Skip to main content
Advertisement
Browse Subject Areas
?

Click through the PLOS taxonomy to find articles in your field.

For more information about PLOS Subject Areas, click here.

  • Loading metrics

Tree Cover Bimodality in Savannas and Forests Emerging from the Switching between Two Fire Dynamics

Abstract

Moist savannas and tropical forests share the same climatic conditions and occur side by side. Experimental evidences show that the tree cover of these ecosystems exhibits a bimodal frequency distribution. This is considered as a proof of savanna–forest bistability, predicted by dynamic vegetation models based on non-linear differential equations. Here, we propose a change of perspective about the bimodality of tree cover distribution. We show, using a simple matrix model of tree dynamics, how the bimodality of tree cover can emerge from the switching between two linear dynamics of trees, one in presence and one in absence of fire, with a feedback between fire and trees. As consequence, we find that the transitions between moist savannas and tropical forests, if sharp, are not necessarily catastrophic.

Introduction

The tree cover distribution of moist savannas and tropical forests has been recently investigated extensively over Africa, Australia and South America [1], [2]. [1] have shown that these biomes co-exist over a very large range of annual rainfall (650–2500 mm/yr) and that at intermediate rainfall (1000–2500 mm/yr) tree cover is bimodal, exhibiting one peak for low woody cover (savanna - characterized by high fire frequency) and one peak for high woody cover (forest - characterized by absence of fire).

The bimodality of tree cover distribution has been used as a proof that savanna and forest are alternative stable states [1][3]. In literature, many simple models (also denominated minimal) exhibit savanna–forest bistability [4][6]. The main advantage of minimal models consists in the possibility of identifying interactions and causal nexi between drivers and state variables [7], [8]. These models can be treated analytically and investigated through the bifurcation analysis. The savanna–forest models of [4][6] are systems of non-linear differential equations, forced by fire and other environmental factors such as rainfall (without exploring its variability though) and herbivores. What is widely accepted is that fire is responsible for bistability: in savanna and forest the tree cover cannot be adequately explained without explicitly considering the dynamics of fire [9][12], and feedbacks fire–trees have been used in literature to argue for bistability (see [13] and references therein).

The literature contains many studies about the existence of alternative stable states (see the reviews by [13], [14]) and models exhibiting bistability [15][17]. However, alternative stable states have been more frequently found in laboratory experiments than in field studies, even after correcting for different number of studies [13]. Bistability has deep ecological consequences on the ecosystem behavior: the existence of critical transitions, which makes the ecosystem fragile around certain thresholds, subject to catastrophic shifts, and thus difficult to manage.

We believe that the bistability of savanna and forest is not the only possible explanation for the bimodality of tree cover distribution. Here we use a minimal model (the same model typology used in literature to prove savanna–forest bistability [4][6]) to provide an alternative explanation to tree cover bimodality. We focus on the representation of fire, which is the key element explaining the bimodality of frequency distribution. In the above mentioned non-linear differential equation models, fire is represented as an a-priori determined parameter. Here we consider the vegetation subject to two possible dynamics: one in presence and the other in absence of fire. The switching between these two dynamics is stochastic, and dependent on the quantity of trees in the ecosystem.

Section Methods gives the methodology. In particular, firstly it illustrates the matrix model of tree dynamics in moist savannas and tropical forests, then it shows how the model can be reduced to a Markov chain, and reports the calculation of the stationary probability distribution of the tree cover. Section Results provides three examples of how tree cover bimodality can be found, including a sensitivity analysis of parameters. Section Discussion comments the results and provides some considerations to support the alternative explanation of tree cover bimodality in savanna–forest dynamics.

Methods

Let us assume the yearly dynamics of trees in moist savannas and tropical forests described by a time-discrete matrix model. This choice is motived by two facts: 1) matrix models are dominant in plant demography description, have an important role in studies of broad ecological and evolutionary questions [18], and the parameters determination is relatively easy [19], [20], as well as the comparison of results obtained using different size or age classes discretization [18]. 2) Matrix models have already been considered to describe the tree dynamics in savannas by [21][23]. In these studies, fire occurrence is assumed independent of the state of the system. In particular [22], use a deterministic fire return period [21], assume a constant probability of fire occurrence [23], considers both these approaches. However, feedbacks between fire and vegetation have been observed [9], [10]. In order to account this element within the vegetation dynamics, we consider fire as a stochastic process with a probability of occurrence dependent on the state of the system.

