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Explores future-boundary influence across quantum, geological, and classical-memory protocols, suggesting new insights into time symmetry.
The asymmetry of causation, according to which physical influences propagate from past events to future events, remains deeply embedded in scientific reasoning. Time-symmetric formulations of quantum mechanics, including the Two-State Vector Formalism (TSVF), challenge the assumption that initial conditions alone provide a complete description of physical systems. Motivated by TSVF and by broader retrocausal interpretations, this paper proposes three falsifiable protocols for testing possible future-boundary influence. Experiment 1 investigates whether weak-measurement records exhibit statistically significant correlations with later postselection conditions in a delayed-choice optical architecture. Experiment 2 evaluates geological asymmetry using impact, extinction, geomagnetic, and large-igneous-province datasets through a predefined correlation-asymmetry statistic near a hypothesized 36 Myr lag. The geological protocol is subject to intrinsic power limitations, as the Phanerozoic record contains only approximately fifteen cycles of the hypothesized 36 Myr period. Experiment 3 examines whether protected classical memory records remain independent of a later quantum-random decision, thereby establishing upper bounds on any putative retrocausal extension beyond standard laboratory TSVF applications. The paper does not claim that retrocausality has been demonstrated; it formulates quantitative null hypotheses, significance criteria, replication requirements, and upper-bound methodologies.
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Denis Saklakov (2026) studied this question.
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