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Meridiolestida

Meridiolestida is an extinct clade of dryolestoid cladotherian mammals endemic to Gondwana, primarily South America, spanning from the Cenomanian stage of the Late Cretaceous to the early Miocene.^[1]^[2] Known for their distinctive dental morphology featuring a reversed triangular occlusal pattern in the cheek teeth—lacking the protocone and basined talonid of tribosphenic therians—they represent a non-therian lineage that achieved ecological diversity as insectivores, carnivores, and possibly herbivores.^[1] Fossils are concentrated in Patagonia (Argentina and Chile), with potential Eocene occurrences in Antarctica, highlighting their role in the isolated Mesozoic and early Cenozoic faunas of the region.^[3]^[4] Within Dryolestoidea, Meridiolestida forms a monophyletic group distinct from northern hemisphere dryolestids, encompassing several families such as Mesungulatidae (e.g., Mesungulatum ferox, one of the largest known members reaching up to 1 meter in length) and Reigitheriidae (e.g., Reigitherium, featuring specialized crushing dentition). Recent reassessments have expanded recognized diversity, including the reassignment of Groebertherium to Meridiolestida based on new specimens from the Allen Formation.^[1]^[4]^[5] Other notable genera include Cronopio dentiacutus (a small, shrew-like form from the early Late Cretaceous), Coloniatherium (with bunodont molars suggesting omnivory), and Necrolestes patagonensis (a Miocene survivor extending the clade's temporal range by nearly 45 million years and demonstrating persistence amid therian radiations).^[3]^[6] Recent discoveries, such as Orretherium tzen from the Campanian-Maastrichtian Dorotea Formation in Chile and Yeutherium pressor from subantarctic deposits, underscore their biogeographic extent and evolutionary innovations in tooth replacement and occlusal wear for processing hard foods.^[1]^[4] Phylogenetically, Meridiolestida is positioned as a derived dryolestoid lineage within Cladotheria, sister to other gondwanan dryolestoids, with analyses supporting their divergence in the early Late Cretaceous following isolation of South America.^[1] Their survival across the Cretaceous-Paleogene boundary into the Paleocene and Miocene illustrates a mosaic of faunal turnover in South America, where they coexisted with early metatherians before declining due to competition from invading therians.^[3] This clade's endemism and morphological adaptations provide critical insights into the diversity of Mesozoic mammal evolution outside the therian-dominated northern record.^[7]

Overview

Definition and Etymology

Meridiolestida is an extinct clade of dryolestoid mammals within the larger group Cladotheria, endemic to Gondwana and primarily documented from fossil remains in South America (especially Patagonia), with possible Eocene occurrences in Antarctica; it ranges temporally from the Coniacian stage of the Late Cretaceous to the early Miocene.^[1]^[3] This group represents a significant radiation of non-therian mammals closely related to the broader Dryolestoidea superfamily.^[8] Members of Meridiolestida were particularly dominant in the mammalian faunas of Late Cretaceous South America, where they comprised a substantial portion of the known diversity as one of the non-therian clades phylogenetically closest to the therian lineage.^[9]^[1] Their persistence into the Cenozoic, as evidenced by Miocene records, underscores their evolutionary success in isolation on the southern continent.^[3] The name Meridiolestida was established by José F. Bonaparte in 1990.^[7]

