390 REPORT-—1890. 
23. Microporella antiqua, Vine, Ib. 1885. 
24. Lunulites cretacea (?), Ib. 
In the material already alluded to there were many fragments of 
Polyzoa, but those of the species numbered 1, 14, and 23, in the above 
list, were unique ; some of the others were abundant, and some few were 
rather rare. The most characteristic of the whole were: Entalophora 
lineata, var. striatopora, Vine ; Osculipora plebeia, Novak ; and Diastopora 
fecunda, Vine. D. megalopora, Vine, was rare; Membranipora Dumerili, 
var. Cantabrigiensis, Vine, fairly abundant. 
Associated with these free forms of Polyzoa were an immense number 
of Foraminifera, Entomostraca,' Brachiopoda, and other organisms. The 
Foraminifera and Entomostraca were catalogued in the second paper on 
the Cambridge Greensand Polyzoa. 
IV. Ponyzoa ATTACHED TO CaMBRIDGE GREENSAND Fossius (B). 
(The fossils are Radiolites Mortoni, Mant.; Ostrea cunabula, Seeley; Pharetrospongia 
Strahani, Sollas.) 
: a, linearis, d’Orb., var. Mortoni, Vine. 
Se a) 
3. Proboscina dilatata,d’ Orb.,var.Cantabrigiensis, Vine. Ut e fen 
4 * ramosa, d’Orb. gs 
5 ches gigantopora, Vine. Adherent to Pharetrospongia 
Strahant. ; 
6. Diastopora foecunda, Vine. On Ostrea, Radiolites, and Pharetro- 
spongia Strahani. 
is af Hagenowi, Reuss. On Radiolites. 
8. = megalopora, Vine. On Ostrea cunabula. 
9. Lichenopora radiata, Aud. On Pharetrospongia Strahani. 
0. Membranipora Dumerili, var. Cantabrigiensis, Vine. (Fine 
colony.) On Iadiolites Mortoni. 
ibis 5 cretacea, d’Orb. On Ostrea cunabula and Radiolites 
Mortoni. 
12. x is var. Francqana, d’Orb. On Radiolites 
Morton. 
13. Lunulites cretacea (so called). Abundant on the outer shell of 
Radiolites Mortoni. 
The counterpart of this peculiar fauna only came into my possession 
on June 15, 1890, consequently I have not been able to allude to the 
species before. During a visit to Professor T. Rupert Jones, F.R.S., on 
the above date, he placed in my hand a small tube containing a number 
of fragments which had been picked out from the Chalk detritus, or Chalk- 
marl, of Charing, Kent, which is briefly referred to in the text, more par- 
ticularly in a note (by ‘ W. H.’) on page 2 of his ‘ Monograph of the 
Entomostraca of the Cretaceous Formation of England.’* The note 
referred to states: ‘The village of Charing stands on a bank of Chalk 
detritus, composed of fragments of white and grey chalk, which gradually 
1 See ‘ Further Notes on the Polyzoa of]the7Lower Greensand,’ &c., Proc. Yorks. 
Geol. Polyt. Soc. vol. xi. pt. ii. pp. 272-274. S—. 
2 Paleontographical Society, 1849. The note is by the late William Harris, Esq., 
¥.G.8., of Charing, Kent. 
