|
Parecis Basin
|
| Fm. Anari |
fine-grained to aphanitic basalts, with subordinate coarsed diabase bodies. Volcanic flows |
southeast of Rondônia (RO) to the Northwest of Mato Grosso (MT) state |
no fossils related |
Lower Jurassic - Hettangian |
Schobbenhaus et al. 1984, Marzoli et al. 1999, Silva et al. 2003. Pedreira & Bahia 2004
|
| Fm Tapirapuã |
similar to basalts from Anari Formation, with columnar disjunction and spheroidal exfoliation |
comprises the Tapirapuã massif in Mato Grosso (MT) state |
no fossils related |
Lower Jurassic - Hettangian |
Schobbenhaus et al. 1984, Marzoli et al. 1999, Silva et al. 2003. Pedreira & Bahia 2004
|
| Fm Rio Ávila |
reddish, friable and eolic sandstones with rounded grains, well to poorly selected |
Outcrops in north of General Carneiro, in the valley of the Culuene river and northwest of Vilhena, Mato Grosso (MT) state |
no macrofossils related |
Jurassic |
Silva et al. 2003, Bahia, 2007
|
| Fm. Botucatu |
large scale cross-bedded bimodal sandstones. Aeolian dunes |
Outcrops in West of Rondônia (RO) and small exposures in southeast of Mato Grosso (MT) |
no macrofossils or ichnofossils related |
Jurassic |
Pedreira & Bahia 2000, 2004 |
|
Parnaíba Basin
|
| Fm Mosquito |
tholeiitic flood basalts, interbedded with sandstones |
arround the municipality of Fortaleza dos Nogueiras, Maranhão (MA) state |
no macrofossils related |
Lower–Middle Jurassic |
Schobbenhaus et al. 1984, Bellieni et al. 1992, Santos & Carvalho 2004
|
|
Alparcata Basin
|
| Fm Pastos Bons |
for the base, se- quences of siltstone, dark shale, and greenish and brownish mud- stones. The upper strata consist of gray to green shales with wavy lamination |
occurs as a south-central belt in Maranhão (MA) state, with some exposure in west of Piauí (PI) |
ostracods; conchostracans; palynomorphs; plant cuticles; fishes (Lepidotus piauhyensis, probable Semionotus and pleuropholids); Crocodyliformes (i.e., Batrachomimus pastosbonensis); |
Upper Jurassic - Oxfordian–Kimmeridgian |
Schobbenhaus et al. 1984, Gallo, 2005, Montefeltro et al. 2013
|
|
Paraná Basin
|
| Fm Botucatu |
mostly composed of fine-to medium-grained quartz sandstones. Friable, rounded and with large-scale cross-bedding related to a wide eolian dunes field. Sand sea of large eolian dunes |
widespread occurrence in the Paraná Basin, which cover great áreas of São Paulo (SP), Paraná (PR), Santa Catarina (SC), Rio Grande do Sul (RS), Mato Grosso (MT) and Mato Grosso do Sul (MS) states, with some portions in Goias (GO) and Minas Gerais (MG) states |
abundant ichnofossils: as footprints and tracks produced by invertebrates (arachnids and insects) and tetrapods (small to medium dinosaurs [i.e., ceratosaurid theropods, ornithopods?] and mammals [e.g., Brasilichnium elusivum]), also urolites attributed to dinosaurs. |
Upper Jurassic - Lower Cretaceous |
Schobbenhaus et al. 1984, Scherer, 2000, Fernandes et al. 2004, Scherer & Lavina 2006, Leonardi et al. 2007
|
| Fm Guará |
composed of fine- to coarse-grained sandstones and rare mudstones of fluvial and eolian depositional systems |
south region of Rio Grande do Sul state (RS) |
ichnoassemblage formed by theropod, ornithopod and sauropod tracks |
Upper Jurassic–Kimmeridgian-Tithonian |
Scherer & Lavina 2005, 2006, Francischini et al. 2017
|
|
Almada Basin
|
| Fm Sergi |
fluvial and eolic deposits. Mostly composed by sandstones, but wiht conglomerates in a finning upward granulometry |
