A biozone is a stratigraphic unit defined by the presence of specific fossil species within a particular rock layer, helping geologists and paleontologists correlate the age of strata across different locations. Biozones are crucial for understanding the distribution of organisms in time and space, and they are particularly useful in biostratigraphy for dating rock layers and correlating fossil records. By identifying biozones, scientists can gain insights into past environmental conditions and the evolutionary history of life on Earth.
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