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   » » Wiki: Talos Sampsoni
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Talos is an of that lived during the late period (late , about 76 million years ago) in the geographic area that is now , United States. It is known from a single species, Talos sampsoni.


Discovery
Talos is known only from the specimen UMNH VP 19479, a partial of a subadult individual including the hindlimbs, pelvis, vertebral fragments, chevrons and the left . It was discovered and collected in 2008 by M. J. Knell during the Kaiparowits Basin Project, initiated by the University of Utah in 2000, from the Kaiparowits Formation within the Grand Staircase–Escalante National Monument. It was first named by , David J. Varricchio, Patrick M. O'Connor, Alan L. Titus, and Michael J. Knell in 2011 and the type species is Talos sampsoni. The generic name comes from , a giant bronze in and is intended to be a pun on the English word talon. The specific name honors paleontologist Dr. Scott D. Sampson for researching and collecting fossils during the Kaiparowits Basin Project.


Description
Talos is a , a group of small, bird-like, . All troodontids have many unique features of the skull, such as closely spaced in the lower jaw, and large numbers of teeth. Troodontids have sickle-claws and , and some of the highest non- encephalization quotients, meaning they were behaviourally advanced and had keen senses. Talos is approximately in length, and its weight has been estimated at thirty-eight kilograms. Talos had a sickle claw. That of the specimen was damaged during life, possibly in an attack on prey.

In 2011 Talos was assigned to the . A analysis indicated it formed a of derived troodontids together with , , Zanabazar and .


Paleoecology

Habitat
The only known specimen of Talos was recovered at the Kaiparowits Formation, in southern Utah. Argon-argon radiometric dating indicates that the Kaiparowits Formation was deposited between 76.1 and 74.0 million years ago, during the Campanian stage of the Late period.Roberts EM, Deino AL, Chan MA (2005) 40Ar/39Ar age of the Kaiparowits Formation, southern Utah, and correlation of contemporaneous Campanian strata and vertebrate faunas along the margin of the Western Interior Basin. Cretaceous Res 26: 307–318.Eaton, J.G., 2002. Multituberculate mammals from the Wahweap (Campanian, Aquilan) and Kaiparowits (Campanian, Judithian) formations, within and near Grand Staircase–Escalante National Monument, southern Utah. Miscellaneous Publication 02-4, UtahGeological Survey, 66 pp. During the Late Cretaceous period, the site of the Kaiparowits Formation was located near the western shore of the Western Interior Seaway, a large inland sea that split North America into two landmasses, to the west and to the east. The plateau where dinosaurs lived was an ancient floodplain dominated by large channels and abundant wetland swamps, ponds and lakes, and was bordered by highlands. The climate was wet and humid, and supported an abundant and diverse range of organisms.Titus, Alan L. and Mark A. Loewen (editors). At the Top of the Grand Staircase: The Late Cretaceous of Southern Utah. 2013. Indiana University Press. Hardbound: 634 pp. This formation contains one of the best and most continuous records of Late Cretaceous terrestrial life in the world.


Paleofauna
Talos shared its paleoenvironment with such as , like , like , such as , the and , the , Nasutoceratops titusi and and the . Paleofauna present in the Kaiparowits Formation included (sharks and rays), , , , and . A variety of early were present including , , and .
(1999). 9781557916341, Utah Geological Survey.


See also
  • Timeline of troodontid research

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