418 A. R. Horwood—Upper Trias, Leicestershire. 
Saurichthys acuminatus, Ag. (teeth), Regarded by Dr. AOS 
Woodward as perhaps the same as Belonorhynchus. 1. Spinney Hills. 
2. Haddon Street, Glen Parva. 
Pholidophorus higginst, Eg. (= P. mottiana, Harrison; P. nitidus, 
Eg.) 26. Spinney Hills, Glen Parva, Crown Hills. 
Dapedius sp. 2. Hast Leake. 
Fisu-reetd, Fisu-pones. 1. Spinney Hills. Copzorrrss at Glen 
Parva, East Leake. 
Ampurpia.—‘‘ Lozomma” (teeth, vertebra, rib bones). 1. Spinney 
Hills. a 
Labyrinthodont remains (jaw, bones, left ramus of the mandible, 
teeth, etc.). 1. Spinney Hills. 2. East Leake, Glen Parva. 
Reprit1a.—‘‘ Plesiosaurus rostratus”’ (teeth, bones, ribs, vertebree). 
1. Spinney Hills. 24.Glen Parva. (Probably these belong, according 
to Dr. Watson, to another species.) 
Ichthyosaurus sp. (teeth, vertebre, bones, coprolites). 1. Spinney 
Hills (vertebra near Moat Road). 
Drvnosavria.—2. Limb-bones, East Leake. 
Rysosteus owent, Woodw. & Sherb. 2. East Leake. Dr. Watson 
considers these may belong to a Plesiosaur as yet undetermined. 
Incerte sedis. Saurian teeth, vertebrz, bones, coprolites, vertebre 
of Amphibia or Reptilia, casts of centra, concavo-convex bodies like 
Discina, small circular bodies like cup-corals (at Glen Parva, coprolites). 
1. Spinney Hills. 
Fragmentary remains of Ampuipra and Reprinia. 1. Glen Parva. 
Savrian Bones anp TertH. 1. Haddon Street. 
The correlation of the sections I have given shows that no beds 
exactly comparable with the White Lias occur in Leicestershire. 
That the top bed (1 of Richardson) may be the Cotham Marble, 
however, is shown by its intermediate character, and that Pseudo- 
monotis occurs in the upper part of the Compound Bed, and may be | 
equivalent to the Psewdomonotis bed as Mr. Richardson suggests, but 
the rarity of this species makes this point inconclusive. Harrison 
said he found it at Spinney Hills, and correlates it with a limestone 
higher up, remarking that he found beds like the Guinea Bed at 
Crown Hills (Lower Lias). 
There is evidence that the Bone-bed, though persistent, and hardly 
recognizable at East Leake, is a very attenuated type of the West 
of England equivalent, whilst there were two at Stanton, as 
elsewhere. 
The similarity of fossils at the points named proves the fauna to be, 
as a whole, uniform. The unfossiliferous character of the Upper 
Rhetic and anomalous juxtaposition of intermediate beds at the top 
under beds with Ammonites planorbis, Ostrea liassica, and Lima 
gigantea, and so close to the Upper Rheetic, as pointed out by 
Mr. Richardson, in conjunction with gaps between the Tea-green 
Marls and the Bone-bed, shows that there were locally as elsewhere 
two periods of alteration of level and conditions. 
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