Shale itself is a clastic sedimentary rock composed of mud that is a mix of flakes of clay minerals and tiny fragments of other minerals, especially quartz and calcite. The unique quality of shale is its ability to preserve delicate organic structures that would be destroyed in coarser-grained rocks like sandstone. When these fine layers of mud solidified under pressure, they captured snapshots of the seafloor ecosystem. In "Tube Shale" formations, the most prominent features are the mineralized or organic tubes created by ancient organisms, such as polychaete worms or other early annelids.
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