Chubutisaurus (lat.) - genus of zauropod dinosaurs from the clan Titanosauriformes . Inhabited during the Lower Cretaceous era in South America . The typical and only species of Chubutisaurus insignis is described in 1975. Its fossils are discovered in the Cerro Barcino Formation and date back to the Albanian age . Closest to the genus Venenosaurus . As of 2015, Chubutisaurus was assigned to the Somphospondyli treasure [1] .
| † Chubutisaurus |
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| Scientific classification |
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| No rank : | Bilateral symmetrical |
| Infraclass : | Archosauromorphs |
| No rank : | Archosauriformes |
| Suborder : | † Sauropodomorphs |
| Infrastructure : | † Zauropods |
| Treasure : | † Titanosauriformes |
| Treasure : | † Somphospondyli |
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| International scientific name |
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Chubutisaurus del Corro, 1975 |
| Single view |
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| † Chubutisaurus insignis del Corro, 1975 |
Geochronology
Albanian age113.0-100.5 Ma | million years | Period | Era | Aeon |
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| 2,588 | Even | | | Ka | F
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R
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th | | 23.03 | Neogene | | 66.0 | Paleogen | | 145.5 | a piece of chalk | M
e
s
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s
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th | | 199.6 | Yura | | 251 | Triassic | | 299 | Permian | P
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e
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th | | 359.2 | Carbon | | 416 | Devonian | | 443.7 | Silur | | 488.3 | Ordovician | | 542 | Cambrian | | 4570 | Precambrian |
◄ Nowadays◄ Cretaceous-Paleogene extinction◄ Triassic extinction◄ Mass Permian Extinction◄ Devonian extinction◄ Ordovician-Silurian extinction◄ Cambrian explosion |
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