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Temporal range: Late Jurassic, 155 Ma
Scientific classification edit
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Order: Saurischia
Suborder: Sauropodomorpha
Clade: Sauropoda
Genus: Tendaguria
Bonaparte et al., 2000
T. tanzaniensis
Binomial name
Tendaguria tanzaniensis
Bonaparte et al., 2000

Tendaguria (/ˌtɛndəˈɡjʊəriə/ TEN-də-GEWR-ee-ə; meaning "the Tendaguru one") is a genus of herbivorous sauropod dinosaur from the Late Jurassic of Tanzania.

Discovery and naming[edit]

In 1911, German geologist Wilhelm Bornhardt at Nambango in German East Africa discovered two sauropod vertebrae, fifteen kilometers (nine miles) southeast of Tendaguru Hill. These were described by Werner Janensch in 1929 but not named.[1]

The finds were formally named by José Fernando Bonaparte, Wolf-Dieter Heinrich and Rupert Wild in 2000. The type species is Tendaguria tanzaniensis (/tænˈzeɪniːˈɛnsɨs/ tan-ZAY-nee-EN-sis) Bonaparte, Heinrich & Wild 2000. The generic name refers to the Tendaguru, the area of the great German palaeontological expeditions between 1909 and 1912. The specific name was "after Tanzania, the country where the holotype was collected".[2] The territory of present Tanzania largely coincides with that of the former German East Africa.

The type specimen consists of two syntypes, MB.R.2092.1 (NB4) and MB.R.2092.2 (NB5), probably uncovered in the Upper Saurian Bed (Obere Dinosauriermergel), Tendaguru Series, dating from the Late Jurassic Tithonian. The specimens are two anterior dorsal vertebrae, part of the collection of the Berlin's Natural History Museum. They probably belong to the same individual, having been found at a short distance from each other.[2]


Tendaguria was a large sauropod from the Tendaguru fossil locality. Its length is estimated at about twenty meters (sixty-six feet). The vertebrae are opisthocoelous (convex at the front, hollow behind) and differ from other known sauropods in their very low, almost non-existent neural spines, which are not distinct bodies of bone, do not rise above the surrounding area of the neural arch and are continuous at their rear with the transverse processes, including the epipophyses. Viewed from above, the spines have the form of a low and broad transverse ridge. Tendaguria is thus a highly derived or apomorphic sauropod; the axial musculature probably shifted from the neural spines to the dorsal surface of the transverse processes. Other autapomorphies are: a depression in the upper part of the outer side of each prezygapophysis; deep depressions in the front side of the transverse processes combined with shallow depressions in the rear side; the possession of robust epipophyses.[2]


Due to its unique morphology, the relationship of Tendaguria to other sauropods is not clear. The naming authors placed it as Sauropoda incertae sedis, though also naming a separate Tendaguriidae. It shows a mix of basal and derived traits, indicating a position outside, respectively inside, Neosauropoda. A cervical vertebra referred to Tendaguria because of a similar low spine shows some similarities to Camarasaurus.[2] In 2014 it was included in a cladogram generated in the redescription of Diamantinasaurus, where it was placed as the sister to Wintonotitan within Somphospondyli.[3]

























  1. ^ Janensch, W., 1929, "Material und Formengehalt der Sauropoden in der Ausbeute der Tendaguru-Expedition", Palaeontographica (Suppl. 7) 2: 1-34
  2. ^ a b c d J.F. Bonaparte, W.-D. Heinrich, and R. Wild, 2000, "Review of Janenschia Wild, with the description of a new sauropod from the Tendaguru beds of Tanzania and a discussion on the systematic value of procoelous caudal vertebrae in the Sauropoda", Palaeontographica Abteilung A 256(1-3): 25-76
  3. ^ Poropat, S.F.; Upchurch, P.; Mannion, P.D.; Hocknull, S.A.; Kear, B.P.; Sloan, T.; Sinapius, G.H.K.; Elliot, D.A. (2014). "Revision of the sauropod dinosaur Diamantinasaurus matildae Hocknull et al. 2009 from the mid-Cretaceous of Australia: Implications for Gondwanan titanosauriform dispersal". Gondwana Research. 27 (3): 995–1033. doi:10.1016/j.gr.2014.03.014.

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