Review of the ammonite genus Pseudokossmaticeras Spath, 1922 from the uppermost Campanian–lower Maastrichtian in Bulgaria

2021 ◽  
Vol 50 (2) ◽  
pp. 3-33
Author(s):  
Docho Dochev ◽  
Lubomir Metodiev
Keyword(s):  
Lower Maastrichtian ◽  
Balkan Area ◽  
Balkan Mountains

New data on the ammonite genus Pseudokossmaticeras Spath, 1922 have been obtained from several uppermost Campanian–lower Maastrichtian strata of the Fore-Balkan Mountains (Bulgaria). A review of the earlier Bulgarian records of the genus is also presented. The following species are here described and illustrated: Pseudokossmaticeras brandti (Redtenbacher, 1873), P. galicianum (Favre, 1869), P. muratovi Michailov, 1951 and P. tercense (Seunes, 1892). Our newly obtained ammonite records were constrained by the inoceramid zonation that has recently been proposed for successions of the Fore-Balkan area. Hence, the Bulgarian data are of importance for correlation with other occurrences of Pseudokossmaticeras across Europe.

scholarly journals Review of the ammonite genus Pseudokossmaticeras Spath, 1922 from the uppermost Campanian–lower Maastrichtian in Bulgaria

2021 ◽  
Vol 50 (2) ◽  
pp. 3-33
Author(s):  
Docho Dochev ◽  
Lubomir Metodiev
Keyword(s):  
Lower Maastrichtian ◽  
Balkan Area ◽  
Balkan Mountains

New data on the ammonite genus Pseudokossmaticeras Spath, 1922 have been obtained from several uppermost Campanian–lower Maastrichtian strata of the Fore-Balkan Mountains (Bulgaria). A review of the earlier Bulgarian records of the genus is also presented. The following species are here described and illustrated: Pseudokossmaticeras brandti (Redtenbacher, 1873), P. galicianum (Favre, 1869), P. muratovi Michailov, 1951 and P. tercense (Seunes, 1892). Our newly obtained ammonite records were constrained by the inoceramid zonation that has recently been proposed for successions of the Fore-Balkan area. Hence, the Bulgarian data are of importance for correlation with other occurrences of Pseudokossmaticeras across Europe.

scholarly journals Inoceramid bivalves from the Maastrichtian of the Western Fore-Balkan Mts (Bulgaria)

2020 ◽  
Vol 49 (1) ◽  
pp. 31-52
Author(s):  
Docho Dochev ◽  
Lubomir Metodiev
Keyword(s):  
Taxonomic Descriptions ◽  
Lower Maastrichtian ◽  
Balkan Mountains

Taxonomic descriptions of newly recorded inoceramid species from the Maastrichtian of the Western Fore-Balkan Mountains (Bulgaria) are presented. The following taxa have been determined: Cataceramus subcircularis (Meek, 1876); Cataceramus palliseri (Douglas, 1942); Cataceramus barabini (Morton, 1834); Cataceramus? glendivensis Walaszczyk, Cobban and Harries, 2001; Cataceramus? cf. bebahoensis (Sornay, 1973); Cataceramus aff. goldfussianus (d’Orbigny, 1847); Trochoceramus tenuiplicatus (Tzankov, 1981); Endocostea typica Whitfield, 1880; Endocostea jolkicevi Walaszczyk, Odin and Dhondt, 2002; Endocostea sp. aff. E. coxi (Reyment, 1955); and “Inoceramus” howletti Walaszczyk, Kennedy and Klinger, 2009. The present record allowed two lower Maastrichtian inoceramid zones, namely the Endocostea typica and Trochoceramus radiosus zones, to be indicated. The material allows for correlation with the Northwestern and Boreal areas of Europe and elsewhere.

scholarly journals Inoceramid bivalve and dinoflagellate cyst integrated biostratigraphy of the topmost Campanian–Maastrichtian in a part of the Western Fore-Balkan Mountains, northwest Bulgaria

