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Nonlinear dynamics of a marine phytoplanktonzooplankton system
Advances in Difference Equations volumeÂ 2016, ArticleÂ number:Â 212 (2016)
Abstract
In the paper, the nonlinear dynamics of a marine phytoplanktonzooplankton system is discussed in detail. The aim is to deeply expound how to use the dynamical laws of marine ecological system to perfectly reflect the operating rules of marine ecosystems. The mathematical work has been pursuing the investigation of some conditions for the local and global stability of the equilibrium, as well as Turing instability, which can deduce a key parameter control relationship and in turn can provide a theoretical basis for the numerical simulation. The simulation work indicates that the theoretical results are correct, and the nonlinear dynamics of the marine system mainly depend on some critical parameters. The results further suggested that the diffusion and the environmental carrying capacity have an important role to play in the interaction between phytoplankton and zooplankton. All these results are expected to be of use in the study of the internal operating rules and characteristics of marine ecosystems.
1 Introduction
It is well known that plankton systems are abundant in marine ecosystems, where they comprise phytoplankton and zooplankton. Phytoplankton are primary producers in the marine ecosystem, where they form the basis of the food chain. Phytoplankton systems also play very important roles in chemical cycles and energy conversion marine ecosystems. Zooplankton can control the amount of phytoplankton via their consumption, where the zooplankton systems then provide a resource that is utilized by consumers at higher trophic levels. Thus, plankton research is highly significant for fishery production and basic theoretical marine science, further the importance of plankton for ecosystems is gradually recognized by contemporary researchers [1].
In marine ecosystems, animal populations often migrate to other habitats to search for food, widen their gene pool, or extend their territory. Factors such as latitude, salinity, ocean currents, and light can also affect their distribution. Thus, the dynamic behaviors present in the trophic interactions of aquatic ecosystems are highly complex. However, it is difficult to describe the dynamics of plankton ecosystems. In recent years, major progress has been made in the mathematical modeling of ecosystems and many studies have described the different dynamical behaviors of marine ecosystems [2â€“5]. In general, these systems are all predatorprey systems. Some previous studies have provided detailed analyses of these predatorprey systems [6â€“10]. There have been numerous investigations of the dynamics of phytoplanktonzooplankton models [11â€“13]. For example, Steele [13] considered the interactions among phytoplankton and herbivore. References [12, 14â€“16] incorporated nutrients into the interactions among plankton. The toxic substances produced by phytoplankton have a major impact on phytoplanktonzooplankton interactions, there have been several analyses of toxicphytoplankton systems [17â€“21]. In [22], a mathematical system was proposed to describe the interaction between nontoxic and toxic phytoplankton in the presence of a single nutrient. In many ways research into plankton is still highly active.
Mathematical systems and methods are often used to study ecological problems [6, 7, 23, 24]. However, some of the mathematical systems used to describe ecological phenomena cannot be applied to planktonic systems. Thus, we need to select specific functions and functional responses to build a model of a planktonic system. In 1952, Turing [25] proposed the reactiondiffusion equation and described the concept of Turing instability. The importance of pattern formation was studied subsequently by Segal and Jackson [26]. Reactiondiffusion processes are now very important for describing the dynamic behavior of phytoplanktonzooplankton systems. In 1965, Holling [27] proposed three types of biological functional responses, called Holling types I, II, and III. In [28], analysis was provided of reactiondiffusion toxinphytoplanktonzooplankton systems with either Hollingtype II or Hollingtype III functional responses. In [29], an analysis was presented of a predatorprey system with a Hollingtype IV functional response. In 1965, Ivlev [30] proposed the Ivlevtype functional response. Subsequent studies also considered a grazing function as Ivlevtype function in a preypredator system [31, 32].
