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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| Sprache: | Englisch |
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2026
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| _version_ | 1866901416336949248 |
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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 |