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Seasonal Cycle of Phytoplankton Community Composition in the Coastal Upwelling System Off Central Oregon in 2009

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Title Seasonal Cycle of Phytoplankton Community Composition in the Coastal Upwelling System Off Central Oregon in 2009
Names Du, Xiuning (creator)
Peterson, William T. (creator)
Date Issued 2014-03 (iso8601)
Note To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Springer and can be found at: http://link.springer.com/journal/12237.
Abstract Coastal upwelling in the northern California Current
varies seasonally, with downwelling in winter and upwelling
in summer, resulting in pronounced variability in
hydrography, nutrients, phytoplankton biomass, and species
composition. Winter was characterized by moderate concentrations
of nitrate and silicate (averages of 10 and 18 μM,
respectively) and low concentrations of chlorophyll a (Chl
a). During the upwelling season, concentrations of the same
nutrients ranged from near 0 μM to approximately 27 and
43 μM and Chl a 0.5<x<15 μg L⁻¹. During autumn, upwelling
weakened and nutrient concentrations were reduced,
but large phytoplankton blooms continued to occur. Variations
in hydrography, nutrients, and phytoplankton also occurred
within the upwelling season due to alternation of the
winds between northerly (active upwelling) and southerly
(relaxation of upwelling), on a 5- to 10-day time scale.
Eleven blooms were observed, most of which occurred near the end of active upwelling events and during relaxation of
upwelling. Nonmetric multidimensional scaling ordination
of species composition of the microplankton revealed four
distinct communities: a winter community, early upwelling
and late upwelling season communities, and an autumn
community. Diatoms (Asterionellopsis glacialis, Eucampia
zodiacus, and several Chaetoceros, Thalassiosira, and Pseudo-nitzschia species) dominated early in the upwelling season,
averaging 80% of the phytoplankton biomass, and dinoflagellates
dominated near the end of the upwelling season, averaging
68% of the phytoplankton biomass. Dinoflagellates
formed two monospecific blooms—Prorocentrum gracile in
late summer and Akashiwo sanguinea in autumn. Changes in
community composition were correlated with bottom temperature
and salinity (representing seasonal variability) and sea
surface salinity (representing within-season event-scale variability
in upwelling).
Genre Article
Topic Upwelling
Identifier Du, X., & Peterson, W. T. (2014). Seasonal Cycle of Phytoplankton Community Composition in the Coastal Upwelling System Off Central Oregon in 2009. Estuaries and Coasts, 37(2), 299-311. doi:10.1007/s12237-013-9679-z

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