In the present study, we consider a twocomponent phytoplankton zooplankton model, which can be described based on the following assumptions: First, it is assumed that the conditions of phytoplankton growth are ideal, thus the phytoplankton population follows logistical growth in the absence of zooplankton. Second, a direct link between the phytoplankton population and zooplankton population cannot be represented unless quantitative methods are applied; the previous work clearly shows that the grazing relationship of zooplankton population on phytoplankton population may follow Holling II response curve in realistic ecosystem, which has been studied by many ecologists, for example, Fussmann et al. have used a Holling II functional response to model the interaction of zooplankton population and phytoplankton population, and the modeling results can well agreed with experimental results [33]. Thus we apply a Holling II functional response to describe their relationship between zooplankton population and phytoplankton population with sufficient accuracy in this paper. Finally, it is assumed that zooplankton population has sufficient resources for alternative food, thus we applied the logistic growth law to describe this characteristic of zooplankton population in the case of extinction of the phytoplankton. This is because alternative food sources may have an important role to play in promoting the persistence of zooplanktonphytoplankton systems [34]. Based on the above assumptions, we can propose the following system:
where P is the density of the phytoplankton population and Z is the density of the zooplankton population at time t; the seven parameters \(r_{1}\), \(K_{1}\), m, \(\beta_{1}\), \(\beta_{2}\), \(r_{2}\), \(K_{2}\) are positive constants; \(r_{1}\), \(K_{1}\) are the intrinsic growth rate and environmental carrying capacity of the phytoplankton, respectively. m is the half saturation constant for a Hollingtype II functional response, \(\beta_{1}\) is the rate of predation of zooplankton, and \(\beta_{2}\) denotes the ratio of biomass consumed by zooplankton during its growth.
In marine ecosystems, turbulent diffusion can also cause the movement of plankton. Thus, this diffusion should also be considered in plankton models. We assume that no plankton species enter or leave the water at the boundary. If we consider the evolution of the plankton model using constant diffusion coefficients, then system (1.1) can be reduced to the following system:
where \(D_{1}\) and \(D_{2}\) are the constant diffusion coefficients of the phytoplankton and zooplankton, respectively. We take the boundary condition of the plankton population \(P(s,t)\) and \(Z(s,t)\) in \(s\in \Omega\), \(t>0\), as follows:
and the initial conditions are
The equilibrium states of system (1.2) are the same as those of the homogeneous system (1.1).
Based on the above considerations, the remainder of this paper is organized as follows. In Section 2, we study the equilibrium of the system and the stability of the system. In Section 3, we consider the system with diffusion. We derive the criteria for diffusive stability and the Turing instability region of the system. Finally, simulations and discussions are presented.
2 Equilibrium and the stability of system (1.1)
2.1 Equilibrium of the system
Let \(f(P,Z)\) and \(g(P,Z)\) be the right hand sides of the equations in (1.1). It is obvious that the equilibria \(E_{0}=(0,0)\), \(E_{1}=(K_{1},0) \), and \(E_{2}=(0,K_{2})\) always exist. By \(f(P,Z)=0\), we can obtain the vertical isoclines \(l_{1}\): \(Z=\frac {r_{1}}{K_{1} \beta_{1}} (P^{2}+(mK_{1}) PK_{1} m)\), and it is a downwards parabola. The axis of symmetry is \(P=\frac{K_{1}m}{2}\), and we have the y axis by \(Z=\frac{r_{1} m}{\beta_{1}}\). By \(g(P,Z)=0\), we can obtain the horizontal isoclines \(l_{2}\): \(Z=K_{2}+\frac{\beta_{2} K_{2} P}{r_{2} (m+P)}\). It is easy to see that the line \(P=m\) is the asymptote of \(l_{2}\). We can see that \(l_{2}\) increases monotonically when \(P\in (m,+\infty)\), and we have the y axis by \(Z=K_{2}\). Next we discuss the existence of positive equilibria.

