213 
5 were found on the right, 3 on the left side and 2 in the (ven- 
tral) middle line (comp. p. 5). 
The localities for the additional specimens are the following: 
1. The association of the Parasitic Copepod with the Hydroid. 
«Tialfe's” Depth of Denth of 
Setion Nr. Lat. N. Long. W. ze Station se re Date 
n Metres n Metre 
336 64906" 559 18' mare 900 8I5. 09. 
2. The Parasitic Copepod, without the Hydroid. 
6 ”g” D epth of Depth of 
Er mme Nr Lat. N. Long. W. an Station — the Capture Date 
sk n Met: in 
171 10? AP 52907 735 600 6]. 08. 
346 (2 spec.) 64? 22' 56890" 300—600 15. 09. 
sn ) 64922" — 559 48" 1040 750—850 — 79/5, 09. 
336 649 06' 55918" 1040—1100 900 815. 09. 
30 a. 68709 569232 375 716. 08. 
434 (2 spec.) 629 53' 549 15' 1660 900—1125 9%. 09. 
Sukkertoppen 658 25: 582 4t 1889. 
3. Stages in Development of the Parasitic Copepod. 
ÅA. Cyclops-stage. 
Depth of Depth of 
"Tjalfe's” : 
Se ore Nr JAR N, Long. W. ne vers the Xerv Date 
386 (2spec,)  64906' 55918"  1140—1100 900 8/5. 09. 
C. 2nd pupal stage 
434 629 58" 549 15' 1660 900—1125 Sie. 09; 
Thus, the northern range of the Sarcotretes has been widened 
from 65? Lat. N. to 70941' L.N., the western extension from 
48? 26' Long. W. to 56? 32" Long. W. (cfr. l.c. p. 3); that is to 
say: this Parasitic Copepod not only occurs east and south of 
Greenland but also west of Greenland through the whole of Davis 
Strait right up to the entrance of the Umanak Fjord, now the 
