Plottier Formation
Geologic formation in Argentina From Wikipedia, the free encyclopedia
The Plottier Formation is a geologic formation that outcrops in the Argentine Patagonian provinces of Río Negro and Neuquén. It is the younger of two formations belonging to the Río Neuquén Subgroup within the Neuquén Group of the Neuquén Basin, with the oldest rocks dating from the late Coniacian and its youngest maybe from the very start of the Santonian. Formerly, that subgroup was treated as a formation, and the Plottier Formation was known as the Plottier Member.[1]
Plottier Formation | |
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Stratigraphic range: late Coniacian-early Santonian ~ | |
Type | Geological formation |
Unit of | Neuquén Group Río Neuquén Subgroup |
Underlies | Río Colorado Subgroup Bajo de la Carpa Formation |
Overlies | Sierra Barrosa Formation |
Thickness | Up to 25 m (82 ft) |
Lithology | |
Primary | Claystone |
Other | Sandstone |
Location | |
Coordinates | 37.4°S 69.1°W |
Approximate paleocoordinates | 42.2°S 49.4°W |
Region | Mendoza, Neuquén & Río Negro Provinces |
Country | Argentina |
Extent | Neuquén Basin |
Type section | |
Named for | Plottier |
Named by | Fossa Mancini et al. |
Year defined | 1938 |
Description
A section near the Neuquén City airport, north of the town of Plottier, is the type locality of the Plottier Formation.[2] At its base, this formation grades into the Portezuelo Formation, and it is in turn overlain conformably by the Bajo de la Carpa Formation, a unit of the Río Colorado Subgroup.
The Plottier Formation is the thinnest formation within the Neuquén Group, with a maximum thickness of only 25 metres (82 ft). It is differentiated from the underlying Portezuelo Formation primarily by its higher content of argillites (mud deposits) and was deposited under fluvial conditions. In 2006, a detailed lithostratigraphic and paleoecological study of a section of the Plottier Formation was published. This section contained alluvial deposits laid down by what was essentially a low-gradient wandering river throughout the millions of years, but often was of a single-channel type with little meandering.[3][1]
Fossil content
Summarize
Perspective
Color key
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Notes Uncertain or tentative taxa are in small text; |
Few animal fossils are known from this formation, including:[4]
Crocodyliformes
Crocodyliformes reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Crocodyliformes indet.[5] | Indeterminate | El Anfiteatro |
|
Resembles peirosaurids such as Peirosaurus and Uberabasuchus | |
Lomasuchus[6][7] | L. palpebrosus | Embalse Cerros Colorados | Skull and partial mandibular ramus | A peirosaurid, specimen originally claimed to originate from the Rio Colorado formation. | |
Mesoeucrocodylia indet.[8] | Indeterminate | Yacimiento Narambuena | Partial skeleton (MAU-PV-N-280) | Subadult specimen showing both derived and primitive traits | |
Peirosauridae indet.[9] | Indeterminate | Puesto Hernández | Partial skeleton (MAU-Pv-PH-437) | A peirosaurid | |
Dinosaurs
Ornithischians
A footprint track of an ornithopod is known from the Middle Loma de la Lata site.[10]
Ornithischians reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Ornithopoda indet.[5][11] | Indeterminate | El Anfiteatro | A pedal ungual phalanx (MPCA-AT 261) | An ornithopod roughly the size of Notohypsilophodon | |
Indeterminate | Puesto Hernández quarry | Partial dorsal neural arch (MAU-Pv-PH-458) | An ornithopod similar to Macrogryphosaurus, estimated to be 6 meters long | ![]() | |
Sauropods
12 footprint tracks of a sauropod are known from the site of Proyecto Dino.[10]
Sauropods reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Aeolosaurini indet.[12] | Indeterminate | Yacimiento Narambuena | Four articulated caudal vertebrae (MAU-Pv-N-414) | A titanosaur | |
Antarctosaurus[13] | A. giganteus | Aguada del Caño | Partial skeleton (MLP 26-316) | A titanosaur | |
Muyelensaurus[14][15] | M. pecheni | Loma del Lindero | Partial skeleton & additional vertebrae | A titanosaur, specimens originally thought to be from the Portezuelo Formation | |
Notocolossus[16][17] | N. gonzalezparejasi | Cerro Guillermo | Two partial skeletons (UNCUYO-LD 301 & UNCUYO-LD 302) | A titanosaur | ![]() |