General Characteristics

Meridiolestida displayed considerable morphological diversity, encompassing small insectivores comparable to modern shrews in size (approximately 10–20 g and 10–15 cm long), such as Cronopio dentiacutus, to larger herbivores or omnivores approaching the mass of a large dog (exceeding 20 kg), exemplified by Peligrotherium tropicalis. This range reflects adaptations to varied ecological niches within Gondwanan terrestrial habitats, from insectivory in forested settings to more robust forms suited for browsing in open environments.^[10]^[11]^[12] Meridiolestidans share a distinctive reversed triangular occlusal pattern in the cheek teeth, lacking the protocone and basined talonid of tribosphenic therians, with variations including sectorial dentition in basal forms and bunodont molars (low, rounded cusps suited for grinding vegetation or crushing food) in derived lineages such as mesungulatoids; this distinguishes them from the more sectorial dentitions of basal dryolestoids. Upper molars lack a parastylar hook, facilitating broader occlusal surfaces for processing diverse diets. Additionally, the lower jaw exhibits an absence of the Meckelian groove in adults, signaling an advanced middle ear configuration and divergence from other dryolestoid lineages. These dental and mandibular features underscore the clade's evolutionary specialization within stem therians.^[1]^[9]^[13] The overall body plan of Meridiolestida was quadrupedal, with limb proportions and skeletal robusticity adapted for terrestrial locomotion across the Late Cretaceous landscapes of South America, where the group achieved faunal dominance. Fossorial or semi-fossorial tendencies in some smaller taxa, inferred from cranial and dental specializations, complemented their ground-dwelling lifestyle, enabling exploitation of burrowing niches amid dinosaur-dominated ecosystems.^[14]^[14]

Taxonomy and Phylogeny

Classification History

The earliest known fossils attributable to Meridiolestida were described by Florentino Ameghino in 1891, based on fragmentary remains of Necrolestes patagonensis from the early Miocene of Patagonia, Argentina; Ameghino classified it as an extinct placental insectivore unrelated to modern South American mammals.^[3] Subsequent discoveries of Cretaceous fossils in the 1980s, including Mesungulatum houssayi described by José F. Bonaparte and María F. Soria in 1984 from the Campanian-Maastrichtian Los Alamitos Formation, expanded the group's temporal range and initially led to interpretations as primitive ungulate-like mammals or basal therians, distinct from Laurasian lineages.^[15] Bonaparte formally erected the clade Meridiolestida in 1990 within Dryolestoidea, based on additional material from the same formation, emphasizing shared dental features like reversed triangular molars among taxa such as Mesungulatum, Coloniatherium, and Peligrotherium.^[16] Early classifications often placed meridiolestidans near sparassodont metatherians due to superficial resemblances in postcranial morphology or as basal therians outside crown Theria, reflecting limited material and uncertainties in Mesozoic mammal phylogeny.^[17] A pivotal shift occurred in studies by Guillermo W. Rougier and colleagues in 2011–2012, which incorporated new specimens like Cronopio dentiacutus and revised Reigitherium, firmly establishing Meridiolestida as a monophyletic clade of dryolestoid cladotherians through phylogenetic analyses highlighting synapomorphies such as single-rooted molars and specific angular process morphology. These works resolved prior ambiguities by demonstrating their position as the dominant southern Gondwanan dryolestoids, sister to northern forms. Recent analyses from 2021 to 2024 have refined this framework, addressing debates on paraphyly and broader affinities. A 2013 proposal by Alexander O. Averianov and colleagues suggested meridiolestidans as non-cladotherian trechnotherians based on alternative character scorings, but this was refuted by subsequent datasets. The description of Orretherium tzen in 2021 supported a cladotherian placement within Mesungulatidae, as the earliest diverging member, reinforcing monophyly through dental and mandibular traits.^[1] Similarly, reassessment of Groebertherium in 2024 integrated it into Meridiolestida based on new Allen Formation material, resolving prior exclusion as a dryolestid and stabilizing the clade against paraphyly concerns.^[16] Necrolestes is now recognized as a Miocene survivor of this radiation.^[3]

