Organic-walled dinoflagellate cyst biostratigraphy of the Well Höflein 6 in the Cretaceous–Paleogene Rhenodanubian Flysch Zone (Vienna Basin, Austria)

Mohamed, Omar; Wagreich, Michael

doi:10.2478/geoca-2013-0015

Cited by 24 publications

(8 citation statements)

References 27 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Bujak et al 1980;Williams et al 2004). The present specimens either prove that (i) G. semitecta first appeared in the Campanian (see also Mohamed and Wagreich 2013), or (ii) constitute a separate, although similar species. The latter option seems to be more reasonable in the presented estimation.…”

Section: Recorded Stratigraphical Rangesupporting

confidence: 53%

Dinoflagellate cysts from the Upper Cretaceous (upper Campanian to lowermost Maastrichtian) of the Middle Vistula River section, Poland

Niechwedowicz

2021

Palynology

View full text Add to dashboard Cite

In this article, the most representative dinoflagellate cyst genera and species recognised in the rich palynomorph assemblages of the upper Campanian-lowermost Maastrichtian succession of the Middle Vistula River section (central Poland) are treated taxonomically: in particular, six genera and 16 species are considered. Oligosphaeridium araneum sp. nov., which possesses processes with relatively long and slim stems and perforate or fenestrate terminations, is described as new. Glaphyrocysta pala comb. nov. and Hystrichosphaeridium brevispinum stat. nov. are proposed. Glaphyrocysta pala comb. nov. has a dorso-ventrally compressed central body and lacks mid-ventral processes connecting the central body with the membrane, suggesting its affinity with Glaphyrocysta, rather than Riculacysta; and H. brevispinum stat. nov. is raised to species rank on the basis of the distinct morphology of its processes. The tabulation pattern and plate arrangement are determined for the first time in Amphorosphaeridium and revised in Callaiosphaeridium. Both genera have a sexiform hypocystal configuration, L-type ventral organisation, and neutral torsion, which indicates their inclusion in the subfamily Leptodinioideae. The species-level taxonomy of the genera Hystrichosphaeridium and Samlandia is discussed. The transfer of Hystrichosphaeridium proprium to Hystrichokolpoma is rejected, and Hystrichosphaeridium? recurvatum is questionably left in Hystrichosphaeridium, although it is characterised by a commonly larger number of processes per plate and the lack of a preapical process.

show abstract

Section: Recorded Stratigraphical Rangesupporting

confidence: 53%

Dinoflagellate cysts from the Upper Cretaceous (upper Campanian to lowermost Maastrichtian) of the Middle Vistula River section, Poland

Niechwedowicz

2021

Palynology

View full text Add to dashboard Cite

show abstract

“…Many of these studies describe diverse and abundant dinocyst assemblages, characteristic of the uppermost Maastrichtian and lowermost Danian (Wilson,1974;J.M. Hansen, 1979;De Coninck and Smit,1982;Firth,1987Firth, , 1993Hultberg and Malmgren, 1987;Habib et al,1992;Moshkovitz and Habib, 1993;Schiøler and Wilson, 1993;Olsson et al, 1997;Schiøler et al,1997;Nøhr-Hansen and Dam,1997;Mohamed and Wagreich, 2013;Vellekoop et al, 2016). Others, often the thinner successions, are usually not very productive and yield poor or barren dinocyst assemblages (Gedl, 2004;Beiranvand et al, 2014;Machalski et al, 2016).…”

Section: Dinocyst Occurrences and Biostratigraphic Markersmentioning

confidence: 99%

Dinocyst stratigraphy and palaeoenvironmental interpretation of the Cretaceous/Paleogene boundary at Stevns Klint, Denmark

FitzPatrick

Forber

Hart

2018

Cretaceous Research

View full text Add to dashboard Cite

A re-examination of the uppermost Maastrichtian chalks and an expanded section of the Fish Clay (Fiskeler Member) undertaken at Stevns Klint, Denmark, one of the classic outcrops of the Cretaceous/Palaeogene boundary, has identified diverse and abundant dinoflagellate cyst assemblages, which are compared with earlier dinoflagellate cyst (dinocyst) studies. The uppermost part of the white coccolith chalk (Sigerslev Member) of the uppermost Maastrichtian is placed in the Palynodinium grallator Zone. The overlying 'Grey Chalk' (Højerup Member) represents a shallowerwater marine succession that is characterised by a series of dune-like structures. The last common occurrence of P. grallator is within the Højerup Member, confirming the Danian age for the Fish Clay (Fiskeler Member) and a latest Maastrichtian age for the P. grallator Zone. Within the Fiskeler Member, Damassadinium californicum (previously known as Danea californica), a key biostratigraphical marker, is only intermittently present, while the distributions of Senoniasphaera inornata and

show abstract

“…In nearby ar eas, in situ Apectodinium spp. were reported from the Rhenodanubian Flysch Zone (Mohamed and Wagreich, 2013).…”

Section: Introductionmentioning

confidence: 99%

The Apectodinium spp. acme as an evidence for the Paleocene-Eocene thermal maximum from the Polish Outer Carpathians

Cybulska

Rubinkiewicz

2020

View full text Add to dashboard Cite

Organic-walled dinoflagellate cyst biostratigraphy of the Well Höflein 6 in the Cretaceous–Paleogene Rhenodanubian Flysch Zone (Vienna Basin, Austria)

Cited by 24 publications

References 27 publications

Dinoflagellate cysts from the Upper Cretaceous (upper Campanian to lowermost Maastrichtian) of the Middle Vistula River section, Poland

Dinoflagellate cysts from the Upper Cretaceous (upper Campanian to lowermost Maastrichtian) of the Middle Vistula River section, Poland

Dinocyst stratigraphy and palaeoenvironmental interpretation of the Cretaceous/Paleogene boundary at Stevns Klint, Denmark

The Apectodinium spp. acme as an evidence for the Paleocene-Eocene thermal maximum from the Polish Outer Carpathians

Contact Info

Product

Resources

About