This is a list of dinosaurs whose remains have been recovered from South America.
This section needs additional citations for verification .(October 2025) |
| Name | Year | Formation | Location | Notes | Images |
|---|---|---|---|---|---|
| Abelisaurus | 1985 | Anacleto Formation (Late Cretaceous, Campanian) | Only known from a single partial skull | | |
| Achillesaurus | 2007 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Potentially a junior synonym of Alvarezsaurus [1] | | |
| Adamantisaurus | 2006 | Adamantina Formation (Late Cretaceous, Turonian to Maastrichtian) | Derived for a titanosaur as indicated by the ball-and-socket articulations of its caudal vertebrae | | |
| Adeopapposaurus | 2009 | Cañón del Colorado Formation (Early Jurassic, Hettangian to Pliensbachian) | May have had a keratinous beak based on the shape of its jaw bones | | |
| Aeolosaurus | 1987 | Allen Formation?, Angostura Colorada Formation, Lago Colhué Huapí Formation, Los Alamitos Formation?, Serra da Galga Formation? (Late Cretaceous, Campanian to Maastrichtian) | Known from the remains of several individuals | | |
| Aerosteon | 2009 | Anacleto Formation (Late Cretaceous, Campanian) | Its bones were extensively pneumatized, suggesting an air sac system like those of modern birds | | |
| Agustinia | 1999 | Lohan Cura Formation (Early Cretaceous, Aptian to Albian) | Originally described as possessing long, vaguely stegosaur-like spikes, although these turned out to be fragments of ribs and other bones [2] | | |
| Alnashetri | 2012 | Candeleros Formation (Late Cretaceous, Cenomanian) | The oldest alvarezsauroid known from South America | | |
| Alvarezsaurus | 1991 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | One of the largest known alvarezsaurids | | |
| Amargasaurus | 1991 | La Amarga Formation (Early Cretaceous, Barremian to Aptian) | Possessed two parallel rows of backward-pointing spines on its neck that may have been covered by keratin sheaths [3] or a skin sail [4] | | |
| Amargatitanis | 2007 | La Amarga Formation (Early Cretaceous, Barremian to Aptian) | Originally described as a titanosaur [5] although it has since been reinterpreted as a dicraeosaurid [6] | | |
| Amazonsaurus | 2003 | Itapecuru Formation (Early Cretaceous, Aptian to Albian) | Had tall neural spines on its caudal vertebrae | | |
| Amygdalodon | 1947 | Cerro Carnerero Formation (Early Jurassic, Toarcian) | Its teeth were shaped like almonds | | |
| Anabisetia | 2002 | Lisandro Formation (Late Cretaceous, Cenomanian to Turonian) | Four specimens are known but the skull remains incompletely known | | |
| Andesaurus | 1991 | Candeleros Formation (Late Cretaceous, Cenomanian) | Several osteological features indicate a basal position within the Titanosauria | | |
| Aniksosaurus | 2006 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Bone bed remains suggest a gregarious lifestyle [7] | | |
| Antarctosaurus | 1929 | Adamantina Formation?, Anacleto Formation, Plottier Formation? (Late Cretaceous, Coniacian? to Campanian) | Multiple specimens have been assigned to this genus, including some from outside South America, but most may not represent the same taxon | | |
| Anteavis | 2025 | Ischigualasto Formation (Late Triassic, Carnian) | Has several neotheropod-like features despite not being a member of this clade | | |
| Aoniraptor | 2016 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Mostly recovered as a megaraptoran [8] but a recent study recovers this genus as a relative of the enigmatic theropod Bahariasaurus [9] | | |
| Arackar | 2021 | Hornitos Formation (Late Cretaceous, Campanian to Maastrichtian) | The most complete sauropod known from Chile | | |
| Aratasaurus | 2020 | Romualdo Formation (Early Cretaceous, Aptian) | All three of its toes were symmetric | | |
| Argentinosaurus | 1993 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | May be the largest known dinosaur | | |
| Argyrosaurus | 1893 | Lago Colhué Huapí Formation (Late Cretaceous, Campanian to Maastrichtian) | Several remains were historically assigned to this genus, but only the holotype can be confidently assigned to it [10] | | |
| Arrudatitan | 2021 | Adamantina Formation (Late Cretaceous, Campanian to Maastrichtian) | Its tail probably curved strongly downwards, with the tip held very low to the ground [11] | | |
| Asfaltovenator | 2019 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Combines traits of both megalosauroids and allosauroids. Its describers suggest paraphyly of the former group [12] | | |
