Biostratigraphy

Biostratigraphy is a branch of stratigraphy that uses fossil content to correlate and determine the relative ages of strata. Its basic units are biozones; you

Biozones or biostratigraphic zones are the fundamental units for naming and classifying stratigraphic sections based on their fossil content. There are five biozones: range (taxon-range,

Biostratigraphic correlation (biocorrelation) involves subdividing larger fossiliferous stratigraphic units into small-scale units or biozones based on fossil content and using these zones to match local,

Biostratigraphy is a part of stratigraphy that studies the distribution of fossils in a stratigraphic record. It uses these fossils to subdivide, organize, and classify