Let be the temporal coordinate, the vector representing the fraction of tree cover divided in size classes: represents the seedlings, and represents adult trees. The superscript stands for transposition, and . Each component of is dimensionless, with .

The yearly dynamics of are described by the following matrix equation:(1)where is a Bernoulli variable describing fire occurrence. is associated to the tree dynamics in presence of fire, and to the tree dynamics without fire. For each year , takes value with probability of fire , and with probability . depends on the status of the ecosystem, i.e., by the amount of grass fuel load, which is negatively correlated to the density of trees [24][26]. In particular, if there are fewer trees, there is more grass in moist savannas, and thus a greater quantity of fuel load enhancing fire probability [27], [28]. Thus we assume a negative relation between tree density and fire probability, considering only implicitly the negative correlation between grass density and tree density. This implies a positive feedback, which means that the more the ecosystem burns, the more it is likely to burn in future [9], [10]. The temporal sequence is a two-state Markov chain with a transition matrix , where , , and similarly and . The vector represents the recruitment. Assuming that new seedlings are recruited in the smallest size class, has the first element (), and elsewhere. is a matrix. In particular , , and is a matrix containing in the first row all elements equal to , and elsewhere. and are Lefkovitch matrices. According to Eq.(1), in each temporal step, the trees are firstly updated according to absence/presence of fire, and then new tree seedling are recruited in the population. Thus the fire can affect the new recruits the following years.

The generic element of represents the proportion of trees of class moving into class in the year if the fire does not occur, while the generic element of represents the proportion of trees of class moving into class in the year if the fire occurs.

According to Eq.(1), the annual variability of trees comes out by the composition of two linear dynamics, one in presence, and the other in absence of fire. Eq.(1) is also known in literature as Hybrid Linear System, or Markov Jump Linear System, see [29]. The switching between the two dynamics is stochastic, and ruled by the fire probability , which is dependent on the amount of trees in the ecosystem, . Let indicate the number of visits the system makes in the dynamics, i.e., the number of years when the fire occurred, while the number of visits in the dynamics, i.e., the number of years without fire. The average number of visits in the dynamics over a period of years is calculated as , and similarly for the dynamics . Thus the permanence ratios and indicate respectively the percentage of time the system spends in no-fire and fire dynamics.

For Eq.(1), two possible steady states can be found. They are summarized in the following equation:(2)where is the identity matrix. By putting , the steady state is found. This corresponds to the undisturbed steady state, and it is obtained if the matrix is always applied, i.e., the system is always in no-fire dynamics. Analogously, putting , the steady state is found, and corresponds to the disturbed steady state, which is obtained if the matrix is always applied, i.e., the system is always in the fire dynamics. Note that each of two steady states is reached if the system stays in one dynamic only (or, let's say, for a certain amount of time). However, the global dynamic of generally oscillates between these two steady states, resulting in non-equilibrium dynamics.

The system of Eq.(1) is asymptotic stable, i.e., it does not go to infinity, if the product of all possible sequences of matrices leads to an asymptotically stable solution, i.e., tends to zero, see [30], [31]. A sufficient stability condition for this is that , , where is any matrix norm function [30]. As matrix norm it is possible to consider the maximum element norm [32]. Here, the conditions and ensure the asymptotic stability of Eq.(1).

