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Alectrosaurus - Wiki latin dict size=27   common dict size=512
이미지 정보 Original File Name: Alectrosaurus_dinosaur.jpg Resolution: 401x217 File Size: 12854 Bytes Date: 2007:08:13 00:16:43 Upload Time: 2007:08:13 00:21:11
올린이 이름 (메일주소): Unknown
사진 제목 Alectrosaurus - Wiki

Alectrosaurus - Wiki; Image ONLY
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Alectrosaurus - Wiki

Alectrosaurus
From Wikipedia, the free encyclopedia

[Photo] Alectrosaurus (ah-LEK-tro-SAWR-us; "unmarried lizard") is a genus of tyrannosauroid theropod dinosaur from the Late Cretaceous Period of Inner Mongolia. It was a bipedal carnivore with a body shape similar to its much larger relative, Tyrannosaurus rex. Alectrosaurus was much smaller though, most likely less than 17 feet (5 meters) long. Created by user:LadyofHats http://commons.wikimedia.org/wiki/User:LadyofHats

Alectrosaurus (IPA: /????l??kt??????s??????s/; "unmarried lizard") is a genus of tyrannosauroid theropod dinosaur from the Late Cretaceous Period of Inner Mongolia. It was a bipedal carnivore with a body shape similar to its much larger relative, Tyrannosaurus rex. Alectrosaurus was much smaller though, most likely less than 17 feet (5 meters) long.

The generic name Alectrosaurus can also be translated as "alone lizard," and is derived from the (Greek words alektros ("unmarried") and sauros ("lizard"). At the time of its discovery, it was unlike any other Asian carnivore known. There is one named species (A. olseni), which is named in honor of George Olsen, who discovered the first specimens in 1923 on the third American Museum of Natural History expedition to Mongolia. Both genus and species were named by American paleontologist Charles Gilmore in 1933.

History of Discovery
The holotype, or original specimen, of Alectrosaurus was a hindlimb discovered in the Iren Dabasu Formation of the Inner Mongolia Autonomous Region (Nei Mongol Zizhiqu) of the People's Republic of China. The age of this geologic formation is not clear, but is commonly cited as the Campanian stage of the Late Cretaceous Period, about 83 to 74 million years ago.

More material, including comparable hindlimb material as well as skull and shoulder elements, has been referred to Alectrosaurus. These fossils were found in the Bayan Shireh Formation of Outer Mongolia, a formation which is also of uncertain age. It may possibly extend into the early Campanian, but recent estimates suggest it was deposited from Cenomanian through Santonian times. Iren Dabasu and Bayan Shireh dinosaur faunas are similar (but see, which claims the Iren Dabasu is probably Campanian-Maastrichtian in age and possibly correlated with the Nemegt Formation) so it is not surprising that a species of Alectrosaurus would be found there.

Furthermore, several more partial skeletons may have been found in both Inner and Outer Mongolia. These remain undescribed as of early 2007.

Taxonomy
Alectrosaurus is undoubtedly a tyrannosauroid, but due to its fragmentary nature, there is presently very little confidence in restoring its relationships with other tyrannosauroids and many recent cladistic analyses have omitted it altogether. One study recovered Alectrosaurus at no less than eight equally parsimonious positions in a tyrannosauroid cladogram.

Alectrosaurus was originally characterized as a long-armed theropod, but this was due to the mistaken association of segnosaur forelimb elements. The remaining material represents the hindlimb of a true tyrannosauroid, although characterized by the low ratio between the length of its tibia and femur, meaning that both bones are about the same size, as opposed to most other tyrannosauroids, where the tibia is usually longer. The hindfoot (and ankle) are also closer in size to the tibia than most tyrannosauroids, where the foot is usually longer.

The Bayan Shireh material may or may not belong to this genus, and needs further study. One cladistic analysis showed that the two sets of specimens group together exclusive of any other taxa, so they are probably at least closely related, if not the same species.

http://en.wikipedia.org/wiki/Alectrosaurus
The text in this page is based on the copyrighted Wikipedia article shown in above URL. It is used under the GNU Free Documentation License. You may redistribute it, verbatim or modified, providing that you comply with the terms of the GFDL.

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