Lithology and planktic foraminifera biostratigraphy of Aptian–Albian boundary as encountered in Jebel Sidi Salem (northeastern Tunisia)

IF 0.7 Q4 PALEONTOLOGY
Meriem Hichi , Nejla Sekatni-Aich , Mohamed Gharbi , Mohamed Ben Youssef
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引用次数: 3

Abstract

The Aptian–Albian boundary has long been difficult to identify along the foreland basin of the Tunisian Atlas, although ammonites occur in the Fahden Formation. The revision of Aptian–Albian series from Jebel Sidi Salem, in the northeastern part of the Tunisian Ridge, provides new data for the recognition of this boundary. The Jebel Sidi Salem section contains a rich succession of planktic foraminifers’ index species which document a complete marine record of Aptian–Albian boundary with no sign of redeposition. Six zones of planktic foraminifera have been identified through the late Aptian to middle Albian; including Globigerinelloides algerianus Zone, Hedbergella trocoidea Zone, Planomalina cheniourensis Zone, Paraticinella eubejaouensis/Ticinella roberti Zone, Hedbergella planispira Zone and Ticinella primula Zone.

突尼斯东北部Jebel Sidi Salem地区Aptian-Albian边界的岩性及浮游有孔虫生物地层学
长期以来,沿突尼斯阿特拉斯的前陆盆地,阿普提安-阿尔比安的边界一直难以确定,尽管菊石出现在法赫登组。突尼斯海脊东北部Jebel Sidi Salem的Aptian-Albian系列的修订,为该边界的识别提供了新的资料。Jebel Sidi Salem剖面包含丰富的浮游有孔虫指数物种序列,这些物种记录了完整的阿普提安-阿尔比安边界的海洋记录,没有再沉积的迹象。在Aptian晚期至Albian中期,已确定了6个浮游有孔虫带;包括阿尔及利亚Globigerinelloides区、绿僵菌(Hedbergella trocoidea)区、cheniourensis区、绿僵菌(Paraticinella eubejaouensis/Ticinella roberti)区、扁僵菌(Hedbergella planispira)区和报春花(Ticinella报春花)区。
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来源期刊
CiteScore
2.50
自引率
0.00%
发文量
17
期刊介绍: La Revue de micropaléontologie publie 4 fois par an des articles de intérêt international, consacrés à tous les aspects de la micropaléontologie. Les textes, en anglais ou en français, sont des articles originaux, des résultats de recherche, des synthèses et mises au point, des comptes rendus de réunions scientifiques et des analyses de ouvrages. La revue se veut résolument ouverte à tous les aspects de la micropaléontologie en accueillant des travaux traitant de la systématique des microfossiles (et de leurs équivalents actuels), des bactéries aux microrestes de vertébrés, et de toutes leurs applications en sciences biologiques et géologiques.
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