Penetrative trace fossils from the late Ediacaran of Mongolia: early onset of the agronomic revolution
The Cambrian radiation of complex animals includes a dramatic increase in the depth and intensity of bioturbation in seafloor sediment known as the ‘agronomic revolution’. This bioturbation transition was coupled with a shift in dominant trace fossil style from horizontal surficial traces in the lat...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
The Royal Society
2018-01-01
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Series: | Royal Society Open Science |
Subjects: | |
Online Access: | https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.172250 |