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In geology, a biofacies refers to a portion of a rock layer where the fossil content, meaning the types of fossilized plants and animals, differs significantly from other parts of the same layer. This concept is a type of sedimentary facies, which describes the physical, chemical, and biological characteristics of a rock bed. Sedimentary facies are formed by the accumulation of sediments and can vary laterally based on depositional environments. Biofacies specifically highlight the biological attributes, using fossils to define these variations within rock sequences. Understanding biofacies helps geologists interpret past environments and the history of life within those environments.12

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