An analysis of geological proxy records shows that Earth’s atmospheric oxygen levels and geomagnetic field strength evolved in parallel over the past 540 million years. The study compares reconstructions of atmospheric oxygen concentration with the virtual geomagnetic axial dipole moment, a standard proxy for the intensity of Earth’s magnetic field at the surface, and identifies a strong correlation at long timescales.
Both datasets display near-linear increasing trends throughout the Phanerozoic, along with a pronounced surge between approximately 330 and 220 million years ago. Correlation coefficients reach 0.72 for the full records when no time lag is applied, indicating synchronous long-term behavior.
After removal of linear trends, the correlation remains strong, with coefficients exceeding 0.64 and time offsets of less than 1 million years, which fall within the temporal resolution limits of the proxy data.
Filtering the records to isolate shorter-period variability shows that the relationship weakens substantially at timescales below about 20 million years. Spectral analysis suggests that atmospheric oxygen proxies contain far less high-frequency power than geomagnetic field reconstructions, consistent with oxygen being governed by slower, integrative Earth-system processes.
As a result, the correlation strengthens steadily as longer band-pass filter windows are applied, reaching its highest values at periods approaching 100 million years and longer.
To assess whether the observed correlation could arise by chance from autocorrelated time series, the authors generated large ensembles of synthetic oxygen records that preserve the statistical structure of the proxy data. Monte Carlo testing places the observed correlation in the 99.9th percentile of expected values, even after detrending and the introduction of additional noise, indicating that the relationship is statistically robust.
NASA scientists summarizing the research noted that measured oxygen escape rates are far too low for geomagnetic shielding alone to account for long-term atmospheric oxygen changes, reinforcing the conclusion that both records reflect deeper planetary processes rather than direct atmospheric control.
The study evaluates and largely dismisses the hypothesis that a stronger geomagnetic field directly regulates atmospheric oxygen by suppressing the escape of oxygen to space. Estimates of modern and long-term oxygen ion escape rates are several orders of magnitude smaller than oxygen source and sink fluxes associated with magmatic degassing, organic carbon burial, and weathering.
The magnitude of geomagnetic field variability observed during the Phanerozoic is insufficient to alter escape rates enough to measurably affect atmospheric oxygen levels.
Instead, the authors identify deep Earth processes as a more plausible common influence on both variables. The long-term strengthening of the geomagnetic field may reflect the onset and progression of solid inner core growth, which enhances compositional buoyancy and drives more vigorous convection in Earth’s liquid core. This mechanism would naturally produce an increase in geomagnetic field intensity over hundreds of millions of years.
The late Paleozoic peak shared by both atmospheric oxygen and geomagnetic field strength coincides with the assembly and persistence of the supercontinent Pangea and with the Kiaman Reversed Polarity Superchron. Supercontinent formation alters heat-flow patterns across the core–mantle boundary and can impose long-lived thermal heterogeneity on the geodynamo, thereby influencing both magnetic field intensity and polarity.
At the surface, the same tectonic configuration affects weathering rates, volcanic degassing, and the global redox balance, all of which influence atmospheric oxygen over comparable geological timescales. Coupled interior and surface processes operate slowly enough that their effects would not necessarily produce an observable lag between geomagnetic and oxygen records.
The authors note that current long-term Earth system models typically treat the geomagnetic field as static or external and do not incorporate its evolution or coupling to mantle dynamics. The observed correlation shows a gap in integrated modeling of Earth’s interior and surface environments and points to the need for coupled simulations capable of resolving interactions across the core, mantle, crust, and atmosphere over geological time.
References:
1 Strong link between Earth’s oxygen level and geomagnetic dipole revealed since the last 540 million years – Weija Kuang et al. – Science Advances – June 13, 2025 –
DOI: 10.1126/sciadv.adu882 – OPEN ACCESS