Crustacea reported from the Cañadon Asfalto Formation |
---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|
Carapacestheria[2] [3] [4] |
| - Cañadón Asfalto
- Cañadón Lahuincó
- Cerro Bayo
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Eosestheriidae (Spinicaudatan). Originally identified as Cyzicus (Euestheria) taschi. This genus is found in identical alkaline lacustrine settings in the also Toarcian Mawson Formation of Antarctica | |
Congestheriella[5] |
| - Sierra de la Manea
- Estancia El Torito
- Cañadón Los Chivos
|
| Isolated Valves | A freshwater (Lacustrine) member of Afrograptidae (Spinicaudatan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation. | |
Darwinula |
| - Cañadón Asfalto
- Cañadón Lahuincó
- Cerro Bayo
- Cañadón Asfalto
- Quebrada Subsidiaria
- Estancia el Torito
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Darwinulidae (Ostracod). | |
Eosolimnadiopsis |
| - Cerro Cóndor
- Estancia Fossati[6]
|
| Isolated Valves | A freshwater (Lacustrine) member of Palaeolimnadiopseidae (Spinicaudatan). | |
Euestheria |
| - Cerro Cóndor
- Cerro Bayo
- Alice Creek
- Quebrada Subsidiaria
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Euestheriidae (Spinicaudatan). | |
Lioestheria | - C. (Lioestheria) sp. B
- C. (Lioestheria) sp. C
| - Cañadón Las Chacritas
- Colan Conhué
- Alice Creek
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Fushunograptidae (Spinicaudatan). | |
Mandelstamia |
|
|
| Isolated Valves | A freshwater (Lacustrine) member of Limnocytheridae (Ostracodan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation | |
Metacypris |
|
|
| Isolated Valves | A freshwater (Lacustrine) member of Loxoconchidae (Ostracodan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation. | |
Penthesilenula[7] [8] | - P. magna
- P. sarytirmenensis
| - Cañadón de la Angostura
- Estancia El Torito
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Darwinulidae (Ostracodan). These species are characteristic of the Middle Jurassic of northern China and where used to correlate the age of the beds | |
Pseudestherites |
| - Estancia El Torito
- Cañadón Los Chivos
|
| Isolated Valves | A freshwater (Lacustrine) member of Antronestheriidae (Spinicaudatan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation. | |
Theryosinoecum |
|
|
| Isolated Valves | A freshwater (Lacustrine) member of Cytheroidea (Ostracodan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation. | |
Timiriasevia |
|
|
| Isolated Valves | A freshwater (Lacustrine) member of Limnocytheridae (Ostracodan). Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation. | |
Wolfestheria | - W. patagoniensis
- W. smekali
| - Cañadón Asfalto
- Cañadón Lahuincó
- Estancia La Sin Rumbo
| - Las Chacritas Member
- Puesto Almada Member
| Isolated Valves | A freshwater (Lacustrine) member of Fushunograptidae (Spinicaudatan). | |
|
Insect eggs of unknown affinity were reported from several layers of the Estancia Fossati locality.[1]
Insects reported from the Cañadon Asfalto Formation |
---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|
Chironomidae | Indeterminate |
|
| Head capsules | Indeterminate Bittacidae (Migdes) remains, associated with lacustrine facies. Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation | |
Coleoptera | Indeterminate | - Cerro Cóndor
- Estancia Fossati
- Estancia El Torito
- Estancia La Sin Rumbo
| - Las Chacritas Member
- Puesto Almada Member
| Elytra and body remains | Indeterminate Beetle remains, associated with lacustrine facies | |
Conchindusia[12] | C. isp. |
| - Las Chacritas Member
- Puesto Almada Member
| Imprints or compressed moulds of larval cases | Indeterminate Trichoptera (Caddisflies) Ichnofossils, associated with lacustrine facies. Larval cases made of conchostracan shells | |
Heteroptera | Indeterminate | - Cerro Cóndor
- Estancia Fossati
- Estancia El Torito
- Estancia La Sin Rumbo
| - Las Chacritas Member
- Puesto Almada Member
