UPWELLINQ AND THE PRODUCTION OF FISH
290
FIQ. 13. Distribution of radiocarbon measurements in the Pacific Ocean in gC/ma per
day (Koblentz-Mishke, 1965). ( I ) 100; (2) 100-150; (3) 150-250; (4) 250-650;
(5) 650 mgC/m*.
International Indian Ocean Expedition), Kabanova (1 968), Holmes
et al. (1957), Forsbergh and Joseph (1964), Corcoran and Mahnken
(1969) and Lloyd (1970). The summaries of Pacific Ocean data in
Koblentz-Mishke (1965) for the Pacific, in Blackburn (1966) for the
eastern tropical Pacific and in Angot (1961) for the western Pacific
have been used extensively as have those of Wooster et al. (1967) for
the Arabian Sea and Kabanova (1968) for the Indian Ocean. Doty
(quoted in Angot, 1961) made many measurements in the Indonesian
region, which are considerably higher than those made by Nielsen and
290
FIQ. 13. Distribution of radiocarbon measurements in the Pacific Ocean in gC/ma per
day (Koblentz-Mishke, 1965). ( I ) 100; (2) 100-150; (3) 150-250; (4) 250-650;
(5) 650 mgC/m*.
International Indian Ocean Expedition), Kabanova (1 968), Holmes
et al. (1957), Forsbergh and Joseph (1964), Corcoran and Mahnken
(1969) and Lloyd (1970). The summaries of Pacific Ocean data in
Koblentz-Mishke (1965) for the Pacific, in Blackburn (1966) for the
eastern tropical Pacific and in Angot (1961) for the western Pacific
have been used extensively as have those of Wooster et al. (1967) for
the Arabian Sea and Kabanova (1968) for the Indian Ocean. Doty
(quoted in Angot, 1961) made many measurements in the Indonesian
region, which are considerably higher than those made by Nielsen and