Phytoplankton depth profiles and their transitions near the critical sinking velocity.
We consider a simple phytoplankton model introduced by Shigesada and Okubo which incorporates the sinking and self-shading effect of the phytoplankton. The amount of light the phytoplankton receives is assumed to be controlled by the density of the phytoplankton population above the given depth. We show the existence of non-homogeneous solutions for any water depth and study their profiles and stability. Depending on the sinking rate of the phytoplankton, light intensity and water depth, the plankton can concentrate either near the surface, at the bottom of the water column, or both, resulting in a "double-peak" profile. As the buoyancy passes a certain critical threshold, a sudden change in the phytoplankton profile occurs. We quantify this transition using asymptotic techniques. In all cases we show that the profile is locally stable. This generalizes the results of Shigesada and Okubo where infinite depth was considered.
Kolokolnikov
Theodore
T
Department of Mathematics and Statistics, Dalhousie University, Halifax, NS, Canada B3H 3J5. tkolokol@mathstat.dal.ca
Ou
Chunhua
C
Yuan
Yuan
Y
D000465:Algorithms; D004058:Diffusion; D017753:Ecosystem; D008027:Light; D008954:Models, Biological; D017711:Nonlinear Dynamics; D010839:Phytoplankton / Q000302:isolation & purification / Q000502:physiology*; D011156:Population Density; D011157:Population Dynamics
Nature. 2006 Jan 19;439(7074):322-5
16421570
Oecologia. 1974 Dec;17(4):281-291
28308943
J Theor Biol. 2002 Jun 21;216(4):397-408
12151257
Bull Math Biol. 2001 Nov;63(6):1095-124
11732178
Am Nat. 2002 Mar;159(3):245-54
18707377