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Rhinolambrus sublitoralis
Taxonomy
Parthenope (Rhinolambrus) sublitoralis was named by Morris and Collins (1991). Its type specimen is BMNH IN 61917, a carapace, and it is a 3D body fossil. Its type locality is Tutong Road, S.5548, which is in a Miocene marine sandstone in the Miri Formation of Brunei Darussalam.
It was recombined as Rhinolambrus sublitoralis by Schweitzer et al. (2010).
It was recombined as Rhinolambrus sublitoralis by Schweitzer et al. (2010).
Synonymy list
| Year | Name and author |
|---|---|
| 1991 | Parthenope (Rhinolambrus) sublitoralis Morris and Collins p. 9 fig. 40 |
| 2010 | Rhinolambrus sublitoralis Schweitzer et al. p. 99 |
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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.
†Rhinolambrus sublitoralis Morris and Collins 1991
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: f = family, o = order, c = class | |||||
| References: Fearon and Clapham 2023, Aberhan 1992, Turnsek 1997 | |||||
Age range: base of the Burdigalian to the top of the Tortonian or 20.45000 to 7.24600 Ma
Collections (5 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Burdigalian | Malaysia (Sarawak) | Parthenope sublitoralis (175184) | |
| Tortonian | Malaysia (Sabah) | Parthenope sublitoralis (185835 185836 185837) | |
| Late/Upper Miocene | Brunei Darussalam | Parthenope sublitoralis (type locality: 173589) |