Phylogenetic Position

Meridiolestida is positioned within Mammaliaformes as a clade of Dryolestoidea, belonging to the broader group Cladotheria, where Dryolestoidea serves as the sister group to Theria (encompassing marsupials and placentals).^[3]^[18] This placement reflects their status as non-therian mammals that diverged before the origin of crown Theria, with Meridiolestida representing a distinct southern Gondwanan radiation adapted to South American ecosystems during the Late Cretaceous.^[3] Phylogenetic analyses incorporating dental and cranial characters consistently recover this relationship, emphasizing Meridiolestida's role in illuminating early cladotherian diversification in Gondwana.^[18] Key synapomorphies linking Meridiolestida to other dryolestoids include specialized dental features such as the presence of a neomorphic cuspulid (cusp e) on lower molars, oriented mesiodistally, and a reduction in the number of premolars, alongside shared traits like a long rostrum and compressed, triangular-cusped teeth.^[3] However, Meridiolestida exhibits unique adaptations, such as bunodont crowns and broad cingulids in derived forms like mesungulatoids, reflecting a trophic shift toward omnivory or herbivory distinct from the more insectivorous northern dryolestids.^[18] These features underscore their endemic evolution in isolation from Laurasian mammal faunas. The phylogenetic position of Meridiolestida remains debated, with some analyses suggesting it as a stem-therian group outside Cladotheria, potentially sister to spalacotheriids within a novel clade Alethinotheria.^[19] This alternative view, based on parsimony analyses of trechnotherian characters, challenges the monophyly of Dryolestoidea by rendering it paraphyletic.^[19] In contrast, more recent studies affirm the monophyly of Meridiolestida as a cohesive, endemic South American lineage within Dryolestoidea, supported by expanded morphological datasets that resolve internal relationships into monophyletic subgroups like Cronopioidea and Mesungulatoidea.^[18]

Included Taxa

Meridiolestida encompasses several families and approximately 10–12 valid genera, primarily known from South American deposits spanning the Late Cretaceous to the early Miocene. The clade is divided into major groups such as Cronopioidea and Mesungulatoidea, with taxa exhibiting diverse adaptations from small insectivores to larger herbivores.^[16]^[1] The family Necrolestidae includes the genus Necrolestes, represented by species such as N. patagonensis and N. mirabilis, which are notable as Miocene survivors of an otherwise Mesozoic radiation, extending the group's temporal range by nearly 45 million years. These small, mole-like forms are characterized by specialized burrowing adaptations and are the most recent known meridiolestidans.^[3] Mesungulatidae comprises larger herbivorous taxa, including Mesungulatum houssayi, Coloniatherium cilinskii, and Orretherium tzen, all from Late Cretaceous deposits in Patagonia and Chile; these genera feature robust dental structures suited for grinding vegetation. Paraungulatum is also tentatively placed within this family based on shared molariform traits. Orretherium tzen represents the earliest diverging member of Mesungulatidae.^[1] Reigitheriidae contains enigmatic carnivorous or omnivorous forms such as Reigitherium bunodontum from the Late Cretaceous of Argentina; these small to medium-sized taxa exhibit crenulated enamel and complex premolars indicative of a varied diet. Yeutherium pressor, described in 2025 from subantarctic deposits, is tentatively placed here based on shared crushing dentition, further extending the biogeographic range.^[1]^[4]^[20] Peligrotheriidae is monotypic, consisting of Peligrotherium tropicalis from the Paleocene of Patagonia; this large, dog-sized genus is distinguished by bunodont molars adapted for a herbivorous diet and represents one of the largest known meridiolestidans.^[3] Basal or cronopioidean genera include Cronopio dentiacutus from the early Late Cretaceous (Cenomanian) Candeleros Formation and Leonardus from the late Late Cretaceous (Campanian-Maastrichtian) Los Alamitos Formation of Argentina, both small insectivores with acute, sectorial teeth for piercing prey. Groebertherium from the Late Cretaceous Allen Formation has been recently reassigned to Meridiolestida from Dryolestidae based on new specimens showing compatible dental morphology.^[3]^[16] Several genera remain incertae sedis within Meridiolestida, including Amarillodon meridionalis from the early Late Cretaceous of Patagonia, known from a single premolar suggesting advanced dental angulation, and Bondesius ferox from the Late Cretaceous, with fragmentary remains indicating possible carnivorous habits. Lakotalestes luoi from the Early Cretaceous of North America has been proposed as a potential extralimital relative based on shared dryolestoid traits, though its exact affinities remain debated.^[21]^[22]^[23]

