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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Multimodus dissitus
Taxonomy
Multimodus dissitus was named by Ren (1995). Its type specimen is CH93072/3, a forewing, and it is an impression. Its type locality is Gaositai railway station, Chengde City, which is in a Barremian lacustrine - large mudstone in the Yixian Formation of China.
Synonymy list
| Year | Name and author |
|---|---|
| 1995 | Multimodus dissitus Ren p. 95 figs. Pl 15, fig 1; text-fig 3.54 |
| 2020 | Multimodus dissitus Sukatsheva and Aristov p. 377 |
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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.
†Multimodus dissitus Ren 1995
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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: Late/Upper Barremian or 125.77000 to 121.40000 Ma
Collections: one only
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Barremian | China (Hebei) | Multimodus dissitus (type locality: 107001) |