r I 



THE PROBLEMS OF THE DEEP SEA 49 



t prove that the shells have been transported into 

 the position in which they are found ; while, on 

 the other hand, the absence of shells in a deposit 

 will not justify the conclusion that the waters in 

 which it was formed were devoid of animal in- 

 habitants, inasmuch as they might have been only 

 too deep for habitation. 



The new line of investigation thus opened by 

 the French naturalists was followed up by the 

 Norwegian, Sars, in 1835, by Edward Forbes, in 

 our own country, in 1840, 1 and by (Ersted, in 

 Denmark, a few years later. The genius of 

 Forbes, combined with his extensive knowledge of 

 botany, invertebrate zoology, and geology, enabled 

 him to do more than any of his compeers, in 

 bringing the importance of distribution in depth 

 into notice ; and his researches in the ^Egean Sea, 



1 In the paper in the Memoirs of the Survey cited farther on, 

 Forbes writes : 



"In an essay 'On the Association of Mollusca on the 

 British Coasts, considered with reference to Pleistocene 

 Geology,' printed in [the Edinburgh Academic Annual for] 1840, 

 I described the mollusca, as distributed on our shores and seas, 

 in four great zones or regions, usually denominated ' The Lit- 

 toral Zone,' 'The region of Laminarice,' 'The region of Coral- 

 lines,' and 'The region of Corals.' An extensive series of 

 researches, chiefly conducted by the members of the committee 

 appointed by the British Association to investigate the marine 

 p-ology of Britain by means of the dredge, have not invalid;ii>-d 

 this classification, and the researches of Professor Loven, in the 

 Norwegian and Lapland seas, have borne out their correct 

 The first two of the regions above mentioned had been ]>r> vi- 

 ously noticed by Lamouroux, in his account of the distribution 

 (vertically) of sea-weeds, by Andouin and Milne Edwards in 

 their Obterralion* on the Natural History of the coast of / V 

 and by Sars in the preface to Ills Bcskrivelser og JayUayelser." 



190 



