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Paleontologists have found more than 260 dinosaur footprints from the Early Cretaceous Period in Brazil and Cameroon, now more than 3,700 miles (6,000 kilometers) apart on opposite sides of the Atlantic Ocean.

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“One of the youngest and narrowest geological connections between Africa and South America was the elbow of northeastern Brazil nestled against what is now the coast of Cameroon along the Gulf of Guinea,” Jacobs said. “The two continents were continuous along that narrow stretch, so that animals on either side of that connection could potentially move across it.”

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But before this gradual change took place, different types of basins formed as Earth’s surface pulled apart. Rivers fed into the basins, forming lakes, Jacobs said.

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“A half graben is an elongate basin formed by pulling apart of the Earth’s surface with a fault forming on one side such that the bottom of the valley tilts down toward the fault along which movement is occurring,” Jacobs said by email. “Hold your hand in front of you. Tilt your fingers down, representing movement along the fault. Rivers will flow down the valley and deposit sediments and sediments will be eroded from the high side of the valley.”

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“Plants fed the herbivores and supported a food chain,” he said. “Muddy sediments left by the rivers and lakes contain dinosaur footprints, including those of meat-eaters, documenting that these river valleys could provide specific avenues for life to travel across the continents 120 million years ago.”

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“Dinosaur tracks are not rare, but unlike the bones usually found, footprints are the proof of dinosaur behavior, how they walked, ran or otherwise, who they walked with, what environment they walked through, what direction they were going, and where they were when they were doing it,” Jacobs said.

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It’s difficult to tell the specific species of dinosaurs that traveled along the basins, but they represent a larger portrait of the ancient climate and how different types of animals thrived in the environment that the continental rifting created.

“If your dog and a coyote walk across the same mudflat, you might know that two dog critters walked there, that they are very similar, but you may not be able to know if they are different species. Ditto the dinosaur track situation,” Jacobs said. “All animals have home ranges. All animals expand their ranges. All animals exploit resources as necessary depending on availability, often related to seasonality. Herbivores follow nutritious plants; carnivores follow their herbivorous food.”

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“Imagine a lush, open basin with vegetation for the herbivores and carnivores following,” said study coauthor Lawrence Flynn, assistant director for the American School of Prehistoric Research and lab safety coordinator within the department of human evolutionary biology at Harvard University. “If nobody is there on the ‘new’ turf, then animals will disperse into it, given no competition.”

Later, once the continents drifted apart, this disruption likely caused a break in genetic continuity, a key driver of evolution, Jacobs said.

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Jacobs then became friends with study author Ismar de Souza Carvalho, now a professor within the department of geology at the Federal University of Rio de Janeiro. Jacobs was studying dinosaur movements from the African side, while Carvalho was studying them from the Brazilian side.

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“We wanted to put new and evolving geological and paleontological evidence together to tell a story more specifically of where and why and when dispersals between the continents happened,” Jacobs said.

“One beauty of this Earth is that any of us can see that Africa and South America used to fit together like puzzle pieces. It is easy to conceive that in a connected world, animals, including dinosaurs, could and would be likely to move from place to place.”

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