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OPISTHOCOELICAUDIA

a plant-eating titanosaurian sauropod dinosaur from the Late Cretaceous of Mongolia.
Pronunciation: o-PIS-tho-SEE-ly-COR-dee-uh
Meaning: Hollow-backed tail
Author/s: Borsuk-Bialynicka (1977)
Synonyms: None known
First Discovery: Gobi Desert, Mongolia
Discovery Chart Position: #255

Opisthocoelicaudia skarzynskii

Discovered in 1965 but not described until 1977, Opisthocoelicaudia was originally identified as a new type of camarasaurid closely related to Euhelopus by Maria Magdalena Borsuk-Bia?ynicka from the Polish Academy of Sciences, but later research by Salgado and Coria showed it to be a titanosaur, possibly a saltasaurid.

Unlike most Titan Lizards, the first fifteen of its thirty-four tail vertebrae has a hollow on the rear and a dome on the front, so each can slot into the next working towards the creatures head. This "ball and socket" design is said to afford great strength to the tail which—with the help of a reinforced pelvic region thanks to a sixth fused hip vertebra (most titanosaurs have five)—may have been used as a prop when when rearing up to feed from treetops.

Known only from a headless skeleton discovered in Mongolia, Opisthocoelicaudia shares some features with Borealosaurus, Sonidosaurus and Huabeisaurus, but it could turn out to be a specimen of Nemegtosaurus which was discovered in the same formation in 1971 and is, funnily enough, known only from a skeleton-less head.
Etymology
Opisthocoelicaudia is derived from the Greek "opisthe" (back) and "koilos" (hollow) and the Latin "cauda" (tail) because of the opisthocoelous or opisthocoelian (both mean "hollowed at the rear") structure of its tail vertebrae.
We were hoping the species epithet, skarzynskii, was named to honour Polish aviator Stanislaw Jakub Skarzynski — famous for his transatlantic solo flight in 1933. Alas, it was named after Mr. Wojciech Skarzynski who prepared the specimen.
Preparators
Wojciech Skarzynski.
Discovery
The first remains of Opisthocoelicaudia were discovered at Altan Uul in the Nemegt Formation, Ömnögovi Aimag (South Gobi Province), Mongolia, by Ryszard Gradzinski during a joint Polish-Mongolian Expedition led by Zofia Kielan-Jaworowska in 1965. The holotype (ZPAL MgD-I/48 - housed at the Institute of Geology in the Mongolian Academy of Sciences, Ulaanbataar) is a partial skeleton, possibly tyrannosaur-scavenged, judging by teethmarks on its pelvis and femur. It was in decent condition, but lacking a skull and neck.
Estimations
Timeline:
Era: Mesozoic
Epoch: Late Cretaceous
Stage: Maastrichtian
Age range: 71-68 mya
Stats:
Est. max. length: 12 meters
Est. max. hip height: ?
Est. max. weight: 14 tons
Diet: Herbivore
References
• Kielan-Jaworowska Z and Dovchin N (1968) "Narrative of the Polish-Mongolian Expeditions 1963–1965". Palaeontologia Polonica, 19: 7–40.
• Borsuk-Bialynicka MM (1977) "A new camarasaurid Opisthocoelicaudia skarzynskii, gen. n., sp. n. from the Upper Cretaceous of Mongolia". Palaeontologia Polonica, 37(5): 5–64.
• Barsbold R (1997) "Mongolian dinosaurs". Page  447–450 in Currie and Padian (eds.) "Encyclopedia of dinosaurs".
• Maryanska T (2000) "Sauropods from Mongolia and the former Soviet Union". Page 457–458 in Benton, Shishkin, Unwin and Kurochkin (eds.) "The Age of Dinosaurs in Russia and Mongolia".
• Upchurch P, Barret PM and Dodson P (2004) "Sauropoda". Page 259–322 in Weishampel, Dodson and Osmólska (eds.) "The Dinosauria: Second Edition".
• Kielan-Jaworowska Z (2013) "The Polish-Mongolian paleontological expeditions, 1963 – 1971, and the nomadic expedition, 2002". Page 35–70 in "In Pursuit of Early Mammals".
• Currie PJ, Wilson JA, Fanti F, Mainbayar B and Tsogtbaatar K (2018) "Rediscovery of the type localities of the Late Cretaceous Mongolian sauropods Nemegtosaurus mongoliensis and Opisthocoelicaudia skarzynskii: Stratigraphic and taxonomic implications". Palaeogeography, Palaeoclimatology, Palaeoecology, 494: 5–13. DOI: 10.1016/j.palaeo.2017.10.035.
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To cite this page:
Atkinson, L. "OPISTHOCOELICAUDIA :: from DinoChecker's dinosaur archive".
›. Web access: 06th Mar 2026.
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