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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Taxonomy
Acastava lerougei was named by van Viersen (2013) [Paratypes: NHMM 2011006B, internal and external moulds of an incompletely exposed enrolled dorsal exoskeleton; NHMM 2011006C, a cephalon; NHMM 2011006D, a partial thoracopygon; all on the same rock slabs (counterparts) as the holotype. Specimens preserved as internal and external moulds; silicone casts created.]. Its type specimen is NHMM 2011006A, an exoskeleton, and it is a mold. Its type locality is Disused Grimbiémont quarry , which is in an Emsian marine siltstone in the Hierges-Hampteau Formation of Belgium.
Sister species lacking formal opinion data
Synonymy list
| Year | Name and author |
|---|---|
| 2013 | Acastava lerougei van Viersen p. 5 figs. Fig. 4A-G, I-J, L |
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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.
†Acastava lerougei van Viersen 2013
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, subo = suborder, c = class | |||||
| References: Aberhan et al. 2004, Whittington et al. 1997, Fortey and Owens 1999 | |||||
Age range: Late/Upper Emsian or 402.50000 to 391.90000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Emsian | Belgium (Luxembourg) | Acastava lerougei (type locality: 229156) |