Anatomy and Morphology

Dental Features

The dentition of Meridiolestida is characterized by a reversed triangular pattern on the molars, lacking tribosphenic features such as a protocone or basined talonid, which distinguishes them from more derived therians.^[1] Upper molars are typically bunodont, featuring low, rounded cusps arranged in a trigon with a prominent paracone and stylocone, but without a metacone or parastylar hook—a key difference from dryolestids, where the parastylar hook connects to the stylocone via the preparacrista.^[1] In larger, more derived forms, the upper molars develop expanded cingula that facilitate grinding, though a true hypocone is absent across the clade.^[24] Tooth counts vary, but commonly include 3–5 premolars and 3–5 molars per quadrant; for instance, Reigitherium exhibits 4 premolars and 3 molars, while Peligrotherium has 2 premolars and 5 molars.^[25]^[24] Lower molars in Meridiolestida feature a triangular trigonid basin formed by the protoconid, paraconid, and metaconid, adapted for shearing, paired with a low talonid that supports crushing functions through crenulated enamel and accessory cuspulids.^[25] The talonid often includes an enclosing structure (enceinte) with intense enamel crenulation, enhancing occlusion in bunodont taxa.^[25] Premolars are generally simple and blade-like in basal forms but become molarized in derived species, contributing to overall dental complexity. Dental variations reflect dietary shifts within Meridiolestida, with insectivorous members like Cronopio dentiacutus displaying sharp, pointed cusps on both upper and lower teeth—such as a tall paracone on uppers and acute protoconid on lowers—for precise cutting and piercing of prey.^[26] In contrast, herbivorous forms like Peligrotherium tropicalis possess broader, low-crowned molars with blunt cusps and fused cingula forming transverse ridges, suited for crushing fibrous plant material.^[24] Evolutionary trends in meridiolestidan dentition show a progression from carnassial-like, shearing morphologies in Late Cretaceous insectivores to more bunodont, grinding adaptations in Paleogene herbivores, bridging plesiomorphic sharp-toothed forms with derived crushing dentitions across the Cretaceous-Paleogene boundary.^[1] This shift correlates with increasing body size and ecological diversification in southern continents.^[1]

Skeletal Morphology

The skeletal morphology of Meridiolestida reflects a conservative body plan relative to therian mammals, retaining several primitive non-therian features while showing adaptations for terrestrial life in Gondwanan environments.^[3] Cranial morphology is characterized by a robust skull structure, including a globular braincase and an upturned rostrum in some taxa, as seen in the Miocene survivor Necrolestes patagonensis. The mandible exhibits a reduced Meckelian groove, a diagnostic feature distinguishing Meridiolestida from more basal dryolestoids.^[3]^[8] Basicranial elements, such as the petrosal bone and large ventral opening of the cavum epiptericum, further align with non-therian patterns, supporting enhanced low-frequency hearing potentially linked to subterranean habits in derived forms.^[3] Postcranial elements indicate adaptations for terrestrial quadrupedalism, with forelimbs showing a parasagittal posture evidenced by a ventrally facing scapular glenoid and well-developed humeral trochlea in mesungulatid taxa. Long bones, including the humerus and femur, are robust in larger species to support body weight, while smaller forms display relatively elongated proportions suited to agile movement. In Necrolestes, the humerus is stout and distally expanded, the ulna features a modified olecranon, and the femur has a shallow patellar groove, all contributing to fossorial capabilities with shortened limbs and inferred strong claws for digging.^[27] Body size varies widely across Meridiolestida, estimated from long bone dimensions and cranial measurements, ranging from approximately 15 cm in length for small insectivores like Cronopio dentiacutus to over 1 m in large mesungulatoids like Mesungulatum ferox, with Peligrotherium tropicalis reaching 50–60 cm.^[28]^[1]

