База данных динозавров:
Общее количество образцов: 1365name | Rhomaleosaurus (Ромалеозавр) |
date_from | Rhaetian Age (Рэтский ярус) |
date_to | 174.1 million years ago |
date_from2 | 208.5 |
date_to2 | 174.1 |
lived_in | a marine environment (морская среда) |
was_a | carnivore (хищники) |
reproduced_by | live birth (живорождение) |
url | https://dinosaurpictures.org/Rhomaleosaurus-pictures |
articles | R. Tate and J. F. Blake. 1876. The Yorkshire Lias R. Owen. 1840. Report on British fossil reptiles. Report of the British Association for the Advancement of Science 8:43-126 T. Wright. 1860. On the Zone of Avicula contorta, and the Lower Lias of the South of England. Quarterly Journal of the Geological Society 16:374-411 A. R. I. Cruickshank. 1994. Cranial anatomy of the Lower Jurassic pliosaur Rhomaleosaurus megacephalus (Stutchbury) (Reptilia: Plesiosauria). Philosophical Transactions of the Royal Society of London B 343:247-260 R. Lydekker. 1889. Catalogue of the Fossil Reptilia and Amphibia, Part II. Containing the orders Ichthyopterygia and Sauropterygia E. T. Newton. 1888. On the skull, brain and auditory organ of a new species of pterosaurian (Scaphognathus purdoni) from the Upper Lias near Whitby, Yorkshire. Philosophical Transactions of the Royal Society of London, Series B 179:503-537 A. S. Smith and G. J. Dyke. 2008. The skull of the giant predatory pliosaur Rhomaleosaurus cramptoni: implications for plesiosaur phylogenetics. Naturwissenschaften 95:975-980 A. S. Woodward. 1895. Catalogue of the Fossil Fishes in the British Museum (Natural History), Part III C. W. Andrews. 1922. Note on the skeleton of a large plesiosaur (Rhomaleosaurus thorntoni, sp. n) from the Upper Lias of Northamptonshire. Annals and Magazine of Natural History 10:407-415 |
trophic_level | carnivore (хищники) |
habitat | marine (морской) |
motility | actively mobile (подвижный) |
points | 54.5333 -0.7, 54.55 -0.883333, 54.4833 -0.6, 52.2167 -1.75, 52.2622 -0.904444, 51.125 -2.73139, 52.7525 -1.14889, 51.1439 -2.54833, 54.49 -0.63, 52.3475 -1.13667, 52.2094 -1.00889, |