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Agglutinated Middle-Upper Eocene foraminifera in Jabal Hafit, Al ...

Agglutinated Middle-Upper Eocene foraminifera in Jabal Hafit, Al ...

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<strong>Agglut<strong>in</strong>ated</strong> <strong>Middle</strong>-<strong>Upper</strong> <strong>Eocene</strong> <strong>foram<strong>in</strong>ifera</strong> <strong>in</strong> <strong>Jabal</strong> <strong>Hafit</strong>, <strong>Al</strong> A<strong>in</strong> area 21<br />

The species has been recorded <strong>in</strong> mid-Tertiary rocks<br />

of some Caribbean Sea (CUSHMAN & RENZ, 1941 <strong>in</strong><br />

Venezuela, CUSHMAN & STAINFORTH, 1945 <strong>in</strong> Tr<strong>in</strong>idad)<br />

and also North Atlantic region (BERGGREN & AUBERT,<br />

1976).<br />

It is recorded only <strong>in</strong> the early Late <strong>Eocene</strong> (P15) of <strong>Jabal</strong><br />

<strong>Hafit</strong>.<br />

Superfamily Verneuil<strong>in</strong>acea CUSHMAN, 1911<br />

Family Prolixoplectidae LOEBLICH & TAPPAN, 1985<br />

Genus Plect<strong>in</strong>a MARSSON, 1878<br />

Type species : Gaudry<strong>in</strong>a ruthenica REUSS, 1851<br />

Plect<strong>in</strong>a emiratensis ANAN, 2003<br />

2003. Plect<strong>in</strong>a emiratensis ANAN, p.534, fig. 4.2.<br />

The species is characterized by its subconical and short<br />

test, coarse-gra<strong>in</strong>ed surface, subterm<strong>in</strong>al and traverse<br />

elongate slit aperture on the apertural face of the last<br />

formed chamber.<br />

This species occurs <strong>in</strong> the top <strong>Middle</strong> <strong>Eocene</strong> (P14) of<br />

<strong>Jabal</strong> <strong>Hafit</strong>.<br />

Family Tritaxiidae PLOTNIKOVA, 1979<br />

Genus Tritaxia REUSS, 1860<br />

Type species : Textularia tricar<strong>in</strong>ata REUSS, 1844<br />

Tritaxia alp<strong>in</strong>a (CUSHMAN, 1936)<br />

Pl. I, fig. 8<br />

1936. Clavul<strong>in</strong>oides alp<strong>in</strong>a CUSHMAN, p. 22, pl. 3, fig. 16.<br />

1975. Tritaxia alp<strong>in</strong>a (CUSHMAN).- PROTO DECIMA & de BIASE,<br />

p. 91, pl.1, fig. 12.<br />

The species was recorded by PROTO DECIMA & de BIASE<br />

(1975) to range from Early to <strong>Middle</strong> <strong>Eocene</strong> of Possagno<br />

section of Italy.<br />

In this study, it is recorded only from the Late <strong>Eocene</strong><br />

(P15-P16) of <strong>Jabal</strong> <strong>Hafit</strong>.<br />

Superfamily Textulariacea EHRENBERG, 1838<br />

Family Eggerellidae CUSHMAN, 1937<br />

Subfamily Dorothi<strong>in</strong>ae BALAKHMATOVA, 1972<br />

Genus Dorothia PLUMMER, 1931<br />

Type species : Gaudry<strong>in</strong>a bullata CARSEY, 1931<br />

Dorothia nacataensis (WHITE, 1929)<br />

Pl. I, fig. 9<br />

1929. Textularia nacataensis WHITE, p. 31, pl. 4, fig. 2.<br />

1978. Marssonella nacataensis (WHITE) - PROTO DECIMA &<br />

BOLLI, p. 794, pl. 1, fig. 15c.<br />

LOEBLICH & TAPPAN (1988, p. 169) noted that the biserial<br />

stage of Dorothia is <strong>in</strong>creas<strong>in</strong>g very slowly <strong>in</strong> size, so<br />

that test has nearly parallel sides and is circular <strong>in</strong> cross<br />

section, while it is rapidly <strong>in</strong>creas<strong>in</strong>g diameter and<br />

conical <strong>in</strong> Marssonella. Hence, it is related here to the<br />

genus Dorothia.<br />

The species was orig<strong>in</strong>ally described from the <strong>Eocene</strong><br />

rocks of the Tampico Embayment of Mexico. It was<br />

also recorded by PROTO DECIMA & BOLLI (1978) from the<br />

Paleocene of southeast Atlantic DSDP Leg 40, west coast<br />

of Africa.<br />

In this study, the species is recorded <strong>in</strong> the top <strong>Middle</strong> to<br />

Late <strong>Eocene</strong> (P14 - P16) of <strong>Jabal</strong> <strong>Hafit</strong>.<br />

Genus Marssonella CUSHMAN, 1933<br />

Type species : Gaudry<strong>in</strong>a oxycona REUSS, 1860<br />

Marssonella hafitensis ANAN, 2003<br />

2003. Marssonella hafitensis ANAN, p. 535, fig. 4.3.<br />

Marssonella hafitensis is recognized from the <strong>Upper</strong><br />

Cretaceous-Paleocene M. oxycona by its nearly equal<br />

length and breadth test, coarse- gra<strong>in</strong>ed wall and concave<br />

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

The species is recorded from the top <strong>Middle</strong> to Late<br />

<strong>Eocene</strong> (P14 - P16) of <strong>Jabal</strong> <strong>Hafit</strong>.<br />

Family Textulariidae EHRENBERG, 1838<br />

Subfamily Textulari<strong>in</strong>ae EHRENBERG, 1838<br />

Genus Textularia DEFRANCE, 1824<br />

Type species : Textularia sagittula DEFRANCE, 1824<br />

Textularia communis (dʼORBIGNY, 1826)<br />

Pl. I, fig. 10<br />

1826. Textilaria communis dʼORBIGNY, p. 263.<br />

1955. Textularia communis (dʼORBIGNY).- ANSARY, p. 21, pl. 1,<br />

fig. 8.<br />

1992. Textularia communis (dʼORBIGNY).- CHERIF et al., p. 46,<br />

pl. 1, fig. 7.<br />

The species was recorded <strong>in</strong> the <strong>Upper</strong> <strong>Eocene</strong> rocks of<br />

Egypt (ANSARY, 1955).<br />

CHERIF et al., (1992) have recorded this species from<br />

the Oligocene of <strong>Jabal</strong> <strong>Hafit</strong>, while it occurs <strong>in</strong> the top<br />

<strong>Middle</strong> <strong>Eocene</strong> (P14/15) of the study section. The rare<br />

found specimens are broken with miss<strong>in</strong>g <strong>in</strong>itial part.<br />

Textularia plummerae LALICKER, 1935<br />

1935. Textularia plummerae LALICKER, p. 50, pl. 6, fig. 10.<br />

1975. Textularia plummerae LALICKER.- PROTO DECIMA & de<br />

BIASE, p. 91, pl. 1, fig. 6.<br />

1989. Textularia plummerae LALICKER.- HULSBOS et al., p. 268,<br />

pl. 1, fig. 7.

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