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biostratigraphy and paleoecology of cretaceous/tertiary boundary in ...

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Chapter Three Biostratigraphy<br />

(Subbot<strong>in</strong>a trilocul<strong>in</strong>oides) Subzone <strong>of</strong> Berggren & Miller, (1988). At studied<br />

sections only the lower part <strong>of</strong> this subzone is studied which atta<strong>in</strong>s a thickness<br />

<strong>of</strong> 15 meters <strong>in</strong> Sirwan section, 10 meter <strong>in</strong> Qulka <strong>and</strong> Gali sections. The<br />

associated planktonic assemblage <strong>of</strong> this subzone differs from the underly<strong>in</strong>g<br />

P1a Subzone by the presence <strong>of</strong> S. trilocul<strong>in</strong>oides (Plummer), <strong>in</strong> addition to the<br />

follow<strong>in</strong>g <strong>in</strong> Gali section like:<br />

Woodr<strong>in</strong>g<strong>in</strong>a hornerstownensis (Olsson), Chiloguembel<strong>in</strong>a midwayensis<br />

(Cushman), Globoconusa daubjergensis (Bronnimann), Parasubbot<strong>in</strong>a<br />

pseudobulloides (Plummer), Subbot<strong>in</strong>a trivalis (Subbot<strong>in</strong>a), Globanomal<strong>in</strong>a<br />

archeocompressa (blow), G. planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita<br />

(Subbot<strong>in</strong>a), E. eobulloides Morozova, Praemurica taurica (Morozova),<br />

P.pseudo<strong>in</strong>constans (blow). In Qulka section slight different were existed <strong>in</strong><br />

planktonic assemblage as below: Chiloguembel<strong>in</strong>a morse (Kl<strong>in</strong>e), Ch.<br />

midwayensis (Cushman), Parasubbot<strong>in</strong>a pseudobulloides (Plummer), Subbot<strong>in</strong>a<br />

trivalis (Subbot<strong>in</strong>a), Globanomal<strong>in</strong>a archeocompressa (blow), G.<br />

planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita (Subbot<strong>in</strong>a), E. eobulloides<br />

Morozova, E. simplicissma Blow Praemurica taurica (Morozova),<br />

P.pseudo<strong>in</strong>constans (blow). In Sirwan section similar assemblages were<br />

observed like: Parvularugoglobiger<strong>in</strong>a alabam<strong>in</strong>sis (Liu & Olsson),<br />

Rectoguembel<strong>in</strong>a cretacea Cushman, Woodr<strong>in</strong>g<strong>in</strong>a clytonensis (Loeblich &<br />

Tappan), W. hornerstownensis (Olsson), Chiloguembel<strong>in</strong>a morsei (Kl<strong>in</strong>e), CH.<br />

midwayensis (Cushman), Parasubbot<strong>in</strong>a pseudobulloides (Plummer), Subbot<strong>in</strong>a<br />

trivalis (Subbot<strong>in</strong>a), S. trilocul<strong>in</strong>oides (Plummer), Globanomal<strong>in</strong>a<br />

archeocompressa (blow), G. planocompressa (Shutskaya), Eoglobiger<strong>in</strong>a edita<br />

(Subbot<strong>in</strong>a), E. eobulloides Morozova, Praemurica taurica (Morozova), P.<br />

pseudo<strong>in</strong>constans (blow),<br />

Based on faunal similarities, the comb<strong>in</strong>ed P1 b Subzones <strong>of</strong> studied<br />

section could be equivalent to the upper part <strong>of</strong> Morozovella pseudobulloides<br />

Zone <strong>of</strong> Bolli, (1966), <strong>and</strong> Blow, (1979). To Caron (1985); Elnady & Shah<strong>in</strong>,<br />

(2001), Samir, (2002) from Egypt; Arenillas et al.,(2000) Tunisia; to the P1c <strong>of</strong><br />

Keller, (1988), <strong>and</strong> Keller et al., (1995), <strong>in</strong> Tunisia; to the S. trilocul<strong>in</strong>oides by<br />

Obaidalla, (2005) <strong>in</strong> Egypt; <strong>and</strong> also it is equivalent to the P1b <strong>of</strong> Berggren <strong>and</strong><br />

80

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