(i)
If \(K_{1}>m\), \(\frac{r_{1} m}{\beta_{1}}\leq K_{2} \leq\frac{r_{1} r_{2} (K_{1}+m)^{3}}{4K_{1} \beta_{1} [r_{2} (K_{1}+m)+\beta_{2} (K_{1}m)]}\), then there exist two positive equilibria \(E_{e1}=(P_{e1}, Z_{e1})\) and \(E_{e2}=(P_{e2},Z_{e2})\) in system (1.1), where \(P_{e1}<\frac {K_{1}m}{2}\), \(P_{e2}>\frac{K_{1}m}{2}\).

(ii)
If \(K_{1}>m\), \(\frac{r_{1} r_{2} (K_{1}+m)^{3}}{4K_{1} \beta_{1} [r_{2} (K_{1}+m)+\beta_{2} (K_{1}m)]}< K_{2}<\frac{r_{1} m}{\beta_{1}}\), then there exists one positive equilibrium \(E_{e3}=(P_{e3}, Z_{e3})\) in system (1.1), where \(P_{e3}<\frac{K_{1}m}{2}\).

(iii)
If â‘ \(K_{1}>m\), \(K_{2}<\min\{\frac{r_{1} m}{\beta _{1}},\frac{r_{1} r_{2} (K_{1}+m)^{3}}{4K_{1} \beta_{1} [r_{2} (K_{1}+m)+\beta_{2} (K_{1}m)]}\}\), or â‘¡ \(K_{1}< m\), \(K_{2}<\frac{r_{1} m}{\beta _{1}} \), then there at least exists one positive equilibrium \(E_{e4}=(P_{e4},Z_{e4})\) in system (1.1), where \(P_{e4}>\frac {K_{1}m}{2}\).
2.2 Stability of the equilibrium
Next, we discuss the local behaviors of the equilibria of system (1.1). The Jacobian matrix takes the following form:
It is obvious that \(E_{0}=(0,0)\) is unstable and \(E_{1}=(K_{1},0)\) is a saddle point. \(E_{2}=(0,K_{2})\) is a saddle point if \(r_{1}>\frac{\beta_{1} K_{2}}{m}\), and is locally asymptotically stable when \(r_{1}<\frac{\beta _{1} K_{2}}{m}\).
We now analyze the local stability of the positive equilibria. Let \(\overline{E}=(\overline{P},\overline{Z})\) be an arbitrary positive equilibrium. We can obtain
so the Jacobian matrix for \(\overline{E} =(\overline{P},\overline {Z})\) is given by
Note that
If \(\overline{P}>\frac{K_{1}m}{2}\), we can obtain \(J_{11}<0\), thus \(\operatorname{tr}(J_{\overline{E}})<0\) and \(\operatorname{det}(J_{\overline{E}})>0\). The equilibrium \(\overline{E}=(\overline{P},\overline{Z})\) is always locally asymptotically stable. If \(\overline{P}<\frac{K_{1}m}{2}\), we can obtain \(J_{11}>0\). Hence, based on the above analysis, we have the following results.
Lemma 2.1
If there exists one positive equilibrium \(E_{e4}=(P_{e4},Z_{e4})\) in system (1.1) and \(P_{e4}>\frac{K_{1}m}{2}\), then the equilibrium is always locally asymptotically stable.
Lemma 2.2
If there exist two positive equilibria \(E_{e1}=(P_{e1},Z_{e1})\) and \(E_{e2}=(P_{e2},Z_{e2})\) in system (1.1), we find that \(E_{e2}=(P_{e2},Z_{e2})\) is always locally asymptotically stable, and \(E_{e1}=(P_{e1},Z_{e1})\) is a saddle point if \(K_{2}\leq m\).
Proof
Define \(F(P)=\frac{r_{1}}{K_{1} \beta _{1}}[P^{2}+(mK_{1})PK_{1} m][K_{2}+\frac{\beta_{2} K_{2} P}{r_{2} (m+P)}]\) where \(0< P<\frac{K_{1}m}{2}\). By combining this with the conditions in (i) we find that \(F'(P)>0\) when \(0< P<\frac{K_{1}m}{2}\).
