Earth:La Irene Formation
| La Irene Formation Stratigraphic range: Maastrichtian ~70–66 Ma | |
|---|---|
| Type | Geological formation |
| Underlies | Chorrillo Formation |
| Overlies | Cerro Fortaleza Formation |
| Thickness | 230 m (750 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Shale |
| Location | |
| Location | Patagonia |
| Coordinates | [ ⚑ ] : 50°24′S 72°12′W / 50.4°S 72.2°W |
| Paleocoordinates | [ ⚑ ] 52°18′S 62°00′W / 52.3°S 62.0°W |
| Region | Santa Cruz Province |
| Country | Argentina |
| Extent | Austral Basin |
  La Irene Formation (Argentina) | |
La Irene Formation is a Maastrichtian geologic formation in southern Patagonia, Argentina. The formation is 230 metres (750 ft) thick and underlies the Chorrillo Formation and rests on top of the Cerro Fortaleza Formation.[1]
Description
The formation comprises lithified, sandy sandstones and lithified, argillaceous, sandy shales deposited in a fluvial deltaic environment.
At the base of Cerro Calafate a column of about 230 metres (750 ft) in thickness was measured along the road. The 110 m below represent a succession of sandy banks clear yellowish brown color to white and dark pelitic packages fining upwards cycles are stacked to form a sequence with a clear trend growing grain and stratum. Sandy banks (coarse to fine sand) show increasing thickness from 2 m at the base to more than 9 m, whereas intercalated mudstones show an opposite trend with thickness ranging from 15 m at the base to 1 m. At the top of lower shaly packets (the thickest) are preserved carbonaceous shale intervals, thinly laminated. 120 m above correspond to a succession of amalgamated conglomeratic sandy banks where preservation is extremely rare shaly intervals.[2]
Fossil content
The formation has provided many fossil pollen of:[3]
- Podocarpaceae
- Monocotyledoneae
- Liliidae
- Cycadopsida
- Pteridopsida
- Polypodiopsida
- Schizaeaceae
- Gleicheniaceae
- Selaginellaceae
- Lycopodiaceae
- Magnoliopsida
- Dinophyceae
References
- ↑ Marenssi et al., 2003, p.406
- ↑ La Irene Formation at Fossilworks.org
- ↑ Povilauskas et al., 2008
Bibliography
- Povilauskas, L.; Barreda, V.; Marenssi, S. (2008), "Polen y esporas de la Formación La Irene (Maastrichtiano), sudoeste de la provincia de Santa Cruz, Argentina: primeros resultados", Geobios 41 (6): 819–831, doi:10.1016/j.geobios.2008.07.002, Bibcode: 2008Geobi..41..819P, http://sedici.unlp.edu.ar/handle/10915/154340
- Marenssi, Sergio A.; Casadío, Silvio; Santillana, Sergio N. (2003), "Estratigrafía y sedimentología de las unidades del Cretácico superior-Paleógeno aflorantes en la margen sureste del lago Viedma, provincia de Santa Cruz, Argentina", Revista de la Asociación Geológica Argentina 58: 403–416, http://www.scielo.org.ar/pdf/raga/v58n3/v58n3a11.pdf, retrieved 2018-08-30
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