Abstract
Abstract Diverse palynomorph assemblages of late early Miocene age were obtained from 19 conventional core samples taken from the Robulus “L”; #2 and #5 sands of Texaco Well #6, located offshore Vermilion Parish, Louisiana. Approximately 60 dinocyst, 100 miospore and 17 fungal spore taxa were recovered. Seven palynofacies were defined in the sands. These palynofacies are characterized sedimentologically by lithofacies distribution and palynologically by dinocyst distribution. The depositional sequences of the Robulus “L” sands were the result of cyclic deposition influenced by high energy events.
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