Hence, the inequality of \(\frac{\beta_{1} \beta_{2} K_{2}}{(m+P)^{2}}<\frac{r_{1} r_{2}}{mK_{1}}(m+2PK_{1})\) (\(0< P<\frac{K_{1}m}{2}\)) is established. Therefore
Thus, if \(m\geq K_{2}\), then \(\operatorname{det}(J_{E_{e1}})<0\).
Hence, \(E_{e1}=(P_{e1},Z_{e1})\) is a saddle point if \(K_{2}\leq m \).â€ƒâ–¡
Lemma 2.3
If there exists one positive equilibrium \(E_{e3}=(P_{e3},Z_{e3})\) for system (1.1) and \(P_{e3}<\frac {K_{1}m}{2}\), then the equilibrium \(E_{e3}=(P_{e3},Z_{e3})\) is locally asymptotically stable when \(K_{2}\geq m\) and \(\frac{r_{1}}{r_{2}+\beta _{2}}<\frac{K_{1}}{K_{1}m}\), or \(K_{2}\geq m\) and \((r_{1} K_{1}r_{1} mr_{2}K_{1}K_{1} \beta_{2})^{2}8r_{1} r_{2} K_{1} m<0\).
Proof
In the same manner, we define
Under the conditions of (ii), we can find that
Thus
Therefore
when \(m\geq K_{2}\), we obtain \(\operatorname{det}(J_{E_{e1}})>0\).
Here
When
or
then \(\operatorname{tr}(J_{E_{e3}})<0\).
Hence, according to the above conditions, \(E_{e3}=(P_{e3},Z_{e3})\) is locally asymptotically stable.â€ƒâ–¡
Theorem 2.1
The positive equilibrium \(E_{e4}=(P_{e4},Z_{e4})\) (\(P_{e4}>\frac{K_{1}m}{2}\)) is globally asymptotically stable in the presence and the absence of diffusion if \(0< K_{1}\leq\frac{r_{1} m(m+P_{e4})}{\beta_{1} Z_{e4}}\) holds.
Proof
Define a Lyapunov function
We note that \(V_{1}(P,Z)\) is nonnegative and \(V_{1}(P,Z)=0\) if and only if
Furthermore,
By substituting the expressions for \(\frac{dP}{dt}\) and \(\frac {dZ}{dt}\) from system (1.1) in the absence of diffusion, we obtain
Using the condition that
(2.3) can be simplified as
Because \(Z_{e4}>K_{2}\), we have
and \((\frac{r_{1}}{K_{1}}+\frac{\beta_{1} Z_{e4}}{(m+P_{e4})(m+P)})(PP_{e4})^{2}\leq0\) always occurs when
Therefore, \(\frac{dV_{1}}{dt}<0\) if \(0< K_{1}\leq\frac{r_{1} m(m+P_{e4})}{\beta_{1} Z_{e4}}\) holds.â€ƒâ–¡
3 Stability and instability of the system with diffusion
In this section, we consider how the diffusion affects the stability of system (1.2). The stability and instability of system (1.2) are considered as follows.
Let \(0=u_{0}< u_{1}< u_{2}<\cdots<\infty\) (\(\lim_{i\rightarrow\infty } u_{i}=\infty\)) be the eigenvalues of \(\nabla^{2}\) on Î© with the zeroflux boundary condition. Set
and we then consider that \(X=\bigoplus^{\infty}_{i=0}X_{i}\), where \(X_{i}\) is the eigenspace corresponding to \(u_{i}\).
Theorem 3.1
The positive equilibrium \(E_{e2}=(P_{e2},Z_{e2})\) in system (1.2) is uniformly asymptotically stable in the presence of diffusion.
Proof
The linearization of system (1.2) at the positive equilibrium \(E_{e2}=(P_{e2},Z_{e2})\) is
where \(f_{n}(\varepsilon_{1},\varepsilon_{2})=O(\varepsilon ^{2}_{1}+\varepsilon^{2}_{2})\) (\(n=1,2\)).
