Unifying deterministic and stochastic ecological dynamics via a landscape-flux approach

TL;DR

This paper introduces a landscape-flux framework that combines deterministic and stochastic ecological dynamics to analyze stability, transitions, and the emergence of new states like grasslands under fluctuations.

Contribution

The landscape-flux approach unifies deterministic and stochastic models, revealing new quasi-stable states and providing quantitative measures of stability and bifurcations in ecological systems.

Findings

Identification of a new Grassland state under fluctuations

Analysis of flux and entropy production near bifurcations

Quantitative measures for ecological stability and transitions

Abstract

We develop a landscape-flux framework to investigate observed frequency distributions of vegetation and the stability of these ecological systems under fluctuations. The frequency distributions can characterize the population-potential landscape related to the stability of ecological states. We illustrate the practical utility of this approach by analyzing a forest-savanna model. Savanna, and Forest states coexist under certain conditions, consistent with past theoretical work and empirical observations. However, a new Grassland state, unseen in the corresponding deterministic model, emerges as an alternative quasi-stable state under fluctuations, providing a novel theoretical basis for the appearance of widespread grasslands in some empirical analyses. The ecological dynamics are determined by both the population-potential landscape gradient and the steady-state probability flux. The flux quantifies the net input/output to the ecological system and therefore the degree of nonequilibriumness. Landscape and flux together determine the transitions between stable states characterized by dominant paths and switching rates. The intrinsic potential landscape admits a Lyapunov function, which provides a quantitative measure of global stability. We find that the average flux, entropy production rate, and free energy have significant changes near bifurcations under both finite and zero fluctuation. These may provide both dynamical and thermodynamic origins of the bifurcations. We identified the variances in observed frequency time traces, fluctuations and time irreversibility as kinematic measures for bifurcations. This new framework opens the way to characterize ecological systems globally, to uncover how they change among states, and to quantify the emergence of new quasi-stable states under stochastic fluctuations.