| Literature DB >> 34808693 |
Zhenpeng Ge1, Quan-Xing Liu1,2.
Abstract
Biological behaviour-driven self-organized patterns have recently been confirmed to play a key role in ecosystem functioning. Here, we develop a theoretical phase-separation model to describe spatiotemporal self-similar dynamics, which is a consequence of behaviour-driven trophic interactions in short-time scales. Our framework integrates scale-dependent feedback and density-dependent movement into grazing ecosystems. This model derives six types of selective foraging behaviours that trigger pattern formation for top-down grazing ecosystems, and one of which is consistent with existing foraging theories. Self-organized patterns nucleate under moderate grazing intensity and are destroyed by overgrazing, which suggests ecosystem degradation. Theoretical results qualitatively agree with observed grazing ecosystems that display spatial heterogeneities under variable grazing intensity. Our findings potentially provide new insights into self-organized patterns as an indicator of ecosystem transitions under a stressful environment.Entities:
Keywords: herbivores-grazing systems; movement behaviour; phase separation; scaling law; self-organization
Mesh:
Year: 2021 PMID: 34808693 PMCID: PMC9299242 DOI: 10.1111/ele.13928
Source DB: PubMed Journal: Ecol Lett ISSN: 1461-023X Impact factor: 11.274
Joining the theoretical and experimental ecologists' perspectives on terms and interpretations of spatial‐temporal dynamics
| Term | Interpretation | Mathematical expression |
|---|---|---|
| Thermodynamic phase separation | Two distinct phases generate from a single homogeneous mixture, driven by an associated reduction in free energy of the system. A classic example is that when water and oil are mixed together, they spontaneously separate to form a water phase and an oil phase. The mobility of the phase‐separating components is similar. |
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| Motility‐induced phase separation | The mobility of self‐propelled organism/particle is featured with density‐dependent movement. Self‐propelled individuals tend to accumulate where they move more slowly, whereas dissipate from over‐dense areas. This positive feedback makes the system separate into dense and dilute phases. | Equation (2) and Equation ( |
| Spinodal instability | In phase‐separation principle, one homogeneous mix phase spontaneously separates into two distinct phases with infinitesimal disturbance. |
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| Velocity‐induced drift flux | Drift is the slow movement of an object toward something, and the drift velocity is the average‐velocity of an object during drift. Drift flux is defined as the volumetric flux of either component relative to a surface moving at drift velocity. |
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| Biased random walk | Non‐Brownian diffusion, a random walk that is biased in certain directions, leading to a net drift on average of particles in one specific direction. A random walk can be based on three circumstances: 1) a higher probability of moving to certain directions under uniform moving step lengths; 2) suppose the probabilities of moving to all directions remain equal, but nonuniform moving step lengths; 3) nonuniform moving directions and moving step lengths. | Codling et al., |
| Coarsening/Ostwald ripening | A phenomenon originally observed in solid solutions or liquid sols that describes the change of an inhomogeneous structure over time: the growth of large clusters at the expense of smaller ones (Movie |
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| Hyperuniform structure | In |
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FIGURE 1Patterns of some grazing ecosystems. (a) Overgrazed and 30 years grazing‐excluded grassland in inner Mongolia, China [reprinted with permission from Hobley et al. (2018)]. (b) Lightly grazed salt marsh in north Germany. Photo credit: Leser Nicolas. (c) Moderately grazed grassland in Madagascar. Photo credit: Maria S. Vorontsova. (d) Heavily grazed dryland in southeast Spain [reprinted with permission from Mueller et al. (2014)]. (e) The spatial pattern of grass biomass after grazing in the Zumwalt Prairie, northeast Oregon [reprinted with permission from Jansen et al. (2019)]. (f) The spatial pattern of sheep on Ölling, Bayern, Germany [Image credit: Klaus Leidorf]. (g) and (h) Ripley's L function and pair correlation function for the point pattern of sheep in (f), and is Euclidean distance. The lighter blue shaded areas represent 95% simulation envelopes to distinguish from complete spatial randomness. Details of images analyses are in the Supporting Information. (i) Densities (mean ± SD) of adult Thomson's gazelles in relation to grass biomass over 16 censuses during 1995–1996 in Serengeti. This figure was modified from Fryxell et al. (2004)
FIGURE 2The density‐dependent movement of herbivores leads to diverse spatial patterns of vegetation. (a) Selective foraging behaviour of herbivores. Herbivores prefer short and low‐biomass plants and stay around while they dislike tall and high‐biomass plants and speed off. (b) An example of herbivore movement speed depending on plant density with and . (c) Schematic representation of the feedback in phase separation. Low plant density induces the aggregation of herbivores while high plant density triggers the dispersion of herbivores. (d) and (e) The transient spatial patterns under different stocking rates with , , and . is the spatial average of herbivore density corresponding to the stocking rate
FIGURE 3Six types of selective foraging behaviours leading to pattern formation derived from the model. Top: specific examples of six types of selective foraging behaviours. See the Supporting Information for the constraints of behaviour coefficients and (Table S1). Bottom: the phase diagram of grazing intensity and behaviour coefficients for six types of selective foraging behaviours in the model (Equation (S12) in the Supporting Information). Shaded areas are spinodal zones where infinitesimal perturbation to the initial uniform condition of herbivores or vegetation can cause pattern formation. In every image, the spatial pattern is a transient vegetation pattern with , and the parameters of the spatial pattern are associated with the dot
FIGURE 4The occurrence of phase separation in Equation (5). (a) The growth rates of six types of selective foraging behaviour corresponding to Figure 3. (See the Supporting Information for details of ). (b) The scaling law of coarsening dynamics of patch size based on numerical analysis of the vegetation patterns in the model. is the spatial average of herbivore density. (c) The vegetation patterns, corresponding to the dotted blue line as shown in (b), show spatiotemporal self‐similarity through structure factor analysis. (d) The coarsening vegetation patterns of the dotted blue line in (b)
FIGURE 5The phase diagram of our phase‐separation model. (a) The phase diagram with , and is obtained by Equation (S12) in the Supporting Information. This system mainly undergoes the first‐order phase transition between spatially homogeneous state and patterned state, and shows the continuous phase transition close to the critical point. The characters ‘1’–‘5’ are corresponding to Figures c1‐c5. The spinodal line and binodal line separate the phase diagram into three zones: the interior of the spinodal line is the unstable zone (light blue region) where infinitesimal perturbation to the initial uniform condition of herbivores or vegetation can cause phase separation; the portion between the spinodal line and the binodal line is the metastable zone (light red region) where large enough perturbation to the initial uniform condition of herbivores or vegetation can trigger phase separation; the portion beyond the binodal line is the stable zone (white region) where any initial states of herbivores and vegetation turn into near‐homogeneous states without the occurrence of phase separation. (b) The numerical simulation of spinodal instability shows decent consistency with the theoretical analysis of spinodal instability (Table 1). (c1)‐(c5) The transient spatial patterns that locate at the five different zones described in panel (a) with