Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Taxonomy
Conophillipsia subtriangularis was named by Engel and Morris (1984) [= Phillipsia cf. gemmulifera McCoy 1847, p. 231.]. Its type specimen is AMF 80518, a cephalon/head (internal mould of cranidium), and it is a 3D body fossil. Its type locality is NU L353. Dungog Council Quarry, Dungog, which is in a Visean transition zone/lower shoreface sandstone/limestone in the Ararat Formation of Australia.
It was recombined as Monodechenella subtriangularis by Vanderlaan and Ebach (2015).
It was recombined as Monodechenella subtriangularis by Vanderlaan and Ebach (2015).
Synonymy list
Year | Name and author |
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1984 | Conophillipsia subtriangularis Engel and Morris pp. 39 - 41 fig. 10–11. |
2015 | Monodechenella subtriangularis Vanderlaan and Ebach pp. 20 - 21 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Monodechenella subtriangularis Engel and Morris 1984
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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Source: f = family, o = order, c = class | |||||
References: Hendy 2009, Fortey and Owens 1999, Aberhan et al. 2004 |
Age range: base of the Tournaisian to the top of the Visean or 358.90000 to 330.90000 Ma
Collections (3 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Tournaisian | Australia (New South Wales) | Monodechenella subtriangularis (217049) | |
Tournaisian - Visean | Australia (New South Wales) | Phillipsia gemmulifera (217050) | |
Visean | Australia (New South Wales) | Conophillipsia subtriangularis (type locality: 217048) |