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| Produced 
        by the Population Genetics and Evolution class, Furman University | ||||
|  | The 
          Jurassic: Giraffatitan |  | ||
| Originally 
        Brachiosaurus brancai, this species of dinosaur was discovered 
        in a series of five incomplete fossils near Lindi, Tanzania in the early 
        1900s. The change in genus name is based on 26 synapomorphies primarily 
        in the vertebral column (Taylor 2009), and is still contested for over 
        a decade after it was originally proposed in 1988 (Everything Dinosaur 
        2008). Like the other Brachiosaurs, Giraffatitan brancai is characterized 
        by a neck like a giraffe’s and a short tail in proportion to its 
        body. G. brancai is in fact the tallest of the Brachiosaurs, 
        estimated at up to 25 m, with a shoulder height of up to 6.79 m, indicating 
        a monstrous neck that would allow this tremendous herbivore to eat out 
        of the highest levels of foliage (White and Kaslev 2010). Other differences 
        between G. brancai and others of its immediate clade include 
        a more slender, lighter build, and some changes in proportions of vertebrae 
        and skull shape. It is thought the species diverged geographically due 
        to migration along the supercontinent that existed during the Jurassic 
        period (Everything Dinosaur 2008). In addition, this migration likely 
        occurred in herds, based on the large numbers apparently present, indicating 
        a lifestyle very similar to that of modern, large, herbivorous mammals 
        (White and Kaslev 2010). Page by Will Towler |  | 
| Giraffatitan brancai. Pcture from: scientific-web.com | |
| Everything Dinosaur. 2008. Everything Dinosaur Blog. Accessed March 30, 2010. White T, Kazlev MA. 2010. Sauropodomorpha. www.palaeos.com. Accessed March 30, 2010. Taylor M. 2009. A re-evaluation of Brachiosaurus altithorax Riggs 1903 (Dinosauria, Sauropoda) and its generic separation from Giraffatitan brancai (Janensch 1914). Journal of Vertebrate Peleontology 29(3):787-806. |