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Maip
Temporal range: Late Cretaceous, early? Maastrichtian[1]
Known material (A), reconstruction of the thoracic cavity at level of sixth dorsal vertebra (B), and interpretative drawing of the excavation (C)
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Clade: †Megaraptora
Family: †Megaraptoridae
Genus: †Maip
Aranciaga Rolando et al., 2022
Species:
†M. macrothorax
Binomial name
†Maip macrothorax
Aranciaga Rolando et al., 2022

Maip is a genus of large megaraptorid theropod dinosaur from the Late Cretaceous (Maastrichtian) Chorrillo Formation of Santa Cruz, Argentina. The genus contains a single species, M. macrothorax, known from an incomplete, disarticulated skeleton. Maip may represent the largest megaraptorid known from South America, and possibly the world.[2]

Discovery and naming

[edit]
Holotype bones

The Maip holotype specimen, MPM 21545, was discovered by Alexis Rolando on the La Anita Farm, 30 kilometres (19 mi) west of El Calafate, Santa Cruz province, Argentina, in 2019. The specimen was found disarticulated but in association over an area of 5 by 3 square metres (54 sq ft × 32 sq ft). The known fossil material consists of the axis, several dorsal and caudal vertebrae, cervical and dorsal ribs, gastralia, a left coracoid, fragmentary scapula, partial right pubis, and partial metatarsal. Some of these bones were described in 2019 by Novas et al.[3] The holotype specimen includes some bones previously unknown in other megaraptorids. Although fragmentary, it represents one of the most complete megaraptorid skeletons known.[2]

Maip was first announced in a Research Square preprint in 2021. However, since the paper did not meet the necessary requirements, the taxon was considered informally named.[4] In 2022, the fossil material was validly described as belonging to a new genus and species of megaraptorid by Aranciaga Rolando et al. The generic name, "Maip", references a malicious being in Aonikenk mythology that is "the shadow of death" that "kills with cold wind." The specific name, "macrothorax", is derived from the Greek "makrós", meaning "large", and the Latin "thorax", meaning "chest", in reference to its large thoracic cavity.[2]

Description

[edit]
Size compared to a human

Maip is estimated to have been around 9–10 metres (30–33 ft) long in life. As such, it may be the largest megaraptorid currently known. Members of the Megaraptoridae as a whole increased in body length following the extinction of the carcharodontosaurids in the Southern Hemisphere in the early Late Cretaceous.[5] It is hypothesized that the absence of these large apex predators allowed other theropods to diversify and fill the empty niche space. Megaraptorids, in addition to abelisaurids and unenlagiids, then became the primary predators in their ecosystems. An analysis of known megaraptorans shows that members of the clade in Asia, South America, and Australia ranged from 4–4.5 metres (13–15 ft) long during the Barremian-Aptian, after which Aptian-early Turonian forms increased to 4.5–6 metres (15–20 ft) in Australia and South America. Turonian-Coniacian megaraptorids, only known from South America, were larger, at 6–7 metres (20–23 ft) long, and the final Santonian-Maastrichtian forms were larger still, at 7–10 metres (23–33 ft).[2]

Traces on the preserved ribs were interpreted by the describing authors as being attachment points for ligaments. From these, it was inferred that Maip would have likely had a respiratory system comparable to those of modern birds, rather than those of other extant reptiles, such as crocodilians.[2]

Classification

[edit]
Life restoration

In their phylogenetic analyses, Aranciaga Rolando et al. (2022) recovered Maip as a derived megaraptorid in a polytomy with other Argentinian megaraptorids. They also noted the presence of two distinct clades: a more inclusive clade, comprising all megaraptorids except Fukuiraptor and Australovenator, (shown below as "Clade A"), and a more exclusive clade of larger, entirely South American megaraptorids (shown below as "Clade B"). Like some previous analyses by other authors, Megaraptora is nested within Coelurosauria, as the sister taxon to Tyrannosauroidea. The cladogram below displays the megaraptoran results of the phylogenetic analyses by Aranciaga Rolando et al. (2022).[2]

Megaraptora

Phuwiangvenator

Vayuraptor

Fukuiraptor

Megaraptoridae

Australian megaraptorid indet. (LRF 100–106)

Australovenator

"Clade A"

Aoniraptor

Bajo Barreal Formation megaraptorid indet. (UNPSJB-Pv 944/958)

Paleoecology

[edit]
Dinosaurs named from the Chorrillo Formation (Maip in dark orange, center)

Maip is known from the Maastrichtian-dated Chorrillo Formation of southern Argentina. Other named dinosaurs known from the formation include Isasicursor, an elasmarian ornithopod, and Nullotitan, a titanosaurian sauropod.[3] Indeterminate remains belonging to ankylosaurs, euiguanodontians, hadrosaurids, noasaurids, and unenlagiids have also been recovered from the formation. Fossils of indeterminate anurans, fish, mammals, mosasaurs, snakes, turtles, and gastropods are also known.[6] Very fragmentary fossil material, including teeth and a dorsal centrum, has been classified as having megaraptorid affinities, but it is too fragmentary to be assigned to Maip or any other taxon.[2]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

