-Sç.alç. poj; 



:3^ 

 %o 



û " 



m. 



33»r7ilt.lciruûl 



3v 



yUnn. 

 ■n7areK 



29 

 30 



12 - 

 II-- 



10- - 

 9__ 



I6----8- - 

 31 («t..../,- 



12 6--- 



32 10 S--- 



8 f-- 



33 6 3— - 



4..... 2-.. 

 3V -2 1--- 



0-- 



■ ■ j^uci-ctge. ■î'u'TObcr oF tool pry f»r |ia,u.L O-lOITv- 



Dçf»tf7 op lïopykr? I.Oil U.T70HT Au-TfaLCt.. 



Fig 9. 



The study of these dia- 

 grams shows us quite plain- 

 ly that the hydrographical 

 changes in both fjords have 

 been accompanied here by 

 a universal decrease in the 

 number of pelagic fish fry. 

 Evidently the upheaval of 

 salt vfater has in both 

 fjords raised the level of 

 the fry and swept masses 

 of them into the coast 

 current. 



These main features in 

 the results gained by these 

 investigations will convey a 

 strong impression, that eggs 

 and pelagic fry occurring in 

 these waters cannot be con- 

 sidered as being isolated. 

 Eggs and larvae are without 

 doubt carried in as well as 

 out of these fiords. The 

 transportation of these orga- 



.% % H ^% .eL „^ 



. ^ ^ 'K ^% 'y . pa. 



31/ It/ 3/ 

 nm /3 A /s 



2?^ 



/S P»l o m A 



'% 



'■% % 



Sandnot.*, fjord 



■ 20 



Sörjd«.Iedf jorW 



Fig. 10. Diagram showing location of isopykn ofl'021 

 on four occations in the Sandnes and S0ndeled Fjords. 

 The average number of pelagic cod fry pr. haul of 

 5 minutes is recorded in those depths which hawe 

 been examined. 



S Pel 

 i.îFlatfisli 



Sandrioft^f jord. 



Söndclftdf jord . 



Fig. 11. Diagram showing location of isopykn of \'0-i\ 

 on four occasions in the Sandnes and Sondeled Fjords. 

 The average number of pelagic flatfish fry pi', haul 

 of 5 minutes is recorded at the depths which have been 

 examined. 