| Astigmasaura | 2025 | Huincul Formation (Late Cretaceous, Cenomanian) | Despite not being complete, the only known skeleton was fully articulated | | |
| Atacamatitan | 2011 | Tolar Formation (Late Cretaceous, Cenomanian to Maastrichtian) | Only known from a single, fragmentary skeleton | | |
| Aucasaurus | 2002 | Anacleto Formation (Late Cretaceous, Santonian to Campanian) | Known from almost the entire skeleton, including most of the skull | | |
| Austrocheirus | 2010 | Cerro Fortaleza Formation (Late Cretaceous, Campanian to Maastrichtian) | Initially described as an abelisauroid but this has been disputed by subsequent research [13] | | |
| Austroposeidon | 2016 | Presidente Prudente Formation (Late Cretaceous, Campanian to Maastrichtian) | The largest dinosaur known from Brazil | | |
| Austroraptor | 2008 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Possessed an elongated snout paralleling that of spinosaurids | | |
| Baalsaurus | 2018 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | Had a squared-off dentary with its teeth crowded to the front | | |
| Bagualia | 2020 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Represents an early radiation of eusauropods that displaced earlier basal sauropodomorphs after a global warming event [14] | | |
| Bagualosaurus | 2018 | Santa Maria Formation (Late Triassic, Carnian) | Its hindlimbs were very robust | | |
| Bajadasaurus | 2019 | Bajada Colorada Formation (Early Cretaceous, Berriasian to Valanginian) | Possessed elongated, forward-pointing spines erupting in pairs from the neck | | |
| Barrosasaurus | 2009 | Anacleto Formation (Late Cretaceous, Campanian) | Only known from three vertebrae but are well-preserved enough to warrant recognition as a distinct genus | | |
| Baurutitan | 2005 | Serra da Galga Formation (Late Cretaceous, Maastrichtian) | Originally described from an associated series of nineteen vertebrae. New remains were discovered later [15] | | |
| Berthasaura | 2021 | Goio-Erê Formation (Early Cretaceous, Aptian to Albian) | Possessed a short, toothless beak, indicating a herbivorous or omnivorous diet | | |
| Bicentenaria | 2012 | Candeleros Formation (Late Cretaceous, Cenomanian) | Several individuals were preserved together, suggesting a gregarious lifestyle [16] | | |
| Bonapartenykus | 2012 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Its holotype was preserved with two eggs that may have been within its oviducts when it died [17] | | |
| Bonapartesaurus | 2017 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Belongs to the Austrokritosauria, a clade of hadrosaurids endemic to South America [18] | | |
| Bonatitan | 2004 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Analysis of its inner ear suggests a decreased range of head movements compared to other sauropods [19] | | |
| Bonitasaura | 2004 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | The proportions of its body were somewhat similar to those of diplodocoids, likely through convergent evolution | | |
| Brachytrachelopan | 2005 | Cañadón Calcáreo Formation (Late Jurassic, Oxfordian to Tithonian) | Possessed the shortest neck of any known sauropod | | |
| Brasilotitan | 2013 | Adamantina Formation (Late Cretaceous, Maastrichtian) | Had an L-shaped dentary similar to that of Antarctosaurus and Bonitasaura | | |
| Bravasaurus | 2020 | Ciénaga del Río Huaco Formation (Late Cretaceous, Campanian to Maastrichtian) | Discovered close to a large concentration of titanosaur eggs | | |
| Buitreraptor | 2005 | Candeleros Formation (Late Cretaceous, Cenomanian to Turonian) | May have been a pursuit predator due to its long legs [20] | | |
| Buriolestes | 2016 | Santa Maria Formation (Late Triassic, Carnian) | Unlike all other sauropodomorphs, it was completely carnivorous, with serrated teeth to match | | |
| Bustingorrytitan | 2023 | Huincul Formation (Late Cretaceous, Cenomanian) | Large yet distantly related to other gigantic titanosaurs [21] | | |
| Caieiria | 2022 | Serra da Galga Formation (Late Cretaceous, Maastrichtian) | Its caudal vertebrae had an unusual anatomy | | |
| Campananeyen | 2024 | Candeleros Formation (Late Cretaceous, Cenomanian) | Had a notably pneumatized ilium [22] | | |
| Campylodoniscus | 1961 | Bajo Barreal Formation (Late Cretaceous, Cenomanian) | Only known from a single maxilla with seven teeth | | |
| Carnotaurus | 1985 | La Colonia Formation (Late Cretaceous, Maastrichtian) | Possessed a pair of short horns on the top of its skull | | |