Maip

View on Grokipedia
from Grokipedia
Maip is a of large megaraptorid theropod that lived during the period, approximately 70 to 66 million years ago, in what is now , . The type and only known , M. macrothorax, is represented by an incomplete including vertebrae, ribs, and a , discovered in the Maastrichtian at La Anita Farm near , Santa Cruz Province. Named after an entity from Aonikenk (Tehuelche) mythology meaning "," with "macrothorax" referring to its notably wide measuring about 1.2 meters across, Maip measured roughly 9.5 meters in and is estimated to have weighed approximately 5 tons (based on 2022 analyses), making it one of the largest known megaraptorids and among the final non-avian dinosaurs before the . As a member of the clade within , Maip exhibits specialized anatomical features typical of its group, such as elongated manual claws for predation and a robust with progressive pneumaticity that likely aided in supporting its massive frame while reducing weight. The specimen, unearthed by a team from the Argentine (MACN-CONICET), provides crucial insights into the late evolution of megaraptorids in southern , where they diversified as apex predators following the decline of earlier large theropods like carcharodontosaurids. Phylogenetic analyses place Maip within a derived South American clade including genera like , , and , underscoring the group's persistence until the end of the ; a 2025 study further describes Joaquinraptor casali, another Maastrichtian megaraptorid from a nearby formation, highlighting ongoing discoveries of late theropod diversity. Notable traits include saddle-shaped parapophyses on mid-dorsal vertebrae and a with a prominent anterior projection, features that distinguish it from earlier megaraptorids and suggest adaptations for powerful use in hunting large prey. This discovery, detailed in a 2022 study by Novas et al., enriches our understanding of theropod diversity in the final stages of the dinosaur era.

Discovery and etymology

Discovery history

The specimen of Maip macrothorax, cataloged as MPM 21,545, was discovered in 2019 during a paleontological expedition in the on Estancia La Anita farm, approximately 30 km southwest of in . The initial find, led by Argentine paleontologist Mauro Aranciaga Rolando along with a team from the National Scientific and Technical Research Council (CONICET), included exposed bones that prompted further excavation. Excavation efforts recovered an incomplete but substantial disarticulated spread over a 5 × 3 m area within a sedimentary bed no thicker than 1 m, preserving elements such as the axis vertebra, multiple dorsal vertebrae (including dorsals 2–7 and 9–13), caudal vertebrae, , , a partial left , pubis, and partial metatarsal II. The work was conducted by a multidisciplinary team including Aranciaga Rolando, Matías J. Motta, Federico L. Agnolín, and international collaborators, though the global in 2020 temporarily halted field activities after the initial recovery phase. This specimen stands out for its preservation and relative completeness among megaraptorid theropods, providing key thoracic and axial material that was previously scarce for the group. The formal scientific description of Maip macrothorax was published in 2022 by Aranciaga Rolando, Motta, Agnolín, and colleagues in Scientific Reports, establishing it as a new genus and species within Megaraptoridae based on the Chorrillo Formation material. This publication marked the first naming of a megaraptorid from the Maastrichtian stage in southern Patagonia, highlighting the specimen's significance in late Cretaceous theropod research.

Etymology

The genus name Maip is derived from the Aonikenk (Tehuelche) mythology of the of , where it refers to a malevolent, shadow-like spirit of known as "" that brings darkness, eclipses, and kills with a cold wind while roaming the mountains. This naming choice honors the Tehuelche heritage and evokes the dinosaur's predatory as a formidable apex hunter in its Late environment. The species epithet macrothorax combines the Greek words makros (large) and thōrax (chest), alluding to the notably expanded in the specimen, which measures over 1.20 meters in width and distinguishes it among megaraptorids. By incorporating both indigenous cultural elements and classical , the binomial Maip macrothorax underscores the fossil's ties to Patagonian indigenous traditions while highlighting its unique skeletal features.

Description

Size and morphology

Maip macrothorax is estimated to have reached a body length of approximately 9–10 meters (30–33 feet), making it the largest known member of the Megaraptoridae family, with comparisons drawn to related taxa such as riccolorum for scaling skeletal proportions. Weight estimates place it at up to 5 tons, reflecting its substantial build as one of the terminal large-bodied theropods of the . This size underscores its role as a dominant predator, with a robust overall morphology characterized by a deep and broad thoracic region—evident from preserved vertebrae and ribs measuring approximately 1.4 meters in width—that provided structural support for its massive frame. The dinosaur's body plan featured extensive pneumaticity in the vertebrae and ribs, indicating an inferred bird-like with that likely enhanced oxygen intake and lightened the for efficiency in a large theropod. This , observed in the holotype's , aligns with trends in derived coelurosaurs and suggests improved respiratory capacity suited to its active predatory lifestyle. Within Megaraptoridae, Maip represents an evolutionary peak in body size, with South American members of the clade showing a progressive increase from around 5–6 meters in earlier forms to 8–10 meters by the Maastrichtian, coinciding with the decline of larger carcharodontosaurid competitors and allowing megaraptorids to occupy apex niches in southern continents.

