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Amphicoelias fragillimus vertebra

E. D. Cope's original illustration of the vertebra of Amphicoelias fragillimus. The bone is now lost.

Amphicoelias was a large sauropod dinosaur that lived in the Late Jurassic of North America. One species, A. fragillimus, may be the largest dinosaur so far discovered.

DescriptionEdit

Both species of Amphicoelias are known from incomplete remains. In general, the genus is similar in body shape to Diplodocus, although Amphicoelias has proportionally longer forelimbs.

The type species, A. altus, is estimated to have measured about 25 meters in length, similar in size to Diplodocus. However, A. fragillimus, which was known only from an incomplete vertebra, may have reached lengths of almost 60 meters, larger than any other dinosaur by far.[1]

ClassificationEdit

Edward Drinker Cope placed the two Amphicoelias species in their own family, but it is now generally accepted that they are part of the family Diplodocidae. It was first suggested by Henry Fairfield Osborn that A. fragillimus was merely a large example of the type species A. altus. Currently, the two are treated as separate species.[2]

In 2007, John Foster suggested that Amphicoelias and Diplodocus were actually synonymous genera. Since Amphicoelias was named earlier, Diplodocus would have to be abandoned in favor of the older name (a similar situation occurred with the genera Apatosaurus and "Brontosaurus").[3] This suggestion has not been adopted by other researchers.

In 2010, a monograph arose that suggested all diplodocid species from the Morrison Formation were actually Amphicoelias specimens in various stages of growth.[4] Such a classification has not been widely accepted, and the paper has yet to be formally published.[5]

HistoryEdit

The type species, A. altus, was named by Edward Drinker Cope in 1877 (though not published until 1878).[6] He also named a second species, A. latus, in the same paper, but it is now generally regarded to be a synonym of A. altus.

An extremely large sauropod vertebra was uncovered by one of Cope's fossil collectors in Colorado during 1878. Although in poor condition, Cope described it as A. fragillimus and noted its unusual size. Though he believed that the rocks in which the bone was found were of Cretaceous age, it is now known that they are part of the Morrison Formation, a Jurassic-age site.[7] Since then, however, the bone disappeared, and all attempts to locate it have failed.[8] The bone itself was very fragile and the rock it was preserved in fragmented easily, so Cope may have simply discarded the fossil after he had described it.

PaleobiologyEdit

In his 2006 redescription of Amphicoelias, Ken Carpenter argued that ferns were likely a dominant source of nutrition for this animal. Though this suggestion had previously been refuted by earlier papers,[9] Carpenter believed that the digestive system of sauropods was adapted for processing low-quality foods such as ferns.

ReferencesEdit

  1. Carpenter, K. (2006). "Biggest of the big: a critical re-evaluation of the mega-sauropod Amphicoelias fragillimus." In Foster, J.R. and Lucas, S.G., eds., 2006, Paleontology and Geology of the Upper Jurassic Morrison Formation. New Mexico Museum of Natural History and Science Bulletin 36: 131–138.
  2. Osborn, H.F., and Mook, C. C. (1921). "Camarasaurus, Amphicoelias and other sauropods of Cope." Memoirs of the American Museum of Natural History NS, 3(3): 249–387.
  3. Foster, J. (2007). Jurassic West: The Dinosaurs of the Morrison Formation and Their World. Indiana University Press.
  4. Galiano, H. and Albersdorfer, R. "A new basal diplodocid species, Amphicoelias brontodiplodocus, from the Morrison Formation, Big Horn Basin, Wyoming, with taxonomic reevaluation of Diplodocus, Apatosaurus, and other genera." Dinosauria International, LLC. 44pp. Published online 2010.
  5. Mike Taylor. "The elephant in the living room: Amphicoelias brontodiplodocus". Sauropod Vertebra Picture of the Week.
  6. Cope, E.D. (1878a). "On the Vertebrata of the Dakota Epoch of Colorado." Proceedings of the American Philosophical Society, 17: 233–247.
  7. Turner, C.E., and Peterson, F. (1999) "Biostratigraphy of dinosaurs in the Upper Jurassic Morrison Formation of the Western Interior, U.S.A." In. Gillette, D., ed., Vertebrate Paleontology in Utah: Utah Geological Survey Miscellaneous Publication, 99(1): 77–114.
  8. McIntosh, J.S. (1998) "New information about the Cope collection of sauropods from Garden Park, Colorado." In Carpenter, K., Chure, D. and Kirkland, J.I., eds., The Morrison Formation: an interdisciplinary study: Modern Geology, 23: 481–506.
  9. Engelmann, G.F., Chure, D.J., and Fiorillo, A.R. (2004). "The implications of a dry climate for the paleoecology of the fauna of the Upper Jurassic Morrison Formation." In Turner, C.E., Peterson, F., and Dunagan, S.P., eds., Reconstruction of the extinct ecosystem of the Upper Jurassic Morrison Formation: Sedimentary Geology, 167: 297–308

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