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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Kinkaidia triserrata
Taxonomy
Microdoma triserrata was named by Batten (1966). It is not extant. Its type locality is Cliff Quarry, 450 yards W27˚S of Compton Martin Church, Compton Martin, Mar, which is in a Brigantian carbonate limestone in the Hotwells Formation of the United Kingdom.
It was recombined as Kinkaidia triserrata by Wagner (2023).
It was recombined as Kinkaidia triserrata by Wagner (2023).
Sister species lacking formal opinion data
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.
†Kinkaidia triserrata Batten 1966
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, superf = superfamily, c = class | |||||
| References: Bambach et al. 2007, Kiessling 2004, Bandel et al. 2002 | |||||
Age range: Brigantian or 335.90000 to 330.30000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Brigantian | United Kingdom (England) | Microdoma triserrata (type locality: 57131) |