Anatomical features

The holotype specimen of Maip macrothorax (MPM 21,545) consists of an incomplete, disarticulated skeleton preserving elements primarily from the axial and appendicular skeleton, with no cranial material recovered. The axial skeleton includes the axis vertebra, which is proportionately dorsoventrally low and taller than long, featuring a low and robust neural spine less than half the height of the neural arch, a rugose subtriangular intercentrum, and a single pneumatopore on each side indicating pneumatic invasion. Mid-dorsal vertebrae (D2–D7 and D9–D13) exhibit robust construction with camellate internal texture and well-developed pneumatic fossae; a notable autapomorphy is the saddle-shaped articular surface of the parapophyses on D6, while transverse processes are upturned at approximately 30° and reinforced by prominent laminae such as the pre- and postspinal laminae. Ribs associated with the cervical and dorsal regions show evidence of pneumatization, with foramina and a honeycomb-like internal structure on the tuberculum of the first dorsal rib (DR1), consistent with advanced respiratory adaptations in megaraptorids; related taxa like Aerosteon riocoloradensis possess ossified uncinate processes extending caudally from the ribs, which enhance thoracic rigidity and efficiency in costal movements during breathing. The thoracic cavity is markedly expanded, termed "macrothorax," with a width of approximately 1.4 m at the level of D6, supported by large dorsal ribs and gastralia segments reconstructing to up to 60 cm in length for medial elements, suggesting increased thoracic volume potentially linked to enhanced lung capacity or muscle attachments. In the pectoral girdle, the left is preserved as a robust, ovoid element more than twice as tall as long, characterized by a prominent anterior projection (an autapomorphy), absence of a subglenoid , and a deep ventromedial margin for articulation with the . The pelvic girdle includes only a proximal fragment of the right pubis, which appears elongated based on the preserved shaft portion, aligning with the slender, rod-like pubes typical of megaraptorids for supporting a narrow . A distal portion of metatarsal II from the is preserved, indicating a robust consistent with powerful pedal support in this , though proximal details are lacking. No manual elements are preserved in Maip, but as a megaraptorid, it likely possessed the derived hand morphology of the group, featuring elongated digits with large, curved manual adapted for slashing or grappling prey, as seen in relatives like wintonensis where the primary reaches approximately 30 cm in length. Cranial material is absent, precluding direct observation of the ; however, in megaraptorids is inferred to consist of robust, labiolingually compressed teeth with strongly concave distal margins, fine denticles along both carinae, and D-shaped cross-sections suited for piercing and tearing flesh.

Classification

Taxonomic placement

Maip is a genus of large theropod dinosaur from the of , , formally classified under the binomial name Maip macrothorax Aranciaga Rolando et al., 2022. The taxon is placed within , more specifically in the clade , and recognized as a member of Megaraptoridae, a family of large-bodied carnivorous theropods primarily known from South American deposits. Megaraptoridae is characterized by hypertrophied manual unguals and robust forelimbs adapted for predatory functions, distinguishing it from other theropod groups. The superfamily-level placement of Megaraptoridae remains debated, with earlier analyses suggesting ties to Allosauroidea due to shared cranial and postcranial features, while more recent phylogenetic studies, including the description of Maip, support an affinity to within , positioning megaraptorids as derived members of this clade. This consensus views Maip as a late-surviving, specialized megaraptorid, extending the temporal range of the family into the .

