2001
DOI: 10.4319/lo.2001.46.8.1998
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Algal games: The vertical distribution of phytoplankton in poorly mixed water columns

Abstract: Phytoplankton often face the dilemma of living in contrasting gradients of two essential resources: light that is supplied from above and nutrients that are often supplied from below. In poorly mixed water columns, algae can be heterogeneously distributed, with thin layers of biomass found on the surface, at depth, or on the sediment surface. Here, we show that these patterns can result from intraspecific competition for light and nutrients. First, we present numerical solutions of a reaction-diffusion-taxis m… Show more

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Cited by 266 publications
(358 citation statements)
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“…In stratified lakes with low external nutrient sources, CYAN growth occurs in the deep part of the lakes where P is more abundant, given sufficient light availability. This hypothesis is supported both by existing empirical data on deep phytoplankton maxima, and by models of maximum algal growth in relation to vertical light and nutrient availability (Fee, 1976;Klausmeier and Litchman, 2001).…”
Section: Introductionsupporting
confidence: 55%
“…In stratified lakes with low external nutrient sources, CYAN growth occurs in the deep part of the lakes where P is more abundant, given sufficient light availability. This hypothesis is supported both by existing empirical data on deep phytoplankton maxima, and by models of maximum algal growth in relation to vertical light and nutrient availability (Fee, 1976;Klausmeier and Litchman, 2001).…”
Section: Introductionsupporting
confidence: 55%
“…At the two shallowest stations, maximum Chl a fluorescence was found at the height measured closest to the lake bottom. These patterns are predicted to occur as a consequence of high water clarity combined with a supply of nutrients from the lake bottom (Klausmeier and Litchman 2001). At some time following offshore stratification, the DCM receded in the shallowest depths.…”
Section: Methodsmentioning
confidence: 99%
“…Dense subsurface aggregations of viable phytoplankton are predicted to arise in waters with a pycnocline, a gradient of nutrient concentration supplied from depth, and sufficient water-column transparency to support photosynthesis at depth (Klausmeier and Litchman 2001;Hickman et al 2009). These dense aggregations of phytoplankton can be manifest as deep chlorophyll maxima (DCMs), a phenomenon that is observed widely, reported from all the world's oceans (Cullen 1982;Huisman et al 2006), from coastal shelves (Hickman et al 2009), as well as from transparent stratified lakes of a wide range of sizes and geographic distribution (Camacho et al 2003;Burnett et al 2006;Pannard et al 2011).…”
mentioning
confidence: 99%
“…This can be described by the following set of partial differential equations (Klausmeier and Litchman 2001;Huisman et al 2004):…”
Section: Theorymentioning
confidence: 99%