Together, the genetic data and archaeological evidence suggest maize moved out of Mexico in two waves. After it was domesticated from parviglumis in the Balsas River Basin in what is now the state of Guerrero about 9000 years ago, maize quickly spread south along the Pacific coast, reaching Panama by 7800 years ago and Peru by 6700 years ago. The ancient cob from Peru was the result of this first wave. Then, starting about 6000 years ago, maize moved up into Mexico’s highlands, where it crossed with the local mexicana teosinte.
Shortly after, this new hybrid maize exploded out of central Mexico, mixing with or replacing every first-wave variety in Central and South America. It also headed north, reaching the southwestern U.S. about 4000 years ago. It all amounts to “a much more complete panorama of maize’s evolutionary history,” says co-author Miguel Vallebueno-Estrada, a paleogenomicist at the Gregor Mendel Institute of Molecular Plant Biology.
Just why the new hybrid varieties spread so widely is a mystery. “It made sense that introgression from mexicana was important for adaptation to the highlands,” says Maud Tenaillon, a population geneticist who studies maize at CNRS, France’s national research agency, and Paris-Saclay University. “But that it’s everywhere—it’s something no one would have guessed.”
One would think “this new maize must have had an incredible advantage” over firstwave varieties, Tenaillon says. But that’s not what Ross-Ibarra’s team found. Genetic analyses and ancient cobs show first-wave maize already had large ears, soft kernels, and other desirable traits that differentiate maize from teosinte. The researchers identified a few possible advantages in second-wave maize, including slightly bigger cobs, more kernels per row, and the ability to withstand more hours of sunlight, which could have helped as it moved north and south to places with long summer days. But nothing stands out as truly transformative. “Frustratingly, we don’t have a smoking-gun answer,” Ross-Ibarra says.
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