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 />
age estimation <strong>of</strong> this biozone <strong>in</strong>dicates Early Maastrichtian age. Li <strong>and</strong> Keller<br />
(1998a), recorded the time span <strong>of</strong> this biozone from 72.48Ma to 70.39 Ma<br />
estimated by absolute ages based on magnetochron ages. Premoli Silva et al.,<br />
(1998), <strong>in</strong> their study <strong>of</strong> bio-isotope stratigraphy on eastern Mediterranean, <strong>and</strong><br />
Maestas et al., (2003), recorded the Globotruncana aegyptiaca Zone from the<br />
Upper Campanian age.<br />
The Geologic Time Scale (GTS2004) by Gradste<strong>in</strong> et al., (2004), (Fig.3.12),<br />
accompany<strong>in</strong>g International Stratigraphic Chart, issued under auspices <strong>of</strong> the<br />
International Commission on Stratigraphy (ICS), shows the current<br />
chronostratigraphic scale <strong>and</strong> ages with estimation <strong>of</strong> uncerta<strong>in</strong>ty for all stage<br />
boundaries, placed this span <strong>of</strong> time 72.48Ma to 70.39 Ma under the upper limit<br />
<strong>of</strong> Campanian. The chronostratigrapic duration age was estimated based on<br />
different techniques <strong>and</strong> methods to construct a GTS (2004) placed the<br />
Maastrichtian stage between time <strong>in</strong>tervals <strong>of</strong> (70.6 - + 0.6 Ma) at the base, <strong>and</strong><br />
to (65.5 + - 0.3 Ma) at the top.<br />
3.2.1.2- Gansser<strong>in</strong>a gansseri Interval Zone (CF7)<br />
The Gansser<strong>in</strong>a gansseri (CF7) zone was <strong>in</strong>troduced by Bronnimann (1952),<br />
as Globotruncana gansseri Zone for the first time <strong>and</strong> placed <strong>in</strong>to the Early<br />
Maastrichtian <strong>of</strong> Tr<strong>in</strong>idad <strong>in</strong> (Samir, 2002). In the studied section, this Biozone is<br />
def<strong>in</strong>ed by the <strong>in</strong>terval between the FAD <strong>of</strong> nom<strong>in</strong>ate species Gansser<strong>in</strong>a<br />
gansseri (Bolli) <strong>and</strong> the FAD <strong>of</strong> Contusotruncana contusa (Cushman), (plate. 2,<br />
Figs. 1-3) at Gali section (Smaquli area), lower part <strong>of</strong> reddish to pale brown<br />
succession. This zone covered abundant occurrence <strong>of</strong> the nom<strong>in</strong>ate species for<br />
(20m.). Most <strong>of</strong> the workers <strong>in</strong> the zonal scheme placed Gansser<strong>in</strong>a gansseri<br />
zone <strong>in</strong>formally at the middle- lower Maastrichtian (Li <strong>and</strong> Keller, 1998a), <strong>and</strong><br />
(Abramovich et al., 2002) <strong>in</strong> DSDP Site 525A. (Fars, 1984), (Abdel-Kareem &<br />
Samir, 1995), (Lun<strong>in</strong>g et al., 1998), (Elnady <strong>and</strong> Shah<strong>in</strong>, 2001), <strong>and</strong> (Samir,<br />
2002), Egypt. (Kassab 1974, 1975c, 1975d & 1976b), (Abawi et al., 1982)<br />
(Abdel-Kareem, 1986a, b), (Kassab et al., 1986), (Al-Mutwali, 1996), (Al-Mutwali<br />
<strong>and</strong> Al-Jubouri, 2005), <strong>and</strong> (Sharbazheri 2007), Iraq. (Chacon <strong>and</strong> Mart<strong>in</strong>-<br />
Chivelet, 2005), Spa<strong>in</strong>. (Premoli Silva et al., 1998), Italy. (Changkham <strong>and</strong> Jafar,<br />
1998), India. While (Khalil <strong>and</strong> Mashally, 2004), <strong>in</strong> Egypt, <strong>and</strong> Caron (1985), <strong>in</strong><br />
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