Ancient Rocks Hold Clues to How Earth Avoided a Mars-Like Fate

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Ancient Rocks Hold Clues to How Earth Avoided a Mars-Like Fate
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New paleomagnetic research suggests Earth’s solid inner core formed 550 million years ago and restored our planet’s magnetic field. Swirling liquid iron in the Earth’s outer core, located approximately 1,800 miles beneath our feet, generates our planet’s protective magnetic field, called the magn

A depiction of Earth, first without an inner core; second, with an inner core beginning to grow, around 550 million years ago; third, with an outermost and innermost inner core, around 450 million years ago. University of Rochester researchers used paleomagnetism to determine these two key dates in the history of the inner core, which they believe restored the planet’s magnetic field just before the explosion of life on Earth.

However, about 565 million years ago, the magnetic field’s strength dropped to 10 percent of its strength today. Then, mysteriously, the magnetic field bounced back, regaining its strength just before the Cambrian explosion of multicellular life on Earth.This rejuvenation happened within a few tens of millions of years according to new research from scientists at the University of Rochester.

Because of the magnetic field’s relationship to Earth’s core, scientists have been attempting for decades to ascertain how Earth’s magnetic field and core have changed throughout our planet’s history. They cannot directly measure the magnetic field due to the location and extreme temperatures of materials in the core.

“Because we constrained the inner core’s age more accurately, we could explore the fact that the present-day inner core is actually composed of two parts,” Tarduno says. “Plate tectonic movements on Earth’s surface indirectly affected the inner core, and the history of these movements is imprinted deep within Earth in the inner core’s structure.

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