4+ 



The references are taken from the last two authorities. Pro- 

 fessor G. O. Sars describes three specimens from south of the 

 Cape. One of these was a mjale, 25 mm- (an inch) long-, with 

 only three teeth on the outer margin of the antennal scale- The 

 specimen now noted measured at least an inch, and has four teeth 

 on the outer margin of the scale- The distal part of the telson 

 was unfortunately broken ofif. The bipinnate branchiae add much 

 to the beauty of this species as the series is visible at each side of 

 the translucent carapace, and two rows at right angles to the 

 others meet along the centre of the ventral surface- Sars has 

 called attention to the curious circumstance that this schizopod, 

 first known from Norway and the Shetland Isles and then from 

 the neighbourhood of the Cape, so far ren-^ains unknown from 

 intermediate waters. 



Locality :— Cape St. Blaize, N.E- by N. ^ N- 11^ miles- Depth, 

 40 fathoms. Bottom, sand and rock- 



S rOMATOPODA. 



1852- SquiUoidea, Dana, U-S. Expl. Exp., vol. 13, Crustacea, p- 



614. 

 1876. '■'• Stoiiiatofodcii^' Claus, Unters. geneal. Crustaceen- 



S}-stems, p. "j^i, etc- 

 1883. Sqitilhcca, Boas, Morphologisches Jahrbuch- vol. 8, p. 574. 



1885. Stonmpoda, Cams, Prodromus Faunae Mediterraneae, vol- 



I, p. 464. 



1886. Stoiuatopoda, Brooks, Challenger Stomatopoda, Reports, 



vol. 16- 



1893. Stomatopoda, Stebbing, History of Crustacea, p. 279- 



1894. Stomapoda, Alcock, Ann- Nat. Hist., sen 6, vol. 13, p- 409. 



1894. Stomatopoda, Bigelow, Proc- U.S. Mus., vol- 17, p. 490. 



1895. Stomatopoda, Hansen. Isop- Cumac. und Stomatopoden 



Plankton-Exp., p- 64. 



The name Stomapoda of Latreille is far older than the term 

 Stomatopoda, but the latter has the advantage of keeping in mind 

 Latreille's authorship, without perpetuating the confusion 

 involved in the group as he understood it- 



Fam. : Squillid.ve- 



As this is the only family at present assigned to the order, the 

 above references will be a sufficient guide to the sources of in- 

 formation, whicli are numerous. 



