Where: Mendoza, Argentina (34.8° S, 69.9° W: paleocoordinates 40.5° S, 29.3° W)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Arroyo Malo Formation, Rhaetian (208.5 - 201.3 Ma)
• 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.
• bed-level stratigraphic resolution
Environment/lithology: prodelta; lithified, nodular mudstone
Size class: macrofossils
Preservation: mold/impression
Reposited in the MLP
• The material described here was collected over many years from different fossiliferous levels of the Arroyo Malo Formation during several field seasons.
Primary reference: S. E. Damborenea and M. O. Manceñido. 2012. Late Triassic bivalves and brachiopods from southern Mendoza, Argentina. Revue de Paléobiologie, Genève, vol. spéc 11:317-344 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 132723: authorized by Matthew Clapham, entered by Matthew Clapham on 25.08.2012
Creative Commons license: CC BY (attribution)
Taxonomic list
Bivalvia | |
Palaeocardita cf. peruviana Cox 1949 clam | |
Septocardia cf. peruviana Cox 1949 cockle | |
Liostrea sp. Douvillé 1904 oyster | |
Asoella campbellorum Damborenea 2012 scallop | |
? Praechlamys cf. valoniensis Defrance 1825 scallop | |
Palaeoneilo cf. elliptica Goldfuss 1837 clam |