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A walk through poppy seeds yields a model for paleontology

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Posted December 11, 2014

What could a guineafowl strolling through a bed of poppy seeds have to do with a dinosaur footprint made 200 million years ago?

Fossilized footprints: Highly specialized X-ray technology and substrate simulation allow researchers to study the 3-D profile left by an animal walking in a soft medium. What they learn from modern animals helps researchers read the fossil record left by moving animals hundreds of millions of years ago. Screenshot from video below. Credit: Gatesy lab/Brown University

Fossilized footprints: Highly specialized X-ray technology and substrate simulation allow researchers to study the 3-D profile left by an animal walking in a soft medium. What they learn from modern animals helps researchers read the fossil record left by moving animals hundreds of millions of years ago. Screenshot from video below. Credit: Gatesy lab/Brown University

Stephen Gatesy, professor of ecology and evolutionary biology at Brown, and his former postdoctoral fellow Peter Falkingham, now at the Royal Veterinary College in the United Kingdom, used measurements from X-ray videos of the 3-D foot movement of a chicken-like bird as an input for a computer simulation of a substrate of poppy seeds. In this way, they could visualize the displacement of seeds through time and study the “birth” of tracks at different depths. The researchers then used the model to clarify previously unexplained features of a Jurassic dinosaur track.

Gatesy described a video summarizing the approach: “On the left, a guineafowl walking through poppy seeds is captured by high-speed (250 fps) video using X-ray and standard light imaging. Three-dimensional bone models have been registered by X-ray Reconstruction of Moving Morphology (XROMM) and overlaid on both videos. On the right are animations of our particle simulation produced using the real foot motion by the discrete element method (DEM). Simulations enable visualization of how footprints form at any depth through interaction among foot shape, foot movement, and substrate properties. In this dry, sand-like material, very clear tracks are preserved below the surface, but these reflect foot entry and exit rather than static anatomy. Relating track features to formation dynamics helps explain the origin of track diversity in the fossil record and aids reconstruction of dinosaur locomotion.”

More information about the study, which appears the week of December 8 in the Proceedings of the National Academy of Sciences, is available online.

Source: Brown University

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