Turning avalanches in schooling fish
The study
A large-statistics empirical analysis of spontaneous turning avalanches — large heading changes propagating across a group — in freely swimming schools (black neon tetra, ; avalanche events). It applies the full condensed-matter/seismology avalanche toolkit and finds scale-free behaviour — power laws, an exponent scaling relation, and data collapses — which it is careful to call a necessary (not sufficient) condition for criticality.
Definition and observables
An individual’s turning rate (angular-velocity magnitude); above a threshold a fish is “active.” An avalanche is a run of consecutive frames with active fish, characterised by duration , size , and interevent time ; the activity rate is the fraction of frames inside an avalanche.
Distributions, scaling relations, collapses
At : (), (), average size with — obeying the crackling-noise scaling relation
and interevent times (). Distributions for different collapse (bar the finite-size tails). At fixed activity rate, duration and interevent-time distributions collapse across ; the interevent times obey the SOC form ; and the avalanche shape obeys — a universal temporal profile.
The key methodological point
The authors are explicit that power laws alone don’t demonstrate criticality (other mechanisms make them); the tighter evidence is the data collapses and the relation between exponents (, the shape collapse), which indicate quantitatively universal avalanche dynamics across scales. With no externally tuned parameter, a near-critical school would be an instance of self-organized criticality.
Boundaries, function, correlations
- Dragon kings. The distribution tails carry over-represented extreme events generated by a different mechanism — tank-wall interactions (large avalanches cluster at corners). Restricting to the tank centre removes them (statistical test: overall vs. centred) and extends the clean power law to ~2 decades.
- Function. Large avalanches occur at the speed minima of the burst-and-coast cycle, temporarily reduce polarization and then recover it — i.e. they are collective decision-making about a new heading (U-turns are a special case). Boundary individuals are the frequent initiators (higher social influence / more risk-exposed).
- Aftershocks. Using seismology’s Gutenberg–Richter (, , ) and an Omori law , correlated aftershocks cluster below a half-turn timescale (~250 frames), with — a faster decay than earthquakes, and no collective memory beyond that timescale.
Why it’s collected here
This is, almost exactly, the empirical protocol for the reorientation-cascade experiment on our own next-set list — turning avalanches, defined by a heading-change threshold, analysed with , , the scaling relation, data collapse and avalanche-shape collapse. Three things to carry straight over: the exponents to compare against (–2, ); the insistence that collapses + exponent relations, not a bare power law, are the real test (the Muñoz/Watkins caution, operationalised); and the dragon-king / boundary lens — our torus has no walls, but the source is a boundary-like attractor, so the same “are the extreme events a different mechanism?” question applies. It also makes turning = collective decision-making, feeding the collective-decision-task idea in our plan.
References
Puy et al. (2024), Phys. Rev. Research 6, 033270 · Múgica et al. (2022), Sci. Rep. 12, 10783 · Poel et al. (2022), Sci. Adv. 8, eabm6385 · Gómez-Nava et al. (2023), Nat. Phys. 19, 663 · Sethna, Dahmen & Myers (2001), Nature 410, 242 · Friedman et al. (2012), Phys. Rev. Lett. 108, 208102 · Muñoz (2018), Rev. Mod. Phys. 90, 031001 · Baiesi & Paczuski (2004), Phys. Rev. E 69, 066106 · Sornette & Ouillon (2012), Eur. Phys. J. Spec. Top. 205, 1.