Figure 4b shows the spectra of the chlorophyll-specific coefficient aph*(chla)(λ) for all the samples recorded as well as the average value, and the average

± SD. The variability in average aph*(chla) across all wavelengths lies within the CV range from about 29% to 94% (see also row 6 of Table 2). The smallest values of CV (29%) is reached at 675 nm, i.e. in the vicinity of the ‘red’ peak of absorption by phytoplankton pigments (the respective average value of aph*(chla) (675) is 0.0228 m2 mg−1). Throughout the range of light wavelengths between 440 and 600 nm, CV values also remain relatively small (not exceeding 40%). The presented average aph*(chla) spectra can be compared with the average spectra reported for oceanic waters by Bricaud et al. (1998) (see the dotted lines in Figure 4b representing different aph*(chla) spectra calculated Doxorubicin for four different values of Chl a   – 0.3, 1, 3 and 10 mg m−3). Our average

aph  *(chl a) spectrum is similar in shape to the two given by Bricaud et al. (1998) for Chl a   values of 3 and 10 mg m−3, but regardless of this similarity, the absolute values of our average spectrum are distinctively higher (we recall that in our study, the values of Chl a   changed over a range from less than 0.4 to more than 70 mg m−3 with an average value of about 7.6 mg m−3). Examples of best-fit power functions between aph  (440) find more and Chl a  , and aph  (675) and Chl a  , found for our Baltic data are given in Table 3. The relationship between aph  (675) and Chl a   is also plotted in Figure 5d. Compared with the similar power function fit of

aph   vs. Chl a   for oceanic waters reported by Bricaud et al. (1998) (see the dotted line in Figure 5d representing the equation for the adjacent wavelength of 674 nm: aph  (674) = 0.0182(Chl a  )0.813), the power function fit obtained in the present work shows a similar value of the power, but the value of the constant C  1 is about 50% higher. This again suggests that on average the efficiency of light Montelukast Sodium absorption (this time absorption by phytoplankton pigments alone) per unit of chlorophyll a   in our southern Baltic Sea samples is higher when compared with average oceanic results. As we said earlier, since we cannot directly compare PSDs for our Baltic samples with the size distributions for oceanic samples reported by Bricaud et al. (1998), we can only speculate about the reasons for such differences in the chlorophyll-specific absorption coefficient. Interestingly, Babin et al. (2003b) reported a qualitatively similar feature – distinctively higher aph*(chla) values for at least for some parts of the visible light spectrum for their Baltic Sea samples compared with averaged oceanic results (see the spectrum and spread of data points representing Baltic samples in their original Figures 6c and 7). Unfortunately, apart from these figures, Babin et al.