Abstract
Endolithic organisms that live inside rocks, shells and wood use two processes, bioerosion and embedment, to produce boring and bioclaustration residential cavities. In the trace fossil record, borings and bioclaustrations preserve the distinctive and often stereotypic activity of particular endolithic organisms, thereby linking important biological and ecological information to this special group of trace fossils. In order to use these fossils to study aspects of evolutionary paleoecology, an ecologically-significant framework is needed to logically group and subdivide hard substrate trace fossils.
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