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Arkell.1956.Jurassic..

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268 NORTH AFRICA<br />

TITHONIAN<br />

Red and white shaly marls with interbedded hard limestones have yielded<br />

Ptychophylloceras ptychoicum and other spp., Sowerbyceras loryi Munier-<br />

Chalmas, Haploceras caractheis (Zeusch.), Berriasella callisto, Spiticeras<br />

cf. pseudogroteanum Djanelidze, aptychi and Pygope janitor Pict.<br />

KIMERIDGIAN<br />

Evidence for this stage is inconclusive. Lacoste (1934, pp. 178-80)<br />

assigns several ammonites to the Lower Kimeridgian, of which Phylloceras<br />

cf. canavarii Menegh., Simoceras parateres Canavari, Nebrodites doublieri<br />

(d'Orb.) and Taramelliceras trachynotum (Oppel) alone may be<br />

Kimeridgian.<br />

UPPER OXFORDIAN<br />

To this substage belong Sowerbyceras tortisulcatum (d'Orb.) and some<br />

Perisphinctids (Lacoste, 1934, pp. 178-80).<br />

LOWER OXFORDIAN AND CALLOVIAN have yet to be found, but Lacoste<br />

believes the succession to be continuous. The presence of Callovian<br />

not many miles away, in the misnamed 'Eastern Rif (Marcais, 1931),<br />

suggests that he may be right.<br />

LOWER BATHONIAN<br />

At Jebel Arechko, in red marly limestones like the Bajocian, Lacoste<br />

(1934, p. 176) obtained Morphoceras aff. multiforme (= polymorphum<br />

d'Orb.), Ebrayiceras cf. pseudoanceps (Ebray) and Cadomites or Polyplectites.<br />

MIDDLE BAJOCIAN<br />

At Zerhoun in the Pre-Rif (north of Meknes and west of Fez) and at<br />

Mjara in the Southern Rif, a rich Bajocian fauna has been found. At<br />

Mjara the facies is red marls and marly limestones; at Zerhoun it is in the.<br />

form of thick sandstones, oolites, freestones, dolomites and marls, changing<br />

rapidly and reminiscent of the English Inferior Oolite of the Cotswolds<br />

(Lacoste, 1934, p. 176, Gubler, 1938). The only Upper Bajocian ammonite<br />

recorded is Strigoceras truellei (d'Orb.), but as this was found associated<br />

with many Middle Bajocian ammonites, it was probably one of the earlier<br />

species of Strigoceras. The other ammonites are Stephanoceras humphriesianum<br />

(Sow.), S. plicatissimum (Quenst.), Skirroceras freycinati (Bayle),<br />

Normannites braikenridgei (Sow.) [? orbignyi Buckman], Otoites contractus<br />

(Sow.), Sphaeroceras brongniarti (Sow.), Dorsetensia subtecta (Buck.),<br />

Poecilomorphus cycloides (d'Orb.). At Mjara in the Southern Rif Holcophylloceras<br />

mediterraneum and its allies are common. In addition to these,<br />

some Sonninids of the Sowerbyi Zone are said to occur intimately mixed<br />

in the fauna of the Lower Bajocian in the Pre-Rif (Gubler, 1938, pp.<br />

137-8); they are Sonninia propinquans Bayle (the type species of the genus),<br />

S. deltafalcata (Quenst.), Witchellia sayni Haug (corrugata Douv. non<br />

Sow.), and W. crassifalcata Dorn.<br />

http://jurassic.ru/

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