Distribution and Fossil Record

Temporal Range

The fossil record of Meridiolestida primarily spans the Late Cretaceous to the early Miocene, with the earliest definitive records dating to the Coniacian stage (approximately 89–86 Ma) from the Los Bastos Formation in Patagonia, Argentina, representing the oldest known mesungulatoid member of the clade. Earlier potential dryolestoid relatives appear in the Cenomanian (about 100 Ma), marking the onset of their radiation in South America, though unambiguous meridiolestidans are confined to the later Late Cretaceous.^[8] The group underwent its main diversification during the Campanian–Maastrichtian stages (83–66 Ma), achieving peak diversity in South American ecosystems, as evidenced by diverse assemblages from formations such as the Allen Formation.^[16] Following the Cretaceous–Paleogene extinction event, Meridiolestida persisted into the Paleocene (66–63 Ma), exemplified by the genus Peligrotherium from Patagonian deposits, indicating survival of non-therian lineages amid the rise of tribosphenic mammals.^[3] Possible records extend into the Eocene (56–34 Ma), including a tentative brandoniid tooth fragment from the La Meseta Formation on the Antarctic Peninsula, though this material is now lost and requires confirmation.^[29] The clade's final known representatives occur in the early Miocene (23–16 Ma), with Necrolestes patagonensis from the Santa Cruz Formation in Patagonia, extending the group's ghost lineage by nearly 45 million years beyond previous expectations.^[3] Meridiolestida likely declined due to competitive pressures from immigrant therian mammals following the erosion of South America's Gondwanan isolation in the late Cenozoic, with the last confirmed fossils dating to around 18 Ma.^[3] This temporal distribution underscores their role as a relict Gondwanan radiation, bridging Mesozoic and Cenozoic faunas in southern continents.^[1]

Geographic Distribution

Meridiolestida fossils are primarily known from Patagonia in South America, encompassing regions of present-day Argentina and Chile. In Argentina, key occurrences include the Neuquén Basin in Neuquén Province, where specimens have been recovered from the Coniacian Los Bastos Formation, and Río Negro Province, with finds from the Campanian-Maastrichtian Anacleto and Allen Formations.^[8]^[16] Extensions into southern Chile are documented by taxa such as Orretherium tzen from the Late Cretaceous Dorotea Formation in the Río de Las Chinas Valley, Magallanes Region.^[1] A possible record from Antarctica exists based on a tentative identification of a lower molar fragment as ?Meridiolestida from the Eocene La Meseta Formation on [Seymour Island](/page/Seymour Island), though the specimen was lost prior to formal description and requires confirmation.^[30] Meridiolestida exhibit strong Gondwanan endemism, with all confirmed records restricted to southern continents and no verified occurrences in the Northern Hemisphere, aside from the dubious Early Cretaceous Lakotalestes from North America, whose affinities remain uncertain.^[1] Their distribution reflects vicariance following the breakup of Pangea and subsequent Gondwanan fragmentation, limiting dispersal to isolated southern landmasses during the Late Cretaceous.^[1]

