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Ammonite occurrence in the Barremian-Aptian boundary beds in North-Eastern Bulgaria.

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Abstract

Studies are conducted on the ammonite sequences in cross-sections of the Lower Cretaceous on the basis of which two ammonite zones are separated in the Lower Aptian sediments: Procheloniceras pachystephanum and Deshayesites deshayesi. In the beds around the Barremian-Aptian boundary in a cross-section at Kacelovo village is established a rarely encountered joint development of the ammonite genera Colchidites and Procheloniceras. The precise dating of this stratigraphic level suggests that the representatives of Colchidites genus have continued their existence after this boundary in the beginning of the Aptian Age.-from Abstracts of Bulgarian Scientific Literature
... By the beginning of the 1980s only the Deshayesites deshayesi Zone had been clearly defined (Dimitrova et al., 1961;Nikolov, 1962Nikolov, , 1969Manolov, 1962;Breskovski and Dimitrova, 1968;Dimitrova et al., 1972). New biostratigraphic data were published subsequently (Nikolov et al., 1983;Stoykova, 1986Stoykova, , 1990Ivanov, 1992Ivanov, , 1995Ivanov and Stoykova, 2001). Recently intensive investigations have been carried out on the Barremian and partially on the Aptian Stage Idakieva, 2008, 2009). ...
Article
Sediments of Early Aptian age in Bulgaria can be assigned to four different facies: platform carbonates (Urgonian complex), shallow-water siliciclastics, hemipelagic and flyschoid siliciclastics. The taxonomic analysis of the ammonite faunas of 18 sections from these four different facies resulted in a revision of the existing ammonite zonation scheme so far applied in Bulgaria and adjoining areas. A new biostratigraphic scheme, which bridges the western and eastern Tethys, is thereby proposed for the Lower Aptian of Bulgaria.
Chapter
In general, the ammonite successions of Bulgaria agree with those of the rest of the Mesogée. However, some particularities make it evident that these faunas form the link between those of Western Europe and the Crimea-Caucasus region. This has to be considered when biogeographical questions concerning the Lower Cretaceous are discussed. Each of the numerous biostratigraphical zonations contains a certain speculative element and is therefore not very satisfactory for the geological correlation and for the solution of still open biostratigraphical problems. Only physically existing sections may reveal the vertical distribution of ammonites and are therefore suitable for solving these problems. The Bulgarian sections are continuous and rich in ammonites. They are therefore important for solving the biostratigraphical problems of the Lower Cretaceous.
Article
The study, in terms of sequence stratigraphy (with ammonite zone control), of numerous cross-sections of Lower Cretaceous (Hauterivian to Aptian) series cropping out along two transects A-B (Fore Balkan and southern part of the Moesian Platform) and C-D (northeastern part of the Moesian Platform) shows the eastwards extension of the North-Tethyan palaeogeographic pattern platform-basin-platform, previously established in central Bulgaria. However, the two boundaryplatforms are strongly assymetrical, this assymetry being revealed by the importance, to the south, of the relative lowstand prograding siliciclastic bodies (supplied by continental erosions linked to extensional tectonics) during the synrift phase (not marked to the north) and by the age, the facies (oolitic to the north, Urgonian to the south) and the number of the calcareous tongues interpreted as the transgressive systems tracts of backstepping depositional sequences, well-marked at the shelf/basin transition.
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