Early Jurassic benthic foraminiferal diversification and biozones in shallow-marine carbonates of western Tethys

Author:

BouDagher-Fadel Marcelle K.,Bosence Dan W. J.

Publisher

Springer Science and Business Media LLC

Subject

Paleontology

Reference88 articles.

1. Andreo, B., García-Hernández, M., Martín-Algarra, A., Rey, J. &Vera, J. A. (1991): La sedimentación carbonatada del Lías en la transversal de Vélez Rubio (Subbético Interno). — Revista de la Sociedad Geológica de España,4: 165–178.

2. Banner, F. T. &Pereira, C. P. G. (1981): Some biserial and triserial agglutinated smaller foraminifera: their wall structure and its significance. — Journal of Foraminiferal Research,11: 85–117.

3. Banner, F. T., Simmons, M. D. &Whittaker, J. E. (1991): The Mesozoic Chrysalidinidae (Foraminifera, Textulariacea) of the Middle East: theRedmond (Aramco) taxa and their relatives. — Bulletin of the British Museum (Natural History), Geology series,47: 101–152.

4. Banner, F. T., Whittaker, J. E., BouDagher-Fadel, M. K. &Samuel, A. (1997):Socotraina, a new Hauraniid genus from the Upper Lias of the Middle East (Foraminifera, Textulariina). — Revue de Micropaléontologie,40: 115–123.

5. Barattolo, F. (1991): Mesozoic and Cenozoic marine benthic calcareous algae with particular regard to the Mesozoic dasycladaceans. — In:Riding, R. (ed.), Calcareous algae and stromatolites. — Springer Verlag, Berlin: 504–540.

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