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Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Celtencrinurus praecursor
Taxonomy
Encrinurus praecursor was named by Tripp (1954). Its type specimen is A.3940a, b, a cephalon/head (cranidium), and it is a 3D body fossil. Its type locality is Craighead Quarry, which is in a Caradoc marine mudstone in the Craighead Formation of the United Kingdom.
It was recombined as Celtencrinurus praecursor by Tripp (1980).
It was recombined as Celtencrinurus praecursor by Tripp (1980).
Synonymy list
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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.
†Celtencrinurus praecursor Tripp 1954
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Diagnosis
Reference | Diagnosis | |
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R. P. Tripp 1957 | Glabella broad posteriorly, strongly convex; frontallobe not more than half length ofglabella. Tubercle formula: 1-0; ll-III- 1, 2, 3; (iv-O); IV-1, 2, 3; (v-0); V-1, 2. Fixed cheeks sparsely tuberculate, with two large tubercles one behind the other. |
Measurements
No measurements are available
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Source: f = family, c = class | |||||
References: Hendy 2009, Aberhan et al. 2004 |
Age range: Cheneyan or 452.50000 to 451.30000 Ma
Collections (3 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Caradoc | United Kingdom (Scotland) | Encrinurus praecursor (type locality: 188938) | |
Cheneyan | United Kingdom (Scotland) | Encrinurus praecursor (164953 169254) |