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- W2078506773 abstract "Colonies of the green alga Botryococcus occur in the Precambrian and throughout the Phanerozoic succession and have been interpreted as indicators of freshwater environments or influence. It has long been known that Botryococcus is a source of hydrocarbons in geological deposits and this has stimulated much research on the research on the living alga. B. braunii Kützing. This research has shown, for example, that the nature of the hydrocarbon produced may be related to the physiological state of the alga. In a study of Mesozoic samples it has been observed that the Botryococcus colonies exhibit different stages of development, similar to the physiological states of the living alga; the different stages appear to be specific to certain samples and are seldom, if ever fo und together. Material from Swedish Palaeozoic and Mesozoic sediments has been studied to investigate possible relationships between environment and the state of development of the alga. Torbanite from Scotland, kerosene shale from New South Wales, Australia, and colonies of modern Botryococcus have also been studied for comparative purposes. Detailed examination and the recognition of the stages of development at which Botryococcus colonies are preserved may yield more information about the palaeoenvironment than was previously recognised, leading, in some cases, to firmer interpretations of depositional conditions." @default.
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- W2078506773 date "1992-04-01" @default.
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- W2078506773 title "Botryococcus as an aid in the interpretation of palaeoenvironment and depositional processes" @default.
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- W2078506773 doi "https://doi.org/10.1016/0034-6667(92)90155-a" @default.
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