PHYLOGENY. 



127 



from the papers of Dr. Rowe (' Proc. G-eol. Assoc.,' vols, xvi, xvii), and also 

 from notes furnished by Dr. H. P. Blackmore and Mr. T. H. Withers. 





e 



© 



O § 



Zone of 



Belemnitella 



mucronata. 



Zone of 



Actinocamax 



quadratus. 



o'l 

 ° Cs 



Zone of 



Micraster 



cor-anginum. 



Zone of 

 M. cortes- 

 tudinarium. 



if 



o 



hi 



O V3 



si 



o « 



N a, 



§1 



Zone of 



Rhynchonella 



Cuvieri. 



03 



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 O <r> 



hi z 



** 2 



if 



■ 

 © 



O at 



a » 



o ^ 

 N S 



Nymphaster Goombei, Forbes 

 oligoplax, Sladen 

 Pentagonaster quinqueloba, 



Goldfuss 

 obtusus, Forbes 

 Metopaster Parhinsoni, Forbes 

 uncatus, Forbes . 

 quadratus, n. sp. 

 cornutus, Sladen 

 Mitraster Hunteri, Forbes . 



rugatus, Forbes 

 Pycinaster angustatus, Forbes 

 senonensis, Valette 

 Stauranderaster bulbiferus, Forbes 

 Boysi, Forbes 

 ocellatus, Forbes . 

 pistilliferus, Forbes 

 argus, u. sp. . 

 Arthraster Dixoni, Forbes . 

 ,, cristatus, n. sp. 





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THE PHYLOGENY OF THE CRETACEOUS ASTEROIDEA. 



If we examine the various species of a genus or group of related genera of 

 Cretaceous Asteroids, we find that there is a similar transition from smooth to 

 spinous forms through an intermediate form, to that which has been observed in 

 Ammonites and Brachiopods. 



Both in Ammonites and Brachiopods single specimens show the whole life- 

 history of the individual, for the shell of the animal is not materially altered in 

 character after it has once been formed. It is therefore possible to show, e. g., 

 that the character of the ornament of the shell of an Ammonite was smooth 

 in its infancy, costate in its adolescence, spinous in the adult, and it has also been 

 shown that this life-history depicted by the individual is an epitome of the 

 phylogenetic history of the species (Buckman, ' Mon. Amnion. Inf. Oolite,' Pal. 

 Soc, 1905, p. cc). Similar observations have been made with regard to Brachio- 

 pods (Buckman, ' Quart. Journ. Geol. Soc.,' vol. lxiii, 1907, p. 338) ; primitively the 

 Brachiopod shell is smooth externally, more advanced forms are progressively 

 costate and then spinous. Occasionally species may regress towards a primitive 



