402 Journal of the Asiatic Society of Bengal. [November, 1913. 
geographically, must be considered as belonging to the 
same zoogeographical province. Their similarity may be 
interpreted as due both to their proximity in geographical 
ition, and to their stratigraphical homotaxis. i 
correlation places the anthracolithic faunas of the Shan 
States on the same level as the middle and upper Pro- 
ductus limestone of the Salt Range or of exotic block of 
Chitichun No. 1.’’! 
Although somewhat beyond the region treated of in 
this paper mention may be made of the fact that both devo- 
nian and anthracolithic limestones attain a considerable 
Mogok, Ruby Mines District, and in some of the Jalor caves 
there are large beds of freshwater shells and mammalian bones. 
PART IIl.—THE FAUNA OF THE CAVES. 
___ The following list of the animals that have been recorded 
from the limestone caves o Burma and Malaya, or are repre- 
Malayenses, and from papers on the late Signor Fea’s Burmese 
collection in the Ann. Civ, M us. Genova (1889-1897). 
© have added obeservations of our own, more particu- 
larly on the Orthoptera and Pedipalpi. 
! C, Diener, Anthracolithi oe a sae 
New Series, Vol. II, ep ae Pagans of the Shan States. Pal. Ind., 