For each i (\(i=0,1,2,\ldots\)), \(X_{i}\) is invariant under the operator Î“, and \(u_{i}\) is an eigenvalue of Î“ on \(X_{i}\) if and only if \(\lambda_{i}\) is an eigenvalue of the matrix
Note that
It is obvious that \(\operatorname{tr}(H_{i})<0\), \(\operatorname{det}(H_{i})>0\). and the two eigenvalues \(\lambda^{+}_{i} \) and \(\lambda^{}_{i}\) have negative real parts. For any \(i\geq0\), we can get the following.
If \((\operatorname{tr}(H_{i}))^{2}4\operatorname{det}(H_{i})\leq0\), then \(\operatorname{Re}(\lambda^{\pm }_{i})=\frac{1}{2}\operatorname{tr}(H_{i})\leq\frac{1}{2}\Gamma_{11}<0\); and if \((\operatorname{tr}(H_{i}))^{2}4\operatorname{det}(H_{i})>0\), since \(\operatorname{tr}(H_{i})<0\) and \(\operatorname{det}(H_{i})>0\), we have
where C is dependent on i.
Thus, a negative constant C exists, which is independent of i, such that \(\operatorname{Re}(\lambda^{\pm}_{i})< C\) for any i. By referring to [35], we find that the positive equilibrium \(E_{e2}=(P_{e2},Z_{e2})\) of system (1.2) is uniformly asymptotically stable in the presence of diffusion. The proof is complete.â€ƒâ–¡
Theorem 3.2
If there exists one positive equilibrium \(E_{e4}=(P_{e4},Z_{e4})\) in system (1.2) and \(P_{e4}>\frac {K_{1}m}{2}\), then \(E_{e4}=(P_{e4},Z_{e4})\) is globally asymptotically stable in the presence of diffusion if \(0< K_{1}\leq\frac{r_{1} m(m+P_{e4})}{\beta_{1} Z_{e4}}\) holds.
Proof
By referring to [36, 37] and the proof of Theorem 2.1, define
Then by differentiating \(V_{2}\) with respect to time t along the solutions of system (1.2), we can obtain
Using Greenâ€™s first identity in the plane, we obtain
where
Based on the above analysis, if
then \(\frac{dV_{1}}{dt}<0\), and thus \(\frac{dV_{2}}{dt}<0\).
This completes the proof.â€ƒâ–¡
Next, we analyze the formation of patterns. Based on the analysis above, we know that the positive equilibrium point \(E_{e3}=(P_{e3},Z_{e3})\) of system (1.2) is locally asymptotically stable when \(K_{2}\geq m\) and \(\frac{r_{1}}{r_{2}+\beta_{2}}<\frac {K_{1}}{K_{1}m}\), or \(K_{2}\geq m\) and \((r_{1} K_{1}r_{1} mr_{2} K_{1}K_{1} \beta _{2})^{2}8r_{1} r_{2} K_{1} m<0\) holds. In this case, we can reach the following conclusion.
Theorem 3.3
If the positive equilibrium \(E_{e3}=(P_{e3},Z_{e3})\) is locally asymptotically stable in system (1.1), then for system (1.2), the equilibrium \(E_{e3}=(P_{e3},Z_{e3})\) is stable when
and the criterion for Turing instability for system (1.2) satisfies the following condition:
where
is the Jacobian matrix at \(E_{e3}=(P_{e3},Z_{e3})\).
