APA 6th Edition Fouache, E., Faivre, S., Dufaure, J., Kovačić, V., Tassaux, F. i Tronche, P. (2004). Morska razina u rimsko doba na području Istre. Vjesnik Arheološkog muzeja u Zagrebu, 37 (1), 173-190. Preuzeto s https://hrcak.srce.hr/18714
MLA 8th Edition Fouache, Eric, et al. "Morska razina u rimsko doba na području Istre." Vjesnik Arheološkog muzeja u Zagrebu, vol. 37, br. 1, 2004, str. 173-190. https://hrcak.srce.hr/18714. Citirano 15.01.2021.
Chicago 17th Edition Fouache, Eric, Sanja Faivre, Jean-Jacques Dufaure, Vladimir Kovačić, Francis Tassaux i Pierre Tronche. "Morska razina u rimsko doba na području Istre." Vjesnik Arheološkog muzeja u Zagrebu 37, br. 1 (2004): 173-190. https://hrcak.srce.hr/18714
Harvard Fouache, E., et al. (2004). 'Morska razina u rimsko doba na području Istre', Vjesnik Arheološkog muzeja u Zagrebu, 37(1), str. 173-190. Preuzeto s: https://hrcak.srce.hr/18714 (Datum pristupa: 15.01.2021.)
Vancouver Fouache E, Faivre S, Dufaure J, Kovačić V, Tassaux F, Tronche P. Morska razina u rimsko doba na području Istre. Vjesnik Arheološkog muzeja u Zagrebu [Internet]. 2004 [pristupljeno 15.01.2021.];37(1):173-190. Dostupno na: https://hrcak.srce.hr/18714
IEEE E. Fouache, S. Faivre, J. Dufaure, V. Kovačić, F. Tassaux i P. Tronche, "Morska razina u rimsko doba na području Istre", Vjesnik Arheološkog muzeja u Zagrebu, vol.37, br. 1, str. 173-190, 2004. [Online]. Dostupno na: https://hrcak.srce.hr/18714. [Citirano: 15.01.2021.]
Sažetak The shores of Istra have long been acknowledged as being characterised by a recent submersion. Numerous submerged Roman ruins on the Istrian peninsula have led to different estimations of
the sea level in the Ist and IInd century AD. Degrassi (1955) proposed 1.5 m below the recent mean sea level, while Vrsalovi} (1979) proposed 2 m. In investigations, carried out since 1999 as part of two international projects: »The oil of Istria« (archaeological project) and »Dynamics and evolution of the Adriatic littoral and human occupation in Holocene (Croatia, Albania)« (geomorphological
project), the question arose again.We have determined precise archaeological markers such as Roman fish-tanks, quarries, jetties and the tidal notch as a geomorphological marker. According to our
investigations the sea level in the Ist and IInd century AD varied between 50 and 60 cm below the recent level.