Late Ordovlcian-Early Silurian trace fossils from the Matapedia Group, Tobique River, western New Brunswick
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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 late Precambrian to vertically penetrative trace fossils in the Cambrian. Here we show the existence...
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ژورنال
عنوان ژورنال: Atlantic Geology
سال: 1986
ISSN: 1718-7885
DOI: 10.4138/1623