BEAM ATTENUATION BY MICROORGANISMS AND DETRITAL PARTICLES IN THE EQUATORIAL PACIFIC

The transmissometer has been actively used to monitor the variability of particulate matter in the surface ocean. Attenuation due to water ( c(w)) is constant at a given wavelength, so variability in the signal is due primarily to particles (beam c(p)) Most of the beam c signal ap pears to originate from particles < 20 mu m, which, in the euphotic zo ne, are most likely to be microorganisms. However, how much of the bea m c(p) (lambda = 660 nm) is attributable to any given organism categor y or the detrital component is poorly known. To answer this question, at least numerical abundances and optical (scattering) cross sections of each category are needed. During the two transect cruises (TT007 an d TT011) of the Joint Global Ocean Flux Study (JGOFS) Equatorial Pacif ic (EqPac) program (12 degrees N - 12 degrees S, 140 degrees W), parti culate matter attenuation (beam c(p)) and abundances of four microorga nism categories (heterotrophic bacteria, Prochlorococcus, Synechococcu s, and small autotrophic eukaryotes) with their forward angle light sc attering (FALS) information (flow cytometer) were simultaneously measu red from the same water samples. The bulk scattering coefficients of e ach population and total scattering coefficients (b(p)) of these four picoplankton populations (b(p)(PICO)) were calculated and compared wit h beam c(p). In the equatorial Pacific, heterotrophic bacteria and Pro chlorococcus were the most significant contributors to the beam c(p) ( 16 and 7% of beam c(p), respectively) via scattering, and autotrophic eukaryotes and Synechococcus were less important contributors (2 and 1 %, respectively) in the equatorial Pacific. If absorption was also inc luded, similar to 30% of the beam c(p) could be accounted for by these four populations in the euphotic zone, supporting the argument that a transmissometer at 660 nm is an effective tool in measuring the net b iological processes in the open ocean. A rough estimate for the beam c (p) signal from nonliving detrital particles was also made in surface waters of the region.