312 REPORTS ON THE STATE OF SCIENCE. 
referable to that genus; but in ‘ Q.J.G.S.’, 1876, p. 218, he states that it should have 
been recorded as coming from the Rheetic.) 
13. (1875) Plant, J.—‘ Report of the Leicester Lit. and Phil. Soc.,’ p, 45. (Records 
from the Upper Keuper sandstone of Dane Hills and elsewhere, fish-remains [spines, 
teeth, and scales] Estheria minuta, worm-tracks, worm-holes, and ‘cololitic’ remains 
of marine worms.) 
14. (1876) Harrison, W. J.—‘ On the Occurrence of the Rhzetic Beds in Leicester- 
shire, ‘Q.J.G.S.’, pp. 212-218. (Fish-scales and an insect-wing recorded from the 
‘ Tea-Green’ marls, then classed with the Rhetics.) 
15. (1877) Harrison, W. J.—‘ Sketch of the Geology of Leicestershire and Rutland, 
pp. 33-35. (A summary of previous records is given, and some fresh material is 
included.) 
16. (1882) Harrison, W. J.—‘ Geology of the Counties of England and North and 
South Wales,’ p. 155. (This contains a general summary of Triassic palwontology 
in the county.) 
17. (1889) Browne, M.—‘The Vertebrate Avimals of Leicestershire and Rutland,’ 
pp. 174, 199, 200. (Records Acrodus heuperinus and Hybedus sp.) 
18. (1891) Browne, M.—‘ Notes upon Cvlobvdus, a genus of Mesozoic Fishes, 
‘ Brit. Assoc. Rep.,’ 1891, pp. 664-5. 
19. (1893) Browne, M.—‘ A Contribution to the History of the Geology of the 
Borough of Leicester, ‘Trans. Leicester Lit. and Phil. Soc.’, pp. 123-240. (Gives a 
complete summary of all previous records within the area of the borough, and 
map and sections.) 
20. (1900) Fox-Strangways, C., and Professor W. W. Watts.—‘ The Geology of the 
Country between Atherstone and Charnwood Forest,’ ‘Mem. Geol. Survey,’ sheet 
155, p. 33. (Labyrinthodon, Castle Donington.) 
21. (1903) Fox-Strangways, C.—‘ The Geology of the Country near’ Leicester,’ 
Appendix III., Palzontological Tables, sheet 156, pp. 104-123. (This complete 
analysis gives in the tables all the organic remains recorded from Leicestershire.) 
22. (1904) Seward, Professor A. C.—‘ Catalogue of the Mesozoic Plants in the 
British Museum.’ II, Liassicand Oolitic Floras of England, p, 8. (Refers to specimen 
named Gorgonia heuperi, but exhibited in the Fossil Plant Gallery, and compared, 
with others, to probably remains of Voltzia.) 
23. (1905)! Fox-Strangways, C., and Professor W. W. Watts.—‘ The Geology of the 
Country between Derby, Burton-on-Trent, Ashby-de-la-Zouch, and Loughborough,’ 
‘Mem. Geol. Survey,’ sheet 141, p. 31. (Labyrinthodon footsteps recorded from 
Weston Cliff, Donington Park.) 
24. (1905)? Lomas, J.—‘ Report of the British Association’ for 1904, p, 14 of reprint. 
Investigation of the Faunaand Flora of the Trias of the British Isles, Second Report 
of the Committee. (Record of Coniferous remains from Leicester in report by Dr, 
A,S. Woodward of Triassic fossils in the British Museum.) 
Note on the Fossils from the Lower Keuper of Bromsgrove. 
By L. J. Wits, B.A., P.G.S., King’s College, Cambridge. 
At the request of the Secretary of the Trias Committee I have put 
together the following notes on the fossils which I have found at 
Bromsgrove, in Worcestershire, as recorded in the ‘ Geological Magazine,’ 
January 1907, p. 28. The horizon at which they occur is towards the 
top of the Lower Keuper of the older writers ; that is to say, completely 
below the Keuper Marl. The majority are found in lenticular beds of 
marl and shale, while some appear in the sandstone. These lenticular 
patches are made of various types of rock, some being true marls, others 
sandy shales, green, brown, or red in colour. These last have so far 
proved barren. Some are very carbonaceous, and then appear to contain 
abundance of arachnid remains in a very fragmentary state. Just as the 
red marl, so the red sandstone is barren, the plants occurring in the grey, 
which they often stain red-brown. Most of the bones come from a marl 
conglomerate, Indications of similar plants have heen traced at various 
