The application of micropalaeontology consists of the identification of foraminifera, diatoms, radiolaria and ostracods.
It is used to determine the relative age of a significant boundary, horizon, formation or stratigraphical sequence. As with all biostratigraphic disciplines, when combined with palynology and/or nannopalaeontology; it is possible to achieve a powerful biostratigraphic correlation and high resolution stratigraphic breakdown.
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