Bio-optical properties of the subtropical North Atlantic. I. Vertical variability

Studies of the physiological and optical properties of phytoplankton of the subtropical open ocean are rare. Yet, assessing the spatial and temporal v ariation in the photo-physiological parameters and chlorophyll-specific abs orption coefficients of marine phytoplankton is essential if we are to acco unt for the relative importance of pelagic systems in the global carbon eco nomy. As a contribution to this general goal, the photosynthetic and bio-op tical properties of phytoplankton were measured at 5 stations across a broa d swath of the subtropical North Atlantic Ocean. Similar vertical patterns in pigment composition, chlorophyll-specific absorption coefficients and th e photosynthesis-irradiance parameters were observed at all 5 stations. A c onsiderable proportion of the vertical variation in the chlorophyll-specifi c absorption coefficients was caused by vertical changes in the proportion of the non-photosynthetic pigment (NPP) zeaxanthin relative to chlorophyll a. On the other hand, pigment packaging appeared to have a minor influence on the optical characteristics of the picoplankton-dominated region: chloro phyll-specific absorption coefficients observed at the red peak frequently exceeded 0,92 m(2) (mg chi a)(-1). Multiple, linear-regression analysis was used to examine the value of some commonly-measured environmental variable s as potential predictors of the photosynthetic parameters alpha(B) and P-m (B). The results showed that indices of ambient irradiance, nutrient flux o r nutrient concentration, separately or in combination, account for a signi ficant fraction of the total variance in the photosynthetic parameters. The stability in the distribution patterns of both the photosynthetic paramete rs and absorptive characteristics of subtropical phytoplankton assemblages and in the principal factors governing the variability in these properties may facilitate the selection of appropriate input parameters for use in mod els of primary production for this hydrographic region.