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Lasiosyne multituberata
Taxonomy
Notocupes multituberatus was named by Lin (1980). Its type specimen is NIGP 38565, an exoskeleton, and it is a compression fossil. Its type locality is ZH269, Laozhu, Lishui, which is in an Aptian terrestrial siliciclastic in the Shouchang Formation of China.
It was considered a nomen dubium by Kirejtshuk (2020); it was recombined as Lasiosyne multituberata by Li et al. (2021).
It was considered a nomen dubium by Kirejtshuk (2020); it was recombined as Lasiosyne multituberata by Li et al. (2021).
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.
†Lasiosyne multituberata Lin 1980
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: c = class, p = phylum | |||||
| References: Kiessling 2004, Bush and Bambach 2015 | |||||
Age range: Early/Lower Aptian or 121.40000 to 119.57000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Early/Lower Aptian | China (Zhejiang) | Notocupes multituberatus (type locality: 155613) |