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Acid-resistant, organic-walled microfossils, or palynomorphs, are common in most fine-grained sediments ince early Paleozoic. They can be extremely useful in solving geological problems both biostratigraphically and paleoenvironmentally. This article provides a review on two major groups of palynomorphs, dinoflagellate cysts and pollen/spores, and their application to sedimentary environmental nalyses. Palynofacies is also discussed.

Application of organic-walled microfossils (palynomorphs) to sedimentary environmental analyses