Eq.(1) is a time-discrete Markovian process, which for simplicity of analysis, we represent through a finite-state Markov chain, i.e., with discrete and finite states, discretizing the domain of the variable. Let the domain of each component of be divided into intervals of width . Thus the domain of () is discretized into hypercubes, where the element is identified through its center of coordinates . Of the hypercubes, some of these have no points satisfying the condition , thus these elements are not physically acceptable. Let be the number of physically acceptable hypercubes. Let be the fire probability of the hypercube , evaluated in its center. Each hypercube can be considered as the state of a Markov chain. Let be the transition matrix associated to the Markov chain, where the generic element contains the probability that the system passes from the state to the state . Let be the transition matrix containing in each element the proportion of points of the hypercube mapping into the hypercube when the dynamics of are ruled by the no-fire dynamics, and be the transition matrix containing in each element the proportion of points of the hypercube mapping into the hypercube when the dynamics of are ruled by the fire dynamics. For the theorem of total probability, . Let be the vector representing the stationary distribution of the states of the chain, whose elements are non-negative and sum to 1. The stationary distribution satisfies the equation , or equivalently . If the Markov chain is irreducible and aperiodic, then the stationary distribution is unique. In this case the converges to a rank-one matrix in which each row is the stationary distribution. The distribution will have a bimodal or unimodal shape depending by the mixing of the two dynamics, fire and no-fire. In particular, if the system persists in a single dynamic will be unimodal, otherwise it will have a bimodal, or unimodal shape, depending on the value of the permanence ratios.

Results

Here we give three examples of tree cover bimodality emerging from the switching between fire and no-fire dynamics.

As first example, we consider the simplest case , i.e., , the dynamics of tree cover is described only by one size class. The matrices and and the vectors and are scalar and therefore for this case are not shown in bold. We consider this case to limit the number of parameters to five, nevertheless the conclusions we draw apply also to , reasoning in terms of total tree cover.

The fire probability, , is assumed a decreasing linear function of the tree cover . In particular for , for , and for , where and are two thresholds (Fig. 1a). The choice of the shape of results from two arguments: 1) the fire probability may be assumed to be a linear increasing function of dead grass biomass as in [11], [12], [33] and according to field data showed in [34]. 2) Grass production increases as the tree cover decreases [24][26].

thumbnail
Figure 1. Example of tree cover distribution.

Panel a) reports the fire probability, , with the indication of the steady states of tree cover: and . Panel b) shows the histogram of tree cover when fire is not present. Panel c) shows the histogram of tree cover when fire is present. Panel d) gives the stationary state distribution of tree cover. In panels b–d, bins of 0.1 width are used.

https://doi.org/10.1371/journal.pone.0091195.g001

is the probability the ecosystem stays in the state , whereas represents the risk of the ecosystem to leave . Similarly, represents the probability of staying in and is the risk of leaving . If, for instance, and is very close, but different from zero, the ecosystem tends to stay in the undisturbed state. However, because the probability of fire is not zero, a fire event may happen. If this occurs, the ecosystem reduces its tree cover, and at same time it increases the probability of fire. In other terms, the more the ecosystem burns and more likely it is likely to burn in the future [10]. Analogously, if and is very close, but different from unit, the ecosystem tends to stay in the disturbed state, because fire is likely to occur every year. However, because the fire probability is not one, in a certain year, the fire event could not occur. In this case, in the following year the ecosystem will increase its tree cover, and at same time reduce the probability of fire. Thus, if the ecosystem does not burn in a year, it is unlikely to burn the following year [9], [10]. The above reported function includes the feedback between fire and tree cover.

Let us assume for the five parameters the following values: , , , , and . These values are calculated with transition matrices of Acacia nilotica [21] using the collapsing algorithm proposed by [19]. corresponds to a grass fuel load of 1000 kg/ha, value under which ; to a grass fuel load of ∼11000 kg/ha, values above which have , see [33], [35]. The stable states of the two dynamics are , and with fire probabilities respectively and . We have made a 5000 yr simulation of the model starting from the initial condition . It is important to make simulations on long time horizons (millennia) in order to avoid partial representations of the ecosystem behaviour [36], [37]. The permanence ratios in the two dynamics are respectively in the no-fire dynamic, and in the fire dynamic. The histograms of tree cover evaluated with bins of 0.1 width are reported in Fig. 1: the histogram of the no-fire dynamics has a mode around the state (Fig. 1b) and the histogram of the fire dynamics has a mode around the state (Fig. 1c). Then, we have discretized the variable using bins of 0.01 width, calculated the Markov transition matrix , and consequently the stationary probability distribution , given in panel d) of Fig. 1. From this, it is evident that the stationary distribution of tree cover is bimodal.

