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Chlorophyll a also showed similar seasonal trends with respect to location (Figures 18,19). However, measured monthly means of bioluminescence did not correlate with Chl a either at SDB or SCI. Mean monthly surface seawater temperature did not correlate with mean monthly bioluminescence at either site; that is, maximum bioluminescence did not always correlate with either maximum or minimum seawater temperatures (Figures 11, 12), although minimum bioluminescence was measured during the coolest water temperatures (winter) at SDB in 1994 and 1996.
Listing is by mean light output. Seasonal Changes of Bioluminescence in Photosynthetic and Heterotrophic Dinoflagellates at San Clemente Island Species Spr’94 Sum’94 P. de. 1e9; 9 cells P. di. 6e9; 11 cells P. cur. 9e8; 3 cells P. 8e9; 3 cells P. stei. 9e9; 3 cells Table 3. Light output for other Protoperidinium spp. (mean photons cell-1) 1994 – 1996. Species Spr’94 Sum’94 Fall’94 Win’95 Spr’95 Sum’95 Fall’95 Win’96 Spr’96 G. poly. 3e8; 12 cells 15 cells G. spin. 4e8; cells 12 cells G. grind. 8e8; 2 cells cells G.
1993). Assessment of marine bioluminescence. Nav. Res. Rev. 45: 31-41. G. (1965). Measurements of diurnal changes in bioluminescence from the sea surface to 2,000 meters using a new photometric device. Limnol. Oceanogr. 10 (supplement), R54-66. C. (1967). Nutrient limitation in the sea: dynamics, identification and significance. Limnol. Oceanogr. 12: 685-695. H. (1978). Gradients in phytoplankton stocks and nutrients off southern California in 1974-76, Estuarine Coastal Mar. Sci. 7: 291-301. W.