Paraticinella rohri () as the valid name for the latest Aptian zonal marker species of planktonic foraminifera traditionally called bejaouaensis or eubejaouaensis

Ando, Atsushi; Huber, Brian T.; Silvá, Isabella Premoli

doi:10.1016/j.cretres.2013.05.002

Cited by 25 publications

(7 citation statements)

References 25 publications

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“…14a). The upper Aptian Paraticinella rohri Zone (P. eubejaouaensis Zone, see Ando et al, 2013) is assigned to 8.65 to 11.09 m (Fig. 14a) and contains Hedbergella gorbachikae and H. trocoidea.…”

Section: Foraminiferal Biostratigraphymentioning

confidence: 99%

The Lindi Formation (upper Albian–Coniacian) and Tanzania Drilling Project Sites 36–40 (Lower Cretaceous to Paleogene): Lithostratigraphy, biostratigraphy and chemostratigraphy

Berrocoso

Huber

MacLeod

et al. 2015

Journal of African Earth Sciences

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Section: Foraminiferal Biostratigraphymentioning

confidence: 99%

The Lindi Formation (upper Albian–Coniacian) and Tanzania Drilling Project Sites 36–40 (Lower Cretaceous to Paleogene): Lithostratigraphy, biostratigraphy and chemostratigraphy

Berrocoso

Huber

MacLeod

et al. 2015

Journal of African Earth Sciences

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“…This is supported by the presence of Pseudoplanomalina cheniourensis (Sigal, 1952) (Fig. 8.12-15), a species that ranges no higher than the lower part of the P. bejaouensis Zone (Moullade et al, 2002;Bellier and Moullade, 2002;Ando et al, 2013). Additional taxa include G. ferreolensis and H. trocoidea (Fig.…”

Section: Globigerinelloides Algerianus Zone: Samples Mttk 187 -Mttk 208mentioning

confidence: 90%

“…Planktonic foraminifera often form 50% or more of the total assemblage. Notwithstanding considerable discussion of the taxonomy of Early Cretaceous planktonic foraminifera (BouDagher-Fadel et al, 1997;Moullade et al, 2002;Moullade, T. L. Luber et al, 2018 / Cretaceous Research 2002;Verga and Premoli Silva 2003a, b; Premoli Silva and Verga, 2004;Ando et al, 2013) and remaining uncertainties regarding precise stratigraphic range, their fundamental stratigraphic utility remains. The taxa are identifiable with reference to the extensive literature on age-equivalent cosmopolitan, Mediterranean and North-West European material (e.g.…”

Section: Figure 7: Prefered Placementmentioning

confidence: 99%

“…9.2-4), two species that range throughout the upper Aptian (Moullade et al, 2002). The name P. bejaouensis is retained for reference to the standard literature, although proposals exist to correct the name of this species and its nominate zone to Paraticinella rohri (Ando et al, 2013).…”

Section: Globigerinelloides Algerianus Zone: Samples Mttk 187 -Mttk 208mentioning

confidence: 99%

“…It is very likely that the uppermost Aptian "H". jacobi Zone is missing in the Tiskatine section as P. cheniourensis occurs near the top of the formation, a species with a LAD well below the top of the Aptian or reported "uppermost Gargasian" (Moullade et al, 2002;Ando, et al, 2013).…”

Section: Age Interpretation -Foraminiferamentioning

confidence: 99%

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A revised chronostratigraphic framework for the Aptian of the Essaouira-Agadir Basin, a candidate type section for the NW African Atlantic Margin.

Luber¹,

Bulot²,

Redfern³

et al. 2018

Preprint

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The Essaouira-Agadir Basin (EAB) of Morocco contains the most extensive exposure of Aptian to Lower Albian strata onshore the NW African Atlantic Margin. This paper documents the first high-resolution, multi-disciplinary stratigraphic approach for the Aptian to Lower Albian on the NW African Atlantic Margin. Previous biostratigraphic work almost exclusively relied on long-distance correlation of ammonoids to the Mediterranean – Caucasian Realm. Recent biostratigraphic work has questioned some of the previous interpretations, highlighting significant faunal endemism and complications with correlation to other key Aptian sections. This study focuses on 5 key sections: Tiskatine, Id Amran, Assaka, and DSDP 416/370. Distribution of ammonoids, foraminifera, and calcareous nannofossils are reported from a bed-by-bed collection made at Tiskatine.The analysis of foraminiferal and calcareous nannofossil assemblages enable correlation to standard zonation schemes; but also highlights the urgent need of revision and future work on the integration of these schemes across disciplines. The study, further, includes δ13Ccarb, δ13Corg, and total organic carbon (TOC) data that is compared to reference material from the Vocontian Basin. The combined litho-, bio-, chemo-, and sequence stratigraphic analysis establishes a robust chronostratigraphic framework for regional and super-regional correlations and a type section is proposed for the Aptian of NW Africa at Tiskatine.

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Evolution and Biostratigraphy

Gradstein¹

2020

Geologic Time Scale 2020

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Paraticinella rohri () as the valid name for the latest Aptian zonal marker species of planktonic foraminifera traditionally called bejaouaensis or eubejaouaensis

Cited by 25 publications

References 25 publications

The Lindi Formation (upper Albian–Coniacian) and Tanzania Drilling Project Sites 36–40 (Lower Cretaceous to Paleogene): Lithostratigraphy, biostratigraphy and chemostratigraphy

The Lindi Formation (upper Albian–Coniacian) and Tanzania Drilling Project Sites 36–40 (Lower Cretaceous to Paleogene): Lithostratigraphy, biostratigraphy and chemostratigraphy

A revised chronostratigraphic framework for the Aptian of the Essaouira-Agadir Basin, a candidate type section for the NW African Atlantic Margin.

Evolution and Biostratigraphy

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