2016
DOI: 10.1515/agp-2016-0002
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The lower and middle Berriasian in Central Tunisia: Integrated ammonite and calpionellid biostratigraphy of the Sidi Kralif Formation

Abstract: :Maalaoui, K. and Zargouni, F. 2016. The lower and middle Berriasian in Central Tunisia: Integrated ammonite and calpionellid biostratigraphy of the Sidi Kralif Formation. Acta Geologica Polonica, 66 (1), 43-58. Warszawa.The lower and middle Berriasian sedimentary succession of the Sidi Kralif Formation has been a subject of biostratigraphic study in two key sections in Central Tunisia. Our contribution is an attempt to better define the basal Berriasian interval, between the Berriasella jacobi Zone and the Su… Show more

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Cited by 9 publications
(3 citation statements)
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“…It seems that Radwańska (2017) sourced the description of geological setting mainly from Matyja and Tarkowski (1981) and Trammer (1982Trammer ( , 1985. Unfortunately, these valuable papers were based upon the Upper Jurassic exposures from the early 1980s.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…It seems that Radwańska (2017) sourced the description of geological setting mainly from Matyja and Tarkowski (1981) and Trammer (1982Trammer ( , 1985. Unfortunately, these valuable papers were based upon the Upper Jurassic exposures from the early 1980s.…”
Section: Discussionmentioning
confidence: 99%
“…Unfortunately, these valuable papers were based upon the Upper Jurassic exposures from the early 1980s. Radwańska (2017, p. 433) describes the Oxfordian succession as follows: "…variegated marls and marly limestones (about 2 m thick) of the Cordatum Zone, covered by a carbonate buildup (cyanobacte-ria-sponge bioherm), and by thin-bedded limestones and marls, or platy limestones (about 10 m thick) of the Middle Oxfordian Tenuicostatum Subzone of the Plicatilis Zone (see Matyja and Tarkowski 1981, figs 2−3)". This paragraph is almost identical with the description of Oxfordian succession in Radwańska (2005, pp.…”
Section: Discussionmentioning
confidence: 99%
“…The Oxfordian (Text-fig. 2B) starts with marls and marly limestones representing the Cardioceras bukowskii and Cardioceras costicardia subzones (Matyja and Tarkowski 1981;Górka and Bąk 2000). In their topmost part, they are quite rich in sponges, ammonites, belemnites and brachiopods.…”
Section: Geological Settingmentioning
confidence: 99%