Clearly, this is only an example, and the results are dependent on the specific parametric configuration. A sensitivity analysis of parameters can clarify the circumstances under which a bimodal distribution of tree cover can emerge. In order to quantify the bimodality of the tree cover distribution, we introduce here a bimodality index , where is the mean of the distribution , while is the mean of associated to the more frequent dynamic. To estimate , we built a histogram of the values associated to the more frequent dynamic with the same bins of the distribution. Then , where is the center of the bin, the absolute frequency of the bin. If then the distribution is unimodal. If then the distribution is bimodal. We found that 0.1 can be used as threshold to discriminate between unimodal and bimodal shape. We have then considered the index to analyze the shape of firstly varying the demographic parameters, , and , and keeping the other parameters constant as in the example previously reported, and secondly varying the parameters of the fire dynamics and , i.e., adjusting the thresholds , and , and keeping the other parameters constant as in the example. In panels a) and b) of Fig. 2 we report the results of the sensitivity analysis. Because the demographic parameters must satisfy the constraint , and similarly for the parameters of the fire dynamics , then the graphs in Fig. 2 are triangular. In the panels of Fig. 2 we also report the isolines of , so that in the case of unimodal distribution we have information about the location of the histogram peak.

thumbnail
Figure 2. Sensitivity analysis of the shape of the probability distribution of tree cover using the bimodality index .

In panel a) the demographic parameters and are varied. In panel b) the parameters of fire probability and are varied. The black lines represent -isolines.

https://doi.org/10.1371/journal.pone.0091195.g002

If and , then the distribution is bimodal, otherwise it is unimodal (Fig. 2a). If , i.e., at the top and right vertices of the triangle, then the two dynamics tend to collapse into one, and the distribution is unimodal. In particular, if , is located in the right part of its variability range (i.e., high values of the tree cover), while if , is located in the left part of its variability range (i.e., small values of the tree cover).

For and , the distribution is bimodal, otherwise it is unimodal (Fig. 2b). For small values of , and consequently , the ecosystem is seldom disturbed by fire, and is characterized by high values of the tree cover. The distribution is unimodal and located in the right part of its variability range. Conversely, for high values of , and , the ecosystem is frequently disturbed by fire and is characterized by low values of tree cover. The distribution is unimodal, and located in the left part of its variability range.

As second example, we mimic a spatial sampling of tree cover. In literature [1], [2] the tree cover distribution is empirically obtained collecting data at different points in space, and at a certain time instant, rather than sampling the data at a given location over time, i.e., using the spatial information in place of the temporal one. In order to mimic the spatial sampling of tree cover from distinct and independent sites at a given instant time, we have made 1000 simulations, each 5000 yr long with using for each simulation parameter values extracted uniformly from the following intervals: , , , , and . We have adopted narrow ranges for the parameters associated to the no-fire dynamic, i.e., and , and wider variability ranges for the parameters associated to the fire dynamic, i.e., , and , as well as the recruitment parameter , in this way, we include different fire vulnerability of different tree species [23]. Depending on the evolutive strategies of trees, there are trees very resistant to fire with a thick bark or resprouting mechanisms (savanna trees), and there are trees very vulnerable to fire (forest trees). Conversely, the mortality of trees without fire is far less variable. Note that the intervals chosen for and correspond to bimodal distributions of tree cover (Fig. 2a). Sampling the tree cover from the 1000 simulations, in any time instant (except for the first 100 yrs possibly influenced by the initial state), we have found a bimodal distribution, with values of the bimodality index in the range 0.1–0.23. Panel a) of Fig. 3 reports the empirical distribution of tree cover sampled at yrs.

thumbnail
Figure 3. Frequency distribution of tree cover obtained sampling from 1000 simulations, each one 5000 yr long, at the time t = 300 yrs.

