Naslov
The Cenomanian-Turonian boundary in the northwestern part of the Adriatic Carbonate Platform (Ćićarija Mtn., Istria, Croatia): Characteristics and implications

Autori
Brčić, Vlatko ; Glumac, Bosiljka ; Fuček, Ladislav ; Grizelj, Anita ; Horvat, Marija ; Posilović, Hrvoje ; Mišur, Ivan

Izvornik
Facies (0172-9179) 63 (2017), 3; 17-1

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Cenomanian–Turonian, OAE2, Adriatic Carbonate Platform (AdCP), Ćićarija Mtn., Sv. Duh Formation, Glauconite

Sažetak
The Cenomanian–Turonian boundary (CTB) in the Ćićarija Mountain region (northern Istria, Croatia) is characterised by calcisphere limestone successions with a firmground and glauconite horizon, bioturbated intervals, tempestites and slumped structures as well as microbially laminated and organic rich interbeds deposited in the northwestern part of the intra-Tethyan Adriatic Carbonate Platform (AdCP). Compilation of the results from three studied sections (Vodice–Jelovica, Martinjak and Planik) of litho-, bio-, and microfacies analyses, X-ray diffraction, SEM, EDS and stable isotope analyses allowed reconstruction of marine paleoenvironmental conditions during this time period. Shallow-marine carbonate deposits of the Milna Formation) underlie a drowned-platform succession of the Sveti (Sv.) Duh Formation. The contact between these two formations is sharp and commonly marked by slumped deposits. The Sv. Duh Formation consists of about 100 m calcisphere wackestone enriched in organic matter. The results of preliminary δ13C and δ18O stable isotope analyses indicate the influence of the global Oceanic Anoxic Event (OAE2) on the deposition of this carbonate succession. Anoxic and hypoxic conditions in the water column lead to major changes in the shallow-marine carbonate system of the AdCP. Numerous benthic foraminifera declined during that time, but planktonic foraminifera and calcareous dinoflagellates diversified and expanded greatly. The results of this research provide new insights into the character of the CTB interval in this part of the Tethyan realm. Local and regional synsedimentary tectonics combined with global upper Cretaceous sea-level dynamics allows the correlation of the investigated deeper-marine lithostratigraphic units with OAE2.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA