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ERB102 Depositional Environments Sample 1.10

ERB102 Depositional Environments Sample 1.10

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The primary grain size in the sample stands out. Larger fossils are unmistakably corals, while smaller ones are crinoids, closely related to starfish. Are these organisms situated in their growth position or have they been disassembled and worn away by abrasion? What proof do you see of fossil transportation? What would be the hydrodynamic energy level of the environment and why is this so? The likely depositional environment remains unclear.

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