1859.] PARKER AND JONES FORAMINIFERA. 2G1 



3. M. appressa, n. sp. 3. E. arcuata, n. sp. 



4. M. Cyclops, Busk. 4. E. oculata, n. sp. 



5. Lepralia, Johnston. 5. E. bimarginata, n. sp. 



1. L. — < — , sp. ? 6. E. hastigera, n. sp. 



2. L. submarginata, n. sp. 7. E. inornata, n. sp. 



3. L. subcarinata, n. sp. 8. E. , sp. ? 



4. L. doliiformis, n. sp. 8. Retepora, Imperato. 



6. Cellepora, 0. Fair. 1. R. , sp.? 



1. C. Gambierensis, n. sp. 9. Psileschara, nov. gen. 



2. C. hemisphaerica, n. sp. 1. P. pustulosa, n. sp. 



3. C. mimmularia, n. sp. 2. P. subsulcata, n. sp. 



4. C. eostata, n. sp. 10. Coeleschara, nov. gen. 



5. C. tnbulosa, n. sp. 1. C. australis, n.sp. 



6. C. spongiosa, n.sp.? 11. Melicerita, M. -Edwards. 

 7. Eschara, Linn. 1. M. angustiloba, n.sp. 



1. E. simplex, n. sp. 12. Scutularia, nov. gen. 



2. E. papilkta, n. sp. 1. S. prima, n. sp. 



II. P. CYCLOSTOMATA. 



1 . Pustulopora, Blahiville. 3. Hornera, Lamx. 



1. P. distans, n. sp. 1. H. Gambierensis, n. sp. ? 



2. Idmonea, La mx. 2. H. rugulosa, n. sp. ? 



1. I. Milneana, D'Orbigny. 

 ? 2. I. ligulata, n. sp. 



Note on the Foraminifera from the Bryozoan Limestone near 

 Mount Gambier, South Australia. By W. K. Parker, Esq., and 

 T. Hupert Jones, E.G.S. 



A small portion of the deposit has yielded several Foraminifera, 

 namely, — 



Polymorphina lactea, J". Sf W. Rather large. 1 

 Textularia pygmaea, D'Orb. Small. I Not rare. 



agglutinans, IP Orb. SmaU. 



Globigerina bulloides, L v Orb. Small. Common. 



Cassidulina oblonga, lien.ts. Small. Rather common. 



Etosalina Berthelotiana, D'Orb. (a variety of Sotalia Turbo, D'Orb.). 



Small. Bather common. 

 BotaliaT7ngeriana,2) , Or6. Rather large. Abundant. "] Varietiesofifo- 



Haidingerii, UOrb. Small. Not ancommon. ( talia (Planor- 



reticulata, Oz ;/.<■/•. Small. Nut rare. ( bvUna)farcta, 



(Anomalina) Etotnla, D'Orb. Small. Rare. J F.&M. 



The above-named Rhizopods exist ;it the present day, and for 1 1 1« • 

 most part live in rather deep water, at Gram 200 to 300 fathoms. It 

 would hence appear that the fragmentary Bryozoa forming the mass 

 of the deposit were washed down from a higher zone of sea-bottom 

 and mingled with the Foraminifera inhabiting deep water. 



