278 BULLETIN: MUSEUM OF COMPARATIVE ZOOLOGY. 
all other Salpae put together. And the few chains of S. confoederata 
which were seen, or collected, it was nowhere abundant, were re- 
stricted to Gulf Stream Stations (10071, 10076) and to the outer part 
of the shelf (10070, 10073, 10074). Salpa tilesii, on the contrary, was 
not taken at all at Stations 10064 and 10071, but was found in adulter- 
ated Gulf Stream water at Station 10076, and was more or less com- 
mon along the edge of the continental shelf (Stations 10061, 10070, 
10077); and in the eastern part of the Gulf of Maine (Station 10096). 
Salpae as a whole were far less numerous along the inner edge of the 
Gulf Stream in July, 1913, than they were in July, 1908 (1909, p. 198), 
when they were more abundant on the surface south of Nantucket 
than I have ever seen them. 
THE HYPERIID AMPHIPODS. 
Hyperiid amphipods often form a large part of the macroplankton — 
in boreal waters and are of considerable importance as food for pelagic — 
fishes. The species so far captured in the GRAMPUs hauls, all of which 
are easily recognizable, are Hyperia medusarum, Hyperia galba, Hype- 
‘roche kréyeri, Parathemisto oblivia, Euthemisto compressa, Euthemisto 
bispinosa, Phronima atlantica, Phronima sedentaria, Tyro atlantica, 
and Vibilia jeangerardi. ‘Their occurrence, in the summer of 1913, 
is shown in the following table (p. 279). 
(The identifications follow Bovallius, 1887-1889, and Sars, 1895. 
For previous records off the New England coast, see Holmes, 1905, 
and Rathbun, 1905). 
The most widely distributed hyperiids in the coast re as well as 
the most abundant numerically, were the two species of Euthemisto, 
compressa and bispinosa (Fig. 68). This genus as a whole (the rela- 
tionship of the two species to each other will be considered later) was 
generally distributed over the Gulf of Maine (Stations 10058, 10087 
to 10105); it was present on George’s Bank (Station 10059), in the 
waters over Nantucket Shoals (Station 10060), over the outer part of 
the continental shelf, south of Block Island and Long Island (Stations 
10062, 10063, 10065, 10066); and in the mixed water at the inner edge | 
of the Gulf Stream (Stations 10061, 10064, and 10076). But we did 
not find it in Gulf Stream water proper (Station 10071, 10073), in 
any of the tows in the comparatively fresh water off Chesapeake Bay 
(Stations 10077 and 10078), or at any of the stations near shore be- 
tween New York and the Chesapeake (Stations 10067, 10068, 10079- 
10083), except in one instance (Station 10075). 
