Where: Valdivia, Chile (39.9° S, 73.2° W: paleocoordinates 40.2° S, 70.9° W)
• coordinate stated in text
When: Santo Domingo Formation, Late/Upper Miocene (11.6 - 5.3 Ma)
• Overlying Formation: Unknown. Underlying Formations: Unconformably overlies the Paleozoic metamorphic rocks of the Bahía Mansa complex. It also overlies the Pupunahue-Catamutún formation, although it is not clear whether the contact with this unit is gradational or if there is a discontinuity, as suggested by the abrupt transition from a coal-bearing unfossiliferous succession to a silty, fossil-rich unit that can be observed in bore holes drilled at the Catamutún mining area southeast of Valdivia. (Alfaro et al., 1990; Elgueta et al., 2000; Feldmann et al., 2010). Thickness: Maximum thickness of the unit at Cuesto Santo Domingo is 110 m, but this must be considered as a minimum estimate because there is no place where a complete section can be measured.
Environment/lithology: submarine fan; brown, gray, sandy siltstone and medium-grained sandstone
Size class: macrofossils
Preservation: cast, mold/impression
Primary reference: R. M. Feldmann, C. E. Schweitzer, and A. Encinas. 2010. Neogene Decapod Crustacea from Southern Chile. Annals of Carnegie Museum 78(4):337-366 [J. Wolfe/A. Lynch/A. Lynch]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 228523: authorized by Joanna Wolfe, entered by Arthur Lynch on 11.12.2022
Creative Commons license: CC BY (attribution)
Taxonomic list
Malacostraca | |
Trichopeltarion levis Casadio et al. 2004 crab | |
Archaeogeryon navidad Feldmann 2005 crab |