| Cathartesaura | 2005 | Huincul Formation (Late Cretaceous, Cenomanian) | Had a well-muscled neck although it could not move strongly up or down | | |
| Chadititan | 2025 | Anacleto Formation (Late Cretaceous, Campanian) | Represents a new fossil locality of the Anacleto Formation [23] | | |
| Chakisaurus | 2024 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Known from various partial skeletons belonging to differently-aged individuals | | |
| Chilesaurus | 2015 | Toqui Formation (Late Jurassic, Tithonian) | Combines traits of theropods, sauropodomorphs and ornithischians, with far-reaching implications for the evolution of the Dinosauria | | |
| Choconsaurus | 2017 | Huincul Formation (Late Cretaceous, Cenomanian) | One of the most completely known basal titanosaurs | | |
| Chromogisaurus | 2010 | Ischigualasto Formation (Late Triassic, Carnian) | Its discovery suggests that early dinosaurs were more diverse than previously thought | | |
| Chubutisaurus | 1975 | Cerro Barcino Formation (Late Cretaceous, Cenomanian) | Unusually, its forelimbs were shorter than its hindlimbs [24] | | |
| Chucarosaurus | 2023 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Smaller and more slender than the contemporary Argentinosaurus | | |
| Cienciargentina | 2025 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | The fourth named rebbachisaurid from the Huincul Formation, suggesting a quick faunal turnover for this group | | |
| Clasmodosaurus | 1898 | Cerro Fortaleza Formation, Mata Amarilla Formation (Late Cretaceous, Cenomanian to Maastrichtian) | Similarly to Bonitasaura , its teeth were polygonal in cross-section | ||
| Coloradisaurus | 1990 | Los Colorados Formation (Late Triassic, Norian) | Originally called Coloradia, although that genus name is preoccupied by a moth | | |
| Comahuesaurus | 2012 | Lohan Cura Formation (Early Cretaceous, Aptian to Albian) | Its holotype was originally assigned to Limaysaurus , but it was named as a separate genus due to several morphological differences | | |
| Condorraptor | 2005 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Closely related to the coeval Piatnitzkysaurus but could be distinguished by several osteological features | | |
| Diuqin | 2024 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Only known from a humerus and fragmentary vertebrae | | |
| Dreadnoughtus | 2014 | Cerro Fortaleza Formation (Late Cretaceous, Campanian to Maastrichtian) | The heaviest land animal whose mass can be calculated with reasonable certainty | | |
| Drusilasaura | 2011 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Potentially the oldest known member of the lognkosaurian lineage [25] | | |
| Ekrixinatosaurus | 2004 | Candeleros Formation (Late Cretaceous, Cenomanian) | Had robust bones, indicating a massive build and a greater resistance to injuries [26] | | |
| Elaltitan | 2012 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Extremely large as indicated by its long femur | | |
| Elemgasem | 2022 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | The first abelisaurid known from the Turonian-Coniacian interval | | |
| Emiliasaura | 2025 | Mulichinco Formation (Early Cretaceous, Valanginian) | Initially described as a rhabdodontomorph, [27] though a later study instead recovers it as a styracosternan [28] | | |
| Eoabelisaurus | 2012 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Shows a transitional arm morphology for an abelisauroid, with a shortened lower arm and hand, along with an unreduced humerus | | |
| Eodromaeus | 2011 | Ischigualasto Formation (Late Triassic, Carnian) | Well-adapted for cursoriality despite its early age [29] | | |
| Eoraptor | 1993 | Ischigualasto Formation (Late Triassic, Carnian) | Possessed different types of teeth, suggesting it was omnivorous | | |
| Epachthosaurus | 1990 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Its caudal vertebrae were procoelous, meaning they were concave at the front and convex at the back | | |
| Erythrovenator | 2021 | Candelária Formation (Late Triassic, Carnian to Norian) | Known from the Riograndia Assemblage Zone, an area which is unusually dominated by cynodonts | | |
| Futalognkosaurus | 2007 | Portezuelo Formation (Late Cretaceous, Coniacian) | Possessed meter-deep cervical vertebrae with distinctive shark fin-shaped neural spines | | |
| Gasparinisaura | 1996 | Anacleto Formation (Late Cretaceous, Campanian) | Known from specimens of both adults and juveniles | | |
| Genyodectes | 1901 | Cerro Barcino Formation (Early Cretaceous, Aptian to Albian) | Had extremely large and protruding teeth | | |
