Mysterious Radioactive Anomaly Under the Pacific Ocean

Thursday 20 February 2025
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Scientists have discovered a radioactive anomaly deep beneath the Pacific Ocean, marked by a surge in Beryllium-10, dating back 9–12 million years. This finding could reshape our understanding of Earth's geological and cosmic history, with potential links to ocean currents or cosmic events.

Mysterious Radioactive Anomaly Discovered Deep Under The Pacific Ocean

A peculiar radioactive anomaly has been detected deep beneath the Pacific Ocean, puzzling scientists and raising new questions about Earth's geological and cosmic history. Researchers in Germany, analyzing thin layers of seafloor crust, have identified a sudden surge in the radioactive isotope Beryllium-10, dating back approximately 9–12 million years.

The anomaly was discovered in seabeds of the Central and Northern Pacific, but scientists suspect it may extend across the entire ocean, possibly even the globe. Led by physicist Dominik Koll of the Helmholtz-Zentrum Dresden-Rossendorf research institute, the study suggests several possible explanations for this mysterious radioactive blip.

The Source of the Beryllium-10 Surge

Beryllium-10 is a radioactive isotope continuously produced when cosmic rays interact with Earth's atmosphere. Over time, it settles into the ocean and integrates into slow-growing, metal-rich crusts on the seafloor. Scientists believe that more than 9 million years ago, a major shift in ocean currents could have led to an increased deposition of Beryllium-10 in the Pacific. Alternatively, the surge may have been triggered by a cosmic event, such as a nearby supernova or the Solar System’s passage through an interstellar cloud, both of which could have intensified cosmic ray activity.

Unlocking Earth's Geological Timeline

Ferromanganese crusts, where Beryllium-10 accumulates, serve as geological archives, preserving millions of years of ocean chemistry in just a few millimeters. Unlike carbon dating, which is limited to about 50,000 years, Beryllium-10’s half-life of 1.4 million years allows scientists to date oceanic crusts spanning up to 10 million years. This makes it a crucial tool in deciphering Earth’s past.

The research team found an unexpected anomaly in their Pacific Ocean samples, with nearly twice the amount of Beryllium-10 than anticipated. This discovery presents a new geological marker that could serve as a reference point for future studies on Earth's history.

The Mystery Deepens

Further studies are required to determine whether this anomaly was a localized event caused by changes in ocean circulation or a global phenomenon influenced by cosmic activity. Scientists plan to analyze additional samples to gain a clearer understanding of this unique discovery. If confirmed as a global event, it could reshape our understanding of Earth’s interaction with the cosmos and past environmental shifts.

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