NASA uncovers 540‑million‑year magnetic rhythm affecting oxygen levels
Using advanced satellite data and geological records, researchers discovered that fluctuations in Earth’s magnetic field strength correlate with a long-term cycle of weakening and strengthening. These magnetic cycles appear to directly affect the shielding of Earth from solar radiation and cosmic rays. When the magnetic field is strong, the planet is better protected, allowing more stable and oxygen-rich atmospheric conditions. Conversely, weaker magnetic phases may expose Earth to more solar particles, triggering changes in climate and possibly reducing global oxygen levels.
Remarkably, this 540-million-year magnetic rhythm aligns with major biological and environmental shifts, including mass extinctions and the rise of new life forms. The Cambrian explosion, for instance — when a massive diversification of life occurred — took place around the time of a magnetic field peak. The findings suggest a deeper planetary feedback loop where deep Earth processes, like the movement of molten iron in the core, could have governed atmospheric chemistry and biological evolution over hundreds of millions of years.
NASA’s discovery provides a new lens to understand Earth’s complex history, not only in terms of tectonic and biological evolution but also its magnetic behavior. This adds a crucial layer to our understanding of planetary habitability and may even help identify habitable exoplanets by analyzing their magnetic fields.
As researchers continue to explore the interaction between Earth's core dynamics and its atmosphere, this revelation reinforces the magnetic field's vital role as Earth's invisible shield — a force that has subtly steered the course of life for eons.
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