| Giganotosaurus | 1995 | Candeleros Formation (Late Cretaceous, Cenomanian) | One of the largest known terrestrial carnivorous dinosaurs | | |
| Gnathovorax | 2019 | Santa Maria Formation (Late Triassic, Carnian) | Known from a well-preserved, almost complete skeleton | | |
| Gondwanatitan | 1999 | Adamantina Formation, Cambabe Formation? (Late Cretaceous, Maastrichtian) | For a titanosaur, it had relatively gracile limb bones | | |
| Gonkoken | 2023 | Dorotea Formation (Late Cretaceous, Maastrichtian) | The southernmost basal hadrosauroid known to date. Known from more southern latitudes than true hadrosaurids | | |
| Guaibasaurus | 1999 | Caturrita Formation (Late Triassic, Norian) | Combines features of both early theropods and sauropodomorphs | | |
| Gualicho | 2016 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Originally described as having highly reduced arms with only two fingers, convergent with tyrannosaurids, although one study suggests that a third finger was present [30] | | |
| Guemesia | 2022 | Los Blanquitos Formation (Late Cretaceous, Campanian) | Unlike other abelisaurids, it lacked any ornamentation on its skull [31] | | |
| Herrerasaurus | 1963 | Ischigualasto Formation (Late Triassic, Carnian) | One of the largest early carnivorous dinosaurs. Usually considered a basal saurischian but may be just outside the Dinosauria [32] | | |
| Huallasaurus | 2022 | Los Alamitos Formation (Late Cretaceous, Campanian to Maastrichtian) | Remains originally misidentified as belonging to a southern species of Kritosaurus | | |
| Huayracursor | 2025 | Santo Domingo Formation (Late Triassic, Carnian) | Larger and longer-necked than more basal sauropodomorphs. Closely related to Bagualosaurus [33] | | |
| Huinculsaurus | 2020 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | The youngest known elaphrosaurine | | |
| Ibirania | 2022 | São José do Rio Preto Formation (Late Cretaceous, Santonian to Campanian) | May have attained its small size due to its arid inland habitat, unlike other dwarf titanosaurs which were affected by insular dwarfism [34] | | |
| Ilokelesia | 1998 | Huincul Formation (Late Cretaceous, Cenomanian) | Its skull retains some basal abelisauroid traits | | |
| Inawentu | 2024 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Possessed a short neck and squared-off snout, convergent with the rebbachisaurids that went extinct shortly before this genus lived | | |
| Ingentia | 2018 | Quebrada del Barro Formation (Late Triassic, Norian to Rhaetian) | One of the earliest known very large sauropodomorphs [35] | | |
| Irritator | 1996 | Romualdo Formation (Early Cretaceous, Albian) | May have been the apex predator of its habitat, hunting both aquatic and terrestrial prey [36] | | |
| Isaberrysaura | 2017 | Los Molles Formation (Middle Jurassic, Bajocian) | Preserves gut contents including whole seeds | | |
| Isasicursor | 2019 | Chorrillo Formation (Late Cretaceous, Maastrichtian) | Four individuals of different ages were found together, suggesting it lived in herds [37] | | |
| Itapeuasaurus | 2019 | Alcântara Formation (Late Cretaceous, Cenomanian) | The holotype is known from six vertebrae | | |
| Jakapil | 2022 | Candeleros Formation (Late Cretaceous, Cenomanian) | May represent a novel lineage of ornithischians characterized by small size, deep jaws and a bipedal stance | | |
| Joaquinraptor | 2025 | Lago Colhué Huapí Formation (Late Cretaceous, Maastrichtian) | May have preyed upon crocodyliforms as suggested by the associated remains of one [38] | | |
| Kaijutitan | 2019 | Sierra Barrosa Formation (Late Cretaceous, Coniacian) | One of the latest-surviving basal titanosaurs | ||
| Katepensaurus | 2013 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Distinguished by a certain opening in its dorsal vertebrae | | |
| Kelumapusaura | 2022 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Known from the remains of various individuals | | |
| Koleken | 2024 | La Colonia Formation (Late Cretaceous, Maastrichtian) | Contemporary with its larger relative Carnotaurus | | |
| Kurupi | 2021 | Marília Formation (Late Cretaceous, Maastrichtian) | Would have had a stiff tail as indicated by the anatomy of its caudal vertebrae | | |
| Lajasvenator | 2020 | Mulichinco Formation (Early Cretaceous, Valanginian) | One of the smallest known allosauroids | | |
| Lapampasaurus | 2012 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Known from a partial skeleton lacking the skull | ||
