Dip Your Finger in the Sea...
               nean region. During the Last Glacial Maximum,   construction of the channel that would resolve
               sea level was approx. 120–134 metres below its pres-  the debate concerning its archaeological construc-
               ent position. The subsequent post-glacial rise led to   tion date. Instead, preliminary results suggest that
               the inundation of extensive coastal areas formerly   the connection between Osor Bay and the Lošinj
               inhabited by human populations, resulting in the   Channel via the Osor Channel was likely estab-
               submergence of numerous coastal archaeological   lished during the Bronze Age, implying that nat-
               sites that remain concealed beneath the sea surface   ural processes played a substantial role in its for-
               today. Consequently, submerged landscapes have   mation. Furthermore, the results indicate that the
               been the focus of many geoarchaeological investi-  Jaz area remained part of the coastal land until
               gations. However, until recently, the eastern Adri-  AD 170 ± 100, when rising sea levels caused ma-
               atic coast has remained relatively understudied in   rine waters to advance inland. On this basis, pres-
               this respect.                               ent-day Jaz Bay can be excluded as a (Roman) city
                   This study focuses on the submerged land-  harbour.
               scapes surrounding Osor, an Iron Age and Ro-
               man town located on the northern Adriatic island   Povzetek
               of Cres. The Osor beyond the myth project arose   Spremembe morske gladine v poznem pleistocenu
               from the need to reinterpret the history of this re-  in  holocenu  so  pomembno  oblikovale  sredozem-
               gional trading port. Given Osor’s coastal setting,   ski prostor. Med zadnjim ledenim maksimumom
               particular emphasis was placed on reconstructing   je bila morska gladina približno 120–134 metrov
               natural (topographic) conditions alongside broad-  nižja kot danes. Poznejši postglacialni dvig morske
               er archaeological questions. The results present-  gladine je povzročil poplavljanje obsežnih obalnih
               ed here offer new insights into Holocene relative   območij, ki so jih naseljevale človeške skupnosti,
               sea-level rise, past environmental changes, and the   kar je vodilo do potopitve številnih obalnih arhe-
               coastal configuration and maritime accessibility of   oloških najdišč, ki so še danes skrita pod morsko
               Osor.                                       gladino. Posledično so potopljene krajine predmet
                   A central research question concerns the con-  številnih geoarheoloških raziskav, vendar je bila
               struction of the Osor Channel, traditionally be-  vzhodna obala Jadranskega morja do nedavnega v
               lieved to have been excavated for maritime purpos-  tem pogledu razmeroma slabo raziskana.
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