Bulletin 35 
332 
184 
ered. Mr. Forrest says : The quarry in which the fossil fish was 
found is at Golden Grove situated at about three-quarters to one 
mile south of St. John or three quarter mile W. S. \V. of Drew- 
hill or Belmont Estate. It is in the central plain and is not a 
calcareous formation. To the central plain belong also the beds 
of chert with land and freshwater shells and silicified fossil woods 
and beds of fine grained sandstone with leaf impressions.” 
The nearest relations of this fossil fish are found in the 
eocene of Europe (Monte Bolca, etc.) and living in the Pacific 
and Indian Seas. 
PAPER Xo. 24. 
FURTHER NOTES ON THE CARON/ SERIES AT 
SA VANETA. 
Paper read before the Agricultural Society Sept. 13, 1912 
and published as Societ}' Paper Xo. 520, Agr. Soc. Trinidad and 
Tobago, 1912. Paging of Separate from i to 5. 
Paf^e / 
By the kindness of F. J. Morris, Esq., of Forres Park, 1 was 
able to make a second visit to the Springvale Quarry and akso 
have a general look at the country in the neighbourhood which I 
had not seen for some 3'ears. This enabled me to gain some ad- 
ditional information of importance in settling the position, &c. 
of the Springvale Shellbed. Indeed, I found that the bed named 
was reall}’ an outcrop of the same .series as that discovered bj* the 
late Louis Alexander Lero\’. the fossils from which I have al- 
read}’ described and named. Mr. Morris took me to the Quarry 
where I found that the later excavations had revealed the thick- 
ness dip and position of the Shellbed. It was apparenth' from 
three to four feet thick. The dip was about 30 degrees to the X. 
\V. The Shellbed la^- conformabh' upon which I might call a 
mudbed ; a stratum of impure cla}' with comminuted shells. 
These observations bring the Springvale Shellbed into line with 
