The presence of diverse Eocene dinoflagellate assemblages in addition to intertidal sediments suggests that portions of the coal-bearing Latrobe Group were deposited in marginal-marine/tidal settings! #FossilFriday #Palynology #NewResearch pic.twitter.com/itWS5WeaD2— Vera Korasidis (@VeraKorasidis) May 10, 2019
Sunday, May 12, 2019
Past organisms living on sediments
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