Proof
The linearized form of (1.2) that corresponds to the equilibrium state \(E_{e3}=(P_{e3},Z_{e3})\) is given by
where \(P=P_{e3}+p\), \(Z=Z_{e3}+z\), and \((p,z)\) are small perturbations of \((P,Z)\) about the equilibrium \(E_{e3}=(P_{e3},Z_{e3})\). We expand the solution of system (1.2) into a Fourier series:
where k is the wave number of the solution. By combining (3.4) and (3.5), we obtain
Hence, we can obtain the characteristic equation as follows:
where
In order to allow the system to reach Turing instability, at least one of the following conditions must be satisfied: \(\operatorname{tr}_{k}>0\) and \(\Delta _{k}<0\). However, it is obvious that \(\operatorname{tr}_{k}<0\). Thus only the condition \(\Delta_{k}<0\) can give rise to instability. Therefore, a necessary condition for the system to be unstable is that
We define
If we let \(k^{2}_{\mathrm{min}}\) be the corresponding value of \(k^{2}\) for the minimum value of\(F(k^{2})\), then
Thus, the corresponding minimum value of \(F(k^{2})\) is
If we let \(F(k^{2}_{\mathrm{min}})<0\), the sufficient condition for the system to be unstable reduces to
which yields
â€ƒâ–¡
In Theorem 3.3, we found that (3.7) is a sufficient condition for the diffusive instability of system (1.2). If criterion (3.7) is satisfied, the diffusion of the plankton population can cause the system to shift from a stable state to an unstable state. In ecological terms, this means that if the zooplankton diffusion rate is higher than the phytoplankton diffusion rate and (3.7) is satisfied, then the instability will continue to prevail. At this time point, we can use the system parameters to obtain the patterns of the plankton populations. The patterns of the plankton populations are considered in Section 4.
4 Numerical results
4.1 Numerical analysis
In this section, we will explore the carrying capacity of zooplankton \(K_{2}\) and the half saturation constant m and the influence on the steadystate transformation problem of the proposed system (1.1) and (1.2) using a numerical simulation analysis; thus, some parameters are fixed as follows: \(r_{1}=0.8\), \(K_{1}=1\), \(\beta_{1}=0.8\), \(\beta_{2}=0.7\), \(r_{2}=0.7\).
Figure 1A describes a doubleparameter bifurcation diagram, which shows how the parameters \(K_{2}\) and m affect the stability of system (1.1). It is easy to find from Figure 1A that system (1.1) is globally asymptotically stable in the gray area (I) and is locally asymptotically stable in the green area (III). Nevertheless, system (1.1) has two equilibria in the yellow area (II), one is locally asymptotically stable and the other is unstable. But it is a pity that system (1.1) does not have a positive equilibrium in the red area (IV). These results are consistent with the results in Section 2, which suggested the correctness and feasibility of the theoretical deduction.
In order to comprehensively analyze the parameter \(K_{2}\) and \(D_{1}\) and the influence on the stability of system (1.2), we set \(r_{1}=0.8\), \(K_{1}=1\), \(\beta_{1}=0.8\), \(\beta_{2}=0.7\), \(r_{2}=0.7\), \(m=0.5\). On setting \(D_{2}=10\), the Turing bifurcation curve can be obtained, as is shown in Figure 1B. Now, it is worthwhile to point out from Figure 1B that system (1.2) is globally asymptotically stable in the gray area (I), locally asymptotically stable in the green area (II), and unstable in the blue area (III), respectively. Moreover, it should be stressed that the red curve indicates the Turing bifurcation curves in system (1.2), and the yellow area in which there is no positive equilibrium. According to the premise \(D_{1}< D_{2}\), we can determine the range of the parameter \(K_{2}\) in the region III in Figure 1B; system (1.2) may shift from a stable state to an unstable state when we adjust the size of \(D_{1}\), so that system (1.2) can reach Turing instability in the whole of area III, which also verifies the conclusion of Theorem 3.3. Further, on setting the range of the parameter \(D_{1}\) in the region III, system (1.2) can also shift from a stable state to an unstable state when we adjust the size of \(K_{2}\). Based on the above results, it is worth to point out that the parameters \(K_{2}\) and \(D_{1}\) are sensitive in the steadystate transformation problem of system (1.2). Furthermore, it is evident from Figure 2 that the considered equilibrium is stable when \(K_{2}=0.38\) and is unstable when \(K_{2}=0.47\). These results suggested that system (1.2) has a dynamic conversion process from the steadystate solutions to the nonstationary solutions with varying parameter \(K_{2}\), which can provide a simulation verification to further elaborate the sensitiveness of the environmental carrying capacity \(K_{2}\) in terms of the steadystate transformation.
