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Portunites nodosa
Taxonomy
Portunites nodosus was named by Schweitzer and Feldmann (2000). It is a 3D body fossil. Its type locality is RB-32, Kydikabbit Point, which is in a Priabonian submarine fan siltstone in the Hoko River Formation of Washington.
It was corrected as Portunites nodosa by Schweitzer et al. (2010).
It was corrected as Portunites nodosa by Schweitzer et al. (2010).
Sister species lacking formal opinion data
Synonymy list
Year | Name and author |
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2000 | Portunites nodosus Schweitzer and Feldmann p. 638 figs. Figures 1, 2 |
2010 | Portunites nodosa Schweitzer et al. p. 108 |
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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.
†Portunites nodosa Schweitzer and Feldmann 2000
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Diagnosis
Reference | Diagnosis | |
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C. E. Schweitzer and R. M. Feldmann 2000 | Carapace wider than long, ovate-hexagonal; in- ner orbital spines triangular; orbits quadrate, directed forward; anterolateral margins with five spines including outer orbital spines; epibranchial region arcuate, with two large tubercles; branchial regions with weak, longitudinal ridges; posterolateral margins concave; posterior corner with well-developed reen- trant. |
Measurements
No measurements are available
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Source: f = family, o = order, c = class | |||||
References: Turnsek 1997, Fearon and Clapham 2023, Aberhan 1992 |
Age range: Priabonian or 38.00000 to 33.90000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
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Priabonian | USA (Washington) | Portunites nodosus (type locality: 202365) |