MICROPALEONTOLOGIA DA FAIXA SEDIMENTAR COSTEIRA RECIFE - JOÃO PESSOA

IVAN DE MEDEIROS TINOCO

Resumo


In the investigated area, the author finds two foraminiferal assemblages. First, a Globotruncana contusa-stuarti assemblage, characteristic of the Maestrichtian in the whole world and present in the Gramame Formation. In the phosphatic facies of this formation occurs also Fallotia santosae. Second, a Globigerina pseudobulloides-triloculinoides and Chilloguembelina assemblage is found in the Maria Farinha Formation, being typical of the Paleocene. The other formations are without microfossils.

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