ECHINUIDKA. II. ,j 



and not cup-shaped at tlie upper eud; tlie ucck is well developed. The blade is coarselv dentate along 

 the whole edge; the lower part of the blade is \-ery narrow, forming a small tube. The basal part is 

 not distinctly developed, tlie articular surface is broad and well developed. Some larger forms, verv 

 .similar to these, might also be termed triphyllous pedicellaricc, but from analogv with tin- Ech.grandi- 

 porits described below, in which species there can be no doubt that tlie.se are tridentate pedicellaria;, 

 the larger ones may also be termed tridentate in pxsillus. |I'l. XII. Kig. 23I. The blade is more elono-- 

 ated than in the triphyllous; the edge is .serrate, the .serrations on the point being the larger, often 

 con.siderably larger than in the one figured; the basal part as in the triphxllou.s. Size ca. o-o8— o-og""". 



The buccal membrane does not contain any plates or spicules; the same holds good for the 

 internal organs. The genital organs are much branched and interlaced, but apparently not anastomos- 

 ing, forming a broad ring. The axial organ shows some distinct swelling.s. The niadreporic plate has 

 on the inside a deep and large impression for the axial organ and the ampulla. 



The largest .specimen of this .species seen by me is 15""" in length. The .size 9 lines (20""") 

 given in Zoologia Danica |loc. cit.) seems hardly correct. It is ver\- variable as regards the shape of 

 the test. This has caused older authors ( L. Agassi z, Forbes) to distinguish a number of species» 

 based almost exclusively on differences in the shape of the test, \'iz. among the recent forms: E. pn- 

 sillus, angulosus and farcnfinits. besides a number of fossil species from the Tertiaries. Philippi (op. 

 cit.) has first pointed out that these differences are unreliable for specific characters, since all the dif- 

 ferent forms may be found among .specimens from the same localitx'. Philippi and all the later 

 authors after him (except Forbes) therefore regard all the recent forms from the European seas as 

 one species including also several of the fossil species . I quite agree with this, and might further 

 add as synonymous the E. liispidiihis Forb. and E. ovifoniiis Forb., both from the Crag, examples of 

 the same shape as these occurring likewise aiiu)ng the recent specimens. — Forbes further disting- 

 uishes no less than six different varieties of Ecli. pnsilliis. all of which, he agrees, may be taken in 

 one localit)' at the present day . It is evident that all these forms cannot rank as varieties , thev 

 represent merely individual variations in the shape of the test. — Perhaps the specimens from the 

 Faeroe Islands ma\ rank as a distinct variety. On comparing them with specimens from the Kattegat 

 and the Mediterranean I find that the number of pores is upon the whole a little smaller in the former 

 (comp. the tables given below, p. 34); but it is no constant feature, specimens from the Fseroe Islands 

 occurring with as large a number of pores as is generalh' found in the specimens from tlie Kattegat. The 

 shape of the test is upon the whole more elongated than in the specimens from the Kattegat; akso, the 

 primary spines are generally somewhat less serrate than those of the t\-pical form, sometimes even quite 

 smooth ones may be found. — The specimens from the Limfjord nia\' also be distingui.shed as a local 

 form, remarkable for the close tuberculation. — The Mediterranean form I am unable to distinguish as a 

 separate variety: they closel\- agree with the specimens from the Kattegat. The same holds good for 

 the specimens from the Azores. 



This species was taken b\- the Ingolf at St. 86 (Brede Bugt, Iceland, 7 dead tests). At the 

 Westmanoer, Dr. A. C. J oh an sen has taken 4 dead tests (30 fathoms); in the Zoological ]Mnseuni is 

 found further an old dead test from Reykiavik. These are, so far as I know, the only specimens of 

 Echinocyamus pusillus known from Iceland; it thus seems that the species does not live there now, 



