Phytoplankton variability in the central and eastern tropical Pacific

• Published in: Deep-sea research. Part II, Topical studies in oceanography Vol. 43; no. 4; pp. 835 - 870
• Main Authors: Chavez, Francisco P., Buck, Kurt R., Service, Susan K., Newton, Jan, Barber, Richard T.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 1996
• Subjects: Marine; Synechococcus; ISE, Equatorial Pacific; Tropical Pacific
• ISSN: 0967-0645; 1879-0100
• DOI: 10.1016/0967-0645(96)00028-8

An extensive set of measurements of phytoplankton production, biomass and composition, and microzooplankton grazing from the coast of Peru to 170°W during 1992, together with similar data collected over the previous decade, has allowed recalculation of the primary production supported by equatorial upwelling and improved description of the variability in phytoplankton properties. Equatorial region surface chlorophyll and phytoplankton biomass were low, averaging 0.2 μg 1 −1 and 20 μg C 1 −1, respectively, and showed low variance. Phytoplankton in the open ocean of the tropical Pacific were dominated by small < 5 μm) solitary organisms, primarily prochlorophytes, Synechococcus, eukaryotic picoplankton, haptophytes and dinoflagellates, while coastal populations were dominated by larger organisms or colonies (primarily diatoms). At a few open ocean locations high numbers of diatoms were found. The chlorophyll maximum observed in the equatorial Pacific was a function of increased chlorophyll per cell rather than an increase in cell numbers. Surface phytoplankton carbon to chlorophyll was highly variable and a function of available irradiance and upwelling strength. On the order of 40% of the particulate nitrogen retained by GF/F filters was estimated to be phytoplankton nitrogen. Phytoplankton growth rate estimates using daily carbon uptake and phytoplankton carbon estimated from microscopic enumeration ranged from 0.55 to 0.70 day −1. Estimates of growth rates from dilution experiments gave estimates of the order of 1 day −1 and microzooplankton grazing rates that were significantly lower, 0.4 day −1. The mean mass specific grazing rate for microzooplankton was estimated to range from 1.6 to 1.8 day −1. The mean productivity for the equatorial Pacific from 90° to 180°W, 5°N−5°S, was estimated to be 900 mg C m −2 day −1 for the period from 1990 to the present, twice that estimated previously. The maximum f-ratio (new to total production) was estimated to be 0.36. Assuming that between 25 and 50% of the upwelled nitrate is never taken up by phytoplankton between 5°N and 5°S, new production would be 162–244 mg C m −2 day −1 and f would range from 0.18 to 0.27.