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dinocyst
Dinocysts or dinoflagellate cysts are typically 15 to 100 µm in diameter and produced by around 15-20% of living dinoflagellates as a dormant, zygotic stage of their lifecycle, which can accumulate in the sediments as microfossils. Organic-walled dinocysts are often resistant and made out of dinosporin. There are also calcareous dinoflagellate cysts and siliceous dinoflagellate cysts.
Many books provide overviews on dinocysts.〔Evitt, W. R. 1985. Sporopollenin Dinoflagellate Cysts: Their Morphology and Interpretation. American Association Stratigraphic Palynologists Monograph Ser. 1.〕
== History ==
The first person to recognize fossil dinoflagellates was Christian Gottfried Ehrenberg, who reported his discovery in a paper presented to the Berlin Academy of Sciences in July 1836. He had observed clearly tabulate dinoflagellates in thin flakes of Cretaceous flint and considered those dinoflagellates to have been silicified. Along with them, and of comparable size, were spheroidal to ovoidal bodies bearing an array of spines or tubes of variable character. Ehrenberg interpreted these as being originally siliceous and thought them to be desmids (freshwater conjugating algae), placing them within his own Recent desmid genus ''Xanthidium''. Though summaries of Ehrenberg's work appeared earlier, it was not published in full until 1837 or 1838; the date is uncertain.〔W.A.S. Sarjeant, 2002. 'As chimney-sweeps, come to dust': a history of palynology to 1970. pp. 273–327 In: Oldroyd, D. R. The earth inside and out: some major contributions to geology in the twentieth century. Geological Society (London) Special Publication no. 192.〕
A first relation between dinoflagellate thecae and cysts was made through morphological comparison of both by Bill Evitt and Susan E. Davidson.〔Evitt, W.R. and Davidson, S.E. 1964. Dinoflagellate studies. 1. Dinoflagellate cysts and thecae. Stanford university publications X (1), pp. 3–12.〕 Further evidence came from detailed culture studies of dinoflagellate cysts by David Wall and Barrie Dale at Woods Hole Oceanographic Institution in the sixties.〔Wall, D. and Dale, B. 1966. "Living" fossils in western Atlantic plankton. Nature 211. 5053, 1025-1026, doi:10.1038/2111025a0.〕〔Wall, D. and Dale, B. 1968. Modern dinoflagellate cysts and evolution of the Peridiniales. Micropaleontology 14 (3), 265-304.〕
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