DISCOVERY REPORTS 



Table 63. Average gatherings in the East Wind drift. {Samples from surface 

 and oblique i-m. nets. Corrected figures) 



Table 64. Average gatherings at South Georgia and in the Bransfield Strait. {Samples from surface 



and oblique i-m. nets. Corrected figures) 



might be responsible for the slight measure of larval abundance we have recorded there. They are 

 (i) the influence of surface-borne incursions from the Bellingshausen Sea (p. 360), (2) the influence 

 of the Antarctic bottom v^^ater (pp. 305-6), and (3) simply because this is a region in which, hydro- 

 logical boundaries being what they are, it is often rather difficult to separate true West Wind 

 occurrences from Weddell ones. 



REFERENCES 



Aagaard, B., 1930. Fangst og Forskning i Sydishavet (Oslo). 



Ahlstrom, E. H., 1943. Studies on the Pacific pilchard or sardine (Sardinops caerulea). 4. Influence of temperature on the rate of 



development of pilchard eggs in nature. Spec. Sci. Rep. U.S. Fish Wildl. Serv. no. 23, pp. 1-26. 

 Allen, G. M., 1916. The whalebone lohales of New England. Mem. Boston See. Nat. Hist, viii, no. 2, pp. 107-322. 

 1942. Extinct and Vanishing Mammals of the Western Hemisphere. American Committee for International Wild Life 



Protection, Special Publication no. 1 1 (Lancaster, Pa.). 

 Allen, J. A., 1899. Fur-seal hunting in the Southern Hemisphere. Paper no. 12 in D. S. Jordan's The Fur Seals and Fur-Seal 



Islands of the North Pacific Ocean, pt. 3 (Washington). 