| Laplatasaurus | 1929 | Anacleto Formation (Late Cretaceous, Campanian) | Osteoderms have been assigned to this taxon although this referral is uncertain | | |
| Laquintasaura | 2014 | La Quinta Formation (Early Jurassic, Hettangian) | One study recovered it as a basal thyreophoran [39] despite the fact no osteoderms have been found | | |
| Lavocatisaurus | 2018 | Rayoso Formation (Early Cretaceous, Aptian to Albian) | May have possessed a keratinous beak [40] | | |
| Leinkupal | 2014 | Bajada Colorada Formation (Early Cretaceous, Berriasian to Valanginian) | The youngest known diplodocid | | |
| Leonerasaurus | 2011 | Las Leoneras Formation (Early Jurassic, Sinemurian to Toarcian) | Has an unusual combination of basal and derived traits | | |
| Lessemsaurus | 1999 | Los Colorados Formation (Late Triassic, Norian) | Grew very large despite lacking the anatomical traits usually seen as a support for gigantism [35] | | |
| Leyesaurus | 2011 | Quebrada del Barro Formation (Early Jurassic, Hettangian to Toarcian) | Had an unusually small skull | | |
| Ligabueino | 1996 | La Amarga Formation (Early Cretaceous, Barremian to Aptian) | Known from a single, very small skeleton belonging to a juvenile animal | ||
| Ligabuesaurus | 2006 | Lohan Cura Formation (Early Cretaceous, Aptian to Albian) | Its forelimbs were extremely long, with similar proportions to those of brachiosaurids [41] | | |
| Limaysaurus | 2004 | Candeleros Formation, Huincul Formation (Late Cretaceous, Cenomanian) | Possessed elongated neural spines on its dorsal vertebrae | | |
| Llukalkan | 2021 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | May have had a keen sense of hearing due to the shape of its ear [42] | ||
| Loncosaurus | 1899 | Cardiel Formation, Metasiete Formation? (Late Cretaceous, Campanian to Maastrichtian) | Poorly known | ||
| Loricosaurus | 1929 | Allen Formation (Late Cretaceous, Maastrichtian) | Potentially synonymous with Neuquensaurus or Saltasaurus | ||
| Lucianovenator | 2017 | Quebrada del Barro Formation (Late Triassic, Norian to Rhaetian) | One of the few theropods known from the Rhaetian | | |
| Macrocollum | 2018 | Candelária Formation (Late Triassic, Norian) | One of the oldest sauropodomorphs with an extremely elongated neck | | |
| Macrogryphosaurus | 2007 | Sierra Barrosa Formation (Late Cretaceous, Coniacian) | Preserves a series of mineralized plates along the side of the torso | | |
| Mahuidacursor | 2019 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Its holotype was sexually mature but not fully grown | ||
| Maip | 2022 | Chorrillo Formation (Late Cretaceous, Maastrichtian) | The largest known megaraptoran | | |
| Malarguesaurus | 2008 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | Large and robustly built | ||
| Manidens | 2011 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | May have been arboreal due to the structure of its feet, with toes adapted for grasping [43] | | |
| Mapusaurus | 2006 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | At least seven specimens of different growth stages are known, possibly suggesting that this taxon lived and/or hunted in packs | | |
| Maxakalisaurus | 2006 | Adamantina Formation (Late Cretaceous, Maastrichtian) | Unusually for a sauropod, it had ridged teeth | | |
| Megaraptor | 1998 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | Possessed a large, strongly curved claw on its first finger | | |
| Mendozasaurus | 2003 | Sierra Barrosa Formation (Late Cretaceous, Coniacian) | Had spherical osteoderms that were probably located in rows along the flanks [44] | | |
| Menucocelsior | 2022 | Allen Formation (Late Cretaceous, Maastrichtian) | Coexisted with multiple other titanosaurs that may have niche-partitioned [45] | ||
| Meraxes | 2022 | Huincul Formation (Late Cretaceous, Cenomanian) | Possessed reduced forelimbs convergent with several other groups of theropods | | |
| Microcoelus | 1893 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | May be a synonym of Neuquensaurus | | |
| Mirischia | 2004 | Romualdo Formation (Early Cretaceous, Albian) | Its holotype preserves an intestine | | |
| Murusraptor | 2016 | Sierra Barrosa Formation (Late Cretaceous, Coniacian) | Had a brain morphology similar to that of tyrannosaurids but its sensory capabilities were closer to the level of allosauroids [46] | | |
| Mussaurus | 1979 | Laguna Colorada Formation (Early Jurassic, Sinemurian) | Multiple specimens from different growth stages are known. Juveniles may have been quadrupedal and shifted to bipedality as adults [47] | | |
