Page 35 - Studia Universitatis Hereditati, vol 13(2) (2025)

it was particularly important to investigate the We would like to thank the excavation staff,
natural (topographic) conditions alongside oth- in particular Matija Makarun and Mateja Bariče-
er archaeological questions. vić, for sharing the results of the recent rescue ex-
Although the precise timing remains uncer- cavations in Osor (2022–2025) with us. These ex-
tain in the moment, the gradual increase in ter- cavations were led by the Croatian Conservation
14
restrial organic carbon and the initial C data Institute. We would also like to express our sin-
suggest that an increased contribution, possibly cere thanks to Igor Miholjek, Croatian Conserva-
resulting from human activities such as deforest- tion Institute and his team of divers. Our speci-
ation, may have started as early as 5621–5313 cal al goes to the residents of Osor, particularly Ser-
BP (3672–3364 cal BC). It is also plausible that gio Zuclich, Mirjana Jurlina and Đoni Britvec, for
sharing their memories of Osor’s history with us
material from the Lošinj Channel wetland was during countless conversations and their help du-
transported by currents towards Osor Bay. This ring the field work. Finally, we would like to thank
suggests that marine communication through Mia Rizner, Conservation Department in Rijeka, 35
present-day Osor Channel was feasible during for providing efficient support and cooperation.
the Bronze Age. More precise dating and ge-
ochemical proxies will allow marine commu- References
nication through the strait to be determined Allen, J. R. L., and D. M. Thornley. 2004. ‘Laser
more accurately. There is a gradual increase in Granulometry of Holocene Estuarine Silts:
the amount of terrestrial organic carbon enter- Effects of Hydrogen Peroxide Treatment.’ Dip Your Finger in the Sea...
ing the bay from 5.5 to 2.2 cal ka BP (3500–200 Holocene 14 (2): 290–5.
BC), resulting from the significant input of char- Baričević, M. 2023. ‘Kulturno-povijesna urbana
coal caused by human activities in Osor. After cjelina naselja Osor.’ Hrvatski restauratorski
1.7 - 1.4 cal ka BP (270– 584 cal AD), the source zavod, May 28. https://www.hrz.hr
of the organic carbon changes dramatically and /aktualno/novosti-i-obavijesti/kulturno
abruptly. This indicates a gradual decline in the -povijesna-urbana-cjelina-naselja-osor/.
dominance of terrestrial-derived organic carbon Benac, Č., M. Juračić, and I. Blašković. 2008b.
in favour of primary marine production of or- ‘Tidal Notches in Vinodol Channel and
ganic matter. Bakar Bay, NE Adriatic Sea: Indicators of
The results presented in this paper provide Recent Tectonics.’ Marine Geology 248 (3–
deeper insights into questions concerning the 4): 151–60.
coastal area and the maritime accessibility of Benac, Č., M. Juračić, D. Matičec, and I.
Osor. While some of the new findings were ex- Ružić. 2008a. ‘Fluviokarst and Classical
pected, others came as a complete surprise. The Karst: Examples from the Dinarics (Krk
results should encourage further archaeological Island, Northern Adriatic, Croatia).’
Geomorphology 184:64–73.
investigations in the region and demonstrate the Benjamin, J., A. Rovere, A. Fontana, et al. 2017.
value of taking an interdisciplinary approach. ‘Late Quaternary Sea-Level Changes and

Acknowledgements Early Human Societies in the Central
and Eastern Mediterranean Basin: An
The presented paper is part of a research project Interdisciplinary Review.’ Quaternary
Osor beyond the myth, funded by the Austri- International 449:29–57.
an Science Fund (FWF): Grant-DOI: 10.55776/ Benndorf, O. von. 1880. ‘Ausgrabungen in
I6039. For open access purposes, the author has Ossero.’ Archäologisch-epigraphische
applied a CC BY public copyright license to any Mitteilungen aus Österreich 4:73–82.
accepted manuscript version arising from this sub- Blečić Kavur, M. 2014. At the Crossroads of
mission. Worlds at the Turn of the Millennium: The
Late Bronze Age in the Kvarner Region.