This work defines thresholds for molecular stability and complexity across cosmic and chemical domains, linking environmental factors.
Chemical complexity requires environments in which molecular interactions can persist long enough to form stable reaction networks. This work defines pre-chemical closure as a set of physical persistence thresholds spanning cosmic dust formation, planetary stabilization, and environmental shielding. Together, these thresholds enable molecular stability, collision-driven reactions, and the accumulation of chemical complexity without invoking specific biochemical pathways. The proposed framework integrates established results from astrophysics, planetary science, and chemistry into a cross-scale persistence model linking large-scale structure formation to chemical closure conditions. Within this model, a closure functional and a transition operator are introduced as formal devices representing threshold-gated admissibility between closure layers. These devices allow domain-specific models to be unified within a common structure while remaining fully compatible with established physical laws. This work does not propose new chemical pathways or origin-of-life mechanisms. Instead, it formalizes the environmental conditions required for chemical persistence, providing a structural bridge between astrophysical processes and chemical complexity. By expressing persistence thresholds in a unified framework, the model supports quantitative testing across observational and laboratory domain
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John Francis Osborne (2026) studied this question.
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