868 P. T. CLEVE, ON THE ORIGIN OF »GULF-STREAM WATER». 



May. From 41° N. 16° W. to the mouth of tbe English 

 Channel. From 49° N. 23° W. to 41 N. 62° W. — North of 

 South America, 6° 20' N. 55° 45' W. 



June. The space between the Azores, 42 N. 9° W., the 

 English Channel and 48° N. 35° W. — Antilles current, 19° N. 

 63° W. 



July. The Azores, at 39° N. 23° W. Along 48°— 50" N. 

 from 11° to 22° W. At 40° N. 69° W. 



August. The space between 48° N. 23° W., the English 

 Channel and 56° N. 20°— 28° W. North of Scotland, 58° N. 

 5° W. At 60° N. 3° E. 



September. The space between 46° N. 11° W., the 

 English Channel, 56° N. 27° W. and 48° N. 24° W. 



October. At 42° N. 15° W., 50° N. 20° and 10° W. At 

 38° N. 74° W. 



November. Rio Janeiro, abundant. At 34° N. 10° W.., 

 45° N. 7° W., 51° N. 20°— 1° W. At 56° N. 36° W. and 47° 

 N. 42° W. 



December. South America, 29 S. 49^ W. At 44° N. 

 57° W. 



In samples, collected by the Dutch Fregatte Atjeh in May 

 1899, west of South Africa (32°— 29° S. 13°— 9° E., in the 

 Benguela current), this copepod was also found. Paracalanus 

 parvics occurs thus along the whole African coast from the Cape of 

 Good Hope, the Gulf of Guinea, Cape Verde to the Canaries, 

 the Azores, between the Azores and the English Channel at 

 least to 56° N. — In the west it occurs in the southern hemi- 

 sphere in the Brazil current and in the northern hemisphere 

 along the north coast of South America into the Caribbean Sea, 

 but does not spread either in the Sargasso Sea or in the 

 Florida current. Its occurrence at the Newfoundland banks 

 cannot thus be explained by a drift with the Florida current. 



