2009
DOI: 10.1007/s00027-009-9165-7
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Phosphorus sources and demand during summer in a eutrophic lake

Abstract: In pelagic systems, phytoplankton biomass may remain abundant or near equilibrium while concentrations of the limiting nutrient are below detection. In eutrophic lakes, it has been thought that episodic algal blooms are due to mixing events that break down this equilibrium by adding nutrients to the mixed layer. Alternatively, rapid rates of biotic recycling among primary producers and heterotrophic consumers could maintain high phytoplankton biomass, yet the recycling process has been difficult to observe in … Show more

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Cited by 31 publications
(42 citation statements)
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“…(e.g., Cole et al 2000;Hanson et al 2003;Staehr et al 2010), we can achieve a wealth of strong empirical data to quantify in situ undisturbed processes and test the relations of GPP, NEP, and R to irradiance, temperature, nutrient availability, and food web structure. A most creative use of metabolism estimates has been estimation of nutrient recycling in the epilimnion of Lake Mendota (Kamarainen et al 2009). …”
Section: Future Researchmentioning
confidence: 99%
“…(e.g., Cole et al 2000;Hanson et al 2003;Staehr et al 2010), we can achieve a wealth of strong empirical data to quantify in situ undisturbed processes and test the relations of GPP, NEP, and R to irradiance, temperature, nutrient availability, and food web structure. A most creative use of metabolism estimates has been estimation of nutrient recycling in the epilimnion of Lake Mendota (Kamarainen et al 2009). …”
Section: Future Researchmentioning
confidence: 99%
“…The interrelationships between Chl-a and N and P have been explored during the past few decades (e.g. Brown et al, 2000;Kamarainen et al, 2009). These relationships suggest the potential use of Chl-a to estimate N and P concentrations.…”
Section: Introductionmentioning
confidence: 99%
“…Through sedimentation, spring diatom blooms can remove a significant fraction of phosphorus (P) from a lake early in the season (Kufel 2001). This removal subsequently limits the amount of P available for recycling in the photic zone, the principle source of P to primary pro-ducers during the stratified period (Kamarainen et al 2009). Reynolds (1998) referred to the removal of P from the water column through sedimentation of the spring diatom bloom as a nutrient-sponge which influences the community composition of phytoplankton during the stratified period.…”
Section: Introductionmentioning
confidence: 99%