In panel a) the 1000 simulations are obtained uniformly sampling the parameters from the following intervals: , , , , and . In panel b) from the following intervals: , or , , , and . Bins of 0.1 width are used.

https://doi.org/10.1371/journal.pone.0091195.g003

We have also sampled tree cover using parameters extracted uniformly from the following intervals: , or , , , and . Note that the intervals chosen for and correspond to unimodal distributions of tree cover (Fig. 2a). In particular, the configurations belonging to are characterized by high values of tree cover, while configurations belonging to the range by small values of tree cover. The frequency distribution of tree cover obtained from the spatial sampling is however bimodal in any time instant (except for the first 100 yrs possibly influenced by the initial state), with values of the bimodality index in the range 0.18–0.2. Panel b) of Fig. 3 gives the frequency distribution of tree cover sampled at yrs.

As third example, we consider , i.e., a tree population classified in three size classes. In particular, class 1 includes small trees (i.e., height m), class 2 medium trees (i.e., height m), and class 3 large trees (i.e., height m). The matrices , and the recruitment vector are respectively equal to , , . These values are derived from [33] passing from the seasonal matrices to the annual ones. The parameters and of the fire probability refer to the tree cover calculated over the last two classes, i.e., , assuming that the first height class does not contribute significantly to the vegetation cover. As in [33], we use and , and as initial condition . Figure 4 shows in the top panel a 5000 yr simulation of the tree cover, in the intermediate panel the occurrences of fire, and in the bottom panel the stationary probability distribution of the tree cover.

thumbnail
Figure 4. Tree cover dynamics (panel a), fire occurrence (panel b), and probability distribution of tree cover (panel c) of a tree population classified in three height classes.

In panel c), bins of 0.1 width are used.

https://doi.org/10.1371/journal.pone.0091195.g004

Discussion

The three examples show how the model in Eq.(1) can exhibit the tree cover bimodality under different ways. For certain parameter combinations, a double peak could be shown in the frequency histogram of the states visited along a trajectory over time (first and third example), or equivalently, in the stationary state probability distribution of the Markov chain associated to the system (first example). Bimodality of tree cover has also been obtained in the frequency histogram of the states visited by many simulations (each one representing a different site) at a certain time instant (second example). In all these cases, bimodality simulated through the model is not in contradiction with bimodality observed in data [1], [2] and it does not involve the concept of bistability.

The first example, showing tree cover bimodality in a single non-equilibrium trajectory along time, is in agreement with some statements of [13], [38] according to which data may not necessarily represent steady states, but may be snapshots of the system which is not at the steady state.

The sensitivity analysis explains in which parametric configurations bimodality can be obtained in the trajectory. In the first two examples, the demographic parameter is representative of how fast the woody cover grows in absence of fire. The higher this parameter is, the more the tree dynamics without fire tend towards the undisturbed state . The parameter is representative of the resistance of the tree vegetation to fire disturbance. The lower this parameter is, the more attractive are the tree dynamics with fire towards the state . If trees are fast growing and highly resistant to fire (i.e, the top corner of Fig. 2a), the woody cover tends to be unimodal with a high average value (). If trees are slow growing with a low fire resistance (i.e., the bottom right corner of Fig. 2a), the woody cover tends to be unimodal with a low average value (). Bimodality occurs when the system is fast growing and very vulnerable to fire, in other words, when both dynamics (with and without fire) are strongly attractive to their steady states. Assuming that all the couples in Fig. 2a are equiprobable, in of the parametric configurations the tree cover distribution is bimodal, and in unimodal.

If the fire probability in the disturbed steady state is high , the ecosystem tends to be frequently burned, has a low risk to be left, the dynamics with fire are more frequent, and the woody cover is in average low (). If the fire probability is low in both steady states (the bottom corner of Fig. 2b), the dynamic without fire is more frequent, has a low risk to be left and the woody cover is in average high (). Bimodality occurs when the fire probability is very low in and relatively high in , , so that the dynamics with fire tend to be maintained when the ecosystem is in , and the dynamics without fire tend to be maintained when the ecosystem is in . Assuming that all the couples in panel b) of Fig. 2 are equiprobable, in of the parametric configurations the tree cover distribution is bimodal and in unimodal. In general, the tree cover tends to be bimodal when both steady states have a low risk to be left.