south-central coast of Bahia state (BA) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Scherer et al. 2007, Bongiolo & Scherer 2010, Adegas et al. 2012
|
|
Camumu Basin
|
| Fm Sergi |
similar as above |
central coast of Bahia state (BA) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Ferreira et al. 2009, Kuchle et al. 2011, |
|
Recôncavo Basin
|
| Fm Sergi |
similar as above |
central-eastern of the State of Bahia (BA) |
ostracods (e.g, Bisulcocypris pricei); silicified wood attributed to coniferous Dadoxilon benderi |
Upper Jurassic (Tithonian, Dom Joao local age) |
Pedreira, 2000, Kuchle et al. 2011, Guzmán et al. 2015, Vilas Boas et al. 2018
|
| Fm Aliança |
formed by Capianga e Boipeba members. A gondwanic pre-rift sequence |
central-eastern of the State of Bahia (BA) |
permineralized wood reported (from Tucano and Jatobá deposits) ostracods (e.g., Darwinula, Bisulcocypris pricei, B. uninodosa) conchostracans (e.g., Cyzicus brauni); fish remains (e.g., hybodontid sharks, coelachants [e.g., Mawsonia gigas], Lepidotes and ceratodontid dipnoics); mesoeucrocodylian remains |
Upper Jurassic (Tithonian, Dom Joao local age) |
Netto & Oliveira, 1985, Ricardi-Branco 2004Kuchle et al. 2011, Silva et al. 2011, Guzmán et al. 2015, Vilas Boas et al. 2018, Carvalho et al. 2021
|
| Mb Capianga |
lacustrine muddystones. A gondwanic pre-rift sequence |
central-eastern of the State of Bahia (BA) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Scherer et al. 2007, Kuchle et al. 2011, Vilas Boas et al. 2018
|
| Mb Boipeba |
fluvial sandstones, compacted and cemented by quartz, anhydrite and calcite toward the base. A gondwanic pre-rift sequence |
central-eastern of the State of Bahia (BA) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Salem et al. 2000, Scherer et al. 2007, Kuchle et al. 2011, Vilas Boas et al. 2018
|
|
Tucano Basin
|
| the same depositional units as observed for Recôncavo Basin |
the same lithostratigraphy as observed for Recôncavo Basin units (sup. cit.) |
Observations: Subdivided in North-Jatobá-Tucano and South-Central Tucano. Synchronic depositional sequence with Reconcavo and Jatobá units as consequence of Recôncavo-Tucano-Jatobá aborted intracontinental rift |
Vita & Cupertino 1988, Milani et al. 2007, Costa et al. 2007a, Kuchle et al. 2011
|
|
Jatobá Basin
|
| except by Boipeba Member, the same depositional units as observed for Recôncavo and Tucano basins |
expected by Boipeba Member, the same lithostratigraphy as observed for Recôncavo and Tucano depositional units (sup. cit.) |
Observations: Synchronic depositional sequence with Reconcavo and Tucano units as consequence of Recôncavo-Tucano-Jatobá aborted intracontinental rift |
Vita & Cupertino 1988, Milani et al. 2007, Costa et al. 2007b, Kuchle et al. 2011
|
|
Sergipe Basin
|
| Fm Serraria |
coarse grained, poorly sorted, kaolinitic sandstones of fluvial braided depositions |
coastal margin of Sergipe state (SE) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Azambuja Filho 1998, Melton 2008, Borba et al. 2011, Kuchle et al. 2011, Freitas & Silveira 2017, Franco 2018
|
| Fm Bananeiras |
lacustrine red shales |
coastal margin of Sergipe state (SE) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Azambuja Filho, 1998, Melton 2008, Borba et al. 2011, Kuchle et al. 2011, Freitas & Silveira 2017 |
|
Alagoas Basin
|
| Bananeiras and Serraria formations are same depositional units as observed for Sergipe Basin |
