THE SHAPES OF VERTEBRATE SKELETONS. 199 



thin, but more decided and comparatively distant fissures aa 

 they become thick. Fig 289, which is a 

 horizontal longitudinal section, shows 

 how these thickening layers will adjust 

 themselves on the convex and the con 

 cave surfaces, supposing the fibres of 

 which they are composed to be oblique, 

 as their function requires ; and it is not difficult to see that 

 when once definite divisions have been established, they will 

 advance inwards as the layers develop ; and will so produce 

 a series of muscular bundles. Here then we have something 

 like the myocommata which are traceable in the Amphioxus, 

 and are conspicuous in all superior fishes. 



256. These speculative conceptions I have ventured to 

 present with the view of showing that the hypothesis of the 

 mechanical genesis of vertebrate structure, is not wholly at 

 fault when applied to the most rudimentary vertebrate ani 

 mal. Lest it should be alleged that the question is begged 

 if we set out with a type which, like the Amphioxus, already 

 displays segmentation throughout its muscular system, it 

 seemed needful to indicate conceivable modes in which there 

 may have been mechanically produced those leading traits 

 that distinguish the Amphioxus. It seemed needful to 

 assign an origin for the iiotochord ; and to this we see a 

 clue in the differentiating effects of the transverse strain. It 

 seemed needful to account for the existence of muscular 

 divisions while yet there are no vertebral divisions ; and for 

 this, also, the transverse strain furnishes a feasible reason. 



But now, having shown that the actions and reactions in 

 volved by its mode of locomotion, are possible causes of those 

 rudimentary structures which the simplest vertebrate animal 

 presents, let us return to the region of established fact, and 

 consider whether such actions and reactions as we actually 

 witness, are adequate causes of those observed differentiations 

 and integrations which distinguish the more-developed ver 



