396 Mr. R. Bullen Newton on a Marine 
Hinnites cf. inequistriatus (Voltz), Thurmann. 
(Pl. XL fig. 8.) 
Hinnites inequistriatus, Voltz, in Thurmann (list name only), Mém. 
Soc. Hist. Nat. Strasbourg, 1833, vol. i. part 2, p. 13; Thurmann 
and Etallon, Lethea Bruntrutana, 1862, pl. xxxvii. fig. 13, p. 267. 
Hinnites ( Pleuronectites) inequistriatus, Futterer, Zeitsch. Deutsch. 
Geol. Ges. 1897, vol. xlix. pp. 588, 589, pl. xix. figs, 6, 7. 
This specimen is quite fragmentary, with fractured margins 
throughout. It consists of part of the interior of an upper 
valve embedded in matrix in which can be traced four or 
five distant radial costee with subsidiary and weaker ones 
between, the whole being crossed by occasional concentric 
growth-lines. As the specimen exhibits only internal cha- 
racters, it is impossible to surmise any details of the outer 
ornamentation of the principal ribs, such structure in the type 
being composed of more or less distant recurring tubular 
spiniform growths. Speaking generally, the Arabian fossil 
shows considerable resemblance to Futterer’s interpretation 
of Thurmann and Etallon’s original figure of this shell. 
Distribution. The species has been recognized from Se- 
quanian and Kimeridgian rocks, the original specimen having 
been described from the Kimeridgian (Strombian) of 
Porrentruy, Switzerland, whereas the example referred to 
by Futterer was obtained from a similar horizon at Shoa, 
Southern Abyssinia. 
Locality. Bachain. 
BRACHIOPODA. 
Terebratula subsella, Leymerie. 
(Pl. XE. figs..9, 10.) 
Terebratula subsella, Leymerie, Statistique Géol. Mineral Dep. de 
l’Aube, 1846, pp. 224, 248, pl. x. fig. 5; H. Douvillé, Bull. Soc. Géol. 
France, 1886, sér. 3, vol. xiv. p. 282, pl. xii. fig. 2. 
Terebratula suprajurensis, Futterer, Zeitsch, Deutsch. Geol. Ges. 1897, 
vol. xlix. p. 617. 
Terebratula subsella, Dacqué, Beftr. Pal. Geol. Osterr.-Ungarns Orients, 
1905, vol. xvii. p, 129, pl. xiv. figs. 5, 6, and pl. xvii. fig. 6. 
This well-known Upper Jurassic species is represented by 
a small example (18x16x12 mm.) with both valves in 
closed association. It has been recognized from Abyssinia 
(Shoa) by Douvillé and Futterer, and by Dacqué from 
Somaliland. Both Davidson and J. F. Walker have referred 
to its occurrence in British Corallian (Sequanian) rocks. 
—. 