| Fragmentary wings | Indeterminate Heteroptera remains, associated with lacustrine facies | |
Neorthophlebidae[13] | Indeterminate |
|
| Wings and parts of body | Indeterminate Bittacidae (Scorpionfly) remains, associated with lacustrine facies. Given the stratigraphic uncertainty, it may come from the Cañadón Calcáreo Formation | |
Ostracindusia | O. isp. |
| - Las Chacritas Member
- Puesto Almada Member
| Imprints or compressed moulds of larval cases | Indeterminate Trichoptera (Caddisflies) Ichnofossils, associated with lacustrine facies. Larval cases made of ostracodan shells | |
Terrindusia | T. isp. | - Cerro Cóndor
- Estancia Fossati
- Gan Gan
| - Las Chacritas Member
- Puesto Almada Member
| Imprints or compressed moulds of larval cases | Indeterminate Trichoptera (Caddisflies) Ichnofossils, associated with lacustrine facies. Larval cases made of clasts or terrigenous particles | |
Trichoptera[14] [15] | Indeterminate | - Cerro Cóndor
- Estancia Fossati
- Estancia El Torito
- Estancia La Sin Rumbo
| - Las Chacritas Member
- Puesto Almada Member
| Wings and larval cases | Indeterminate Trichoptera (Caddisflies) remains, associated with lacustrine facies | |
|
During a campaign conducted in early 2021, remains of a large theropod dinosaur were found near the town of Las Chacritas. In 2020 a new fossil locality was found, named Cañadón de las Huellas due to the large number of sauropod, and probably theropod, footprints on one of the canyon walls. In the same locality in 2021, articulated remains where recovered and represent at least one sauropod and one large theropod.[28] At least four theropod morphotypes, including one with ceratosaur and another with Piatnitzkysauridae affinities, are known from the Cañadón Bagual.[29]
Theropoda reported from the Cañadón Asfalto Formation |
---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|
Asfaltovenator[30] | A. vialidadi | Cerro Condor | Las Chacritas Member | Nearly compete skull and largely complete front half of the skeleton forward of the hips, distal pubis and fermur and proximal fibula and tibia, partial foot | A probable early member of Allosauroidea | |
Averostra[31] | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated teeth: MPEF BA 182/08, BA 40/08, BA 09/80, BA 88/08, BA 252G+165/08 A, BA 252G+165/08 B, BA 252G+165/08 C | Theropod dinosaur teeth that resemble those assigned to the families Ceratosauridae, Megalosauridae and Abelisauridae | |
Ceratosauridae[32] | Indeterminate | Cañadon Bagual | Las Chacritas Member | A dentary with teeth in situ, MPEF-PV 6775 | It resembles the dentary of Ceratosaurus | |
Condorraptor[33] [34] | C. currumili | Las Chacritas | Las Chacritas Member | Partial articulated skeleton | A relative of Piatnitzkysaurus from the same formation, and a possible junior synonym of it as well. | |
Dromaeosauridae | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated Teeth: MEPF BA 61/08, BA 103/08, BA 32/08 A, BA 32/08 B, BA 104/08, BA 226B/08, PV 3498, BA 29/08, BA51/08, BA 270/08 a, BA 270/08 b, BA 270/08 c | Theropod dinosaur teeth that resemble those assigned to the family Dromaeosauridae. Alternatively, they could belong to basal members of Coelurosauria | |
Eoabelisaurus[35] | E. mefi | Jugo Luco | Las Chacritas Member | A nearly complete articulated skeleton | A Neoceratosaur, that was suggested to be a basal member of Abelisauria, but also a member of Ceratosauridae | |
Megalosauridae | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated Teeth: MPEF PV 1175, BA 66/08, PV 1356, PV 1357 | Theropod dinosaur teeth that resemble those assigned to the family Megalosauridae. | |
Neotheropoda | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated Teeth: MPEF BA 68/08, BA 92/08, PV 3499, BA 68/08, BA 183/08 | Theropod dinosaur teeth that resemble those assigned to basal neotheropods, such as members of Coelophysoidea. | |
