34 THE AGE OF THE EARTH 



to palacontoloi^^y as a oruidc in unravelling the tangled 

 history of animal evolution. Peripatus is alive to-day, 

 and can be studied in all the details of its structure 

 and developmcMit ; it is inHnitely more ancestral, and 

 tells of a far more remote past than any fossil Arthropod, 

 although such fossils are well known in all the older 

 of the Palaco/oic rocks. And )('t Peri[)atus is not 

 known as a fossil. Peripatus has come down, with 

 but little chauLTe, from a time, on a moderate estimate, 

 at least twice as remote, and probably many times as 

 remote, as the earliest known Cambrian fossil. The 

 agencies which, it is believed, have crushed and heated 

 the Archaean rocks so as to obliterate the traces of 

 life which they contained were powerless to efface this 

 ancient t)pe, for, although the passing generations may 

 have escaped record, the likeness of each was stamped 

 on that which succeeded it, and has continued down 

 to the present da)'. It is, of course, a perfectly trite 

 and obvious conclusion but not the less one to be 

 wondered at, that the force of heredity should thus far 

 outlast the ebb and flow of terrestrial chansje throuorhout 

 the vast period over which the geologist is our guide. 



If, however, the older Palaeozoic rocks tell us nothing 

 of the origin of the antenna-bearing Arthropods, what do 

 they tell us of the history of the Myriapod and Hexapod 

 Classes ? 



The Myriapods are well represented in Palaeozoic 

 strata, two species being found in the Devonian and no 

 less than thirty-two in the Carboniferous. Although 

 placed in an Order (Archipolypoda) separate from those 

 of living M)riapods, these species are by no means 

 primitive, and do not sup[>ly an)' information as to the 

 steps by which the Class arose. The imperfection of 

 the record is well seen in the traces of this Class ; for 

 between the Carboniferous rocks and the Oligocene 

 there are no remains of undoubted IMyriapods. 



We now come to the consideration of insects, of which 

 an adequate discussion w^ould occupy a great deal too 

 much of your time. An immense number of species 

 are found in the Palaeozoic rocks, and these are con- 