the same lithostratigraphy as observed for Bananeiras and Serraria sequences (sup. cit.) |
coastal margin of Alagoas state (AL) |
same as Sergipe Basin |
Azambuja Filho, 1998, Melton 2008, Borba et al. 2011, Kuchle et al. 2011, Freitas & Silveira 2017 |
| Fm Candeeiro |
iterbedding of fine to medium-grained sandstones with reddish siltstones and shales |
coastal margin of Alagoas state (AL) |
no macrofossils related |
Upper Jurassic (Tithonian, Dom Joao local age) |
Azambuja Filho, 1998, Freitas & Silveira 2017 |
|
Araripe Basin
|
| Fm Missão Velha |
consists of quartz sandstones, sometimes feldspar and/or kaolinic, locally conglomeratic. River plains of interlaced systems characterized by shallow, high-energy channels. A gondwanic pre-rift sequence |
south of Ceará state (CE) |
abundant silicified wood, attributed to coniferous Dadoxilon benderi |
Upper Jurassic (Tithonian? Dom Joao local age) |
Assine, 1992, 2007, Fambrini et al. 2009 Kuchle et al. 2011 |
| Fm Brejo Santo |
shales and red lamitos from a lacustrine deposition. A gondwanic pre-rift sequence |
south of Ceará state (CE) |
ichnofossils; continental ostracodes (e.g., Bisulcopypris pricei, Darwinula oblonga, Theriosynoecum miritiensis); conchostraceans (i.e., Cyzicus pricei); gastropods; bivalves; fishes (i.e., Mawsonia gigas, Lepidotes sp.); crocodyliforms teeth and dinosaurians remains |
Upper Jurassic (Tithonian? Dom Joao local age) |
Assine 1992, 2007, Kuchle et al. 2011, Vieira de Melo & Carvalho 2017
|
|
Tacutu basin
|
| Fm Pirara |
consists of halites in the areas central for granite and laterally interdigitated schists and, less frequently, siltstones and carbonates |
central-northeast sector of Roraima state (RO). The Tacutu hemigraben deposits extends between Brazil and Guyana |
no macrofossils related |
Upper Jurassic |
Crawford et al. 1984, Eiras & Kinoshita 2006, Vaz et al. 2007
|
| Fm Manari |
siltstones, shales and, locally, calcisiltites and dolomites, produced by a lake sedimentary environment |
central-northeast sector of Roraima state (RO). The Tacutu hemigraben deposits extends between Brazil and Guyana |
no macrofossils related |
Upper Jurassic |
Crawford et al. 1984, Eiras & Kinoshita 2006, Vaz et al. 2007
|
| Fm Apoteri |
massive tholeiitic basalts to amigdaloidals, occasionally interspersed with sandstones at the base of Takutu basin; diabase dikes |
central-northeast sector of Roraima state (RO). The Tacutu hemigraben deposits extends between Brazil and Guyana |
no macrofossils related |
Upper - Jurassic |
“BRASIL, Radambrasil Project”1975, Crawford et al. 1984, Schobbenhaus et al. 1984, Eiras & Kinoshita 2006, Milani, et al.2007, Vaz et al. 2007 |
|
Mangabeira, Lavras da Mangabeira and Iborepi
|
| Fms Serrote do Limoeiro and Iborepi |
fluvial depositions, generally formed by conglomeratic layers to the base, with fining upward red sandstones with interbedded pelites to the top |
three small basins (63km2 total area) for the south of Ceará state (CE) |
rhizolites and ichnofossils related to invertebrates (e.g., Skolithos sp.); conchostraceans (i.e., “Pseudestheria” pricei); and fragments of other invertebrates (e.g., Anodontites), plants, and vertebrates (indet.) |
Lower Jurassic (Iborepi and Serrote do Limoeiro [?] formations) / Upper Jurassic ? (Lavras da Mangabeira) |
Carvalho 1993, Carvalho & Fernandes 1993, Rocha et al. 2008Hessel, 2014
|