Piatnitzkysauridae[36] | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated Teeth & Cranial remains: MPEF 1717 CC 205, PV 3440A A, PV 3440A B, PV 3440A C, PV 3440A D, PV 3440A E, PV 3440A F, PV 3440A G | Theropod dinosaur teeth that resemble those assigned to members of Piatnitzkysauridae. | |
Piatnitzkysaurus[37] | P. floresi | Cerro Cóndor South | Las Chacritas Member | Two "fragmentary skulls with associated postcranium."[38] | Possible senior synonym of Condorraptor from the same formation. | |
Spinosauridae | Indeterminate |
| Las Chacritas Member | Isolated Teeth : MEPF PV 1350 | Theropod dinosaur teeth resembling those assigned to members of Spinosauridae. Alternatively, they could belong to members of Ceratosauria | |
Tetanurae | Indeterminate | - Cerro Cóndor
- Puesto el Quemado
- Cerro Bayo
| Las Chacritas Member | Isolated Teeth : MEPF BA 84/08, BA 49/08 A, BA 49/08 B, BA 64/08, BA 65/08, BA 266/07 | Theropod dinosaur teeth that resemble with those assigned to members of Megalosauridae and Dromaeosauridae | |
Theropoda | Indeterminate |
| Las Chacritas Member | Isolated Teeth : MPEF PV 1640 | "Outlier" tooth that doesn't fit in any previously known morphotype, maybe due to preservation | |
Theropodipedia[39] | Indeterminate |
| Las Chacritas Member | Footprints | Possible theropod footprints, unassigned to any concrete ichnogenus | |
|
A sediment tubular shaped mass enriched in organic matter, closely associated within the ventral area of articulated remains of a sauropod, was recovered at Cerro Condor, composed of a high concentration of pollen grains & cuticular fragments, mainly leaves of two morphotypes (Araucariaceae and Cheirolepidaceae), probably representing the gut contents of the sauropod, inferring a conifer-based diet.[40]
Possible freshwater "calcareous algae", associated with conifer shoots and aquatic invertebrates, have been reported from Cerro Caracoles.[59]
Genus | Species | Location | Member | Material | Ecogroup | Palaeoclimate requirements | Notes | Images |
---|
Baculatisporites[64] |
|
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Affinities with the family Osmundaceae in the Polypodiopsida. Near fluvial current ferns, related to the modern Osmunda regalis. | |
Biretisporites |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Affinities with the Marattiaceae in the Polypodiopsida. Fern spores from low herbaceous flora. | |
Cadargasporites | - C. sp. cf. C. reticulatus
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Uncertain affinity Fern SporesFilicopsida incertae sedis | |
Cladophlebis |
| - Cañadon Asfalto
- Cañadon Lahuincó
- Paso de Indios
- Pomelo locality
|
| Isolated Pinnae | Lowland and Riverside | Warm to temperate, relatively wet | Plants of the family Osmundaceae. | |
Clavatisporites |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Filicopsida incertae sedis | |
Deltoidospora |
|
|
| Spores | Upland, Lowland and Riverside | Warm to temperate, relatively wet | Affinities with the families Cyatheaceae/Dicksoniaceae Dipteridaceae/Matoniaceae in the Polypodiopsida. | |
Dictyophyllidites |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet |
Gleichenites |
|
|
| Isolated Pinnae | Lowland and Riverside | Warm to temperate, relatively wet | Plants of the family Gleicheniales. | |
Ischyosporites |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Upland, Lowland Riverside | Warm to temperate, relatively wet | Affinities with the family Lygodiaceae and Schizaeaceae in the Polypodiopsida. Climbing or herbaceous fern spores. | |
Klukisporites | - K. lacunus
- K. variegatus
- K. sp. cf. K. scaberis
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Upland, Lowland Riverside | Warm to temperate, relatively wet |
Obtusisporis |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Filicopsida incertae sedis | |
Rugulatisporites |
|
|
| Spores | Lowland and Riverside | Warm to temperate, relatively wet | Affinities with the family Osmundaceae in the Polypodiopsida. | |
Sphenopteris |
| - Cañadon Asfalto
- Cañadon Lahuincó
|
