Abstract

The presence of self-organized criticality in biology is often evidenced by a power-law scaling of event size distributions, which can be measured by linear regression on logarithmic axes. We show here that such a procedure does not necessarily mean that the system exhibits self-organized criticality. We first provide an analysis of multisite local field potential (LFP) recordings of brain activity and show that event size distributions defined as negative LFP peaks can be close to power-law distributions. However, this result is not robust to change in detection threshold, or when tested using more rigorous statistical analyses such as the Kolmogorov–Smirnov test. Similar power-law scaling is observed for surrogate signals, suggesting that power-law scaling may be a generic property of thresholded stochastic processes. We next investigate this problem analytically, and show that, indeed, stochastic processes can produce spurious power-law scaling without the presence of underlying self-organized criticality. However, this power-law is only apparent in logarithmic representations, and does not survive more rigorous analysis such as the Kolmogorov–Smirnov test. The same analysis was also performed on an artificial network known to display self-organized criticality. In this case, both the graphical representations and the rigorous statistical analysis reveal with no ambiguity that the avalanche size is distributed as a power-law. We conclude that logarithmic representations can lead to spurious power-law scaling induced by the stochastic nature of the phenomenon. This apparent power-law scaling does not constitute a proof of self-organized criticality, which should be demonstrated by more stringent statistical tests.

Highlights

  • Many natural complex systems, such as earthquakes or sandpile avalanches, permanently evolve at a phase transition point, a type of dynamics called self-organized criticality (SOC) [1,2]

  • The detected local field potential (LFP) negative peaks are clearly related to neuronal firing, as evidenced by the wave-triggered average (WTA) of the unit activity

  • The same procedure was repeated for all channels, leading to rasters of negative peaks of the LFPs (nLFPs) activity (Fig. 2, bottom)

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Summary

Introduction

Many natural complex systems, such as earthquakes or sandpile avalanches, permanently evolve at a phase transition point, a type of dynamics called self-organized criticality (SOC) [1,2]. One of the signatures of such critical states is that the size of the avalanches is distributed as a power law, which is interesting for the scale invariance it presents (more precisely, if the probability of observing value x for a given variable is a power-law, p(x)~ax{a, scaling x by a constant factor yields to a proportional law: p(c x)~ac{ax{a). Another notable property is the universality of power-laws in physical phenomena such as phase transitions. Diverse systems show the same critical exponent as they approach criticality, indicating the same fundamental dynamics

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