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Fig. 1. (A) Spectral irradiance (E ) of downwelling daylight for the Gulf of California at 19m depth (solid line) (after Tyler and Smith, 1970) and for the English Channel at 20m depth (filled circles) (after Atkins, 1945). Spectral absorption (S ) of the squid rhodopsin (broken line) for a maximum optical density of 0.5 (calculated after Knowles and Dartnall, 1977) with the wavelength for maximum absorption ( max) at 499nm (Morris et al., 1993). Maximum values have been made equal to 100. (B) Angular distribution of daylight in the sea: grey solid line, after an equation and constants suggested to one of us by Dr J. E. Tyler for oceanic waters off the Azores (see Denton et al., 1972); short dashed line, for Lake Pend Oreille (Tyler, 1960); long dashed line, for turbid water at a depth of 40m off Japan (Sasaki et al., 1962, cited in Jerlov, 1976); black solid line, for Mediterranean waters (Lundgren, 1976, cited in Jerlov, 1976). Radiances for 0° (vertically downwards) have been made equal to 100.
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