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The Pastos Bons Formation is a Late Jurassic (Oxfordian to Kimmeridgian ) geologic formation of the Parnaíba Basin in Maranhão, northeastern Brazil. The formation forms part of the sag phase of the basin. It overlies the Sardinha Formation and is overlain by the Mosquito Formation .[ 1] The fluvial to lacustrine sandstones and shales have provided fossils of a coelacanth fish, Parnaibaia maranhaoensis and a paralligatorid named after the formation, Batrachomimus pastosbonensis .
The following fossils were reported from the formation:[ 2]
Color key
Notes Uncertain or tentative taxa are in small text ; crossed out taxa are discredited.
Plants of the Pasto Bons Formation
Genus
Species
Location
Stratigraphic position
Material
Notes
Images
Araucariaceae Indet.
^ De Castro et al., 2016, p.532
^ Pastos Bons Formation at Fossilworks .org
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^ Gallo, V.; de Paiva, H. C. L.; Petra, R.; Brito, P. (2022). "Lophionotus parnaibensis , sp. nov. (Semionotiformes, Semionotidae) in the Upper Jurassic of the Parnaíba Basin, Northeastern Brazil". Journal of Vertebrate Paleontology . 41 (4). e1994983. doi :10.1080/02724634.2021.1994983 . S2CID 246164511 .
^ Yabumoto, 2007
^ Hanna Carolina Lins de Paiva; Valéria Gallo (2018). "Quasimodichthys gen. nov. (Neopterygii: Semionotiformes): A morphological and ontogenetic study". Journal of South American Earth Sciences . 88 : 132–143. Bibcode :2018JSAES..88..132P . doi :10.1016/j.jsames.2018.08.010 . S2CID 134986658 .
De Castro, David Lopes; Bezerra, Francisco Hilário; Fuck, Reinhardt Adolfo; Vidotti, Roberta Mary (2016), "Geophysical evidence of pre-sag rifting and post-rifting fault reactivation in the Parnaíba basin, Brazil" , Solid Earth , 7 (2): 529–548, Bibcode :2016SolE....7..529L , doi :10.5194/se-7-529-2016 , retrieved 2020-07-07
Yabumoto, Y (2007), "A New Mesozoic coelacanth from Brazil (Sarcopterygii, Actinistia)", Paleontological Research , 12 (4): 329–343, doi :10.2517/prpsj.12.329