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Dissacus serratus
Taxonomy
Plagiocristodon serratus was named by Chow and Qi (1978). Its type specimen is IVPP V5480 and is a 3D body fossil. Its type locality is Bayan Ulan site (lower 3 m), which is in a Paleocene terrestrial siltstone in the Nomogen Formation of China.
It was recombined as Dissacus serratus by Meng et al. (1998) and Solé et al. (2018).
It was recombined as Dissacus serratus by Meng et al. (1998) and Solé et al. (2018).
Synonymy list
| Year | Name and author |
|---|---|
| 1978 | Plagiocristodon serratus Chow and Qi |
| 1998 | Dissacus serratus Meng et al. |
| 2018 | Dissacus serratus Solé et al. figs. Table 9 |
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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.
†Dissacus serratus Chow and Qi 1978
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
| References: Hendy et al. 2009, Ji et al. 2002, Carroll 1988, Archibald 1998, Lillegraven 1979 | |||||
Age range: Late/Upper Paleocene or 58.70000 to 55.80000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Gashatan | China (Nei Mongol) | Dissacus serratus (71076) | |
| Late/Upper Paleocene | China (Nei Mongol) | Plagiocristodon serratus, Dissacus serratus (133389) |