20 AXEL OHLIN, ARCTIC CRUSTACEA. 



stat. 5. lat. 75° 49' N., long. 24" 25' E., between Beeren Island 



and Hope Island, depth 80 m., bottom terap. — 1,42° C, 



rocky bottom, 21 /VI, six spec. 

 > 12. Recherche Bay near to Fox Glacier, West Spitzbergen, depth 



90 m., stony bottom, 4/VII, one spec. 

 » l.S. Recherche Bay, off Fox Glacier, depth 75 m., stouy bottom 



with dead shells and soft grayish-blue clay, 5/VII, six spec. 

 j> 16. Recherche Bay, between Reindeer Point and Fox Glacier, 



depth 90 m., rocky bottom with soft gray-bluish clay, 8, VII, 



two spec. 

 » 17. Recherche Bay, the anchorage, depth O — 20 m., stony bottom, 



13 VII, three spec. 

 » 23. lat. 78° 15' N., long, 13° 55' E., Ice Fjord, Safe Harbour, 



depth 50 — 90 m., soft grayish mud, 23/VII, one spec. 

 » 38. lat. 79° 47' N., long. 14° 28' E., entrance of Liefde Bay, 



depth 140 m., stony bottom with red algse, 25 VIII, one 



spec. 

 » 39. lat. 79° 43' N., long. 10° 52' E., Danish Island, »Virgo's» 



harbour, depth 25 — 30 m., gray mud, Laminarise, 27/VIII, 



two spec. 

 » 41. lat. 75° 58' N., long. 13' 18' E., 56 miles S. W. of South 



Cape, Spitzbergen, depth 350 m., bottom terap. + 2,73° C, 



grayish clay, l/IX, one spec. 



in 1899: 



Tromsö, depth 60 — 70 m., 22/VI, many spec. Wulff. 



West Spitzbergen, Green Harbour, depth 110 m., 30 VI, three spec, 



Wulff. 

 North Spitzbergen, Danes Gat, depth 20 — 30 ra., 7/VII, one spec. 



Wulff. 



in 1900: 



stat. 1. West Spitzbergen, Ice Fjord, Coal Bay depth 50 m., stony 

 bottom with dead shells, 16/VI— 20/VI, det. Lönnberg. 

 » 8. West Spitzbergen, Kings Bay, depth 10 — 30 ra., pebbles and 

 sand with Laminarise, 29 VI, det. Lönnberg. 



This species seems to be subjected to very great varia- 

 tions as to the degree of the pubescense and to the form of 

 the left chelse which has produced an almost inextricable 

 confusion in the synonymy.^ As I have examined specimens 

 only from Spitzbergen and Tromsö, which closely agree with 

 the type as figured by Kröyer, I am of course not able 



' To this haa also, without doubt, contributed that Kröyer in his 

 descriptions has, by a lapsus calami. as to the chelae written >dextr8e> in- 

 stead of »sinistrae», as Brandt was the first to suspect. 