| Isolated Pinnae | Upland, Lowland and Riverside | Warm to temperate, relatively wet | Plants of the group Sphenopteridae, whose affinity for mesozoic specimens is uncertain, yet has been suggested to be fronds of Dicksoniaceae affinity | |
Todisporites |
|
|
| Spores | Upland | Warm to temperate, relatively wet. Can withstand long periods of drought; seasonal climate | Affinities with the family Osmundaceae in the Polypodiopsida. | |
Trilobosporites |
|
|
| Spores | Upland, Lowland and Riverside | Warm to temperate, relatively wet | Affinities with the families Cyatheaceae/Dicksoniaceae Dipteridaceae/Matoniaceae in the Polypodiopsida. | |
Verrucosisporites |
|
|
| Spores | Upland | Can withstand long periods of drought; seasonal climate | Affinities with the family Osmundaceae in the Polypodiopsida. | |
|
Genus | Species | Location | Member | Material | Ecogroup | Palaeoclimate requirements | Notes | Images |
---|
Agathoxylon[68] |
|
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Araucariaceae in the Pinales. | |
Araucariacites | - A. australis
- A. fissus
- A. pergranulatus
- A. cf. A. pergranulatus
- A. sp. A
| - Cañadon Lahuincó
- Cañadón Caracoles
- Cerro Bandera
| - Las Chacritas Member
- Puesto Almada Member
| Pollen | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Araucariaceae in the Pinales. Conifer pollen from medium to large arboreal plants. | |
Araucaritites |
| - Cañadon Asfalto
- Pomelo locality
- A12 locality
- Cañadon Lahuincó
- Estancia La Vistosa
- Paso de Indios
|
| Ovuliferous scales | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Plants of the family Araucariaceae. | |
Athrotaxites |
| - Cañadon Asfalto
- Cañadon Lahuincó
|
| Branched shoots | Upland | ?Warm to temperate, relatively wet | Plants of the family Taxodiaceae | |
Austrohamia[69] |
|
|
| Branched shoots & Ovuliferous cones | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Plants of the family Cunninghamioideae. Along with the also Argentinian species A. minuta, this specimens represent the oldest fossil taxa that can be confidently assigned to Cupressaceae sensu lato | |
Brachyoxylon[70] | B. currumilii |
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Plants of the family Araucariaceae or Cheirolepidiaceae | |
Brachyphyllum | - B. cf. lotenaense
- B. spp.
| - Cañadon Asfalto
- Cerro Caracoles
- Las Chacritas
- Pomelo locality
- A12 locality
- Cañadon Lahuincó
- Paso de Indios
- Canela locality
|
| Branched shoots & Ovuliferous cones | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Plants of the family Araucariaceae or Cheirolepidiaceae | |
Callialasporites | - C. dampieri
- C. microvelatus
- C. turbatus
- C. minus
- C. sp. 1
| - Cañadon Lahuincó
- Cañadón Caracoles
- Cerro Bandera
| - Las Chacritas Member
- Puesto Almada Member
| Pollen | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Araucariaceae in the Pinales. Conifer pollen from medium to large arboreal plants. | |
Cerebropollenites | - C. macroverrucosus
- C. carlylensis
- C. mesozoicus
- C. sp. 1
| - Cañadon Lahuincó
- Cañadón Caracoles
- Cerro Bandera
| - Las Chacritas Member
- Puesto Almada Member
| Pollen | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with both Sciadopityaceae and Miroviaceae in the Pinopsida. This pollen's resemblance to extant Sciadopitys suggest that Miroviaceae may be an extinct lineage of Sciadopityaceae-like plants.[71] | |
Classopollis | - C. classoides
- C. intrareticulatus
- C. simplex
- C. itunensis
- C. torosus
| - Cañadon Lahuincó
- Cañadón Caracoles
- Cerro Bandera
| - Las Chacritas Member
- Puesto Almada Member
| Pollen | Lowland and Coastal lake | Warm to temperate, can withstand long periods of drought; seasonal climate | Affinities with the Hirmeriellaceae in the Pinopsida. Classopollis is the most abundant component of the assemblage, with ranges from 73 to 81.6% to 89.6%-89.7% in some samples. | |
Elatoclaudus | - E. confertus
- E. jabalpurensis
| - Cañadon Asfalto
- Cañadon Lahuincó
- Pomelo locality
|
