PART 3 .] Feistmantel: KarUarh&ri and South Bewah Coal-fields. 
181 
one or two species, occui's in greater numbeis. Two not very favourably pre¬ 
served specimens appear to represent Scldzoneura gondwanensis, Pstm. 
Ho fossils w'cre found as yet from tlie seam above tbe bottom seam in the 
Serampnr area, but the correlation of the second seam in the Karharbari area, 
with that in the Serampnr area, is apparently correct, the bottom seams in both 
areas being the same. 
The Srd seam, Passerahhia. 
There is not much new to be reported from the Srd seam area (1. e. p. 40). I 
have obtained a few specimens fi’om shaft Ho. 17 B' which represent a species 
already known from this place, viz., Noggerathiopsis hislopi, Bunb.; some speci¬ 
mens indicating very large leaves. 
From shaft Ho. 17 C I have obtained one specimen which contains three 
forms new for this place and therefore for the Srd seam. 
Gangamopteris comp, angustifolia, Mc’Coy.—One leaf. 
TFinqed seeds .—Of the same kind as that one figured hy me from Buriadi" and known 
also from Mohpani. Similar seeds, but smaller, are also known from the Damuda 
and Panohet division. I take them to represent the genus Samaropsis (comp 
parvula, Heer and Schmalhausen). 
Seed .—Another large seed also was found. Of this I can form no idea at pi'esent, but I 
shall figure it with all the other new forms in a supplement to the Talohir-Karhar- 
bari flora. 
This third seam appears to be developed in the northern portion of the 
Karharbari area only. 
No. 4 seam, the “hill-seam.'” 
In my already-mentioned paper I also mentioned the seams on the Komaljoro 
and Bhuddua hills, classing them as a 4th scam, and judging from some fossils 
found on the Komaljore (Lumki) hill, and from the very much higher position of 
the seam, I represented them as belonging mo.st probably to the Damuda division. 
Ho fossils were known from the Bhuddua hill. This time, however, I collected 
some fragments from above the coal; they arc Olossopteris; they are of course 
at present quite insufficient for any conclusive decision, but I think there are 
strati graphical points enough which, in combination with tho fossils from the 
Lumki hill, show that it is an independent seam. 
Bali hill in tho western portion of the field is another place where this 
“ hill seam ” is represented. I have not yet examined this locality, but intend to 
do so on the first opportunity, as it is probable that more fossils may be found 
there, from which the horizon may be better fixed. 
^ The sections of tliis shaft, as well as of tho other one, No. IV C, are described in my Talchir- 
Karharbdri flora, ?. c. p. 40-42, where I also uiimed tho fossils. 
»Ibidem, I’hitc XXIV, fig. 5. 