The second example shows that the operation of spatial sampling of tree cover can lead to a bimodal frequency distribution. Data are considered as collected from different sites. A bimodal frequency distribution is obtained if data are collected from sites having (Fig. 3a) all bimodal probability distributions, or alternatively, if one samples from sites (Fig. 3b) having unimodal probability distribution but with both high and low values of the tree cover, i.e., sampling from parameter configurations corresponding to both the top and the bottom right corner of Fig. 2a.

The third example illustrates the presence of rapid transitions between moist savanna and tropical forest, as in [17]. The analysis of the trajectory in Fig. 4 leads to some considerations. It is possible to see how 1) for of time the ecosystem is characterized by a total tree cover , assimilable to a forest state, and for of time by , assimilable to an open savanna state. The forest and savanna states are observable for long periods, see respectively the intervals and in Fig. 4a. 2) The feedbacks between fire and woody cover are evident through the clustering of fire events (see Fig. 4b). 3) Fire-tree feedbacks allow sharp (but not catastrophic) transitions forest→savanna and savanna→forest (Fig. 4a). 4) The stationary probability distribution of the total tree cover is bimodal (Fig. 4c).

Why should this alternative explanation to tree cover bimodality be plausible?

Our explanation of tree cover bimodality stems from a characteristic element of the moist savannas and tropical forest dynamics: the fire occurrence is not constant, but is a variable, dependent on the ecosystem status, with a feedback between fire and trees [9], [10]. If this phenomenological issue is quite evident, the simple models available in literature, i.e., space-implicit ordinary differential equation models, see e.g. [4][6] ignore this element. In particular, these models are non-linear, and assume the fire frequency as a constant parameter. As a consequence, these models lead to bistability between moist savanna and forest. Here, differently, we include the variability of fire occurrence in a matrix model of tree dynamics, where the impact of fire is of on-off type and depends on the tree cover, driving the ecosystem to oscillate stochastically between two dynamics, each one characterized by one steady state. In this way, the relative strength of the two dynamics can determine whether the tree cover is unimodal or bimodal.

Conclusions

Alternative stable states, tipping points, catastrophic transitions, and early warnings are recurrent issues in many ecological dynamics, and the tree cover variability of moist savannas and tropical forests is not an exception [1], [2]. However, evidences of catastrophic transitions and early warnings of tipping points in natural ecosystems are still elusive [13], [39]. Here we have started our analysis from the observed bimodal frequency distribution of tree cover in moist savannas and tropical forests, which is considered a proof of savanna/forest bistability [1], [2]. We have presented an alternative explanation to the bimodal frequency distribution of tree, which does not require alternative stable states and corresponding catastrophic transitions. Because in these ecosystems fire is one of the main determinants of the vegetation dynamics, dependent on the ecosystem state, and with different impact depending on the tree height, we have used a matrix model to represent the yearly dynamics of trees, considering a matrix when fire occurs, and another matrix when fire does not occur, with feedbacks between fire and trees. We have found that 1) the switching between the two tree dynamics, one with and one without fire, with fire-tree feedbacks, may bring out a bimodal stationary probability distribution of tree cover. The matrix model can be assimilated to a Markov chain allowing to determine the stationary probability distribution of tree cover, which can be interpreted as the distribution of the relative frequency of the visits in each state along a simulation. 2) The spatial sampling can facilitate the observation in frequency of tree cover bimodality. 3) The feedbacks between fire and woody cover are included in the dynamics without necessarily having alternative stable states, contrary to what reported in literature [13]. 4) Sharp transitions between savanna and forest are possible, but these are not necessary catastrophic in the system dynamics sense. This change of perspective about the tree cover bimodality could have profound implications in the management of wet savanna and tropical forest ecosystems. In addition, switching mechanisms between different dynamics could be useful to explain the existence of other emerging behaviors, like the formation of vegetation patterns, as depicted by [40] and [41], or to clarify the vegetation transitions in other ecosystems, for example understanding the findings of [42] in drylands.

