680 BEroRT— 18C3. 



TirrhraUiln nifnin, Conr., is very probably Waldhfimiapjdrinafa, G]dL 

 Jiullu jwtroxa. ( i)iir., has the shape of Tonuitina (wimia, Bd. 

 I'l epithila pioi-iipta, Conr., is certainly /;n'«tvy>s, Midd. 

 Tmritflln, sp. iiid., resembles Mvsalin lactcola. 



':l>oliiini pitnmim, Cour., resembles the youiifr of Prime nodosa, Chemn. 

 I'lisiDi (jf)tlcidi(s, Cour. A similar shell has just been taken at the Favallorit* 

 by iJr. Cooper. 



121. To correct the general table of "MoUnsca of the "West Coast of N, 

 America" (First lU'iwrt, pp. 298-345), and the deductions founded upon it 

 (pp. 34()-3(J7), would involve the necessity of reprinting a considerable por- 

 ti )n. The student, being now in possession of all the known sources of 

 fresh information, can with his own pen strike out the spurious species, alter 

 the synonyms, insert the newly discovered forms, and make the requisite 

 corrections in the classiticd results. 



122. With regard to the tropicf.l la ia, the rescaiches at Cape St. Lucas 

 and in the interior of the Gulf of C iifornia, though leaving much to be 

 desired, bear-out the g(Mieral conclusions arrivcd-at in paragraphs 78-87. 

 The evidence for the identity of specific forms on the Atlantic and Pacific sides 

 of Central America has been greatly confirmed. Dr. Gould writes, "The 

 doctrine of local limitations meets with so few apparent exceptions that we 

 admit it as an axiom in zoology that species strongly resembling each other, 

 derived from widely diverse localities, especially if a continent intervenes, 

 and if no known or plausible means of comuiunication can be assigned, 

 should be assumed as different until their identity can be proved {ride E. E. 

 3lloll. Intr. p. xi). Much study of living s])ecimens must be made before 

 the apparent exceptions can be brought under the rule."' It has, however, 

 to be borne in mind that the researches of modern geology clearly point to 

 considerable alterations in the existing configuiation of continents, and vu 

 the consequent direction of ocean-currents, during the ascertained ])eriod of 

 many species now living. Xor are we warranted in the belief that the 

 existing fauna in any locality has been created at i^ny one time, or has 

 radiated from any single s])Ot. To study the relation^ of living shells simply 

 in connexion v^th the existing map of the world must lead but to partial 

 result*;. The tacts accumulating with regard to the British species, by 

 tracing them through the northern drift (now found even on the Snowdonian 

 range), to the oldest crag deposits when Europe was contained in far different 

 boundaries, show how altered may have been the configuration of the ncAV 

 world when the oldest of its molluscs were first created. Coordinately with 

 the glacial period. Central America may have been a group of islands; co- 

 ordinately with the creation oi Sdxicava pholadis and (Jhri/sodomus cinliqituSj 

 the gulf-weed may have floated between the Kocky Mountains in the 

 archipelago of West America, and Japanese molluscs may have known how 

 to migrate to the Mediterranean shores. Dr. Gould's position may there- 

 fore be accepted in theory ; yet, in practice, the " imperfection of the geological 

 record"*, and even of uur knowledge of existing species and their variations, 

 demands that the greatest caution be exercised in building results on deduc- 

 tions from otir ignorance. Already the fossil M(dea rinijens of the Atlantic 

 has proved a " Rosetta Stone " to interpret the Cyprcpa exanthema, Pvrpura 

 jmtula, and other Caribbean shells of the Pacific ; and as the geology of the 

 West Coast advances, so may we expect to find traces of previous denizens of 



• No student of geographical distribution should omit to weigh carefully the chapter 

 on this suhjrt't in Dai'ftiu's ' Origin of Species,' and the information given in L^ell's 

 ' Antiuuitv of Mao.' 



166 



