Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the most widespread and common body forms ranging across all major Ediacaran fossil localities and time slices postdating the Gaskiers glaciation, but uncertainty over their phylogenetic affinities has led to uncertainty over issues of homology and functional morphology between and within organisms displaying this ecomorphology. Here we present the first large-scale, multigroup cladistic analysis of Ediacaran organisms, sampling 20 ingroup taxa with previously asserted affinities to the Arboreomorpha, Erniettomorpha, and Rangeomorpha. Using a newly derived morphological character matrix that incorporates multiple axes of potential phylogenetically ...
Rocks of the Ediacaran System (635–541 Ma) contain fossil evidence for some of the earliest complex ...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
Organisms in possession of a frondose body plan are amongst the oldest and most enigmatic members of...
Abstract: Ongoing discoveries of new rangeomorph fossils from the Ediacaran of Avalonia allow us to ...
The Rangeomorpha are the oldest, most diverse, and most disparate clade of Ediacaran macrofossils. ...
Fossils of the Ediacaran macrobiota (∼571–539 mya) record phylogenetically diverse marine palaeocomm...
Organisms in possession of a frondose body plan are amongst the oldest and most enigmatic members of...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
Rocks of the Ediacaran System (635–541 Ma) contain fossil evidence for some of the earliest complex ...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
Ediacaran fronds are key components of terminal-Proterozoic ecosystems. They represent one of the mo...
Organisms in possession of a frondose body plan are amongst the oldest and most enigmatic members of...
Abstract: Ongoing discoveries of new rangeomorph fossils from the Ediacaran of Avalonia allow us to ...
The Rangeomorpha are the oldest, most diverse, and most disparate clade of Ediacaran macrofossils. ...
Fossils of the Ediacaran macrobiota (∼571–539 mya) record phylogenetically diverse marine palaeocomm...
Organisms in possession of a frondose body plan are amongst the oldest and most enigmatic members of...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...
The recent discovery of a fossilized assemblage of juvenile Ediacaran rangeomorph macro-organisms, f...
Rocks of the Ediacaran System (635–541 Ma) contain fossil evidence for some of the earliest complex ...
The late Ediacaran siliciclastic successions of eastern Newfoundland, Canada, are renowned for their...
The Ediacaran macrofossil Charnia masoni Ford is perhaps the most iconic member of the Rangeomorpha:...