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- W2801807519 abstract "Abstract Precambrian-Cambrian transition is recorded in the northern and northwestern part of the pristine Indian Shield termed as the Greater India. However, barring some granite intrusions around 500 ± 50 Ma, there is a scanty record of geological activity between the early Ordovician and late Carboniferous. Several continental rift basins had developed during the Permo-Carboniferous that filled up with the thick coal-bearing sediments that constituted the Gondwana Supergroup. The onset of Palaeozoic also marks the evolution of a number of life forms showing changes from the soft-bodied late-Precambrian Ediacaran-type biota into hard-skeleton-bearing fossils. Wide-scale diversification in life forms is observed in the development of several invertebrates, vertebrates, and plant life. Extensive peneplanation of the mountainous regions supplied massive quantity of nutrients, and because of that, there was an explosive enhancement of the Cambrian Evolutionary Radiation." @default.
- W2801807519 created "2018-05-17" @default.
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- W2801807519 date "2018-01-01" @default.
- W2801807519 modified "2023-10-17" @default.
- W2801807519 title "Palaeozoic Geological History" @default.
- W2801807519 doi "https://doi.org/10.1016/b978-0-12-809839-4.00014-x" @default.
- W2801807519 hasPublicationYear "2018" @default.
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