The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their fossils of soft-bodied macro-organisms, which may include some of the earliest animals. Despite the potential importance of such fossils for evolutionary understanding, the taxonomic framework within which Ediacaran macrofossils are described is not clearly defined. Rangeomorphs from a newly discovered fossil surface on the Bonavista Peninsula, Newfoundland, require us to reconsider contemporary use of morphological characters to distinguish between genera and species within Ediacaran taxa. The new surface exhibits remarkable preservational fidelity, resolving features smaller than 0.1 mm in dimension in both frondose and non-frondose taxa. ...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
The mid-late Ediacaran Period (~579–541 Ma) is characterized by globally distributed marine soft-bod...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The deep marine Ediacaran fossil record of Avalonia is dominated by the Rangeomorpha, a clade charac...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
The mid-late Ediacaran Period (~579–541 Ma) is characterized by globally distributed marine soft-bod...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The deep marine Ediacaran fossil record of Avalonia is dominated by the Rangeomorpha, a clade charac...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
The presumed affinities of the Terminal Neoproterozoic Ediacara biota have been much debated. Howeve...
The mid-late Ediacaran Period (~579–541 Ma) is characterized by globally distributed marine soft-bod...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...