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

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Chapter Three Biostratigraphy<br />

Norris (1997),Berggren et al.,(1995); Keller, (2002, <strong>and</strong> 2004), Abramovich et<br />

al.,(2002), Olsson (2000); <strong>and</strong> Smit (2005) SE <strong>of</strong> Spa<strong>in</strong>.<br />

The age estimation <strong>of</strong> this <strong>in</strong>terval depend<strong>in</strong>g on Magnetic polarity <strong>and</strong><br />

recorded datum events by (Olsson et al., 2000), (Keller, 2002, 2004) with the<br />

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<br />

<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<br />

Ma. Estimat<strong>in</strong>g absolute ages based on magnetochron ages (Figs. 3.13 -14).<br />

The estimated age is Early Paleocene (Early Danian).<br />

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