are slightly higher and don't show the varia- 

 bility that the other cold bottom water exhibits 

 in the southeastern section of the gulf. This 



may be due to the long residence time of the 

 cold bottom water in Holy Cross Bay before it 

 enters the Gulf of Anadyr. 



REFERENCES 



Arsen'yev, V. S. (1967). The currents and water 

 masses of the Bering Sea, Izdatd'stvo "Nanka", 

 Moscow, English Transl., 135 pp. 



Green, E. J. and D. E. Carritt (1967). New tables for 



oxygen saturation of sea water, Joh7: Mar. Res.. 



25(2), 140-147. 

 Mokievskaya, V. (1956). Some data on the chemistry 



of the biogen elements in the Bering Sea, Tr. WAN . 



in Russian, 17. 

 Ratmanov, G. E. (1937). Kgedrologiy Beringova i 



Chukotskovo morei, Gosudarstv. Gidroloy, inst. Isslcd. 



mor. SSSR. No. 25, 10-174. 

 Saur, J. F. T., J. P. Tully, and E. C. LaFond (1954). 



Oceanographic cruise to the Bering and Chukchi 



Seas, Summer 194".). Part IV : Physical oceanographic 



studies. Vol. 1. Descriptive Report USX Electron. 



Lab. Res. Repi.. 416, 31 pp. 

 UNESCO (1966). International oceanographic tables, 



UNESCO Office of Oceanography, Paris, 118 pp. 

 Zenkevitch, L. (1963). Biology of the seas of the 



USSR. Intei'science, New York, 955 pp. 



