Detailed sampling of Palaeogene sediments from Barbados has resulted i
n the rediscovery of the type locality of the rare siliceous dinoflage
llate Peridinites. Electron microscopic examination has revealed that
Peridinites can only be interpreted as the remains of dinoflagellate m
otile thecate cells, rather than hypnozygotic cysts; it thus represent
s the first unequivocal example of a fossil dinoflagellate theca. Dino
flagellate cysts have also been found and identified as belonging to L
ithoperidinium. Both Peridinites and Lithoperidinium are valid genera,
and are interpreted as being primarily silicified. Peridinites is thu
s the only known dinoflagellate capable of secreting siliceous thecal
plates.