Author Contributions

Conceived and designed the experiments: CDM FA. Performed the experiments: FA. Analyzed the data: CDM FA. Contributed reagents/materials/analysis tools: FA. Wrote the paper: CDM. Revised the manuscript: CDM FA.

References

  1. 1. Staver AC, Archibald S, Levin SA (2011) Tree cover in sub-Saharan Africa: Rainfall and fire 326 constrain forest and savanna as alternative stable states. Ecology 92: 1063–1072.
  2. 2. Hirota M, Holmgren M, Van Nes EH, Scheffer M (2011) Global resilience of tropical forest and savanna to critical transitions. Science 334: 232–235.
  3. 3. Favier C, Aleman J, Bremond L, Dubois MA, Freycon V, et al. (2012) Abrupt shifts in African savanna tree cover along a climatic gradient. Glob Ecol Biogeogr 21: 787–797.
  4. 4. Accatino F, De Michele C, Vezzoli R, Donzelli D, Scholes RJ (2010) Tree-grass co-existence in savanna: Interactions of rain and fire. J Theor Biol 267: 235–242.
  5. 5. De Michele C, Accatino F, Vezzoli R, Scholes RJ (2011) Savanna domain in 333 the herbivores-fire parameter space exploiting a tree-grass-soil water dynamic model. J Theor Biol 289: 74–82.
  6. 6. Staver AC, Archibald S, Levin SA (2011) The global extent and determinants of savanna and forest as alternative biome states. Science 334: 230–232.
  7. 7. Grimm V (1994) Mathematical models and understanding in ecology. Ecological Modelling 115: 129–148.
  8. 8. van Nes EH, Scheffer M (2005) A strategy to improve the contribution of complex simulation models to ecological theory. Ecol Model 185: 153–164.
  9. 9. Cochrane MA, Alencar A, Schulze MD, Souza CM, Nepstad DC, et al. (1999) Positive feedbacks in the fire dynamic of closed canopy tropical forests. Science 284: 1832–1835.
  10. 10. Hoffmann WA, Schroeder W, Jackson RB (2002) Positive feedbacks of fire, climate, and vegetation and the conversion of tropical savanna. Geophys Res Lett 29: 2052.
  11. 11. Beckage B, Platt WJ, Gross LJ (2009) Vegetation, Fire, and Feedbacks: A Disturbance-Mediated Model of Savannas. Am Nat 174: 805–818.
  12. 12. Beckage B, Gross LJ, Platt WJ (2011) Grass feedbacks on fire stabilize savannas. Ecol Model 222: 2227–2233.
  13. 13. Schroder A, Persson L, De Roos AM (2005) Direct experimental evidence for alternative stable states: a review. Oikos 110: 3–19.
  14. 14. Beisner BE, Haydon DT, Cuddington K (2003) Alternative stable states in ecology. Front Ecol Environ 1: 376–382.
  15. 15. May RM (1977) Thresholds and breakpoints in ecosystems with a multiplicity of stable states. Nature 269: 471–477.
  16. 16. Rietkerk M, van de Koppel J (1997) Alternate stable states and threshold effects in semi-arid grazing systems. Oikos 79: 69–76.
  17. 17. Scheffer M (2009) Critical transitions in nature and society. Princeton: Princeton University Press.
  18. 18. Salguero-Gomez R, Plotkin JB (2010) Matrix Dimensions Bias Demographic Inferences: Implica-tions for Comparative Plant Demography. Am Nat 176: 710–722.
  19. 19. Salguero-Gomez R, de Kroon H (2010) Matrix projection models meet variation in the real world. J Ecol 98: 250–254.
  20. 20. Buckley YM, Ramula S, Blomberg SP, Burns JH, Crone EE, et al. (2010) Causes and conse-quences of variation in plant population growth rate: a synthesis of matrix population models in a phylogenetic context. Ecol Lett 13: 1182–1197.
