273 
Post-Eocene.—Table Cape (T.). 
The valve on which was founded P. deformis, and recorded as 
Miocene, has all the appearance of a derived origin. 
FAMILY LIMiIIDAi. 
Genus Lima, Lamarck, 1789. 
L. Bassii, Woods, 1877; id., Tate, 1, p. 117; Harris, &, p. 310. 
Eocene.—River Murray Cliffs, Aldinga Bay, Adelaide-bore 
(S.A.); Bellarine Pen. (H. and P.), Muddy Creek, Gelibrand 
River, Mornington, Belmont, Cape Otway, Maude, Shelford (V.); 
also N.Z. 
Post-Eocrne.—Table Cape (Tasmania). 
L. linguliformis, Tae, 1, p. 118; Harris, &, p. 310. 
EKocene.—Belmont (4. and P.), Muddy Creek, Mornington 
Vv 
Post-Eocens.—Table Cape (Tasmania). 
L. polyactina, Tate, 1, p. 118. 
Eocrenet.—Adelaide-bore. 
Section Limatuta, S. Wood, 1839. 
L. Jeffreysiana, Jae, 1884; id, 1, p. 119; Harris, &, p. 311. 
Lima bullata | Born], Hutton, Cat. Tert. Moll., N.Z., p. 33, 
1873 ; non Born. 
Eocene.—River Murray Cliffs, Aldinga Bay, Mount Gambier 
(S.A.); Waurn Ponds (H. and P.); Muddy Creek, Mornington, 
Shelford (V.); also New Zealand [Oamaru Formation]. 
Post-EocEene.—Spring Creek (V.) ; Zable Cape (T.). 
Miocene.—Edithburg, Aldinga Bay, River Murray Cliffs 
(S.A.); Muddy Creek (V.). 
L. subnodulosa, spec. nov. 
Test stout; shell inflated, slightly inequilateral (the posterior 
side being a little protuberant in the middle line). Ornamented 
with 25 stout, rounded ribs, which are somewhat nodulose 
anteriorly; the narrower interstices are crossed by moderately 
stout threadlets. 
This species has the aspect of a Limea, but there are no traces 
of teeth. 
Dimensions.—Umbo-ventral diameter, 4:5; antero-dorsal 
diameter, 3:5; height of valve, 1:75 mm. 
MiocenE.—Muddy Creek, Victoria (one ex.). The shell is 
somewhat polished, evidently by erosion, and may have been 
derived from the underlying Eocene. 
L. polynema, Tate, 1, p. 119. 
Eocenr.—Adelaide-bore. 