Petrobrasaurus[18] | P. puestohernandezi | Rincón de los Sauces | Partial skeleton | A titanosaur | ![]() |
Sauropoda indet.[15][17] | Indeterminate | 5 kilometers north of Plottier | Partial right tibia (MCF-PVPH-899) | A sauropod | |
Indeterminate | Cerro Guillermo | Incomplete skeleton (IANIGLA-PV.113) | A sauropod | ||
Titanosauria indet.[5][15] | Indeterminate | El Anfiteatro | Incomplete dorsal vertebra (MPCA-AT 024) | A large titanosaur | |
Indeterminate | 5 kilometers north of Plottier | Remains of titanosaurs | |||
Theropods
Theropods reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Abelisauridae indet.[5][19][20] | Indeterminate | Cañadon Amarillo | Tooth | An abelisaur tooth formerly thought to be part of the holotype specimen of Aerosteon | |
Indeterminate | El Anfiteatro | Tooth (Endemas-PV 16) | An abelisaur, tooth originally reported as that of a carcharodontosaurid in 2009 but reclassified in 2021 | ||
Alvarezsauria indet.[21] | Indeterminate | Rincón de los Sauces | Right femur (MAU-Pv-PH-453) | An alvarezsaur | |
Brachyrostra indet.[22] | Indeterminate | Loma del Lindero | Vertebrae, teeth and possible sacrum (MAU-Pv-LL-75) | An abelisaur | |
cf. Carcharodontosauridae[5] | Indeterminate | El Anfiteatro | Tooth (Endemas-PV 16) | Reclassified as an abelisaur tooth in 2021[20] | |
Coelurosauria indet.[5] | Indeterminate | El Anfiteatro | Two teeth (MPCA-AT 263 & 269) | A coelurosaur | |
Maniraptoriformes indet. cf. Unenlagiinae[5] | Indeterminate | El Anfiteatro | Tooth (Endemas-PV 15) | Possible unenlagiine tooth, though more material is needed to confirm this | |
Theropoda indet.[5] | Indeterminate | El Anfiteatro | Incomplete caudal vertebra (MPCA-AT 082) | A "moderately sized" theropod | |
Pterosaurs
Pterosaurs reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Thanatosdrakon[23] | T. amaru | Agua del Padrillo |
|
An azhdarchid | ![]() |
Turtles
Turtles reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Chelidae? indet.[5] | Indeterminate | El Anfiteatro | Plastron plate (MPCA-AT 089) | A chelid | |
Linderochelys[24] | L. rinconensis | Loma de Lindero | Partial skeleton (MAU-PV-LL-69) | A chelid, locality originally assigned to the Rio Neuquén Subgroup with no specific formation. | |
Rionegrochelys[5][25] | R. caldieroi | El Anfiteatro | Shell elements | A chelid, type specimen first reported as an indeterminate chelid in 2009 | ![]() |
Invertebrates
There are also ichnofossils left on the river's mudflats, as well as fossil freshwater bivalves.[1]
Ostracods
Ostracods reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Cypridoidea indet.[26] | Indeterminate | Zampal | A few specimens | A cypridoid | |
Ilyocypris[26] | I. aff. bauruensis | Zampal | A few molts | An ilyocypridid | |
I. cf. riograndensis | Zampal | An ilyocypridid | |||
I. wichmanni | Zampal | An ilyocypridid | |||
Neocyprideis[26][27] | N.? sp. | Zampal | An ilyocypridid | ||
N. zampalensis | Babilonia | 4 valves | An ilyocypridid | ||
Neuquenocypris[26][27] | N. calfucurensis | Babilonia | 3 valve fragments | An ilyocypridid | |
N. cf. minor | Zampal | An ilyocypridid | |||
N. nahuelniyuensis | Babilonia | 6 valves | An ilyocypridid | ||
N. tenuipunctata | Babilonia | 5 adult and 3 juvenile valves | An ilyocypridid | ||
Paralimnocythere[26] | P.? sp. | Zampal | Several carapaces and valves | A limnocytherid | |
Talicyprideinae sp.[26] | Indeterminate | Zampal | Very scarce number of carapaces | An ilyocypridid | |
Vecticypris[27] | V. sp. | Babilonia | 2 valves | A limnocytherid | |
Wolburgiopsis[26] | W. cf. neocretacea | Zampal | A limnocytherid |
Plants
Plants reported from the Plottier Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Angiospermae? indet.[26] | Indeterminate | Zampal | A few seeds | A possible angiosperm | |
Henrisporites[26] | H. sp. | Zampal | Abundant megaspores | A lycopod | |
Lychnothamnus[26] | L. barbosai | Zampal | Over 400 microfossils | A stonewort | |
Nitella[26] | N. sp. | Zampal | 21 microfossils | A stonewort | |
Spermatites[26] | S. sp. 1 | Zampal | Seeds | An angiosperm | |
S. sp. 2 | Zampal | Seeds | An angiosperm | ||
See also
References
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