4.2 Numerical simulations
In order to further expound the environmental carrying capacity \(K_{2}\) and the diffusion \(D_{1}\) affecting the spatial distributions of phytoplankton population, some kinds of patterns will be given using the numerical simulations. Here, we perform extensive numerical simulations of system (1.2) in two dimensional space with the same parameter values as given in Figure 1B. Meanwhile, the value range of the parameters \(K_{2}\) and \(D_{1}\) can be chosen in the area III in Figure 1B.
It is well known that Figure 3A is a hotspot pattern, which comprises green spots on a blue background. Furthermore, it is also illustrated from Figure 3A that the hot spots are isolated zones with high phytoplankton densities, where the zooplankton population has a low density. However, with the change of parameter value, the spatial distributions of the phytoplankton population will have a series of dynamic evolutionary processes. Figure 3B is a hotspotstripes pattern, with small hot spots that can form stripes. Figure 3C is a striped pattern, which required a long time to settle down and we obtained only stripes. Figure 3D is similar to Figure 3E, where both are coldspotstripes patterns, i.e., the cold spots are isolated zones with low phytoplankton densities. However, Figure 3D can contain more stripes than Figure 3E, and the stripes are much longer. Figure 3F and Figure 3G show more complex striped patterns compared with Figure 3C. In Figure 3F, the distribution of stripes and spots is highly irregular, and the density of phytoplankton is low in these stripes and isolated spots. In Figure 3G, the distribution of stripes is more cluttered and similar to a maze. In the stripes shown in Figure 3G, the density of phytoplankton is lower than that in Figure 3F. Figure 3H shows a more interesting hotspot pattern produced by system (1.2). Although Figures 3H and 3A are both spot pattern; they have an obvious difference in the form. Stated succinctly, it is worthy of emphasis that rich patterns in Figure 3 can be obtained by controlling the value of the environmental carrying capacity \(K_{2}\) and the diffusion \(D_{1}\), where the patterns illustrate the complex spatial distribution of phytoplankton in system (1.2).
In order to deeply inquire into the parameters \(D_{1}\) and \(K_{2}\) affecting the spatial distributions of phytoplankton population, a series of patterns will be displayed. It is worth to point out from Figures 4A4C with \(K_{2}=0.475\) that system (1.2) has a hotspot pattern at \(D_{1}=0.01,0.03,0.05\), but the spots in Figure 4B are elliptical and the spots in Figure 4C are bigger than the other two. These results suggested that the spatial distribution of phytoplankton population will gradually become larger with increase of the value of \(D_{1}\). It should also be stressed from Figures 4D4E with \(D_{1}=0.01\) that the spatial distribution of phytoplankton will gradually change from spots to spot stripes and finally stripes with the decrease of \(K_{2}\). These results illustrated that the parameters \(K_{2}\) and \(D_{1}\) have an inherent ability to influence the spatial distribution of phytoplankton. Stated succinctly, it must be emphasized that the diffusion and the environmental carrying capacity have an important role to play in the spatial distribution of phytoplankton.
The above numerical results have shown some dynamics in system (1.2), and it is found that there exist abundant patterns in system (1.2). In order to further reveal the spatial distribution of phytoplankton, another parameter set is employed, as follows: \(r_{1}=2.425\), \(K_{1}=1\), \(\beta _{1}=1.35\) [38], \(\beta_{2}=1.0125\), \(r_{2}=0.97 \), \(m=0.35\), where the parameter \(\beta_{2}\) was derived from the literature [38, 39], and the parameters \(r_{1}\) and \(r_{2}\) were derived from the literature [40]. The other parameters (i.e., \(k_{2}\), \(D_{1}\), and \(D_{2}\)) were chosen as controlling parameters.
