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Sharp gradients in physicochemical properties and currents at ocean fronts are known to alter the composition and structure of plankton communities, often resulting in zones of enhanced primary production and biomass (Boucher , 1993) and Venrick (Venrick, 2000) concluded that the front did not represent a biologically distinguishable feature in terms of chlorophyll, production or phytoplankton composition.
In contrast, Hood , 1991) found evidence of higher chlorophyll and larger phytoplankton in the vicinity of a front off northern California.
Community compositions are compared based on analyses by digital epifluorescence microscopy, flow cytometry and pigment composition by high-pressure liquid chromatography.
Our results show three assemblages sharply delineated in space, with plankton at the front being compositionally distinct and biomass elevated relative to either of the adjacent water masses.
The Niskin bottles were sampled for analyses of total chlorophyll ), phytoplankton accessory pigments by high performance liquid chromatography (HPLC), prokaryotic abundance and biomass by FCM and protistan community abundance and biomass by digital epifluorescence microscopy.
In the present study, we investigate the spatial patterns of phytoplankton and heterotrophic protists across a strong frontal feature that was sampled as part of the California Current Ecosystem (CCE), Long-Term Ecological Research (CCE-LTER) program in October 2008.
SST is merged from MODIS Aqua and Terra satellites from the period of 22–25 October 2008. Concentrations of lipophilic pigments, chlorophylls and carotenoids, were determined using HPLC.