4.4 Article

Bio-optical properties of the northern Red Sea and the Gulf of Eilat (Aqaba) during winter 1999

Journal

JOURNAL OF SEA RESEARCH
Volume 54, Issue 3, Pages 186-203

Publisher

ELSEVIER
DOI: 10.1016/j.seares.2005.04.006

Keywords

light; absorption; phytoplankton; flow cytometer; chlorophyll; Red Sea

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Underwater light field, chlorophyll-a concentration, phytoplankton absorption spectra, chlorophyll-a specific absorption coefficients, and phytoplankton diversity in the Gulf of Eilat (Aqaba) and northern Red Sea, were studied during a cruise on the RV 'Meteor' in winter - early spring, February-March 1999. The mean euphotic depth of the entire area was 86 +/- 8 m. The vertical attenuation coefficient, K-d (PAR), averaged from the surface down to 100 in depth, was only 0.054 +/- 0.006 m(-1), as might be expected from the low chlorophyll-a concentrations (< 0.4 mu g l(-1)). The spectral attenuation coefficients were similar in the entire area. The contribution of yellow substances to attenuation was negligible. Chlorophyll-a specific absorption coefficients for both the UV and PAR domains in the entire study area were representative of the dominant picophytoplankton. When mixing depth reached 600 in, on average each alga was exposed to 3% of surface light. Phytoplankton populations, as quantified by flow cytometry, were typical of oligotrophic oceans. In the Red Sea, the deep chlorophyll maximum developed at about 50-60 m, similar to 1 x 10(8) cells l(-1), dominated by high concentrations of Prochlorococcus (similar to 75%), whereas in the Gulf of Eilat (Aqaba), similar to 4 X 10(7) cells l(-1), eukaryotic algae (similar to 20%), cyanobacteria (Synechococcus) (similar to 50%), and Prochlorococcus (similar to 25%), were distributed throughout the water column. The cell size and pigment concentrations did not depend on depth distribution or geographic location. The northern Red Sea is permanently stratified, while at that time of year, the Gulf waters were deeply mixed. The results illustrate the common features of these two domains, while underscoring their differences. Even though they share the typical phytoplankton attributes of oligotrophic ocean provinces, mixing regimes still set them apart. (c) 2005 Elsevier B.V. All rights reserved.

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