biostratigraphy and paleoecology of cretaceous/tertiary boundary in ...
biostratigraphy and paleoecology of cretaceous/tertiary boundary in ...
biostratigraphy and paleoecology of cretaceous/tertiary boundary in ...
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Chapter Three Biostratigraphy<br />
3.2.1.1- Globotruncana aegyptiaca Interval Zone (CF8)<br />
The Globotruncana aegyptiaca (CF8) zone was orig<strong>in</strong>ally established <strong>and</strong><br />
described by Caron (1985).It is marked by the <strong>in</strong>terval from the First Appearance<br />
Datum (FAD) <strong>of</strong> the nom<strong>in</strong>ate species to the First Appearance Datum (FAD) <strong>of</strong><br />
Gansser<strong>in</strong>a gansseri (Bolli). In the studied Gali section (Smaquli area) is def<strong>in</strong>ed<br />
by the first appearance FAD <strong>of</strong> <strong>in</strong>dex taxon (Globotruncana aegyptiaca<br />
Nakkady,)with<strong>in</strong> the first sample taken from the upper part <strong>of</strong> Shiranish<br />
Formation at the base to the FAD <strong>of</strong> Gansser<strong>in</strong>a gansseri (Bolli) at sample No.8<br />
(plate. 2, Figs. 10-12) with<strong>in</strong> reddish unit at the top. This zone covers frequent<br />
occurrence <strong>of</strong> the nom<strong>in</strong>ate species for 15m. <strong>in</strong>terval <strong>in</strong> the upper part <strong>of</strong> the<br />
Shiranish Formation <strong>and</strong> 8m. from the lower part <strong>of</strong> reddish unit. This <strong>in</strong>terval<br />
may not represent all <strong>in</strong>terval <strong>of</strong> the biozone because the first sample <strong>of</strong> our<br />
section may not fit with<strong>in</strong> the FAD <strong>of</strong> the nom<strong>in</strong>ate species. This part <strong>of</strong><br />
Globotruncana aegyptiaca zone <strong>in</strong>dicates early Maastrichtian for the cropped<br />
<strong>in</strong>terval, <strong>and</strong> corresponds to that <strong>of</strong> Caron (1985), <strong>in</strong> tropical regions, Shah<strong>in</strong><br />
(1992), <strong>in</strong> Egypt, it is equivalent to the same zone recorded <strong>in</strong> the south Atlantic<br />
DSPT Site 525A <strong>and</strong> Tunisia by Li <strong>and</strong> Keller (1998a,b), Abramovich et al.,<br />
(2002), <strong>in</strong> Madagascar, Al-Mutwali <strong>and</strong> Al-Jubouri, (2005), north Iraq,<br />
Sharbazheri (2007). In the studied section a well diversified planktonic<br />
foram<strong>in</strong>iferal species are recorded, e.g. Heterohelix navarroensis Loeblish, H.<br />
globulosa (Ehrenberg), H. striata (Ehrenberg), H. reussi (Cushman), H.<br />
nauttalli (Voorwijk), H. punctulats (Cushman), H. pulchra (Brotzen),<br />
Planoglobul<strong>in</strong>a carseyae (Plummer), P. brazoensis Mart<strong>in</strong>, Rogoglobiger<strong>in</strong>a<br />
rugosa (Plummer), R. scotti (Bronnimann), R. hexcamerata Bronnimann,<br />
R. macrocephala Bronnimann, R. rotundata Bronnimann, R. milamensis Smith<br />
& Pessango, Gansser<strong>in</strong>a wiedenmayeri (G<strong>and</strong>olfi), Globotruncanita stuarti (de<br />
Lapparent), G. stuartiforms Dalbez, G. conica White, Rugotruncana<br />
subcircumnodifer ( G<strong>and</strong>olfi), R. circumnodifer ( F<strong>in</strong>lay), Globotruncana<br />
aegyptica Nakkady, Glt. orientalis El-Naggar, (Carsey), Glt. falsostuarti Sigal,<br />
Glt. mariei Banner & Blow, Glt. arca (Cushman), Glt. gagneb<strong>in</strong>i Tilev, Glt.<br />
bulloides Vohgler, Glt. l<strong>in</strong>neiana (d Orbigny), Glt. ventricosa White, Glt.<br />
<strong>in</strong>signis (G<strong>and</strong>olfi), Glt. dupeublie Caron et al., Glt lapparenti Boli,<br />
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