Earth’s earliest lands, hot and hellish, were sheltered from above. Researchers have found more evidence that our planet had a strong magnetic field 4.2 billion years ago, three-quarters of a billion years earlier than previously thought and just 350 million years after the Earth formed. The field would have shielded Earth, protecting its atmosphere from being stripped away by high-energy particles from the sun—and perhaps helping life gain a foothold.
With few surviving rocks to study, geologists struggle to reconstruct the time known as the Hadean, which ran from 4.55 billion years ago to 4 billion years ago. But fragmentary—and controversial—clues can be found in younger, 3-billion-year-old rocks from the Jack Hills of Western Australia. These rocks contain tiny crystals of a hardy mineral called zircon, which are chips off an even older block: 4.2-billion-year-old Hadean rocks that formed from cooling magma.
The crystals also preserve evidence of an ancient magnetic field, according to an international team led by John Tarduno, a geophysicist at the University of Rochester, New York. Not all researchers are convinced by the result, because it would push back the accepted birth date of Earth’s magnetic field by 750 million years. “There’s been a large research group trying to prove our results wrong,” says Tarduno. “That’s part of science.”
Tarduno’s team says the magnetization was imprinted 4.2 billion years ago, when the original zircon-containing rock first cooled. However, if the magnetite grains, at any point in their history, became hot enough—above about 600°C—they would have lost the magnetic alignment and gained a new one as they cooled down again. And just such a heating event may have occurred about 2.6 billion years ago, says Benjamin Weiss, a geologist at the Massachusetts Institute of Technology (MIT) and leader of a group that has challenged Tarduno’s claims. “These zircons have mind-bogglingly long and largely unknown histories,” he says.
What’s more, the single zircon crystal that did show signs of heating is an outlier in another way: It preserves an unusually weak magnetic signal. In 2015 Tarduno and his colleagues concluded this might be evidence of a strangely variable magnetic field 4.2 billion years ago. But now, he says, it seems that this particular zircon gained its magnetism later, and its weak signal can be ignored in discussions of Earth’s earliest magnetic field. Doing so, says Tarduno, suggests Hadean Earth actually had a magnetic field, and a churning dynamo in its core, as strong as the one operating today.
Mark Harrison, a geologist at the University of California, Los Angeles, isn’t convinced by the new analysis, because it takes both high temperatures and long periods of time for the lithium ions to diffuse across a boundary. If a heating incident brought the zircons above 600°C but persisted for only 10,000 years—a blink of an eye for a geologist—it would be enough time to reset the zircons’ magnetism but not to diffuse lithium. “I don’t think this is even remotely smoking gun evidence,” he says.