We perform a numerical simulation of system (1.2) under the above parameter set, and the results are shown in Figure 5. It is shown from Figure 5 that there exist four kinds of pattern formations at least in system (1.2) based on this parameter set when the parameters \(k_{2}\), \(D_{1}\), and \(D_{2}\) change. By comparison, it can be found that the results shown by Figure 5 are similar to the patterns shown by Figure 3, their distribution of spatial structure are coincident, for example, the spatial structure shown by Figure 5A agrees with the one shown by Figure 3D; and Figure 5B is similar to Figure 3E; the patterns shown by Figures 5C and 5D are coincident with the ones shown by Figures 3G and 3H, respectively. These results suggest that there may be abundant patterns in the spatial distribution of phytoplankton.
5 Discussion
In this study, we studied a nonlinear dynamics of a phytoplanktonzooplankton system with diffusion in detail. The structure of the system is very simple, but the study showed that the composition of the positive equilibrium was highly complex in the system. For system (1.1), our theoretical results show that if \(K_{1}>m\), the value of the environmental carrying capacity of the zooplankton will influence the dynamical behaviors of system (1.1). With the value of \(K_{2}\) changing, the stability of system (1.1) will change. Our numerical simulation leads to the same conclusion, through the results of Figure 1A; if the value of m is smaller, then it is obvious that the stability of system (1.1) may change with the increase of parameter \(K_{2}\). The result can suggest that the environmental carrying of the zooplankton is an important critical factor to influence the system dynamics.
The reactiondiffusion system exhibits some interesting dynamics depending on the parameters of the system. One of the main aims in our study is to analyze the effect of diffusion on the properties, especially the stability of the system. However, the results of Theorems 3.1 and 3.2 show that diffusion did not influence the stability of the system in some situations. The theoretical results show that only if the value of \(\frac{D_{2}}{D_{1}}\) grows large enough, then the equilibrium \(E_{e3}\) will shift from a stable state to an unstable state. We also show this result through a two dimensional bifurcation diagram (see Figure 1B). Our results show that the Turing instability will occur under certain conditions in the reactiondiffusion system. The occurrence of a Turing instability means that a solution which is stable in the absence of diffusion becomes unstable when diffusion is incorporated in the system. An effective way to study it is to give a small perturbation around the steadystate solutions and then obtain the conditions under which these fluctuations increase. In Figure 1B, our numerical results not only show that the diffusion can induce the occurrence of a Turing instability but also indicate that the environment carrying capacity of the zooplankton has an important role to play in the steadystate transformation.
Both theoretical and numerical analysis results have pointed out that the diffusion coefficient and the environment carrying capacity of the zooplankton have a significant impact on the dynamic properties. In 1993 [41], Pearson have presented 12 classic categories of patterns and these pattern formation have been studied further in recent years [42]. Our results show that the dynamics of system (1.2) comprised the diffusion controlled formation of stripes, hot/cold stripes/spots and some more interesting patterns. We aim to further demonstrate the influence of important parameters on the system by patterns formation; thus the results of Figure 4 are intuitive in reflecting the important role in these two parameters in the system. In general, the pattern formation can verify the rich dynamic properties around the Turing line of system, and the importance of the two parameters \(K_{2}\) and \(D_{1}\) is also deduced by the variation of the pattern.
Stated succinctly, the environment carrying capacity of the zooplankton and the diffusion term can seriously affect the dynamical behaviors of systems (1.1) and (1.2). Furthermore, it is our hope that these results can provide some reference value in the study of the internal operating rules and characteristics of marine ecosystems.
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Acknowledgements
This work was supported by the National Natural Science Foundation of China (Grant No.Â 31370381), the National Key Basic Research Program of China (973 Program, Grant No.Â 2012CB426510), and the Key Program of Zhejiang Provincial Natural Science Foundation of China (Grant No.Â LZ12C03001).
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Wang, P., Zhao, M., Yu, H. et al. Nonlinear dynamics of a marine phytoplanktonzooplankton system. Adv Differ Equ 2016, 212 (2016). https://doi.org/10.1186/s136620160935y
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DOI: https://doi.org/10.1186/s136620160935y