1857.] 



BAILY FOSSILS FROM THE CRIMEA. 



161 



Summary of Fossil Invertebrata from the Crimea. 



Number of species 



previously known 



New species 



Total 



O 



SJ 



o 



o 

 S 

 < 



i 

 l 



4 



4 



i 



09 



'a 

 £ 



el 

 u 

 O 

 Ec 



1 



>> 



P. 



O 



o 

 N 



e3 

 eS 



a 



V 



-a 

 o 

 a 



'rC 



u 



09 

 O 

 N 

 O 



pq 



Mollusca. 



o 



- Newer Tertiary. 



Older Tertiary. 



Upper Secondary 

 (Cretaceous). 



Lower Secondary 

 (Jurassic). 



a) 



-a 

 o 

 p< 

 o 



2- 

 u 

 09 



pq 



a 



.2 



"3 

 c 



03 



fi 



09 



09 

 -3 

 O 

 Pi 

 O 

 u 

 go 



§ 



09 



O 

 P. 



_o 



"o9 



ja 

 p< 



0) 



27 



18 



24 

 14 



... 



52 



33 



1 



2 



9 



9 



8 



3 



8 



8 



4 

 5? 



7 



7 



1 

 13 



13 



8 

 4 



45 



8 



42 



7 



38 



10 



7 

 4 



16 



.85 



24 



106 

 11 



Previously known.. 



Previously known- 

 New 



Total 



49 



5 



4? 



11 



2 



1 



16 



17 

 ] 



117 



44 

 16? 



Previously known .. 

 New 



Total 



i 



... 



8 



9? 





19 



9? 



3 



18 



60? 







Species before described, 226. New species, 60. 



Note on the Geology of the Neighbourhood of Sevastopol, 

 and the Southern Coast of the Crimea. By Charles F. 

 Cockburn, Esq., Captain, Royal Artillery. 



During the occupation of part of the Crimea by the xlllied Armies, 

 I availed myself of the opportunity my short stay in that country 

 afforded to collect a series of fossils and rock-specimens illustrative 

 of the geology of the neighbourhood of Sevastopol and Balaclava ; 

 amongst them were characteristic specimens from the shales on the 

 Woronzoff road, described by M. Du Bois de Montpe'reux as the 

 oldest fossiliferous deposits ; resting on these are the Jurassic rocks, 

 composing the mountain-chain which extends along the south-east 

 coast from Balaclava to Kaffa, a distance of upwards of 100 miles. 

 This formation, with the overlying cretaceous deposits, is, according 

 to French geologists, analogous to that of the Caucasus. Of these 

 Jurassic limestones, which are mostly of a hard and crystalline cha- 

 racter, collections were made from the Gorge of Iphigenia and Mo- 

 nastery of St. George, and include a series of the intrusive volcanic 

 rocks (syenite, porphyry, &c.) which have disrupted and pierced them 

 in every direction. 



From the quarries at Inkerman I succeeded in procuring many 

 fine specimens of a large Crania (C. spinulosa, Nilsson) and several 

 species of Ostrea common to the Upper Chalk of Europe. The 



VOL. XIV. PART I. M 



