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- W936388640 abstract "Paleopalynology is the study of microscopic structurally preserved organic matter which can be extracted from siliciclastic rocks by acid maceration. Traditionally, paleopalynology includes the study of various algal remains, microscopic parts of some protists and animals, spores of cryptogamic plants and fungi, and the pollen grains of seed-bearing plants, all of which are thought to possess a resistant organic outer wall composed of sporopollenin, chitin, or a similar derivative. This definition restricts the palynological record prior to the evolution of the terrestrial embryophytic plants to the resistant remains of algal phytoplankton, chitinous scolecodonts, and possible zooplankton such as chitinozoans. However, in this chapter I expand the view of paleopalynology to include some other structurally intact, microscopic organic remains which are thought to be of planktonic origin. This means that phytoplankton preserved in both siliciclastic (Acritarcha) and in cherty carbonate facies (Cryptarcha, sensu Diver & Peat, 1979)) is included." @default.
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- W936388640 date "1994-06-30" @default.
- W936388640 modified "2023-10-03" @default.
- W936388640 title "Sedimentation of palynomorphs in rocks of pre-Devonian age" @default.
- W936388640 doi "https://doi.org/10.1017/cbo9780511524875.024" @default.
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