Gradient-flow SDEs have unique transient population dynamics

arXiv stat.ML / 4/2/2026

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Key Points

  • The paper addresses identifiability in stochastic differential equations by showing that, for gradient-flow SDEs, both drift and diffusion can be inferred from temporal marginals without assuming the diffusivity is known.
  • It proves a necessary-and-sufficient condition for identifiability: joint recovery of drift and diffusion is possible if and only if the process is observed outside of equilibrium.
  • Building on this theory, the authors introduce nn-APPEX, a Schrödinger Bridge–based inference method that learns drift and diffusion simultaneously from observed marginals.
  • Experimental results indicate nn-APPEX mitigates bias seen in prior Schrödinger Bridge approaches, which relied on an assumed (and often incorrect) diffusion value.
  • Overall, the work strengthens the theoretical foundations and practical inference of gradient-flow SDEs relevant to domains like machine learning and single-cell biology.

Abstract

Identifying the drift and diffusion of an SDE from its population dynamics is a notoriously challenging task. Researchers in machine learning and single-cell biology have only been able to prove a partial identifiability result: for potential-driven SDEs, the gradient-flow drift can be identified from temporal marginals if the Brownian diffusivity is already known. Existing methods therefore assume that the diffusivity is known a priori, despite it being unknown in practice. We dispel the need for this assumption by providing a complete characterization of identifiability: the gradient-flow drift and Brownian diffusivity are jointly identifiable from temporal marginals if and only if the process is observed outside of equilibrium. Given this fundamental result, we propose nn-APPEX, the first Schrodinger Bridge-based inference method that can simultaneously learn the drift and diffusion of a gradient-flow SDE solely from observed marginals. Extensive experiments show that nn-APPEX's ability to adjust its diffusion estimate enables accurate inference, while previous Schrodinger Bridge methods obtain biased drift estimates due to their assumed, and likely incorrect, diffusion.