338 
Details of Bores Nos. 1 to 11, etc. — continued. 
Bore No. 3— continued. 
Depth (feet). 
Nature of Rock. 
Details and Fossil Contents. 
226— con¬ 
tinued. 
Gasteropoda. — Liopyrga quadricingulata, 
Tate ; Eglisia triplicata, Tate sp. ; Natica 
substolida, Tate ; Turritella tristira, Tate ; T. 
circumligata , Verco.; T. platyspirci, T. 
W.; Tylospira coronata, Tate sp. ; Lotorium cf. 
tumulosum, Tate sp. ; Zemira praecursoria, 
Tate; Tudicla costata, Tate ; Fasciolaria 
rugata, Tate; Marginellaprceformicula, Chapm. 
and Gabr.; Voluta weldi, T. W. ; Ancilla 
hehera, Hutton sp. ; Terebra simplex, T. 
Woods; T. geniculata, Tate; Pleurotoma 
trilirata, Harr. ; Pleurotoma ( Drillia ) trevori, 
T. W. sp. ; Bela sculptilis, Tate. 
Crustacea.—C helae of crab, indet. 
Pisces. — Lamna compressa, Ag. ; Chimse- 
roid teeth (fragments); (?) Chrysophrys 
(tooth) ; teleostean fish otoliths, indet. 
About 260 
Fragments of fine-grained 
fossiliferous, calcareous 
sandstone; sometimes 
glauconitic 
Algae. — Lithothamnium (a foliaceous and en¬ 
crusting form). 
Foraminifera. — Miliolina vulgaris, d’Orb. 
sp. ; Trillina howchini, Schlumb. ; Orbitolites 
complanata,~L&m. ; Polymorphina gibba, d’Orb.; 
Patellina corrugata, Will. sp. ; Truncatulina 
ungeriana, d’Orb. sp. ; Anomalina polymorpha, 
Costa ; Polystomella imperatrix, Brady ; Oper- 
culina complanata, Defr. 
Anthozoa. — Placotrochus elongatus, Duncan. 
Echestodermata. — Arachnoides ( Mono- 
stychia) australis, Laube sp. 
Polyzoa. — Cellepora sp. (a massive form); 
(?) Schizoporella sp. 
Gasteropoda. —Turritella murrayana, Tate 
(a cast) 
Ostracoda. —Cytherella pulchra, G. S. B. 
Notes on Bore No. 3. 
This series is very imperfect, the samples commencing at 201 feet. There 
is an admixture of Kalimnan and Janjukian forms in the blue clay from 201 
to 220 feet, typical fossils of the Kalimnan from this sample being Glycimeris 
convexus, Limopsis beaumariensis, Liopyrga quadricingulata , and Bathyactis 
bsaumariensis. Among the Janjukian fossils we may cite Deltocyathus fonti- 
ncdis, Pentagonaster sp., and Pleurotoma selwyni. 
The shelly and glauconitic sand from 226 feet is an almost clean deposit 
with a Janjukian fauna, but a few Kalimnan types, as Limopsis beaumariensis 
and Cardita calva, are still in evidence. 
The glauconitic and calcareous sandstone at 260 feet is essentially Jan¬ 
jukian ; whilst the presence of Trillina howchini points to a lower phase of 
the Janjukian series. 