| Branched shoots | Upland and Lowland | Warm to temperate, can withstand long periods of drought; seasonal climate | Plants of the family Cupressaceae | |
Exesipollenites |
|
|
| Pollen | Lowland and Coastal lake | Warm to temperate, can withstand long periods of drought; seasonal climate | Affinities with the Hirmeriellaceae in the Pinopsida. Classopollis is the most abundant component of the assemblage, with ranges from 73 to 81.6% to 89.6%-89.7% in some samples. | |
Indusiisporites | - I. parvisaccatus
- I. sp. 1
- I. sp. 2
- I. sp. 3
| - Cañadón Lahuincó
- Cañadón Caracoles
|
| Pollen | Upland | Temperate, relatively dry | Affinities with the family Podocarpaceae. Pollen from diverse types of Podocarpaceous conifers, that include morphotypes similar to the low arbustive Microcachrys and the medium arbustive Lepidothamnus, likely linked with Upland settings | |
Inaperturopollenites | - I. indicus
- I. giganteus
- I. microgranulatus
- I. cf. reidi
- I. sp. 1
- I. sp. 2
|
|
| Pollen | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Araucariaceae in the Pinales. Conifer pollen from medium to large arboreal plants. | |
Kaokoxylon |
|
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Araucariaceae in the Pinales. Represents the youngest record of the genus, otherwise know from Permain or Triassic strata.[72] | |
Microcachryidites | - M. castellanosii
- M. antarcticus
| - Cañadón Lahuincó
- Cañadón Caracoles
- Cerro Bandera
| - Las Chacritas Member
- Puesto Almada Member
| Pollen | Upland | Temperate, relatively dry | Affinities with the family Podocarpaceae. Pollen from Podocarpaceous conifers similar to the low arbustive Microcachrys | |
Pagiophyllum | - P. divaricatum
- P. fiestmantelli
| - Cañadon Asfalto
- Pomelo locality
- A12 locality
- Cañadon Lahuincó
- Paso de Indios
- Canela locality
|
| Branched shoots | Lowland and Coastal lake | Warm to temperate, can withstand long periods of drought; seasonal climate | Plants of the family Araucariaceae or Cheirolepidiaceae | |
Pelourdea |
|
|
| Pollen Organs | Lowland and Coastal lake | Warm to temperate, can withstand long periods of drought; seasonal climate | Incertae sedis inside Coniferales, suggested as a member of its own family, the "Pelourdeaceae". A hygrophytic riparian conifer with herbaceous or shrubby habit. Some specimens are difficult to identify. | |
Perinopollenites |
|
|
| Pollen | Upland and Lowland | Warm to temperate; seasonal climate | Affinities with the family Cupressaceae in the Pinopsida. Pollen that resembles that of extant genera such as the genus Actinostrobus and Austrocedrus, probably derived from Upland environments. | |
Phrixipollenites | P. sp. |
|
| Pollen | Upland | Temperate, relatively dry | Affinities with the family Podocarpaceae. | |
Pinuspollenites |
| - Cañadon Lahuincó
- Cañadón Caracoles
|
| Pollen | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Pinaceae in the Pinopsida. Conifer pollen from medium to large arboreal plants. | |
Podocarpidites | - P. verrucosus
- P. astrictus
- P. ellipticus
- P. multesimus
- P. variabilis
- P. sp. cf. P. radiatus
- P. sp. cf. P. verrucosus
- P. sp. 1
| - Cañadón Lahuincó
- Cañadón Caracoles
|
| Pollen | Upland | Temperate, relatively dry | Affinities with the family Podocarpaceae in the Pinopsida. | |
Podocarpoxylon |
|
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Podocarpaceae in the Pinopsida. | |
Podosporites |
| - Cañadón Lahuincó
- Cañadón Caracoles
|
| Pollen | Upland | Temperate, relatively dry | Affinities with the family Podocarpaceae in the Pinopsida. | |
Protocupressinoxylon |
|
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Hirmeriellaceae in the Pinopsida. | |
Prototaxoxylon |
|
|
| Fossil Wood | Upland, Lowland and Riverside | ?Warm to temperate, relatively wet | Affinities with the family Taxaceae in the Pinopsida. Alternatively, it can represent woods of the "Mesozoic Prototaxoxylon Group", a unnamed conifer family of possible Permian affinities.[73] | |
|