| Basic info | Taxonomic history | Classification | Included Taxa |
| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Lucianovenator bonoi
Taxonomy
Lucianovenator bonoi was named by Martinez and Apaldetti (2017). Its type specimen is PVSJ 906, a set of postcrania (an articulated vertebral sequence from third cervical vertebra to the fourth dorsal vertebra, sacrum composed of five co-ossified vertebrae articulated to the l), and it is a 3D body fossil. Its type locality is Quebrada del Puma, which is in a Norian fluvial sandstone in the Quebrada del Barro Formation of Argentina.
Synonymy list
| Year | Name and author |
|---|---|
| 2017 | Lucianovenator bonoi Ezcurra p. 507 |
| 2017 | Lucianovenator bonoi Martinez and Apaldetti p. 490–491 |
Is something missing? Join the Paleobiology Database and enter the data
|
|
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.
†Lucianovenator bonoi Martinez and Apaldetti 2017
show all | hide all
Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| R. N. Martinez and C. Apaldetti 2017 | Basal neotheropod dinosaur diagnosed according to the following combination of apomorphies (autapomorphies with asterisk): cervical neural arches with a series of three deep fossae, two blind pockets located within the prezygapophyseal centrodiapophyseal fossa, and the third, communicating with the internal cavity of the neural arch, located within the centropostzygapophyseal fossa; anteroposteriorly elongated fossa on the edge of the posterior centrodiapophyseal lamina that progressively increases in depth and size from C3 to C9*; length of the anterior cervical ribs equivalent to five cervical centra. |
Measurements
No measurements are available
|
|
||||
|
|
||||
|
|
||||
|
|
||||
|
|
||||
|
|||||
|
|
||||
|
|
||||
|
|
||||
| Source: o = order | |||||
| Reference: Marsh 1875 | |||||