| 词条 | Tylosaurinae |
| 释义 |
| name = Tylosaurinae | fossil_range = Late Cretaceous{{Fossilrange|89.3|66}} | image = Tylosaurus kansasensis Clean.png | image_caption = Tylosaurus nepaeolicus mounted skeleton in the Rocky Mountain Dinosaur Resource Center in Woodland Park, Colorado | taxon = Tylosaurinae | authority = Williston, 1895[1] | subdivision_ranks = Genera | subdivision =
}} The Tylosaurinae are a subfamily of mosasaurs,[2] a diverse group of Late Cretaceous marine squamates. Members of the subfamily are informally and collectively known as "tylosaurines" and have been recovered from every continent except for South America.[3] The subfamily includes the genera Tylosaurus, Taniwhasaurus, Hainosaurus and Kaikaifilu. Tylosaurines first appeared in the Coniacian[4] and gave rise to some of the largest mosasaurs within the genera Tylosaurus and Hainosaurus which came to dominate as apex predators in marine ecosystems throughout the Santonian and Campanian, but appear to have been largely replaced by large mosasaurines, such as Mosasaurus, by the end of the Maastrichtian.[5] Nevertheless, the subfamily survived to the end of the Cretaceous, covering a period lasting approximately twenty million years. The etymology of this group derives from the genus Tylosaurus (Greek tylos = "knob" + Greek sauros = "lizard"). DescriptionIn general, tylosaurines were large-bodied marine lizards armed with sturdy, conical teeth and an elongated premaxilla and extensions of the dentaries that do not bear teeth to the very end such as is found in other genera of mosasaurs. Cope's original concept of a "battering ram" snout is not supported by fossil evidence. Stomach contents from a tylosaur recovered in South Dakota[6] included remains of another mosasaur, a bony fish, the large, flightless seabird Hesperornis, and possibly a shark, indicating that tylosaurs were generalists. Another specimen collected by Charles Sternberg [7] included the bones of a small plesiosaur (see also [8]). Lingham-Soliar suggested that tylosaurines were not among the fastest swimming nor the strongest mosasaurids. However, they are lightly built, having greatly reduced the weight of their bodies and possessing relatively small pectoral and pelvic girdles, fore- and hindlimbs. Their bone is highly cancellous and may have been impregated with fat cells during life, adding buoyancy. These traits suggest that tylosaurs may have been ambush predators. Tylosaurs were among the largest mosasaurs, with some species of Tylosaurus and Hainosaurus reaching lengths of 9-12+ meters, making them among the largest of all marine reptiles. Russell (1967, pp. 170 [9]) defined the Tylosaurinae as follows: "Large rostrum present anterior to premaxillary teeth. Twelve or more teeth in dentary and maxilla. Cranial nerves X, XI, and XII leave lateral wall of opisthotic through a single foramen. No canal in basioccipital or basispehnoid for basilar artery. Suprastapedial process of quadrate moderately large, distally pointed. Dorsal edge of surangular rounded and longitudinally horizontal...Twenty nine presacral vertebrae present. Length of presacral series less than that of postsacral series in Tylosaurus, neural spines of posterior caudal vertebrae at most only slightly elongated, do not form an appreciable fin. Haemal arches unfused to caudal centra. Appendicular elements lack smoothly finished articular surfaces." Species and taxonomyTylosaurinae
References1. ^Williston, S. W. 1895. New or little-known extinct vertebrates. Kansas University Quarterly 6:95-98. 2. ^Williston, S. W. 1897. Range and distribution of the mosasaurs with remarks on synonymy. Kansas University Quarterly 4(4):177-185. 3. ^{{Cite web|url=http://fossilworks.org/bridge.pl?a=taxonInfo&taxon_no=128897|title=Fossilworks: Tylosaurinae|website=fossilworks.org|access-date=2017-09-10}} 4. ^Everhart MJ. 2005b. Earliest record of the genus Tylosaurus (Squamata; Mosasauridae) from the Fort Hays Limestone (Lower Coniacian) of western Kansas. Transactions 108 (3/4): 149-155. 5. ^{{Cite journal|last=Polcyn|first=Michael J.|last2=Jacobs|first2=Louis L.|last3=Araújo|first3=Ricardo|last4=Schulp|first4=Anne S.|last5=Mateus|first5=Octávio|date=2014-04-15|title=Physical drivers of mosasaur evolution|url=http://www.sciencedirect.com/science/article/pii/S0031018213002514|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|series=Physical drivers in the evolution of marine tetrapods|volume=400|pages=17–27|doi=10.1016/j.palaeo.2013.05.018}} 6. ^Martin JE, Bjork PR. 1987. Gastric residues associated with a mosasaur from the late Cretaceous (Campanian) Pierre Shale in South Dakota. Dakoterra 3:68-72. 7. ^Sternberg CH. 1922. Explorations of the Permian of Texas and the chalk of Kansas, 1918. Transactions of the Kansas Academy of Science 30(1):119-120. (Papers - Fifty-first annual meeting, 1919), State Printer, Topeka. 8. ^Everhart MJ. 2004. Plesiosaurs as the food of mosasaurs; new data on the stomach contents of a Tylosaurus proriger (Squamata; Mosasauridae) from the Niobrara Formation of western Kansas. The Mosasaur 7:41-46. 9. ^Russell DA, 1967. Systematics and morphology of American mosasaurs. Peabody Museum of Natural History, Yale University, Bulletin 23. Further reading
1 : Mosasaurs |
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