326 Reports and Proceed in ga — Geologiccd Society of London. 



Analysis of Replies. 



(1) Are you in favour of the admission of women to the Geological Society 

 of London r 



Yes 342 



]Vo 133 



Not specified ... ... ... 2 



■ 477 



(2) Are you in favour of the admission of women as Fellows, or as Associates 

 only? The 342 in favour of admission voted — 



As Fellows 248 



As Associates ... ... ... 84 



Not .sijecified ... ... ... 10 



342 



(3) If there should not be a majority of those voting in favour of women as 

 Fellows, are vou in favour of their admission as Associates ? 



Yes 304 



No 35 



Not specified ... 3 



342 



Add votes of those against the admission of 



women at all ... ... ... 133 



And those who are neutral... ... ... 2 



477 



The foregoing analysis shows that there were : 

 In favour of the admission of i ., ,o 



women as Fellows j 



; 133 against the admission of women 

 Against the admission of ^ 917) '"^^ ^^^• 



women as Fellows j " 1 84 in favour of the admission of 



\ women as Associates only. 



3fajority in favour of the \ 

 admission of women as > 31 

 Fellows ) 



The following communication.s were read : — 



1. " On some Fossil Fishes discovered by Professor Ennes de Souza 

 in the Cretaceous Formation at Ilheos, State of Bahia (Brazil)." By 

 Arthur Smith Woodward, LL D., F.R.S., F.L.S , Y.P.G.S. 



This paper proves that the Lower Cretaceous formation of Bahia 

 extends along the coast to a point at least 130 miles south of the area 

 previously described. The fish-remains are referable to new species 

 of the genera Mawsonia, Lepidotus, and Scoiubroclwpea. Mawsonia 

 seems to have been scaleless, and differs from all known Jurassic and 

 Cretaceous Coelacanth fishes in lacking denticles on the fins. The 

 Lepidotus closely resembles the European AYealden L. Mantelli in 

 proportions, but is more strongly ornamented. The Sconibroclupea is 

 peculiar, in exhibiting onlj- scales where the anal finlets usually occur. 



2. " The Bala and Llandovery Rocks of Grlj-n Ceiriog (North 

 Wales)." By Dr. Theodore Groom, M.A., F.G.S., and Philip Lake, 

 M.A., F.G.S. 



In the district around Glyn Ceiriog, which the authors have 

 mapped on the 6 inch scale, the following succession is given : — 



Denbighshire Slates. 



Ty-Draw Slates, with Jl/b«0(j'r«/;i!«.5 J/arri ... ... ... ...1 T.iEAXxoN 



Fron-Frys Slates, with Peniamcncs undatns, Meristina of. cmssa, '■ and 



Nidnlitcs favus, etc. ... ... ... ... ... ... ) Llandovery. 