Phylogenetic analysis

In the original description of Maip macrothorax, Aranciaga Rolando et al. conducted a cladistic using a modified comprising 56 operational taxonomic units and 351 morphological characters, derived from prior theropod phylogenies. This recovered 2560 most parsimonious trees of 1453 steps when including all taxa, and 80 trees of 1455 steps in a pruned version excluding fragmentary specimens. Maip was placed as a derived member of within , forming a with other Argentine megaraptorids such as and , alongside forms like and in the more resolved pruned . The analysis positioned Megaraptora, including Maip, deeply nested within Coelurosauria as the sister taxon to Tyrannosauroidea, with moderate Bremer support (values of 2–3 for key nodes). This placement reinforces the hypothesis of a South American endemic clade of derived megaraptorids, comprising at least two subclades: one including Maip, Aerosteon, Orkoraptor, and Tratayenia, and another with Megaraptor and Murusraptor. These clades are characterized by shared derived features such as bifurcated laminae on dorsal vertebrae forming accessory fossae and rounded articular facets on proximal caudal vertebrae, supporting regional endemism during the Late Cretaceous. A 2025 phylogenetic analysis incorporating additional material from refines this topology, confirming Megaraptora's position as sister to and placing Maip as sister to ( + ) within Megaraptorid Clade 1; this clade also includes the newly described Joaquinraptor casali as an early-diverging member. Key synapomorphies supporting the megaraptorid affinities of Maip include robust manual phalanges with large extensor fossae, elongated and recurved pedal unguals exceeding the length of their respective phalanges, and extensive pneumatic invasion of the vertebrae, particularly in the cervical and dorsal regions. The phylogenetic affinities of megaraptorids, including Maip, have been subject to debate, with earlier studies proposing them as basal coelurosaurs or even carcharodontosaurian allosauroids based on manual morphology and overall . However, the modern consensus, as evidenced by the analysis and subsequent studies, firmly supports their placement as tyrannosauroids within , driven by shared traits like pneumatic axial skeletons and tyrannosauroid-like hindlimb proportions.

Paleoecology

Geological context

The represents an Upper stratigraphic unit in southern , , situated within the Austral-Magallanes Basin. This formation accumulated during the foreland stage of basin evolution and spans approximately 500 meters in thickness, primarily exposed in areas such as La Anita Farm in Santa Cruz Province. The sedimentary profile of the is characterized by fluvial and lacustrine deposits, dominated by fine-grained lithologies including mudstones and siltstones, interspersed with sandstones and minor conglomerates. These form a low-gradient, fine-grained fluvial system with architectural elements such as complex sandy/gravelly channel sheets, sandstone lobes, and both thick and thin fine-grained overbank deposits, indicative of riverine floodplains interspersed with paludal and lacustrine environments marked by poor drainage and hydromorphic paleosols. Age constraints for the formation place it in the lower stage of the , approximately 70–66 million years ago, immediately preceding the Cretaceous-Paleogene . This dating is supported by derived from palynomorph assemblages and vertebrate fossils, alongside stratigraphic correlations with underlying units. Magnetostratigraphic data further corroborate the Maastrichtian assignment. Fossils within the exhibit good preservation attributable to rapid burial in floodplain and overbank settings, which minimized post-mortem transport and . The of Maip macrothorax, recovered from a bonebed spanning a 5 × 3 meter area in a ≤1 meter thick bed on La Anita Farm, exemplifies this taphonomic mode, with disarticulated but associated bones indicating localized accumulation.

Faunal associations and role

Maip macrothorax coexisted with a diverse array of vertebrates in the of southern , forming part of a late Gondwanan ecosystem characterized by fluvial floodplains. Among the contemporaneous dinosaurs, herbivorous ornithopods such as the elasmarian Isasicursor santacrucensis represented potential medium-sized prey, while large sauropods like the titanosaur Nullotitan glaciaris dominated as primary herbivores. Indeterminate remains also indicate the presence of ankylosaurs and hadrosaurs, adding to the ornithischian diversity in this assemblage. Crocodylomorphs, including the peirosaurid Kostensuchus atrox, occupied carnivorous niches as smaller predators or scavengers alongside Maip. The broader faunal assemblage of the included a range of non-dinosaurian vertebrates, reflecting a complex riparian . Amphibians such as indeterminate anurans and calyptocephalellids, along with and amiiform fishes, inhabited aquatic environments within the floodplains. Mammalian remains encompassed dryolestid meridiolestidans like Orretherium and larger mesungulatoids, as well as gondwanatherians (e.g., Magallanodon) and therians (e.g., Patagomaia chainko), indicating a diverse mammal community. Avian taxa, including the neornithine Kookne yeutensis and enantiornithines like Yatenavis ieujensis, contributed to the terrestrial and semi-aquatic biota. Squamates, chelid turtles, and snakes were present, with isolated teeth suggesting occasional marine influence or transport from nearby coastal units. As a late-surviving megaraptorid, Maip occupied the role of apex carnivore in this , preying on large herbivores such as titanosaurs and ornithopods, with its robust build and slashing hand claws adapted for subduing sizable prey through ambush tactics in the forested floodplains. Its estimated length of 9–10 meters and mass exceeding 5 tons positioned it as the top predator, filling the niche vacated by earlier carcharodontosaurids in isolated Gondwanan faunas. This persistence highlights megaraptorid success into the latest , just prior to the K-Pg boundary . Inferred behaviors for Maip suggest it operated as a solitary or small-group hunter, consistent with the ecology of large theropods lacking evidence of pack structures. The specimen, representing an advanced-age adult with extensive , implies a prolonged lifespan potentially supporting extended breeding periods or territorial defense in a resource-rich but competitive environment.
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