| Muyelensaurus | 2007 | Plottier Formation (Late Cretaceous, Coniacian to Santonian) | Relatively gracile for a titanosaur | ||
| Narambuenatitan | 2011 | Anacleto Formation (Late Cretaceous, Campanian) | Its neural spines are very similar to those of Epachthosaurus | | |
| Neuquenraptor | 2005 | Portezuelo Formation (Late Cretaceous, Coniacian) | Potentially synonymous with Unenlagia [48] | | |
| Neuquensaurus | 1992 | Anacleto Formation (Late Cretaceous, Campanian) | One of the smallest known titanosaurs | | |
| Nhandumirim | 2019 | Santa Maria Formation (Late Triassic, Carnian) | Originally described as a theropod [49] but has since been reinterpreted as a sauropodomorph [50] | | |
| Niebla | 2020 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Had a uniquely built scapulocoracoid very similar to that of Carnotaurus | | |
| Ninjatitan | 2021 | Bajada Colorada Formation (Early Cretaceous, Berriasian to Valanginian) | The oldest known titanosaur | ||
| Noasaurus | 1980 | Lecho Formation (Late Cretaceous, Campanian to Maastrichtian) | Originally mistakenly believed to have possessed a dromaeosaurid-like sickle claw | | |
| Nopcsaspondylus | 2007 | Candeleros Formation (Late Cretaceous, Cenomanian) | Named from a single, lost vertebra | | |
| Notoceratops | 1918 | Lago Colhué Huapí Formation (Late Cretaceous, Campanian to Maastrichtian) | Originally described as a ceratopsian but this identity is today doubted | | |
| Notocolossus | 2016 | Plottier Formation (Late Cretaceous, Coniacian to Santonian) | Unusually for a sauropod, its unguals were truncated | | |
| Notohypsilophodon | 1998 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Only known from a juvenile skeleton without the skull | | |
| Nullotitan | 2019 | Chorrillo Formation (Late Cretaceous, Campanian to Maastrichtian) | Would have niche-partitioned with smaller ornithopods | | |
| Orkoraptor | 2008 | Cerro Fortaleza Formation (Late Cretaceous, Campanian) | Had highly specialized dentition similar to that of coelurosaurs | | |
| Overoraptor | 2020 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Shows adaptations for both flight and cursoriality | | |
| Overosaurus | 2013 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | One of the smallest known aeolosaurins | | |
| Padillasaurus | 2015 | Paja Formation (Early Cretaceous, Barremian) | Originally described as a brachiosaurid [51] although it could also be a somphospondylian [52] | | |
| Pampadromaeus | 2011 | Santa Maria Formation (Late Triassic, Carnian) | Some features of its jaws are similar to those of theropods | | |
| Pamparaptor | 2011 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | Had a troodontid-like metatarsal | | |
| Panamericansaurus | 2010 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Known from a single partial skeleton | ||
| Pandoravenator | 2017 | Cañadón Calcáreo Formation (Late Jurassic, Oxfordian to Tithonian) | Inconsistent in phylogenetic placement | ||
| Panphagia | 2009 | Ischigualasto Formation (Late Triassic, Carnian) | Was omnivorous as indicated by its heterodont dentition | | |
| Patagonykus | 1996 | Portezuelo Formation (Late Cretaceous, Turonian to Coniacian) | Its discovery allowed researchers to connect Alvarezsaurus to parvicursorines [53] | | |
| Patagopelta | 2022 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Although originally described as a nodosaurid, later analyses recover it as a parankylosaurian [54] | | |
| Patagosaurus | 1979 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Known from remains of adults and juveniles, depicting how various features developed in sauropods as they aged | | |
| Patagotitan | 2017 | Cerro Barcino Formation (Early Cretaceous, Albian) | One of the largest dinosaurs known from reasonably complete remains | | |
| Pellegrinisaurus | 1996 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | May have lived inland unlike other contemporaneous titanosaurs [55] | | |
| Perijasaurus | 2022 | La Quinta Formation (Early Jurassic to Middle Jurassic, Toarcian to Aalenian) | Only known from a single vertebra | | |
| Petrobrasaurus | 2011 | Plottier Formation (Late Cretaceous, Coniacian to Santonian) | Shares somes features with lognkosaurs, but its membership within this clade cannot be confirmed | | |
| Piatnitzkysaurus | 1979 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | One of the few early theropods with a well-preserved braincase | | |
