Wikipedia

Macroplata

Macroplata
Temporal range: Early Jurassic, 199–195 Ma
Macroplata BW.jpg
Restoration of Macroplata tenuiceps
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Sauropterygia
Order: Plesiosauria
Family: Rhomaleosauridae
Genus: Macroplata
Swinton, 1930
Type species
Macroplata tenuiceps
Swinton, 1930

Macroplata (meaning "big plate") is an extinct genus of Early Jurassic rhomaleosaurid plesiosaur which grew up to 4.5 metres (15 ft) in length. Like other plesiosaurs, Macroplata probably lived on a diet of fish, using its sharp needle-like teeth to catch prey. Its shoulder bones were fairly large, indicating a powerful forward stroke for fast swimming. Macroplata also had a relatively long neck, twice the length of the skull, in contrast to pliosaurs.[1][2]

A different species, Macroplata longirostris (previously called Plesiosaurus longirostris), which lived somewhat later, during the Toarcian stage, was also included in the genus; however, in 2011, Benson et al. reclassified it as a pliosaurid in the genus Hauffiosaurus, H. longirostris.[3]

Description

Macroplata bore an elongated skull, with more than half of its cranial length taken up by a roughly triangular snout. The premaxillae (front upper jaw bones) bear six teeth each. Together, they form the rounded region at the front of the jaw, and have a rough outer surface bearing foramina, ridges, and grooves. The snout is constricted where the premaxillae border the maxillae (the larger upper jaw bones). These bones continue to contact each other until they reach the level of the external nares (openings for the nostrils). While the premaxillae become narrow beyond this point, they extend far back on the skull, forming a ridge rearward of the external nares. The top side of each maxilla is ornamented like that of the premaxillae. The front edges of the orbits (eye openings) are formed by the maxillae. The maxillae also seem to make up the front and outer rims of the external nares, although poor preservation makes it difficult to verify this.[4]

The frontals of Macroplata are long, spanning from external nares to temporal fenestrae (large openings at the back of the skull), and widen towards the back of the skull. They bear foraminae and probably formed the rear edges of the external nares. The frontals are separated from each other by the premaxillae in the front and the parietals (bones at the back of the skull roof) at the rear, with a small area of contact between. The frontals articulate with the prefrontals above the orbits. The prefrontals form part the orbits' upper edge. The postfrontals form the border between the orbits and the temporal fenestrae, and each bone bearing a ridge running perpendicularly to the skull's length. Upon the discovery of Macroplata, its pineal foramen was claimed to be both large and small by different sources. As it was later obscured by plaster, its true size is unknown.[4]

The parasphenoid (a midline bone in the rear part of the palate) is smooth and approximately diamond-shaped, with a wide surface at its front that articulates with the pterygoids. The posterior interpterygoid vacuities (openings located on the palate) are roughly elliptical. Unlike in other plesiosaurs, their hind ends are angled inwards, making this trait an autapomorphy of Macroplata. It is unclear where the parasphenoid meets the basioccipital (the lower bone of the rear braincase), although a possible suture between these bones is present roughly at the level of the hind end of the posterior interpterygoid vacuities. This suggests that the rearmost part of the palate was composed of the basioccipital. The occipital condyle (the surface to which the vertebrae articulate) juts out beyond the palate when viewed from below. The occipital condyle is formed solely by the basioccipital, with the exoccipital-opisthoics (side bones of the rear braincase) not participating. The paraoccipital processes (the elongated regions of the exoccipital-opisthoics) of the latter bones bear wide upper surfaces and slope downwards and forwards. The foramen magnum (the opening above the occipital condyle) is constricted into an 8-shape. The supraoccipital (the top bone of the rear braincase) is wider than tall.[4]

The mandibular symphysis (where the two sides of the lower jaw meet and fuse) bears seven or eight tooth pairs and is covered by foraminae on its sides. The suture between the dentary (tooth-bearing lower jaw bone) and angular (one of the rear mandibular bones) takes the shape of a straight line sloping upwards and backwards. The splenial (an inner mandibular bone) might form part of the mandibular symphysis. It continues to contact the bottom of the dentary until the angular separates them further rearwards. The angular forms the entire lower surface of the rear mandible, widening below the jaw joint before narrowing to form the lower part of the retroarticular process. The articular forms the top part of the retroarticular process (a spikelike projection of bone behind the jaw joint). The retroarticular proccess is broad and weakly angled towards the skull's midline.[4]

Classification

Following Benson et al. (2012):[5]

Plesiosauria

Bobosaurus forojuliensis

Anningasaura lymense

Neoplesiosauria

Pliosauridae

Plesiosauroidea

Rhomaleosauridae

Stratesaurus taylori

Macroplata tenuiceps

Avalonnectes arturi

Eurycleidus arcuatus

Meyerasaurus victor

Maresaurus coccai

Atychodracon megacephalus

Archaeonectrus rostratus

Rhomaleosaurus cramptoni

Rhomaleosaurus thorntoni

Rhomaleosaurus zetlandicus

See also

  • List of plesiosaur genera
  • Timeline of plesiosaur research

References

  1. ^ Ketchum HF, Benson RBJ. Global interrelationships of Plesiosauria (Reptilia, Sauropterygia) and the pivotal role of taxon sampling in determining the outcome of phylogenetic analyses. Biological Reviews
  2. ^ Palmer, D., ed. (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 76. ISBN 1-84028-152-9.
  3. ^ R. B. J. Benson, H. F. Ketchum, L. F. Noe and M. Gomez-Perez. 2011. "New information on Hauffiosaurus (Reptilia, Plesiosauria) based on a new species from the Alum Shale Member (Lower Toarcian: Lower Jurassic) of Yorkshire, UK". Palaeontology 54(3):547-571.
  4. ^ a b c d Ketchum, H. F.; Smith, A. S. (2010). "The anatomy and taxonomy of Macroplata tenuiceps (Sauropterygia, Plesiosauria) from the Hettangian (Lower Jurassic) of Warwickshire, United Kingdom" (PDF). Journal of Vertebrate Paleontology. 30 (4): 1069–1081.
  5. ^ Roger B. J. Benson, Mark Evans and Patrick S. Druckenmiller (2012). "High Diversity, Low Disparity and Small Body Size in Plesiosaurs (Reptilia, Sauropterygia) from the Triassic–Jurassic Boundary". PLoS ONE. 7 (3): e31838. doi:10.1371/journal.pone.0031838. PMC 3306369. PMID 22438869.

External links


This article is copied from an article on Wikipedia® - the free encyclopedia created and edited by its online user community. The text was not checked or edited by anyone on our staff. Although the vast majority of Wikipedia® encyclopedia articles provide accurate and timely information, please do not assume the accuracy of any particular article. This article is distributed under the terms of GNU Free Documentation License.

Copyright © 2003-2025 Farlex, Inc Disclaimer
All content on this website, including dictionary, thesaurus, literature, geography, and other reference data is for informational purposes only. This information should not be considered complete, up to date, and is not intended to be used in place of a visit, consultation, or advice of a legal, medical, or any other professional.