Document Type : Original Research Paper

Authors

1 Ph.D., Islamic Azad University, North Tehran Branch, Tehran, Iran

2 Ph.D., Geological Survey of Iran, Tehran, Iran

3 Professor, Islamic Azad University, North Tehran Branch, Tehran, Iran

Abstract

In this research the Gurpi Formation in the Zagros Basin outcropping in the Dasht-e Arjan section, Shiraz province ,for the purpose of biozonational and Paleobathymetric studies were investigated. The thickness of these sediments is about 130 m and consists of Limestones and Shales.To determine the palaeobathymetry of the Gurpi Formation, Planktonic and benthic foraminifera were investigated . A depth of about 270m to 510m was determined for these sediments based on the ratio of planktonic foraminifera to the total assemblages of foraminifera after omitting infaunal benthic foraminifera (%P*) by using the equation D = e (3.58718+(0.03534 × %P* )).In this study sixty-two species of planktonic foraminifera belonging to eighteen genera were recognised .According to the studied planktonic foraminifera the Upper Cretaceous deposits in this area were divided into nine biozones as following :biozone1- Dicarinella concavata Interval Zone. Biozone2- Dicarinella asymetrica Total Range Zone. Biozone3- Globotruncanita elevata Partial range zone .Biozone4- Globotruncana ventricosa Interval Zone. Biozone5- Radotruncana calcarata Interval zone. Biozone 6- Globotruncanella havanensis Partial Range Zone. Biozone7- Globotruncana aegyptiaca Interval Zone. Biozone 8- Gansserina gansseri Interval Zone. Biozone 9- Contusotruncana contusa Interval Zone
Based on the studied planktonic foraminifera the Early Santonian to Maastrichtian ages were determined for the sediments .

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References                                                                                                                                                
Bolli H. M., Beckman J. P. and Saunders J. B., 1994- Benthic Foraminiferal Biostratigraphy of the South Caribbean Region, Cambridge University.
Bolli, H. M. 1951- The genus Globotruncana in Trinidad, B.W.I.J. Paleontol., 25, 170-188 .
Bolli, H. M. 1966- Zonation of  Cretaceous to Pliocene marine sediments based on Planktonic foraminifera . Boletin Informativo Asociacion Venezolana de Geologia , Mineriay Petroleo, 2-35.
Bolli, M. H., Saunders, J. B and Perch- Nielsen, K., 1985- Plankton Stratigraphy ; Cambridge University Press, Cambridge, vol.I, pp.87-154.
Caron, M., 1985- Cretaceous Planktonic Foraminifera, in Boli et al.: Plankton Stratigraphy, Cambridge University Press, P.17-86 .
Holbourn, A., Kuhnt, W. and Soeding, E., 2001- Atlantic paleobathymetry, paleoproductivity and paleocirculation in the late Albian: the benthic foraminiferal record; Palaeogeography, . Palaeoclimatology, Palaeoecology 170: 171-196.
Li, L., and Keller, G., 1999- Variability in Late Cretaceous climate and deep waters: evidence from stable isotopes; Marine Geology 161: 171-190.
Li, L., Keller, G. and Stinnesbeck, W., 1999- The Late Campanian and Maastrichtian in northwestern Tunisia: Paleoenvironmental inferences from lithology, macrofauna and benthicforaminifera. Cretaceous Research 20, 231-252.
Loeblich, A. R., Jr-  and Tappan, H., 1988- Foraminiferal General and their Classification : Van Nostrand Reinhold Company , New yourk ,2 Volumes, 970p. plus 212p, and 847 pl.
Premoli Silva, I. and Verga, D., 2004- Practical Manual of Cretaceous Planktonic Foraminifera,course 3, in Verga, D., and Rettori, R. (Editors), International School on PlanktonicForaminifera: Universities of Perugia and Milano, Tipografiadi di Pontefelcino, Perugia, Italy, 283 p.
Robaszynski, F. and Caron, M., (Coordinators), 1979- Atlas de Foraminiferes Planctoniques du Cretace Moyen(Mer Boreale et Tethys) , Cahiers de Micropaleontologie  (1) : 1-185p.
Robaszynski, F., Caron, M., Gonzalez Donoso, J. M. and Wanders, A. A. H.  1988- Atlas of  Late Cretaceous Globotruncana .
Sliter, W. V. and Baker, R. A., 1972- Cretaceous bathymetric distribution of benthic foraminifera; Journal of Foraminiferal Research 2: 167-183.
Sliter, W. V. and Leckie, R. M., 1993- Cretaceous planktonic foraminifers and depositional environments from the Ontong Java Plateau with emphasis on Sites 803 and 807. In Berger, W. H., Kroenke, L. W., Mayer, L. A., et al., Procceding ODP Science Results, 130: College Station, TX (Ocean Drilling Program), 63-84.
Van der Zwaan, G. J., Duijnstee, I. A. P., Den Dulk, M., Ernst, S. R. and Kouwenhoven, N. T., 1999- Benthic foraminifers: proxies or problems? A review of paleoecological concepts; Earth Sciences Reviews 46: 213-236.
Van der Zwaan, G. J., Jorissen, F. J. and De Stigter, H. C., 1990- The depth-dependency of planktonic/benthic foraminiferal ratios; constraints and applications; Marine Geology 95: 1-16.