| Pilmatueia | 2019 | Mulichinco Formation (Early Cretaceous, Valanginian) | Had elongated spines on its cervical vertebrae, although they were not as tall as those of Amargasaurus and Bajadasaurus [56] | | |
| Pitekunsaurus | 2008 | Anacleto Formation (Late Cretaceous, Campanian) | Known from several bones from different parts of the body, including a braincase | | |
| Powellvenator | 2017 | Los Colorados Formation (Late Triassic, Norian) | Some of this genus' remains were originally associated with those of a pseudosuchian [57] | ||
| Puertasaurus | 2005 | Cerro Fortaleza Formation (Late Cretaceous, Campanian to Maastrichtian) | Large but only known from very few remains | | |
| Punatitan | 2020 | Ciénaga del Río Huaco Formation (Late Cretaceous, Campanian to Maastrichtian) | Contemporary with Bravasaurus but was most likely distantly related [58] | ||
| Pycnonemosaurus | 2002 | Cachoeira do Bom Jardim Formation (Late Cretaceous, Campanian to Maastrichtian) | Potentially the largest known abelisaurid [59] | | |
| Quetecsaurus | 2014 | Lisandro Formation (Late Cretaceous, Turonian) | Its humerus has a unique shape | | |
| Quilmesaurus | 2001 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Had proportionally robust legs despite its small size | | |
| Rayososaurus | 1996 | Candeleros Formation (Late Cretaceous, Cenomanian) | Very similar to Rebbachisaurus despite being only known from scant remains | | |
| Rinconsaurus | 2003 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Unusually, its caudal vertebrae had a repeating pattern of procoely, amphicoely, opisthocoely and biconvex states | | |
| Riojasaurus | 1969 | Los Colorados Formation (Late Triassic, Norian) | Although commonly depicted as quadrupedal, the structure of its shoulder girdle suggests it may have potentially been bipedal | | |
| Rocasaurus | 2000 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | Small for a sauropod yet was very robust | | |
| Saltasaurus | 1980 | Lecho Formation (Late Cretaceous, Maastrichtian) | Possessed osteoderms in the form of large round nodules connected by a mass of smaller plates | | |
| Sanjuansaurus | 2010 | Ischigualasto Formation (Late Triassic, Carnian) | Coexisted with Herrerasaurus but most likely represents a separate taxon | | |
| Santanaraptor | 1999 | Romualdo Formation (Early Cretaceous, Aptian to Albian) | Preserves soft tissues including the remains of skin, muscle and possibly blood vessels [60] [61] | | |
| Sarmientosaurus | 2016 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Analysis of its inner ear suggests it held its head downwards, possibly indicating a preference for low-growing plants | | |
| Saturnalia | 1999 | Santa Maria Formation (Late Triassic, Carnian) | Known from at least three partial skeletons | | |
| Secernosaurus | 1979 | Lago Colhué Huapí Formation (Late Cretaceous, Maastrichtian) | Would have lived in an arid gypsum desert [62] | | |
| Sektensaurus | 2019 | Lago Colhué Huapí Formation (Late Cretaceous, Campanian) | The first non-hadrosaurid ornithopod recovered from central Patagonia | ||
| Sidersaura | 2024 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | One of the largest known rebbachisaurids | | |
| Skorpiovenator | 2009 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Had an unusually short, deep skull | | |
| Spectrovenator | 2020 | Quiricó Formation (Early Cretaceous, Barremian to Aptian) | Its holotype was found underneath a sauropod skeleton | | |
| Staurikosaurus | 1970 | Santa Maria Formation (Late Triassic, Carnian) | May have been a rare component of its environment as only two specimens are known | | |
| Stegouros | 2021 | Dorotea Formation (Late Cretaceous, Campanian to Maastrichtian) | Possessed a "macuahuitl" at the end of its tail, made of a connected "frond" of pointed osteoderms | | |
| Tachiraptor | 2014 | La Quinta Formation (Early Jurassic, Hettangian) | Closely related to ceratosaurs and tetanurans [63] | | |
| Talenkauen | 2004 | Cerro Fortaleza Formation (Late Cretaceous, Campanian to Maastrichtian) | May have practiced parental care as an adult and a hatchling have been found together | | |
| Tapuiasaurus | 2011 | Quiricó Formation (Early Cretaceous, Aptian) | One of the few titanosaurs from which a complete skull is known | | |
| Taurovenator | 2016 | Huincul Formation (Late Cretaceous, Cenomanian) | Originally known from a single postorbital. Additional remains were described in 2024 [64] | | |
| Tehuelchesaurus | 1999 | Cañadón Calcáreo Formation (Late Jurassic, Oxfordian to Tithonian) | Preserves impressions of scaly skin | | |
