Calcareous nannofossils and paleoenvironments of the Paleocene-Eocene thermal maximum (PETM) interval in central Egypt
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文摘

I studied the Paleocene/Eocene transition in central Egypt.

Four surface sections have been investigated.

The turnover of the calcareous nannofossils was investigated.

The RD assemblage well exist at the transition sequence.

Fasciculithus has it's LAD in the lower part of NP10.

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