Discoasters are microscopic, star-shaped, calcite nannofossils (5-40 μm) of uncertain origin that are generally classified with marine coccolith-bearing algae (see Coccoliths). Discoasters are known as fossils ranging in age from late Paleocene to late Pliocene. Possible living discoaster-producing organisms have been reported (Bursa, 1964, 1971), but are not yet sufficiently documented and belie the well-documented sequential extinction of various forms to the end of the Tertiary. Fossil discoasters are most abundant and diverse in ocean sediment from the tropics where they can be the dominant type of nannofossil. Classified in the organ genus Discoaster Tan (1927)are at least 250 species names. Of these, only about 100 appear to be distinct biologic entities. Because of diagenetic overgrowth and dissolution, diagnostic taxonomic features, such as the relative proportions, taper, and camber of rays and the form of ray tips, can be obscured and misinterpreted. Discoaster species have...
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References
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Bukry, D. (1979). Discoasters . In: Paleontology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-31078-9_50
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