42 Dr. T. Wright on new Species of Echinodermata 
on their under surface, and were united together in the living 
state by a membrane, but in the specimen before us they are 
quite separate from each other ; at the apex of each of the ten 
triangular plates a sharp toothlike process projects downwards, 
which together form an imposing dental circle around the mouth- 
opening. The rays are long, slender, and gently tapering ; we 
have not been able to measure the absolute length of one, as 
those which we have met with were always fractured ; the dorsal 
median pieces of the rays are hexagonal and elongated trans- 
versely, the ventral median pieces are elongated in the direction 
of the length of the ray, and resemble the bodies of small ver- 
tebree which had been deprived of their neural arches ; the mar- 
ginal plates are rounded and finely imbricated, their outward 
free border is toothed with five or six pectinated processes, which 
in the living state supported as many spies; the remains of 
these are sometimes seen attached to their supports; the 
lateral scutal plates clasp the rays firmly and securely, and over- 
lap the median pieces both above and below. 
Affinities and differences—This elegant Sea-star somewhat 
resembles in its: general contour Ophioderma Milleri, but it is 
distinguished from that marlstone species by having a propor- 
tionately larger body-disc, with more slender and more tapering 
rays: in the form and structure of the scutal elements of the 
rays themselves there is likewise a difference, those in O. Milleri 
are of a more elongated and regular form, whilst in O. Gaveyi 
they are shorter, more ridgy and vertebrate-like ; the ten trian- 
gular ventral discal plates are smaller in O. Milleri than in O. 
Gaveyi; they want likewise, in the figures given by Mr. Charles- 
worth in the London Geological Journal, the toothlike spines at 
their apices which are so characteristic of our Ophiura. 
Locality and stratigraphical range-—This Sea-star was col- 
lected by Mr. Gavey from the upper shales of the Lower Lias 
at Mickleton Tunnel near Chippmg Campden, Gloucestershire, 
whilst making the Oxford, Worcester and Wolverhampton Rail- 
way; and we have found some fragments of a Sea-star much 
resembling in structure this species in a Liasic bed of the same 
horizon at Hewlitt’s Hill near Cheltenham, during the excavation 
of the new reservoir of the Water Works Company of that town. 
We dedicate this species to our friend Mr. G. E. Gavey, whose 
careful and minute investigation of the beds exposed in the sec- 
tion which he has so well described*, added to the discovery of 
new forms of Radiata and Mollusca in the same, has enriched 
our knowledge of the Liasic fauna of Gloucestershire. 
* Railway Cuttings at Mickleton Tunnel and Aston Magna, by G. E. 
Gavey, Quart. Journ. Geol. Soc. February 7, 1853. 
