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Arroyo Malo main section, San Rafael Department, Mendoza Province, Argentina
| Lat/Long (Decimal) | -34.822,-69.887 |
|---|---|
| Co-ordinates Derivation | estimated from map |
| Given Location | Mendoza, Argentina |
| Mindat.org Region (for given coordinates) | San Rafael Department, Mendoza Province, Argentina |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Arroyo Malo main section, sample 1 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 10 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 13 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 14 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 16 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | sandstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 17 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 18 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 19 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 2 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 20 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 3 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 4 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 5 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 6 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
| Arroyo Malo main section, sample 8 | Damborenea S. E., Manceñido M. O. (2012) | Arroyo Malo | The report of Choristoceras cf. marshi Hauer from some levels of this sequence (Riccardi & Iglesia Llanos, 1999; Riccardi, 2008c) supports a late Rhaetian age for that part of the succession. Most of the fauna described here was found between 10 and 80 m below the main level with Choristoceras. | mudstone | 208.5 - 201.3 Ma Mesozoic |
Recorded Fossils
References
| Damborenea S. E., Manceñido M. O. (2012) Late Triassic bivalves and brachiopods from southern Mendoza, Argentina, Revue de Paléobiologie, Genève, vol. spéc 11, 317-344 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
