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This vertebra can be differentiated from the middle and posterior caudal vertebrae of Lusotitan and Galveosaurus (Barco, 2009; Mannion et al., 2013), by the presence of a well-developed amphicoelous centrum, a neural arch placed at midpoint of the centrum dorsal surface, and having a centrum, which is not markedly dorsoventrally compressed.

The Porto Novo vertebra is amphicoelous, differing from the condition observed in anterior caudals of Lourinhasaurus that have a flat posterior face with a central smooth concavity (Mocho et al., 2014a).

The anterior centra are amphicoelous. The posterior face becomes progressively flat toward the anterior part of the series.

Systematic review of late Jurassic Sauropods from the Museu Geologico Collections (Lisboa, Portugal)

The vertebra is amphicoelous, with the posterior articular face markedly concave.

This vertebra is also amphicoelous, but with the anterior articular face more concave than the posterior.

Postcranial elements of Maledictosuchus riclaensis (Thalattosuchia) from the Middle Jurassic of Spain

This semi-articulated caudal series comprises several vertebrae with amphicoelous centra and a hexagonal cross-section typical of Ornithopoda (e.g.

La Cantalera: an exceptional window onto the vertebrate biodiversity of the Hauterivian-Barremian transition in the Iberian Peninsula/La Cantalera: una excepcional ventana a la biodiversidad del transito Hauteriviense-Barremiense en la Peninsula Iberica

The amphicoelous, massive centra of the dorsal vertebrae are wider transversely than long anteroposteriorly.

New stegosaurian (Ornithischia, Thyreophora) remains from Jurassic-Cretaceous transition beds of Valencia province (Southwestern Iberian Range, Spain)/ Nuevos restos de estegosaurios (Ornithischia, Thyreophora) del transito Jurasico-Cretacico de la provincia de Valencia (Cordillera Iberica Suroccidental, Espana)