  21. 21. Staver AC, Bond WJ, Stock WD, van Rensburg SJ, Waldram MS (2009) Browsing and fire interact to suppress tree density in an African savanna. Ecol Appl 19: 1909–1919.
  22. 22. Higgins SI, Bond WJ, February E, Bronn A, Euston-Brown DIW, et al. (2007) Effects of four decades of fire manipulation on woody vegetation structure in savanna. Ecology 88: 1119–1125.
  23. 23. Hoffmann WA (1999) Fire and population dynamics of woody plants in a neotropical savanna: matrix model projections. Ecology 80: 1354–1369.
  24. 24. Stuart-Hill GC, Tainton NM (1989) The global extent and determinants of savanna and forest as alternative biome states. J Appl Ecol 26: 285–298.
  25. 25. Scholes RJ, Archer SR (1997) Tree-grass interactions in savannas. Annu Rev Ecol Evol S 28: 517–544.
  26. 26. Ward D (2005) Do we understand the causes of bush encroachment in African savannas? Afr J Range Forage Sci 22: 101–105.
  27. 27. Hoffmann WA, Orthen B, Kielse Vargas do Nascimento P (2003) Comparative fire ecology of tropical savanna and forest trees. Funct Ecol 17: 720–726.
  28. 28. Bond WJ (2008) What limits trees in C4 grasslands and savannas? Annu Rev Ecol Evol S 39: 641–659.
  29. 29. do Valle Costa OL, Fragoso MD, Marques RP (2006) Discrete-time Markov jump linear systems. London, UK: Springer.
  30. 30. Dogruel M, Ozguner U (1995) Modeling and stability issues in hybrid systems. In: 383 Proceedings of the 1995 IEEE International Symposium on Intelligent Control. volume 2, pp. 1324–1329.
  31. 31. Gurvits L (1995) Stability of discrete linear inclusion. Linear Algebra Appl 231: 47–85.
  32. 32. Conlisk J (1973) Quick stability checks and matrix norms. Economica 11: 402–412.
  33. 33. Accatino F, De Michele C (2013) Humid savanna-forest dynamics: A matrix model with vegetation-fire interactions and seasonality. Ecol Model 265: 170–179.
  34. 34. van Wilgen BW, Trollope WSW, Biggs HC, Potgeier ALF, Brockett BHB (2003) Fire as a driver of ecosystem variability. In: Du Toit J, Rogers K, Biggs H, editors, The Kruger experience: ecology and management of savanna heterogeneity, Washington DC, USA: Island press. pp. 149–170.
  35. 35. van Wilgen BW (2009) The evolution of fire management practices in savanna protected areas in South Africa. S Afr J Sci 105: 343–349.
  36. 36. Gavin DG, Hu FS, Lertzman K, Corbett P (2006) Weak climatic control of stand-scale fire history during the late Holocene. Ecology 87: 1722–1732.
  37. 37. Whitlock C, Higuera PE, McWethy DB, Briles CE (2010) Paleoecological perspectives on fire ecology: revisiting the fire-regime concept. Open Ecol J 3: 6–23.
  38. 38. Sankaran M, Hanan NP, Scholes RJ, Ratnam J, Augustine DJ, et al. (2005) Determinants of woody cover in African savannas. Nature 438: 846–849.
  39. 39. Boettiger C, Hastings A (2013) From patterns to predictions. Nature 493: 157–158.
  40. 40. Buceta J, Lindenberg K, Parrondo JMR (2002) Pattern formation induced by nonequilibrium global alternation of dynamics. Phys Rev E 66: 036216.
  41. 41. D'Odorico P, Laio F, Ridolfi L (2006) Vegetation patterns induced by random climate fluctuations. Geophys Res Lett 33: L19404.
  42. 42. Bestelmeyer BT, Duniway MC, James DK, Burkett LM, Havstad KM (2013) A test of criti-cal thresholds and their indicators in a desertification-prone ecosystem: more resilience than we thought. Ecol Lett 16: 339–345.