Marine Ecology Progress Series · 1999 · 44 citations · 11 references
Life SciencesEcologyMarine SciencesEstuarine BiologyMarine EcologyPlankton EcologyEstuariesNutrient DynamicsNutrient LimitationPhytoplankton EcologyBioassay DevelopmentNutrient Uptake By PhytoplanktonOceanic Nutrient LimitationPhytoplankton BiomassPhytoplankton Growth DynamicsPhytoplankton Growth RatesPhytoplankton Nutrient LimitationPhytoplankton Nutrient Uptake
Seasonal vanation in nutnent (nitrogen: N, and phosphorus: P) limitation of phytoplankton biomass growth was studied in the eutrophic estuary, H j a r b ~k Fjord, Denmark. by use of 4 different types of bioassays. These were ( I ) long-term (2 d) nutrient addition bioassay, (2) long-term dilution bioassay, (3) short-term (2 h) nutrient addition bioassay, and (4) short-term dilution bioassay. Types 1 and 2 were conducted as field incubations where increases in chlorophyll a (chl a) were used as a growth indicator, while Types 3 and 4 were laboratory incubations with measurement of I4Cuptake rates. Bioassays were compared with seasonal variations in carotenoid:chl a pigment ratio (480:665 nm), nutrient pools (C:N:P ratios) in seston, concentrations of dissolved nutrients (N and P) in the water, and with the supply of nutnents (N and P) to the photic zone. P-limited growth dominated from May to August according to most bioassays, whereas N limitation was only significant in the longterm nutnent addition bioassay in August. Estimates of nutrient loading to the photic zone included external input from freshwater and manne sources and nutrients regenerated from the sediment. The molar nutnent loading ratio (N:P) decreased through the sumrner from values of 290 and 110 for inorganic and total N:P, respectively, in April to a minimum value of 21 and 24 for inorganic and total N:P, respectively, in August. The minirnum value coincided with the lowest inorganic N:P ratio in the surface water ( 3 5) and with a low ratio (15) of particulate N:P in the water column. Both short-and longterm nutnent addition bioassays corresponded well with the type of nutnent lirnitation that could be predicted from the seasonality in the N:P loading ratio and the inorganic N:P ratio in the surface water. The dilution bioassays gave less clear results, but may still provide information on possible nutrient lirnitation in a situation where the external loadings of both N and P are decreased. The carotenoid:chl a ratio vaned between 1.4 and 2.6 with the lowest values in April and October, where nutnent limitation was less evident, and with the highest value in August. The 480:665 ratio always decreased dunng long-term bioassays when nutnent addition stimulated growth, which implies that it may be indicative of P-as weii as N-limited growth.
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The Ecology of Freshwater Phytoplankton.
Roger I. Jones, C. S. Reynolds · Journal of Ecology · 1985 · 2.9K citations
Silicate as regulating nutrient in phytoplankton competition
JK Egge, DL Aksnes · Marine Ecology Progress Series · 1992 · 775 citations · Full text
Perspectives in Ecological Theory
Ramón Margalef · Oikos · 1969 · 530 citations
Life Sciences, Biology, Ecology +11