Planetary Energy Distribution System: Linking Gravitational Energy, Mantle Convection, Plate Tectonics, and the Planetary Dynamo

Planetary Energy Distribution System: Linking Gravitational Energy, Mantle Convection, Plate Tectonics, and the Planetary Dynamo This work presents a conceptual planetary framework describing how gravitational energy functions as the primary energy reservoir driving internal planetary processes including mantle convection, plate tectonics, volcanic systems, and planetary magnetic field generation. Recent seismic tomography studies have revealed the presence of two large thermochemical structures in the lower mantle known as Large Low Shear Velocity Provinces (LLSVP), located beneath Africa and the Pacific Ocean. These structures appear to represent long-lived deep mantle reservoirs that may influence global mantle convection patterns. This study explores the hypothesis that deep mantle structures act as large-scale planetary energy collectors regulating the distribution of internal heat within the Earth. Through mantle plumes, tectonic systems, and volcanic processes, internal planetary energy is transported from the deep mantle toward the surface. To evaluate this hypothesis, a series of conceptual geophysical correlation tests were conducted. These tests examine spatial relationships between deep mantle structures, tectonic systems, magnetic anomalies, heat flow distribution, ocean circulation patterns, atmospheric circulation systems, and biosphere distribution. The proposed conceptual framework does not replace existing geophysical theories such as mantle convection or plate tectonics but instead integrates them into a broader planetary energy distribution model. A simplified mathematical scaling relationship linking gravitational energy, mantle convection intensity, and planetary dynamo strength is also proposed. The conceptual planetary energy distribution model can be summarized as: Gravitational Energy ↓ Internal Planetary Energy Reservoir ↓ Mantle Convection ↓ Deep Mantle Structures (LLSVP) ↓ Mantle Plumes ↓ Plate Tectonics ↓ Volcanic Systems and Surface Heat Flow ↓ Ocean Circulation ↓ Atmospheric Circulation ↓ Planetary Surface Systems This framework suggests that internal planetary dynamics may organize large-scale energy flows within the Earth system over geological timescales. Conceptual Geophysical Tests Included in This Study Antipodal structure of African and Pacific LLSVP Global mantle convection axis African superplume origin Core–mantle boundary heat flux distribution Outer core flow patterns South Atlantic Magnetic Anomaly Geomagnetic dipole drift Magnetic anomalies relative to LLSVP boundaries Global mantle hotspot distribution Global subduction zone distribution Seismic tomography correlations Supercontinent reconstruction relationships Global geoid anomaly patterns Global surface heat flow distribution Atmospheric circulation patterns ENSO region dynamics Tropical cyclone distribution Major ocean current systems Marine biodiversity hotspots Global seismic and volcanic activity Planetary energy scaling model Research Context This work is part of an ongoing independent research effort investigating planetary energy distribution systems and their relation to: • mantle dynamics • deep mantle structures • planetary magnetic field generation • plate tectonics • planetary-scale geophysical processes. The goal of this research program is to explore integrated models that link deep planetary interiors with surface geophysical and environmental systems. Version Note This publication represents the initial version (v1) of an ongoing research project investigating planetary energy distribution systems linking gravitational energy, mantle convection, plate tectonics, and the planetary dynamo. Future versions will include expanded datasets, additional theoretical developments, and supplementary PDF materials extending the present study. This publication represents version 2 (v2) of the ongoing research project investigating planetary energy distribution systems linking gravitational energy, mantle convection, plate tectonics, and planetary dynamo processes. This version includes revisions and improvements to the conceptual framework presented in the initial release.