Fossils present in lower layers of sedimentary rock are older, according to the principle of superposition.
According to the principle of superposition, in a sequence of sedimentary rocks that has not been distorted, each layer of rock is older than the layer above it and younger than the layer below it. As a result, the youngest rocks are at the top and the oldest rocks are at the bottom of a series.
One of the geological laws that geologists use to calculate the relative ages of rock strata or layers, is the law of superposition. According to this theory, rock layers are stacked or deposited one on top of the other. The bottom will have the oldest rock strata and the top will have the youngest.
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