GCST Framework for Ocean Worlds, Galactic Stability, and Cosmological Complexity Limits Planets-Oceans as Long-Lived Resonators of Complexity in the Universe

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1. Verfasser: Lukin, Roman
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Sprache:Englisch
Veröffentlicht: Zenodo 2026
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author Lukin, Roman
author_facet Lukin, Roman
contents <p>Abstract <br> <br>Ocean worlds — including subsurface ocean moons and Hycean-type exoplanets — represent a special class of planetary systems with exceptional thermodynamic longevity. Within Global Complexity Stability Theory (GCST) and Optimal System Dynamics (OSD v1.2), such worlds can be viewed as large-scale dissipative structures capable of sustaining complex self-organizing processes over extremely long timescales. <br> <br>The dynamics of instability are governed by the field equation: <br> <br>∂Ψ/∂t = D ∇² Ψ + C α − γ Ψ <br> <br>with stability condition γ / (α C) > 1. <br> <br>Ocean planets operate in the deeply stable regime α ≪ 1, γ ≫ 1, making them natural attractors of long-lived complexity. Extending GCST to galactic and cosmological scales reveals hierarchical bounds on complexity: C_max ∝ γ / α at each level. A unified scale-invariant GCST equation emerges, while the variational principle, entropy law, evolution law, phase transitions, and information principle complete a self-consistent theoretical framework for the emergence and limits of complexity across cosmic scales. </p>
format Recurso digital
id zenodo_https___doi_org_10_5281_zenodo_18916767
institution Zenodo
language eng
publishDate 2026
publisher Zenodo
record_format zenodo
spellingShingle GCST Framework for Ocean Worlds, Galactic Stability, and Cosmological Complexity Limits Planets-Oceans as Long-Lived Resonators of Complexity in the Universe
Lukin, Roman
GCST,
ocean worlds,
subsurface oceans,
Hycean planets,
galactic stability bound,
cosmological complexity limit,
scale-invariant GCST equation,
GCST action principle,
GCST entropy law,
GCST evolution law,
GCST phase transitions,
GCST information principle,
dissipative structures,
long-lived complexity,
planetary resonators,
cosmic evolution of complexity,
<p>Abstract <br> <br>Ocean worlds — including subsurface ocean moons and Hycean-type exoplanets — represent a special class of planetary systems with exceptional thermodynamic longevity. Within Global Complexity Stability Theory (GCST) and Optimal System Dynamics (OSD v1.2), such worlds can be viewed as large-scale dissipative structures capable of sustaining complex self-organizing processes over extremely long timescales. <br> <br>The dynamics of instability are governed by the field equation: <br> <br>∂Ψ/∂t = D ∇² Ψ + C α − γ Ψ <br> <br>with stability condition γ / (α C) > 1. <br> <br>Ocean planets operate in the deeply stable regime α ≪ 1, γ ≫ 1, making them natural attractors of long-lived complexity. Extending GCST to galactic and cosmological scales reveals hierarchical bounds on complexity: C_max ∝ γ / α at each level. A unified scale-invariant GCST equation emerges, while the variational principle, entropy law, evolution law, phase transitions, and information principle complete a self-consistent theoretical framework for the emergence and limits of complexity across cosmic scales. </p>
title GCST Framework for Ocean Worlds, Galactic Stability, and Cosmological Complexity Limits Planets-Oceans as Long-Lived Resonators of Complexity in the Universe
topic GCST,
ocean worlds,
subsurface oceans,
Hycean planets,
galactic stability bound,
cosmological complexity limit,
scale-invariant GCST equation,
GCST action principle,
GCST entropy law,
GCST evolution law,
GCST phase transitions,
GCST information principle,
dissipative structures,
long-lived complexity,
planetary resonators,
cosmic evolution of complexity,
url https://doi.org/10.5281/zenodo.18916767