Integrated biostratigraphy and palaeoenvironmental interpretation of the Upper Cretaceous to Paleocene succession in the northern Moldavidian Domain (Eastern Carpathians, Romania)

Ţabără, Daniel; Slimani, Hamid; Mare, Silvia; Chira, Carmen

doi:10.1016/j.cretres.2017.04.021

Cited by 19 publications

(6 citation statements)

References 55 publications

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“…In this type of assemblages the total quantity of Caudammina and H. velascoensis reached up to 45% of the assemblage. An increased number of C. ovulum was reported from the Paleocene of the Eastern Outer Carpathians [45,46], from the Boreal realm from the uppermost Cretaceous [38] and in the Paleocene of the Tasman Sea. The relative abundance of P. placenta and/or Saccammina grzybowskii (Schubert) (Figures 7 and 8) ranges 10% or more in the foraminiferal assemblage.…”

Section: Remarksmentioning

confidence: 99%

“…placenta dominated assemblages were described from the Moravian Paleocene [47]; assemblages with abundance of P. placenta were mentioned in many papers referring to the Outer Carpathian Paleocene deposits [16,[40][41][42]44,[48][49][50][51], as well as the upper Cretaceous and Paleocene deposits, both in the Magura and Silesian domains as well [15,28,52,53]. High amounts of P. placenta were observed in the uppermost Paleocene of the Eastern Carpathians [46].…”

Section: Remarksmentioning

confidence: 99%

“…It was noticed in the Silesian Nappe [28,[55][56][57][58] and in other Western Outer Carpathian areas [30,52], significant amounts were the basis for distinguishing the C. excelsa-R. inclusa beds [57]. In the Eastern Outer Carpathians, the relatively abundant occurrence of C. excelsa is known from the Paleocene [45,46], as well as from the uppermost Cretaceous of the Boreal realm [38].…”

Section: Occurrence and Age Assignmentmentioning

confidence: 99%

“…Relatively abundant H. velascoensis was described in Paleocene deposits of the Magura Nappe [19,40] and in the Paleocene of the Subsilesian Nappe [14,18,61,62]. A value of 6.7% of H. velascoensis was mentioned from the Paleocene of the Eastern Carpathians [46], about a 10% share was reported from Bulgaria [63].…”

Section: Remarksmentioning

confidence: 99%

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Agglutinated Foraminiferal Acmes and Their Role in the Biostratigraphy of the Campanian–Eocene Outer Carpathians

Waśkowska

2021

Geosciences

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The biostratigraphy of the Outer Carpathians is based mainly on the ranges of agglutinated foraminifera. Species acmes provide the opportunity to enhance and support the existing biozonations. Assemblages of agglutinated foraminifera from the Campanian to Eocene of various tectonic-structural units were analyzed in terms of their qualitative and quantitative occurrence. In this stratigraphic interval, 19 species display significantly increased abundance within a relatively short interval: Caudammina gigantea (Geroch) (upper Santonian–lowermost Maastrichtian), Caudammina ovulum (Grzybowski) (Campanian–Danian), Placentammina placenta (Grzybowski)-Saccammina grzybowskii (Schubert) (upper Campanian–Danian), Caudammina excelsa (Dylążanka) (lowermost Maastrichtian–Danian), Caudammina ovuloides (Grzybowski) (Danian–Selandian), Hormosina velascoensis (Cushman) (upper Danian–Selandian), Praesphaerammina gerochi (Hanzlíková) (Thanetian), Glomospira charoides (Jones et Parker)-Glomospira gordialis (Jones et Parker) (uppermost Thanetian–lowermost Ypresian), Trochammina spp. (upper Thanetian–lower Ypresian), Reticulophragmium amplectens (Grzybowski) (Lutetian–Bartonian), Reophax duplex (Grzybowski)-Reophax “pilulifer” Brady group of taxa (Lutetian–Priabonian), Haplophragmoides walteri (Grzybowski)-Haplophragmoides nauticus Kender, Kaminski et Jones (Lutetian–Bartonian), Spiroplectammina spectabilis (Grzybowski) (Lutetian–Priabonian), “Ammodiscus” latus Grzybowski (Bartonian–Priabonian), Praesphaerammina subgaleata (Vašíček) (Lutetian–Bartonian). The biostratigraphic position and quantitative data of species with increased abundance are presented.

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Section: Remarksmentioning

confidence: 99%

Section: Remarksmentioning

confidence: 99%

Section: Occurrence and Age Assignmentmentioning

confidence: 99%

Section: Remarksmentioning

confidence: 99%

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Agglutinated Foraminiferal Acmes and Their Role in the Biostratigraphy of the Campanian–Eocene Outer Carpathians

Waśkowska

2021

Geosciences

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“…These deposits were assigned to the Kremna Formation by Oszczypko & Oszczypko-Clowes (2014 Bujak & Mudge 1994, Powel et al 1996, Iakovleva et al 2001, Slimani et al 2012, Soliman 2012, Mohamed et al 2012, 2013, Mohamed & Wagreich 2013, Țabără et al 2017. Representatives of the genera Glaphyrocysta and Areoligera as well as A. homomorphum, and C. diversispinosum are common.…”

mentioning

confidence: 99%

The tectonics and stratigraphy of the transitional zone between the Pieniny Klippen Belt and Magura Nappe (Szczawnica area, Poland)

Jurewicz

Segit

2018

geol

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Abstract:The Pieniny Klippen Belt is a narrow, complex structure stretching along a tectonic boundary between the Central and Outer Carpathians. Its formation involved two main evolutionary stages, the first, related to Late Cretaceous-Paleocene folding and thrusting, and the second, associated with Miocene orogenic events in the Outer Carpathians. Interactions between the Pieniny Klippen Belt and Outer Carpathians during both the sedimentation and deformation stages have resulted in the establishment of a peri-klippen transitional zone (named the Šariš Transitional Zone), in which the tectonic deformation effects gradually decrease towards the north. The stratigraphy and tectonic position of this zone have been controversial for decades. The key stratigraphic problems concern 1) the lithologic identity and position of the Szlachtowa ("black flysch"), Opaleniec and Pieniny formations and 2) the relation of the Jarmuta Formation, associated mainly with the Šariš Transitional Zone, to the Szczawnica and Zarzecze formations of the Magura Nappe. We provide an early Paleogene dinoflagellate cyst stratigraphic record of deposits that, according to some recent reinterpretations, represent the Neogene "Kremna Formation". The legitimacy of new lithostratigraphic assignments of the "Kremna Formation" at Jaworki is put into question upon the basis of the primacy of units introduced for the same strata earlier.

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Pentadinium dababiyaense: A new organic-walled dinoflagellate cyst from the Upper Cretaceous, Dababiya, Egypt

Soliman

Slimani

2019

Cretaceous Research

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Integrated biostratigraphy and palaeoenvironmental interpretation of the Upper Cretaceous to Paleocene succession in the northern Moldavidian Domain (Eastern Carpathians, Romania)

Cited by 19 publications

References 55 publications

Agglutinated Foraminiferal Acmes and Their Role in the Biostratigraphy of the Campanian–Eocene Outer Carpathians

Agglutinated Foraminiferal Acmes and Their Role in the Biostratigraphy of the Campanian–Eocene Outer Carpathians

The tectonics and stratigraphy of the transitional zone between the Pieniny Klippen Belt and Magura Nappe (Szczawnica area, Poland)

Pentadinium dababiyaense: A new organic-walled dinoflagellate cyst from the Upper Cretaceous, Dababiya, Egypt

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