Earth's first dinner party wasn't impressive, just a bunch of soft-bodied Ediacaran organisms sunk into sediment on the ocean floor, sharing in scraps of organic matter suspended in the water around them.
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Artistic reconstruction of a gregarious community of Ernietta [Credit: Dave Mazierski] |
Paleontologist Simon A.F. Darroch, assistant professor of earth and environmental sciences at Vanderbilt University, and Brandt M. Gibson, a Ph.D. student, developed a series of computational fluid dynamics simulations demonstrating that not only were some of the Ediacara biota suspension feeders, trapping nutrients in deep cavities, but that they oriented themselves within flow currents to amplify eddies as water moved around them. That meant more food being sent into each creature's cavity.
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Well preserved Ernietta with bottom suture and individual modules visible [Credit: Charlotte Kenchington] |
The team used fossil evidence gathered near Bethanie, Namibia, and plans to return to the African nation this summer to study and photograph other samples. Their recent work builds on Darroch's findings last year that Ediacara biota were forming complex communities tens of millions of years before the Cambrian explosion.
"For hundreds of years, we've just stared at the fossils themselves and made judgments on what we believe they're related to," he said. "But Brandt is focused on these unusual bizarre shapes and morphologies and said, 'What if these evolved as a way of dealing with life in moving fluids.'
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Turbulent energy flowlines in multi-model CFD simulation showing recirculating turbulent patterns within and downstream of Ernietta cavities [Credit: Dave Mazierski] |
"They are behaving like animals, and that's a link between them and what we recognize as animals."
The research is published in the journal Science Advances.
Source: Vanderbilt University [June 19, 2019]
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