Spores, pollen and dinoflagellates have been recovered from all strata from the Mid-Late Eocene to the Early Pliocene in borehole MC63. The sequence includes the Early-Mid Miocene marine transgression. The Mid-Late Eocene and Oligocene part of the sequence is similar to that of the eastern part of the Basin; there are a few dinoflagellates throughout. The Early-Mid Miocene marine transgression has relatively few spores and pollen but the dinoflagellate flora is diverse. About 30 species of dinoflagellates have been described. The Late Miocene-Early Pliocene part of the sequence is generally similar to that in the Lachlan River Valley. The Late Miocene-Early Pliocene Nothofagus phase, which forms an excellent marker horizon in the river valleys of the western slopes of the Eastern Highlands has been identified here, albeit in a modified form in accordance with the drier climate of this locality.
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Helene A. Martin (1991) studied this question.
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