Chapter Three Biostratigraphy (Subbot<strong>in</strong>a trilocul<strong>in</strong>oides) Subzone <strong>of</strong> Berggren & Miller, (1988). At studied sections only the lower part <strong>of</strong> this subzone is studied which atta<strong>in</strong>s a thickness <strong>of</strong> 15 meters <strong>in</strong> Sirwan section, 10 meter <strong>in</strong> Qulka <strong>and</strong> Gali sections. The associated planktonic assemblage <strong>of</strong> this subzone differs from the underly<strong>in</strong>g P1a Subzone by the presence <strong>of</strong> S. trilocul<strong>in</strong>oides (Plummer), <strong>in</strong> addition to the follow<strong>in</strong>g <strong>in</strong> Gali section like: Woodr<strong>in</strong>g<strong>in</strong>a hornerstownensis (Olsson), Chiloguembel<strong>in</strong>a midwayensis (Cushman), Globoconusa daubjergensis (Bronnimann), Parasubbot<strong>in</strong>a pseudobulloides (Plummer), Subbot<strong>in</strong>a trivalis (Subbot<strong>in</strong>a), Globanomal<strong>in</strong>a archeocompressa (blow), G. planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita (Subbot<strong>in</strong>a), E. eobulloides Morozova, Praemurica taurica (Morozova), P.pseudo<strong>in</strong>constans (blow). In Qulka section slight different were existed <strong>in</strong> planktonic assemblage as below: Chiloguembel<strong>in</strong>a morse (Kl<strong>in</strong>e), Ch. midwayensis (Cushman), Parasubbot<strong>in</strong>a pseudobulloides (Plummer), Subbot<strong>in</strong>a trivalis (Subbot<strong>in</strong>a), Globanomal<strong>in</strong>a archeocompressa (blow), G. planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita (Subbot<strong>in</strong>a), E. eobulloides Morozova, E. simplicissma Blow Praemurica taurica (Morozova), P.pseudo<strong>in</strong>constans (blow). In Sirwan section similar assemblages were observed like: Parvularugoglobiger<strong>in</strong>a alabam<strong>in</strong>sis (Liu & Olsson), Rectoguembel<strong>in</strong>a cretacea Cushman, Woodr<strong>in</strong>g<strong>in</strong>a clytonensis (Loeblich & Tappan), W. hornerstownensis (Olsson), Chiloguembel<strong>in</strong>a morsei (Kl<strong>in</strong>e), CH. midwayensis (Cushman), Parasubbot<strong>in</strong>a pseudobulloides (Plummer), Subbot<strong>in</strong>a trivalis (Subbot<strong>in</strong>a), S. trilocul<strong>in</strong>oides (Plummer), Globanomal<strong>in</strong>a archeocompressa (blow), G. planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita (Subbot<strong>in</strong>a), E. eobulloides Morozova, Praemurica taurica (Morozova), P. pseudo<strong>in</strong>constans (blow), Based on faunal similarities, the comb<strong>in</strong>ed P1 b Subzones <strong>of</strong> studied section could be equivalent to the upper part <strong>of</strong> Morozovella pseudobulloides Zone <strong>of</strong> Bolli, (1966), <strong>and</strong> Blow, (1979). To Caron (1985); Elnady & Shah<strong>in</strong>, (2001), Samir, (2002) from Egypt; Arenillas et al.,(2000) Tunisia; to the P1c <strong>of</strong> Keller, (1988), <strong>and</strong> Keller et al., (1995), <strong>in</strong> Tunisia; to the S. trilocul<strong>in</strong>oides by Obaidalla, (2005) <strong>in</strong> Egypt; <strong>and</strong> also it is equivalent to the P1b <strong>of</strong> Berggren <strong>and</strong> 80
Chapter Three Biostratigraphy Norris (1997),Berggren et al.,(1995); Keller, (2002, <strong>and</strong> 2004), Abramovich et al.,(2002), Olsson (2000); <strong>and</strong> Smit (2005) SE <strong>of</strong> Spa<strong>in</strong>. The age estimation <strong>of</strong> this <strong>in</strong>terval depend<strong>in</strong>g on Magnetic polarity <strong>and</strong> recorded datum events by (Olsson et al., 2000), (Keller, 2002, 2004) with the time span <strong>of</strong> 64.50Ma from first occurrence <strong>of</strong>, Subbot<strong>in</strong>a trilocul<strong>in</strong>oides, to FAD <strong>of</strong> Globanomal<strong>in</strong>a compressa <strong>and</strong>/or Praemurica <strong>in</strong>constans at the top <strong>of</strong> 63.00 Ma. Estimat<strong>in</strong>g absolute ages based on magnetochron ages (Figs. 3.13 -14). The estimated age is Early Paleocene (Early Danian). 81
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IV Dedicated: To My Wife My Daughte
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VI Abstract The Cretaceous / Tertia
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- Page 136 and 137: REFERENCES Abawi, T. S. Abdel-Kiree
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Cretaceous of the south Constantine
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James, G. A. and Wynd, J. G., 1965.
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Kassab, I. I. M., 1975c. Planktonic
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Liu, C. and Olsson, R. K., 1992. Ev
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Molina, E. Arenillas, I. and Arz, J
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Petters, S. W. EL-Nakhal, H. A. and
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Sissakian, V. K., 2000. Geological
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