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Crioceratites portarum
Taxonomy
Crioceratites (Pseudothurmannia) portarum was named by Etayo-Serna (1968). It is not a trace fossil. Its type locality is Loma de Monsalve, Boyaca, which is in a Barremian marine horizon in the Paja Formation of Colombia.
It was recombined as Crioceratites portarum by Klein et al. (2007).
It was recombined as Crioceratites portarum by Klein et al. (2007).
Sister species lacking formal opinion data
C. andinum, C. andinus, C. angulicostatus, C. apricum, C. apricus, C. balearis, C. bederi, C. binelli, C. curnieri, C. diamantense, C. diamantensis, C. dilata, C. ermerici, C. fallauxi, C. hildesiense, C. ishiwarai, C. kirshnaae, C. lusitanicum, C. majoricensis, C. matsumotoi, C. munieri, C. nolani, C. nowaki, C. piveteaui, C. schlagintweiti, C. schlaginweiti, C. shibaniae, C. tenuicostatum, C. verrucosus, C. villersianus, C. villiersianum, C. hammatoptycha, C. aequicostatus, C. elegans, C. fissicostatus, C. intumescens, C. nolani, C. sablieri, C. tuba, C. andinus
Synonymy list
| Year | Name and author |
|---|---|
| 1968 | Crioceratites (Pseudothurmannia) portarum Etayo-Serna p. 57 figs. pl. 3, figs. 1, 2, 3 |
| 2007 | Crioceratites portarum Klein et al. p. 44 |
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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.
†Crioceratites portarum Etayo-Serna 1968
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: o = order, c = class | |||||
| References: Kiessling 2003, Kiessling 2004 | |||||