| Thanos | 2020 | São José do Rio Preto Formation (Late Cretaceous, Santonian) | Only known from a single vertebra. The generic name honors the Marvel Comics villain Thanos | | |
| Tiamat | 2024 | Açu Formation (Early Cretaceous to Late Cretaceous, Albian to Cenomanian) | Named after a Mesopotamian goddess | | |
| Tietasaura | 2024 | Marfim Formation (Early Cretaceous, Valanginian to Hauterivian) | The first unambiguous ornithischian genus described from Brazil [65] | | |
| Titanomachya | 2024 | La Colonia Formation (Late Cretaceous, Maastrichtian) | The morphology of its astragalus is intermediate between members of the Colossosauria and Saltasauroidea [66] | | |
| Tralkasaurus | 2020 | Huincul Formation (Late Cretaceous, Cenomanian to Turonian) | Exhibits a conflicting blend of characteristics from basal and derived abelisauroids | ||
| Tratayenia | 2018 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | One of the youngest known megaraptorans [67] | | |
| Traukutitan | 2011 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Retained basal features in its caudal vertebrae despite its late age | ||
| Trigonosaurus | 2005 | Serra da Galga Formation (Late Cretaceous, Maastrichtian) | Potentially synonymous with Baurutitan [15] | | |
| Triunfosaurus | 2017 | Rio Piranhas Formation (Early Cretaceous, Berriasian to Valanginian) | Originally described as a titanosaur [68] but similarities have been noted with basal somphospondylians [69] | ||
| Tyrannotitan | 2005 | Cerro Barcino Formation (Early Cretaceous, Albian) | Unlike other carcharodontosaurids, its sacral and caudal vertebrae were not pneumatic | | |
| Uberabatitan | 2008 | Serra da Galga Formation (Late Cretaceous, Maastrichtian) | Several individuals are known, some of which are very large | | |
| Udelartitan | 2024 | Guichón Formation (Late Cretaceous, Cenomanian to Santonian) | Known from at least two fragmentary specimens | | |
| Unaysaurus | 2004 | Caturrita Formation (Late Triassic, Carnian to Norian) | Described as the first plateosaurid-grade sauropodomorph from Brazil | | |
| Unenlagia | 1997 | Portezuelo Formation (Late Cretaceous, Coniacian) | Could potentially be adapted for flapping due to the structure of its shoulder girdle [70] | | |
| Unquillosaurus | 1979 | Los Blanquitos Formation (Late Cretaceous, Maastrichtian) | Has been suggested to be a dromaeosaurid [71] or a carcharodontosaurid [72] | ||
| Velocisaurus | 1991 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | Unusually, its third metatarsal is the thickest, which may be an adaptation to running | | |
| Vespersaurus | 2019 | Rio Paraná Formation (Early Cretaceous to Late Cretaceous, Aptian to Campanian) | Possessed raised claws on its second and fourth toes, making it functionally monodactyl, a possible adaptation to its desert habitat | | |
| Viavenator | 2016 | Bajo de la Carpa Formation (Late Cretaceous, Santonian) | May have relied on quick movements of its head and gaze stabilization when hunting | | |
| Vitosaura | 2025 | Los Llanos Formation (Late Cretaceous, Campanian) | One of the few Argentinian ceratosaurs discovered outside of Patagonia | | |
| Volkheimeria | 1979 | Cañadón Asfalto Formation (Early Jurassic, Toarcian) | Coexisted with at least four other eusauropods | ||
| Willinakaqe | 2010 | Allen Formation (Late Cretaceous, Campanian to Maastrichtian) | As originally described, it represented a chimera of two different taxa, one of which was later named Bonapartesaurus [73] | | |
| Xenotarsosaurus | 1986 | Bajo Barreal Formation (Late Cretaceous, Cenomanian to Turonian) | Its astragalus and calcaneum had an unusual shape | | |
| Yamanasaurus | 2019 | Río Playas Formation (Late Cretaceous, Campanian to Maastrichtian) | The northernmost saltasaurine known to date [58] | | |
| Ypupiara | 2021 | Serra da Galga Formation (Late Cretaceous, Maastrichtian) | May have been a piscivore due to the shape of its teeth [74] | | |
| Zapalasaurus | 2006 | La Amarga Formation (Early Cretaceous, Hauterivian to Aptian) | Known from an incomplete skeleton, including several caudal vertebrae | | |
| Zupaysaurus | 2003 | Los Colorados Formation (Late Triassic, Norian) | Although commonly depicted with head crests, they may in fact be misplaced lacrimal bones [75] | |
This is a timeline of selected dinosaurs from the list above. Time is measured in Ma, megaannum, along the x-axis. Carnivores are shown in red, herbivores in green and omnivores in blue.

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