280 COSMOS. 



and more elevated portions of the old red sandstone, was main 

 tained through all the subsequent epochs to the most recent 

 chalk formations ; amid the peculiar characteristics exhibited 

 in the vegetable forms contained in the coal measures, there 

 is, however, a strikingly-marked prevalence of the same fami- 

 lies, if not of the same species,* in all parts of the earth as it 

 then existed, as in Nsw Holland, Canada, Greenland, and 

 Melville Island. 



The vegetation of the primitive period exhibits forms which, 

 from their simultaneous affinity with several families of the 

 present world, testify that many intermediate links must have 

 become extinct in the scale of organic development. Thus, 

 for example, to mention only two instances, we would notice 

 the Lepidodendra, which, according to Lindley, occupy a place 

 between the Coniferse and the Lycopodiacese,t and the Arau- 

 cariaj and pines, which exhibit some peculiarities in the union 

 of their vascular bundles. Even if we limit our consideration 

 to the present world alone, we must regard as highly import- 

 ant the discovery of Cycadea3 and Conifera side by side with 

 Sagenariae and Lepidodendra in the ancient coal measures. 

 The Conifers are not only allied to Cupulifera and Betulina), 

 with which we find them associated in lignite formations, but 

 also with LycopodiacesB. The family of the sago-like Cyca- 

 deae approaches most nearly to palms in its external appear- 

 ance, while these plants are specially allied to Conifers in re- 

 spect to the structure of their blossoms and seed.J Where 

 many beds of coal are superposed over one another, the fami- 

 lies and species are not always blended, being most frequently 

 grouped together in separate genera ; LycopodiaceaV and cer- 

 tain ferns being alone found in one bed, and Stigmaria3 and 

 Sigillaria3 in another. In order to give some idea of the lux- 

 uriance of the vegetation of the primitive world, and of tho 

 immense masses of vegetable matter which was doubtlessly 

 accumulated in currents arid converted in a moist condition 

 into coal, I would instance the Saarbriicker coal measures, 



* Adolphe Brongniart, Prodrome d'nne Hist, des Vigitaux Fossiles, p. 

 179 ; Buckland, Geology, p. 479 ; Endlicher and Unger, Grundzuge der 

 Bolanik, 1843, s. 455. 



t " By means of Lepidodendron, a better passage is established from 

 flowering to flowerless plants than by either Equisetura or Cycas, or 

 any other known genus." Lindley and Hutton, Fossil Flora, vol. ii., 

 p. 53. 



t Ktinth, Anordwtng der PJlanzenfamilien, in his Handb. der Dotanik, 

 s. 307 und 314. 



That coal has not been formed from vegetable fibers charred b? 



