32 MEDLlCOTTj gItlLLONG PtATEltT, 



indica/ Sioh; Cerithium inanguratum, Stol. ; Tritonidea Requienianaf 

 d^Orb. (two casts); Hemifusus cinctMS, Forbes (one); a Phaaianellaj 

 Turr'itella ; Muspira ; Dentalium ; a Jaiiira, close to J. Fleuriawsianaf 

 d'Orb. (one fragment) ; Bxogyra MatJieroniana, d'Orb., one small speci* 

 men -, Spondilus siriatus, Lam. ; Modiola ti/pica, Forb. i Cardita orMcU" 

 laris, Forb. ; Cardium ; one small specimen of Terehratula, most likely 

 T. carnea ; TurbinoUa ; Hemiaster ; Holaster and BrissuSf with some 

 others^ not fit foi* specific determination . The faeies of this group rather 

 resembles that of the Ootate^or beds of Southern India, 



" From about the same horizon under Mamluh a Conoetypus, iioffc 

 tmlike C. ovatm of d^Orbig-ny, from the Craie chloritee. 



"From the well known fossil locality about two miles from Theria 

 ghat^ on the fourth cross-cut taken by the Khasia path between 

 the zigzags of the made road^ or the first below the DeviFs Bridge^, 

 the most characteristic fossils are Nautilus l(svigatu8, d^Orb., rare } 

 Bacidites vagina^ Forbes^ common; Cyprcea globulosa and pilwlom^ 

 Stol.; Eostellaria palliata, Forbes; Alaria tegulata^ StoL; Alaria 

 glandina, Stol. ; Lyria crassieostata, Stol. ; Tolutilitkes septemcostat%, 

 Forbes; Tritonidea Reqide^iiana, d'Orh.; ZaiMns EeussU, Stol. ; Fseu- 

 doliva siihcostata, Stol. ; Turritella Pondicherriensis, Forbes ; Ttcrr. mnltu 

 striata,^ss. ; Mitreola cytkarina, Forbes; Empira lirata, Sow; Gyrodes 

 pansus, Stol. ; Giibula granulosa, Stol. ; Nerita divaricata, d^Orb. ; Eupty- 

 cha larvata, Stol. ; Actaeon curculio, Forbes, Peden septempUcatus, Nils. ; 

 Janira quadricostata, Sow.; GrypJioea vesicularis, Lam. ; Spondylus striatus^ 

 Lam. ; Peden, closely allied to P. rugosus, Dixon ; fragments of an 

 Inoceramus, etc. ; RhyncJwnella compressa, d*Orb. ; Terehratula, two 

 species, probably T. biplicata and carnea. Ananchytes and Bryssusj 

 several species of both occur, but seem to be distinct from any as jet 

 known. 



" Nearly all the fossils above quoted occur also in the Arrialoor beds 

 of the South-Indian cretaceous series; but there are a number of 



( isa ) 



