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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Microcornus parvulus
Taxonomy
Microcornus parvulus was named by Mambetov (1972) [DISTRIBUTION: Early Cambrian; Kazakhstan.]. It is not a trace fossil. Its type locality is Mally Karatau Range, Uchbas River [Shabakta Suite], which is in an Atdabanian marine dolomite in the Shabakty Formation of Kazakhstan.
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.
†Microcornus parvulus Mambetov 1972
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, p = phylum | |||||
| References: Hendy et al. 2009, Kiessling 2004 | |||||
Age range: base of the Meishucunian to the top of the Botomian or 530.70000 to 512.90000 Ma
Collections (10 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Meishucunian | China (Hubei) | Microcornus parvulus (155446) | |
| Atdabanian | China (Shaanxi) | Microcornus parvulus (57690) | |
| Atdabanian | Kyrgyzstan | Microcornus parvulus (99328 99329) | |
| Atdabanian | Kazakhstan | Microcornus parvulus (type locality: 10172 99303 99324) | |
| Branchian | United Kingdom (England) | Microcornus parvulus (79931 79932) | |
| Botomian | Kazakhstan | Microcornus parvulus (99362) |