Major Discoveries

The earliest significant discovery of a meridiolestidan mammal was that of Mesungulatum houssayi in the 1980s from the Los Alamitos Formation in northern Patagonia, Río Negro Province, Argentina, where an upper molar was initially described as the first Cretaceous mammal from the region, initially misinterpreted as a condylarth before being recognized as a dryolestoid.^[31] This find, based on material collected from outcrops in Río Negro Province, marked a pivotal moment in understanding Mesozoic mammal diversity in South America, as it represented one of the first skeletal elements attributed to the group.^[32] A major advance came in 2011 with the unearthing of Cronopio dentiacutus from the Los Llanos site in Río Negro Province, Argentina, within the early Late Cretaceous Candeleros Formation, yielding two well-preserved skulls and associated postcranial elements that revealed specialized saber-like canines and insectivorous adaptations. This discovery, from the La Buitrera Paleovertebrate Locality, provided the first complete cranial material for a South American meridiolestidan, bridging gaps in early mammalian evolution during the Cretaceous and highlighting nocturnal predatory behaviors. More recent excavations have further enriched the record, including the description of additional dental and dentary fossils of Reigitherium bunodontum in the Late Cretaceous La Colonia Formation of Patagonia, which clarified its bunodont dentition and mesungulatoid affinities, expanding knowledge of dietary diversity within the clade.^[33] In 2021, Orretherium tzen was reported from a partial lower jaw with five cheek teeth discovered in the Late Cretaceous Dorotea Formation near Cerro Guido in southern Chilean Patagonia, representing the southernmost known meridiolestidan and suggesting wider Gondwanan distribution.^[1] An important early specimen is the holotype of Necrolestes patagonensis, described in 1891 from early Miocene strata in Patagonia, Argentina, which consists of a partial skeleton including skull fragments, vertebrae, and limbs recovered from the Santa Cruz Formation.^[3] This near-complete material, long enigmatic and initially classified as a placental insectivore, was reassigned to Meridiolestida in 2012, confirming it as the sole known Cenozoic survivor of the lineage and providing insights into post-Cretaceous persistence.^[3] The 2024 recovery of new mammalian specimens from the Upper Cretaceous Allen Formation in Patagonia, including material referable to Groebertherium, prompted its reassignment from Dryolestidae to Meridiolestida, significantly expanding recognized diversity and refining the phylogeny of Mesungulatoidea through enhanced resolution of dental and mandibular features.^[16] These finds from screenwashing efforts at Cerro Tortuga underscore the untapped potential of the Allen Formation for elucidating late Mesozoic therian evolution in southern continents.^[16] In 2025, Yeutherium pressor was described from a partial maxilla bearing an upper molar in the Late Cretaceous Dorotea Formation, Río de las Chinas Valley, subantarctic Chile. This new reigitheriid taxon, closely related to Reigitherium, features specialized crushing dentition and highlights independent evolution of such adaptations in Meridiolestida, further demonstrating their biogeographic extent and dietary innovations.^[4]

Paleobiology and Evolutionary Role

Diet and Ecology

Members of Meridiolestida exhibited diverse diets inferred primarily from dental morphology. Small-bodied taxa, such as Cronopio dentiacutus, were likely insectivorous, possessing sharp, triangular molars and elongated snouts adapted for capturing and processing insects and other small invertebrates.^[34] In contrast, larger forms like Peligrotherium tropicalis displayed omnivorous to herbivorous adaptations, featuring bunodont molars suited for grinding tough plant material, seeds, and possibly some animal matter, with biomechanical analyses indicating masticatory forces comparable to those of herbivorous ungulates such as the black rhinoceros (Diceros bicornis).^[35] Meridiolestids occupied terrestrial habitats in warm temperate to subtropical environments, including forested floodplains and riverine settings across Patagonia during the Late Cretaceous and early Cenozoic.^[36] Some taxa, notably Necrolestes patagonensis, likely adopted fossorial lifestyles, burrowing in soft soils to exploit subterranean resources, as suggested by their robust cranial features and specialized dentition.^[3] The group's persistently low diversity in post-Cretaceous South America implies effective niche partitioning with co-occurring early marsupials, allowing relictual survival in marginal ecological roles amid the isolation of the continent following the K-Pg boundary.^[3] During the Mesozoic, small meridiolestids such as Cronopio probably served as prey for larger vertebrates, including dinosaurs, in predator-rich ecosystems.^[34] Their endurance into the Cenozoic, exemplified by Peligrotherium and Necrolestes, reflects opportunistic exploitation of vacated niches in isolated South America after the end-Cretaceous extinction, where geographic barriers limited competition from northern therian immigrants.^[3]

