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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The type locality of the Citronelle formation, as designated by Matson in 1916, is significant mainly because of the exposure of plant-bearing clays near Lamberts Station about 5 miles south of Citronelle, Alabama. The flora from these clays was correlated with the Pliocene by Berry. Recent studies have shown that these clays are faulted and overlain unconformably by the sands of the so-called Citronelle formation. The structural evidence indicates that the clays are older than the sands so that the flora of the clays can not be used to correlate the sands. It is suggested that the term Citronelle, as a formation name, be dropped.
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