An archaic crested plesiosaur in opal from the Lower Cretaceous high-latitude deposits of Australia

Umoonasaurus demoscyllus gen. et sp. nov. is a new small-bodied (approx. 2.5 m) pliosauroid plesiosaur from the Lower Cretaceous (Aptian-Albian) of southern Australia. It is represented by several partial skeletons (one with a near complete skull is the most complete opalized vertebrate fossil yet k...

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Bibliographic Details
Published inBiology letters (2005) Vol. 2; no. 4; pp. 615 - 619
Main Authors Kear, Benjamin P, Schroeder, Natalie I, Lee, Michael S.Y
Format Journal Article
LanguageEnglish
Published London The Royal Society 22.12.2006
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ISSN1744-9561
1744-957X
DOI10.1098/rsbl.2006.0504

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Summary:Umoonasaurus demoscyllus gen. et sp. nov. is a new small-bodied (approx. 2.5 m) pliosauroid plesiosaur from the Lower Cretaceous (Aptian-Albian) of southern Australia. It is represented by several partial skeletons (one with a near complete skull is the most complete opalized vertebrate fossil yet known), and is unique in having large crests on the skull midline and above the orbits. Umoonasaurus is surprisingly archaic despite its relatively late age (approx. 115 Myr ago)-being simultaneously the most basal (primitive) and last surviving rhomaleosaurid. Notably, it lacks the 'pliosauromorph' features (large head, short neck, gigantism) typically characterizing many more derived Jurassic rhomaleosaurids; thus, reinforcing the suspected convergent evolution of the 'pliosauromorph' hypercarnivore body plan. Umoonasaurus inhabited an Early Cretaceous high-latitude (approx. 70° S) inland seaway subject to seasonally near-freezing climatic conditions. This extreme environment supported a diverse range of plesiosaur taxa, suggesting that these marine reptiles might have possessed adaptations (e.g. heightened metabolic levels) to cope with cold-water temperatures. Indeed, survival of ancient endemic lineages such as Umoonasaurus is a common phenomenon in Australian Cretaceous vertebrate assemblages and might have been facilitated by isolation in low-temperature high-latitude regions.
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ISSN:1744-9561
1744-957X
DOI:10.1098/rsbl.2006.0504