INTRODUCTIOM. XlX 



on the Continent. Again, Mr. Logan has shown, fiom liis collections in Canada, several 

 Ein-opean species not yet detected in New-York or farther westward, whicli still more 

 assimilate the eastern and western extremities of these formations so widely separated by 

 the Atlantic. 



In commencing our examinations, we find that marine plants are coeval witli the earliest 

 created animal forms ; and that botli appear, though obscurely, in the same rock. 

 Throughout the entire scries of liic lower division, each rock or group appears to be typified 

 by a few peculiar forms of this class, which arc (juite as much restricted in their geological 

 range as are those of animal life. 



Among the lower classes of animals we find an absolute identity in many of the species, 

 and a remarkable similarity in several others. We can hardly refuse to believe that our 

 Graptolite shales are of the same age as those of England, Ireland or Sweden, when we 

 find so many identical species in the two formations ; and tiiougli we here have many not 

 yet recognized in those countries, some of them will doubtless be found there on further 

 examination. The Chatetes petropolitanus of Russia is probably the same with our C. 

 lycoperdon, which likewise occurs in the Caradoc sandstone of Britain.* Nearly all the 

 other Corals of this period, however, are new or undescribcit. 



Among the Crinoiuea, most of the forms appear to be quite new, and to present even 

 generic characters unknown in the higher rocks. We are able to recognize, nevertheless, 

 the occurrence of the family Cystidea, in a species of Echino-encrinites allied to the E. 

 ana-ulosus. Those singular forms, the Sp/iaronites, have not yet been discovered in this 

 country ; and though abundant in Sweden and Russia, have only recently been recognized 

 in Eno-land.f We shall duul)lless yet discover the same fossil in tjiis country, tiiough it is 

 not probable that it will ever become cliaracteristic of the strata. We find that animals of 

 this order commenced their existence among the earliest forms, and as soon as calcareous 

 matter formed any considerable portion of the deposit. 



Of the Brachiopoda, we have several identical and many allied species in the different 

 trencra. The Lhi'nda quadrata is clearly identical witli the Russian species; and another 

 species which we find in our Trenton limestone, is apparently tlie same as the L. attenuata 



* This fossil is often referred to Favosites fibrosa, which is regarded as having a great geological range. In our 

 Trenton limestone species, connecting foramina are never visible; while in the similar form in the Pentamerus and 

 Delthyris shaly limestone, there is no difficulty in distinguishing them. I liave not recently examined good specimens 

 from the Clinton and Niagara groups, but am at present inclined to express some doubt as to the identity of the species 

 in that roclc and the Trenton limestone, and the statement on page 67 maybe received with some allowance. 



t See Geology of Russia in Europe and the Ural Mountains, Vol. i, p. 3S. The facts in relation to the discovery of 

 Cystidea in England, there made known, had escaped my observation at the time I wrote my description oi Echino- 

 encrinites, and translated llie passages from the second volume of the same work. 