Evolutionary Significance

Meridiolestida represents a key clade in mammalian evolution, highlighting diversity among non-therian lineages. As cladotherians within Dryolestoidea, sister to the therian lineage within Cladotheria, they exhibit morphological features that illuminate parallel developments in anatomy to those in therians, particularly in dentition.^[1] Their molars often display a reversed triangular cusp pattern lacking a protocone and basined talonid, though some taxa exhibit bunodont features indicating dietary specialization, while retaining plesiomorphic dryolestoid traits such as reduced premolar count and specialized cingulids.^[1] This dental morphology underscores their role in documenting the evolution of complex mastication in early mammals, providing evidence for the acquisition of features that enabled dietary versatility in parallel lineages.^[5] The clade's Gondwanan radiation exemplifies the underestimated diversity of southern hemisphere mammals during the Mesozoic, prior to the global dominance of therians following the Cretaceous-Paleogene extinction. Meridiolestidans were the predominant mammals in Late Cretaceous South America, diversifying into a range of body sizes and ecologies that filled niches later occupied by therians in northern continents.^[3] Their persistence into the Miocene, as exemplified by the survival of lineages like Necrolestes, demonstrates remarkable resilience amid faunal turnovers, allowing non-therian forms to coexist with incoming therian immigrants for tens of millions of years.^[3] This prolonged Gondwanan persistence highlights a parallel evolutionary trajectory in the south, independent of Laurasian developments.^[37] Recent discoveries challenge traditional northern-biased narratives of mammal evolution by revealing greater taxonomic and morphological diversity among Meridiolestida than previously recognized, informing broader biogeographic patterns of early mammalian dispersal. Studies from 2024, including new material from the Allen Formation, document additional morphotypes and reassign taxa like Groebertherium to the clade, indicating a more extensive herbivore-omnivore guild in Late Cretaceous Patagonia and suggesting that southern mammalian radiations were more precocious and varied.^[5] A 2025 discovery of Yeutherium pressor, a reigitheriid from subantarctic deposits, further highlights specialized crushing dentition as a functional innovation in the clade for processing hard foods.^[4] These findings imply that Gondwanan non-therians played a crucial role in shaping continental faunas, with their innovations contributing to the ecological foundations later exploited by therians.^[37]

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[28]
Dental and mandibular morphology of Peligrotherium tropicalis ...
Apr 29, 2025 · The jaws of Peligrotherium are long and robust. The ventral border of the mandible is slightly convex. Evidence for the dentary in the region of ...Missing: skeletal | Show results with:skeletal
[29]
[PDF] The fossil record of Antarctic land mammals - Arctic Portal Library
Aug 21, 2019 · The disjunct distribution of the monotreme fossil record is currently explained by an australian origin of the group and a later dispersal event.
[30]
https://doi.org/10.13679/j.advps.2019.0021
[31]
(PDF) New Mammalian Remains from the Late Cretaceous La ...
Aug 5, 2025 · Here we describe new mammalian remains collected in outcrops of the La Colonia Formation (Campanian–Maastrichtian) exposed in Chubut Province, ...
[32]
[PDF] Mammals from the Allen Formation, Late Cretaceous, Argentina
Mesungulatum from Los. Alamitos Formation is a medium sized mammal, those from La. Colonia Formation are about 30% larger (Rougier et al., in press), and ...
[33]
https://ri.conicet.gov.ar/handle/11336/81478
[34]
Highly specialized mammalian skulls from the Late Cretaceous of ...
Nov 2, 2011 · Highly specialized mammalian skulls from the Late Cretaceous of South America. Guillermo W. Rougier,; Sebastián Apesteguía &; Leandro C ...
[35]
Reconstructed masticatory biomechanics of Peligrotherium tropicalis ...
Here we present a three-dimensional generalization of the classical “bifulcral” biomechanical model of bite force and joint force estimation.
[36]
The evolution of Patagonian climate and vegetation from the ...
May 31, 2011 · In the Cretaceous and early Palaeogene, the Patagonian floras were situated in a Warm Temperate Biome/climate together with the floras from the ...
[37]
https://www.nature.com/articles/s41598-024-53156-3
[38]
A large therian mammal from the Late Cretaceous of South America
Feb 3, 2024 · We estimate that the body mass of the holotype individual of Patagomaia ranged between 2.6 and 26 kg, with an average estimate of approximately ...Missing: range | Show results with:range<|control11|><|separator|>