2020 ◽  
Vol 49 (3) ◽  
pp. 39-63
Author(s):  
Polina Pavlishina ◽  
Docho Dochev ◽  
Lubomir Metodiev ◽  
Eliza Vladimirova
Keyword(s):  
Depositional Environment ◽  
Dinoflagellate Cyst ◽  
Lower Upper ◽  
Stratigraphic Subdivision ◽  
First Occurrence ◽  
Lower Maastrichtian ◽  
Marine Productivity ◽  
G Ratio ◽  
Balkan Mountains ◽  
Upper Maastrichtian

We present the inoceramid and dinoflagellate cyst record from the topmost Campanian–Maastrichtian strata of three key sections of the Western Fore-Balkan Mountains, northwest Bulgaria. The following inoceramid zones were recognized: “Inoceramus” redbirdensis Zone, Endocostea typica Zone, Trochoceramus radiosus Zone and “Inoceramus” ianjonaensis Zone. The Campanian/Maastrichtian boundary was tentatively drawn slightly below the first occurrence of Endocostea typica. The uppermost inoceramid assemblage was confined to the lower part of the upper Maastrichtian. Dinoflagellate cyst ranges, as well as the first and the last occurrence events of dinocysts, provided valuable markers for the stratigraphic subdivision of the Maastrichtian. The first occurrence of Microdinium carpentierae was documented in proximity to the Campanian/Maastrichtian boundary. The Cerodinium diebelii Zone was recognized with a stratigraphical range from the lower Maastrichtian to the lower upper Maastrichtian. The last occurrence of Alterbidinium acutulum was recorded in the lower Maastrichtian and used as aid for tracing the lower/upper Maastrichtian substage boundary. The marked domination of delicate chorate dinocysts in all sections and the encountered low P/G ratio values are indicative of stable low-energy depositional environment and oligotrophic conditions, with normal marine productivity and nutrient availability in the basin during the Maastrichtian.

Static stress changes associated with normal faulting earthquakes in South Balkan area

2006 ◽  
Vol 96 (5) ◽  
pp. 911-924 ◽  
Author(s):  
E. Papadimitriou ◽  
V. Karakostas ◽  
M. Tranos ◽  
B. Ranguelov ◽  
D. Gospodinov
Keyword(s):  
Static Stress ◽  
Normal Faulting ◽  
Stress Changes ◽  
Balkan Area

Campanian-Maastrichtian ammonite and planktonic foraminiferal biostratigraphy from Tercis, France: Implications for defining the stage boundary

1997 ◽  
Vol 71 (3) ◽  
pp. 407-418 ◽  
Author(s):  
Peter Ward ◽  
William Orr
Keyword(s):  
Planktonic Foraminifera ◽  
New Information ◽  
Biogeographic Provinces ◽  
Lower Maastrichtian ◽  
Stratotype Section ◽  
Stratigraphic Ranges ◽  
Excellent Source ◽  
Source Of Information ◽  
Reference Section ◽  
Upper Campanian

The Campanian-Maastrichtian-aged Grande Carriere quarry near Tercis, southwest France, contains a diverse and abundant assemblage of both micro-and macrofossils from a thick sequence of well-exposed limestones. Its fauna is also a mixture of both Boreal and Tethyan Province species. Because of these two traits, the quarry provides an excellent source of information about integrated biostratigraphic events among diverse taxa, as well as providing a reference section for correlation between the two biogeographic provinces. The quarry has recently been proposed as a candidate for the Campanian/Maastrichtian boundary stratotype section, while one ammonite found there, Pachydiscus neubergicus, has been proposed as the index fossil marking the base of the Maastrichtian Stage. We have made collections of Upper Cretaceous ammonites and planktonic foraminifera from limestones exposed in, and near this site, which yield new information about the relative stratigraphic ranges of Upper Campanian and Lower Maastrichtian ammonites and foraminifera.

A lower Maastrichtian (Upper Cretaceous) concentration Lagerstätte of bourgueticrinid crinoids from the Miechów Trough (southern Poland)

2016 ◽  
Vol 279 (3) ◽  
pp. 239-249 ◽  
Author(s):  
Mariusz A. Salamon ◽  
Rafał Lach ◽  
Anna Wieczorek ◽  
Bruno Ferré ◽  
Tomasz Brachaniec ◽  
...  
Keyword(s):  
Upper Cretaceous ◽  
Southern Poland ◽  
Lower Maastrichtian
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