454 NOTES. 



rate of growth for the massive Astraeidse of 18 feet in a thousand years, 

 whereas Dana allows at the utmost 5 feet. It is not, however, to be 

 supposed that either of these estimates is universally applicable, since 

 the different species of corals, like all other animals, have different rates 

 of growth, and the rapidity might also vary under different circum- 

 stances. It would, indeed, be extremely interesting if only the maximum 

 rapidity of growth in individual corals as those of different reefs 

 could be established by observation ; but to do this would be a highly 

 complicated and difficult task, since the vigour of growth of the animals 

 must depend on a great number of different influences which combine 

 to affect it. 



Note 105, page 229. I have been at great pains in seeking in books 

 of travels or descriptions of the different species of corals for data as to 

 the various forms which coral-blocks are capable of assuming in diffe- 

 rent situations, but the results of my search have been terribly meagre. 

 I found, in fact, only the observations made by Ehrenberg to the effect 

 that Stcpliaiiocora HempricMi, Ehren., in the Bed Sea, forms branched 

 or flattened stocks according to whether it lives in still or in rough 

 water (see Ehren. Corals of the Red Sea). This, in my opinion, is 

 the inevitable result of the faulty methods of investigation hitherto 

 applied to these creatures; naturalists are desirous of distinguishing 

 the species, and accordingly they have above everything paid attention 

 to the distinctive character as with insects, shells, &c. and at the 

 time like Dana in his magnificent work on corals, connected with 

 Wilkes's expedition they have bestowed the utmost pains in ascertain- 

 ing the limits of variability for individual species, as he has done with 

 the greatest care in regard to certain madrepores. Klunzinger's new 

 work on the corals of the Red Sea supplies an abundance of material 

 of this kind. But up to the present time no systematic observa- 

 tions have been carried out bearing on the question which we are 

 especially studying as to how far currents in the sea, variations 

 in temperature, or the saline constituents and other physico-chemical 

 influences, may affect each species individually. The excuse to be 

 offered is evidently this : that the fundamental essence of Darwin's 

 theory is only now beginning to exert its influence, and that we are only 

 now beginning to recognise the necessity for not merely putting off 

 these reacting conditions with an attempt at a hypothetical explanation, 

 but for throwing on them the light of carefully conducted research, and, 

 wherever it is possible, of actual experiment. Another and a very 

 serious hindrance lies in the difficulty of obtaining the living material 

 that is indispensable for such investigations; stationary zoologists, 

 qualified to conduct 1hem, are not many in the tropics, and travellers 

 can never have time enough to make any really valuable observations 

 of this kind. We must hope that we may ere long see a few zoological 

 stations established in the tropical seas, such as that inaugurated with 



