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Chapter Three Biostratigraphy<br />

C R E T A C E O U S T E R T I A R Y PERIOD<br />

LATE CAMP. EARL Y MAASTRICHTIAN ----- LA TE MAASTRICHTIAN P A L E O C E N E EPOCH--AGE<br />

Shiranish Shiranish/Tanjero transition unit Tanjero Kolosh FORMATION<br />

1 3 5 10 15 20 25 30 35 40 45 50 55 60 70 80 90 100 110 115 120 130 140 146 SAMPLE No<br />

LITHOLOGY<br />

1 15 30 50 70 89 100 113 143 171 200 230 THICKNESS m.<br />

CF.zones<br />

CF 8 CF 7 CF 6 CF 5 CF 4 CF 3 CF 2 CF 1 P<br />

(Li&Killer,1998a)<br />

Glt.<br />

aegyptiaca.<br />

G.<br />

gansseri<br />

C.<br />

contusa<br />

P.<br />

<strong>in</strong>term.<br />

R. fructicosa<br />

P.<br />

hariaensis<br />

P.<br />

palpebra<br />

P.<br />

hantk.<br />

0<br />

pá P 1a P1b<br />

SUBZONE<br />

Parvularugoglobigir<strong>in</strong>a eugub<strong>in</strong>a (Luterbacher & Premoli Silva)<br />

Parvularugoglobigir<strong>in</strong>a extensa (Blow)<br />

Rectoguembel<strong>in</strong>a cretacea Cushman<br />

Hedbergella monmouthensis (Olsson),<br />

Woodr<strong>in</strong>g<strong>in</strong>a clytonensis (Loeblich & Tappan)<br />

= hornerstownensis (Olsson)<br />

Chiloguembel<strong>in</strong>a morsei (Kl<strong>in</strong>e)<br />

= midwayensis (Cushman)<br />

Globoconusa daubjergensis (Bronnimann)<br />

Parasubbot<strong>in</strong>a aff pseudobulloides (Olsson et al)<br />

Parasubbot<strong>in</strong>a pseudobulloides (Plummer)<br />

Subbot<strong>in</strong>a trivalis (Subbot<strong>in</strong>a)<br />

= trilocul<strong>in</strong>oides (Plummer)<br />

Globanomal<strong>in</strong>a archeocompressa (blow)<br />

= planocompressa (Shutskaya)<br />

Eoglobiger<strong>in</strong>a edita (Subbot<strong>in</strong>a)<br />

= eobulloides Morozova<br />

= simplicissma Blow<br />

Praemurica taurica (Morozova)<br />

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

Guembelitria cretacea Cushman<br />

----------<br />

----------<br />

------------------<br />

----<br />

-----------------<br />

------------------------------------------<br />

----------------------------<br />

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- ----------------------------------------<br />

----------<br />

--------------------------------<br />

------------------------------------------<br />

---------<br />

-------------- --------- ------------------<br />

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-----------------------<br />

Paleocene planktonic foram<strong>in</strong>ifera<br />

Fig (3.7) Part 2:- Biostratigraphic range chart <strong>of</strong> planktonic foram<strong>in</strong>ifera at<br />

Cretaceous/Tertiary <strong>boundary</strong> <strong>in</strong> Smaquli area (Gali section) Cont<strong>in</strong>ued.<br />

Globiger<strong>in</strong>elloides volutes (White), G. subcar<strong>in</strong>atus Bronnimann, G.<br />

prairiehillensis Pessango, Pseudotextularia elegans (Rzehak), P.<br />

59<br />

deformis<br />

(kiko<strong>in</strong>e), P. <strong>in</strong>termedia (De Klasz), Racemiguembel<strong>in</strong>a poweli Smith &<br />

Pessango, Pseudoguembel<strong>in</strong>a costulata (Cushman), P.<br />

excolata (Cushman),<br />

Hedbergella monmothensis (Olsson), P. holmdelensis Olsson,<br />

Abathomphalus <strong>in</strong>termedius (Bolli), Archaeoglobiger<strong>in</strong>a carteri (Kassab),<br />

Gubler<strong>in</strong>a cuvillieri Kiko<strong>in</strong>e, Gumbelitria cretacea Cushman.<br />

Due to high similarities <strong>of</strong> foram<strong>in</strong>iferal occurance, the present Zone (CF5)<br />

is equvalent to that <strong>of</strong> Li <strong>and</strong> Keller (1998a,b), (Abramovich et al., 2002), (Samir<br />

2002) , it is most likely equivalent to the upper part <strong>of</strong> Gansser<strong>in</strong>a gansseri<br />

Zone recorded <strong>in</strong> the North <strong>and</strong> Northeast <strong>of</strong> Iraq <strong>and</strong> different regions <strong>of</strong> the<br />

world (Al-Mutwali <strong>and</strong> Al-Jubouri, 2005), (Al-Mutwali, 1996), (Hammoudi, 2000),<br />

(Caron 1985), (Ubaidalla, 2005), (Robaszynski et al., 1984), (D Hont & Keller,<br />

1991), <strong>and</strong> it is equivalent to the upper part <strong>of</strong> Glt. contusa Zone <strong>of</strong> (Abawi et al.,<br />

1982, <strong>and</strong> Abdel-Kareem, 1986), <strong>and</strong> Glt.contusa-R. fructicosa Zone <strong>of</strong> (Premoli

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