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- W2366602011 abstract "Precambrian ecosystems are characterized by the flourish of microbiota and wide occurrence of stromatolites and microbially induced sedimentary structures.Metazoans and their trace fossils,occurong after the Neoproterozoic Snowball Earth event,made up of The Garden of Ediacara with microbial mats.Late Neoproterozoic seafloor were characterized by well-developed microbial mats and poor development of vertically-oriented bioturbation,thus it provied a fairly stable,relatively low water content sediment surface with a sharp water-sediment interface.Microbially-bound seafloor became increasingly scarce in shallow-marine settings of Cambrian,largely due to evolution of burrowing organisms with an increasing vertically-oriented component to their bioturbation.This Phanerozoic-style seafloor had a blurry water-sediment interface,greater water content,and lacked well-developed microbial mats.With the reworking increase of metazoans in Cambrian shallow marine settings,the trace fossils tended to be more diverse and complex,and microbial matgrounds retreated to deep sea and gradually disappeared." @default.
- W2366602011 created "2016-06-24" @default.
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- W2366602011 date "2012-01-01" @default.
- W2366602011 modified "2023-09-23" @default.
- W2366602011 title "Cambrian substrate revolution:from matgrounds to bioturbated mixgrounds" @default.
- W2366602011 hasPublicationYear "2012" @default.
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