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The Ischigualasto-Villa Unión Basin (Spanish: Cuenca de Ischigualasto-Villa Unión) is a small sedimentary basin located in the Argentine Northwest, Argentina. It is located in the southwestern part of La Rioja Province and the northeastern part of San Juan Province. The basin borders the Sierras Pampeanas in the east, the western boundary of the basin is formed by the Valle Fértil Fault, bordering the Precordillera, and it is bound in the southeast by the El Alto Fault, separating the basin from the Marayes-El Carrizal Basin.
| Ischigualasto-Villa Unión Basin | |
|---|---|
| Cuenca de Ischigualasto-Villa Unión | |
  Location of the basin in Argentina | |
 Geologic map of the Ischigualasto-Villa Unión Basin - detail | |
| Coordinates | 29°32′S 68°05′W |
| Location | Southern South America |
| Region | Argentine Northwest |
| Country |  Argentina |
| State(s) | La Rioja & San Juan Provinces |
| Cities | Villa Unión |
| Characteristics | |
| On/Offshore | Onshore |
| Boundaries | Sierras Pampeanas (N & E), El Alto Fault (SE), Valle Fértil Fault (W) |
| Part of | Triassic rift basins |
| Area | ~80,000 km2 (31,000 sq mi) |
| Hydrology | |
| River(s) | Talampaya River |
| Geology | |
| Basin type | Rift |
| Plate | South American |
| Orogeny | Break-up of Pangea (Early Triassic) Andean (Cenozoic) |
| Age | Late Permian-Late Triassic |
| Stratigraphy | Stratigraphy |
The basin started forming in the Late Permian, with the break-up of Pangea, when extensional tectonics, including rifting, formed several basins in Gondwana; present-day South America, Africa, Antarctica, India and Australia. The accommodation space in the Ischigualasto-Villa Unión Basin was filled by an approximately 3.5 kilometres (11,000 ft) thick succession of volcaniclastic, eolian, alluvial, fluvial and lacustrine deposits in various geologic formations. The Cenozoic evolution of the basin is mainly influenced by the Andean orogeny, producing folding and faulting in the basin.
The basin is of paleontological significance as it hosts several fossiliferous stratigraphic units providing many fossils of early dinosaurs, synapsids, turtles, mammals, the earliest crocodylomorphs, fish, amphibians and flora, as well as ichnofossils. The Ischigualasto Provincial Park and Talampaya National Park in the basin were designated UNESCO World Heritage Sites in 2000.
The Ischigualasto-Villa Unión was recognized as a sedimentary basin by Stipanicic and Bonaparte in 1979. The basin stretches across a small area in northeastern San Juan Province and southwestern La Rioja Province in northwestern Argentina. The basin is bound by the Valle Fértil Fault to the west, separating the basin from the Precordillera, and the El Alto Fault in the southeast, forming the boundary with the Marayes-El Carrizal Basin. To the northeast, the basin ranges to the Sierras Pampeanas.[1] The basin is a rift basin that started forming early in the break-up of Pangea and its southern latitude paleocontinent Gondwana in the Late Permian to Early Triassic, providing a sedimentary column of approximately 3.5 kilometres (11,000 ft) of Triassic sediments.[2]
The area of the basin is sparsely populated, with Villa Unión in the north of the basin. The Talampaya and Chañares Rivers cross the basin.
The stratigraphy of the Ischigualasto-Villa Unión Basin contains sediments of the Triassic. The earliest deposition occurred in the Early Triassic (Olenekian) with the redbeds of the Talampaya and Tarjados Formations. This sequence is separated from the overlying Agua de la Peña Group by a regional unconformity.[3]
| Age | Group | Formation | Sequence | Environment | Maximum thickness | Notes |
|---|---|---|---|---|---|---|
| Quaternary | alluvium | |||||
| Neogene | Hiatus | |||||
| Paleogene | ||||||
| Cretaceous | ||||||
| Jurassic | ||||||
| Norian | Agua de la Peña | Los Colorados Formation | Second post-rift | Fluvial-lacustrine | 1,000 m (3,300 ft) | [4][5] |
| Carnian | Ischigualasto Formation | Second syn-rift | Floodplain | 900 m (3,000 ft) | [4] | |
| Los Rastros Formation | First post-rift | Deltaic-lacustrine | 1,000 m (3,300 ft) | [4] | ||
| Chañares Formation / Ischichuca Formation | First syn-rift | Fluvial-lacustrine | 70 m (230 ft) | [4] | ||
| Angular unconformity | ||||||
| Early-Mid Triassic | Paganzo | Tarjados Formation | Pre-rift | Arid fluvial | 250 m (820 ft) | [4][6] |
| Olenekian | Talampaya Formation | Aeolian-fluvial | 400 m (1,300 ft) | [4] | ||
| Angular unconformity | ||||||
| Paleozoic | Basement | Tuminico Formation | [7] | |||
| Precambrian | Valle Fértil Complex | [8] | ||||
The Ischigualasto-Villa Unión Basin is renowned for hosting the Triassic-age lagerstätten of the Chañares and Ischigualasto formations. These units have produced numerous fossils of synapsids and reptiles, including the earliest known dinosaurs. Other fossiliferous units within the basin have preserved fish, insects, flora, and ichnofossils. The basin represents one of three locations in Argentina where Triassic trackways were found, together with the Cuyo Basin to the south and Los Menucos Basin in Río Negro Province.[9]
Many of the earliest known crocodylomorphs come from the Ischigulasto-Villa Unión Basin. In the Los Colorados Formation, the crocodylomorphs Hemiprotosuchus leali and Coloradisuchus abelini were found.[10][11]
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