. Geological magazine . )Phr> Fig. 2.—DouviUSiceras euomphalus (Sliarpe).—a, lateral view; b, peripheral viewof the same specimen ; c, suture-line of the same example as seen at the placemarked s in a and b. Lower Chalk: Humble Point, close to Whitlands,west of Lyme Regis. Drawn of the natural size from the example in theBritish Museum (Nat. Hist.) that was collected and presented to theMuseum hy Dr. Eowe and CD. Sherborn, Esq. Among some Chalk fossils recently collected by Dr. Arthur Eowe,, and Mr. C. Davies Sherborn, , from the hard nodularCenomanian Limestone with grit and gr


. Geological magazine . )Phr> Fig. 2.—DouviUSiceras euomphalus (Sliarpe).—a, lateral view; b, peripheral viewof the same specimen ; c, suture-line of the same example as seen at the placemarked s in a and b. Lower Chalk: Humble Point, close to Whitlands,west of Lyme Regis. Drawn of the natural size from the example in theBritish Museum (Nat. Hist.) that was collected and presented to theMuseum hy Dr. Eowe and CD. Sherborn, Esq. Among some Chalk fossils recently collected by Dr. Arthur Eowe,, and Mr. C. Davies Sherborn, , from the hard nodularCenomanian Limestone with grit and green grains, half a mile fromthe shore at Humble Point, close to Whitlands (west of LymeKegi>s), Devonshire, there is a specimen which I consider to bereferable to Sharpes species (see Figs. 2a-c). Being entirelyseptate, and therefore incomplete, it does not furnish the charactersof the adult shell; nevertheless, it is a particularly interestingspecimen, for being larger than either of the previously recordedexamp


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