Constraining the Ediacaran-Cambrian boundary in South China using acanthomorphic acritarchs and Palaeopascichnus fossils
The Ediacaran-Cambrian boundary is arguably the most critical transition in Earth history. This boundary is currently defined by the GSSP (Global Stratotype Section and Point) at Fortune Head (Newfoundland, Canada) at a point that was once regarded as the first appearance of the branching trace foss...
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Virginia Tech
2014
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| Online Access: | http://hdl.handle.net/10919/51047 |