By identifying palynomorphs including pollen, spores, dinoflagellate cysts, acritarchs, algae and chitinozoans; we are able to help correlate the well strata and determine the relative age of a significant boundary, horizon, formation or stratigraphical sequence; producing a robust stratigraphic zonation scheme on a single well or field wide project.
By utilising palynology, it is also possible to interpret the palaeoenvironment by examining the changes in total kerogen assemblages (palynofacies).
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