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Stupendemys
Stupendemys
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Stupendemys
Temporal range: Langhian - Messinian 9.0–7.246 Ma[1]
A young adult Stupendemys specimen
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Order: Testudines
Suborder: Pleurodira
Family: Podocnemididae
Genus: Stupendemys
Wood, 1976
Species
  • S. geographica Wood, 1976
Synonyms
  • S. souzai Bocquentin & Melo, 2006

Stupendemys is an extinct genus of freshwater side-necked turtle, belonging to the family Podocnemididae. It is the largest freshwater turtle known to have existed, with a carapace over 2 meters long. Its fossils have been found in northern South America, in rocks dating from the Middle Miocene to the very start of the Pliocene, about 13 to 5 million years ago. Male specimens are known to have possessed bony horns growing from the front edges of the shell and the discovery of the fossil of a young adult shows that the carapace of these turtles flattens with age. A fossil skull described in 2021 indicates that Stupendemys was a generalist feeder.

History and naming

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Stupendemys was first named in 1976 by Roger C. Wood based on specimen MCNC-244, the medial portion of a large sized carapace with associated left femur, scapulacoracoid and a cervical vertebra. Wood also described several other specimens he referred to Stupendemys, which includes MCZ(P)-4376. This specimen preserves much of the carapace alongside a fragmented plastron and various other bones. The fossils were unearthed by a paleontological excavation of the Harvard University in Venezuela in 1972.[2] In 2006 a second species, Stupendemys souzai was described by Bocquentin and Melo based on material from the Solimões Formation in Acre State in Brazil, also home to the giant Caninemys.[3] In February 2020, Cadena and colleagues published a paper describing material discovered during the routine excavations in the Urumaco Formation, which have been ongoing since 1994. The material includes a relatively complete carapace that set a new maximum size for the genus and was designated as the allotype, meaning the specimen is of the opposite sex of the holotype.[4] Venezuela also yielded fossils of a lower jaw, which has been used to lump Caninemys into Stupendemys in the 2020 study. The authors likewise consider S. souzai to be synonymous with S. geographica. However, more fossils were discovered in the Colombian Tatacoa Desert and formally described by Cadena and colleagues in 2021, including the first definitive skull remains as well as the first remains of a juvenile or early adult specimen (carapace length under 1 meter). The La Victoria Formation also yielded the remains of an adult female as well as more fossils of Caninemys.[5] With definitive skull remains of Stupendemys known in association with a carapace and new fossils of Caninemys, the referral of Caninemys' skull to Stupendemys was contested and the former was re-established as a valid genus.[5]

The name Stupendemys is a combination of "stupendous", meaning extremely impressive, and the Latin word "emys" for freshwater turtle.[2] The species name meanwhile honors the National Geographic Society. However, the name Stupendemys geographicus, as coined by Wood, is grammatically incorrect, as Stupendemys constitutes a feminine generic name. The name was eventually corrected to Stupendemys geographica in 2021 in accordance with the International Code of Zoological Nomenclature (ICZN).[2][5]

Description

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Stupendemys skull

The skull of Stupendemys is roughly triangular in top view and the edges of the jaws converge at the front of the snout in a straight edge. The skull is dorsally extremely inflated by the prefrontals that make up a large area of the front region of the skull, forming a vertical wall above the bony nostril. Following the prefrontals and orbits the skull slopes down drastically before ascending again through the parietals. The orbits are relatively small and oriented to the sides. When viewed from below the premaxillae bear a deep concavity at their center. In this view the premaxillae form most of the anteromedial edge of the skull, meeting each other towards the middle of the skull and narrowing just before the deep concavity. In front view, the premaxillae form the bottom margin of the bony nostrils, tapering as they move down.[5]

Replica of MCZ(P)-4376 in Osaka

The carapace of adult Stupendemys can reach a straight midline length of greater than 2 meters with a low-arched profile. The nodular contours on the surface are irregular and the frontal margin of the shell is characterized by a deep notch flanked by large horns in male specimens. These horns are deeply grooved, suggesting that they were covered by a keratinous sheath. In addition to these horns, the front margin of the nuchal-peripheral bones is notably thickened and upturned. The surface is smooth to striated or lightly pitted. The margins of the posterior peripheral bones are moderately scalloped. The costal scutes of the carapace are relatively thin. In overall shape the carapace of Stupendemys is longer than it is wide.[4]

Size

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Traditional illustration created with graphite and colored pencils on letter-size bond paper. Digitally edited. Author: Edwin Chávez "Disfrasaurio".
Life reconstruction of a male by Edwin Chávez

Stupendemys is the largest known species of freshwater turtle currently known to science, with several specimens reaching a carapace length exceeding 2 meters. The largest specimen of Stupendemys is CIAAP-2002-01, an almost complete carapace with a parasagittal length of 2.86 meters. This exceeds the size of the Vienna-specimen of the Cretaceous sea turtle Archelon, the largest known turtle, (carapace length 2.20 meters).[4]

The weight of Stupendemys was estimated based on the straight carapace length, with calculations indicating a weight of 871 kg for CIAAP-2002-01 and 744 kg for MCZ(P)-4376, the former largest known specimen of Stupendemys. However, these estimates do not compensate for the large embayment present at the front of the shell. A more precise body mass estimate might be achieved by calculating the average between the results of weight estimates based on midline length and parasagittal length. Applying this method yields a weight of 1,145 kg for the largest Stupendemys specimen.[4]

The evolution of such an enormous size may have been multi-facetted and caused by a combination of factors including pressure from predators, habitat size and favorable climatic conditions, although Stupendemys temporal range indicates that it managed to survive through times of global cooling following the middle Miocene climatic transition (MMCT). Lastly, the giant size could have a phylogenetic link and be ancestral to Stupendemys, with several other related forms being known to have possessed gigantic proportions.[4]

Phylogeny

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Although initially believed to be a pelomedusid by Wood,[2] later studies consistently recovered Stupendemys as a podocnemidid turtle instead.[3][4][5] In 2020 Stupendemys was recovered as a basal member of Erymnochelyinae.[4] However, this position was influenced by the inclusion of material belonging to Caninemys. In their 2021 publication, Cadena and colleagues again attempted to determine the relationship between Stupendemys and other pan-pleurodiran turtles using the morphological characters established previously by Joyce and colleagues (2021), 268 characters across 104 species of turtles. The analysis was run once with all taxa and once with a focus on Podocnemidoidae, removing all other taxa safe for Proganochelys quenstedti, Notoemys laticentralis, and Platychelys oberndorferi. The single most parsimonious tree resulting from the second analysis recovered Stupendemys as an early branching member of a clade with Peltocephalus dumerilianus at its base. Caninemys, now recognized as a distinct taxon, nested at the base of Erymnochelyinae.[5] Similar results were later recovered in the 2024 description of Peltocephalus maturin.[6]

Podocnemidoidae

Brasilemys josai

Hamadachelys escuilliei

Paleobiology

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Paleoecology

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Following the 2021 research of Cadena and colleagues, the Pebas Mega-Wetlands housed at least two species of giant side-necked turtles: Stupendemys and Caninemys. Despite their similar size (both sporting a carapace length greater than 2 meters), they vary greatly in skull morphology, with Caninemys proposed to have been deploying a vacuum feeding strategy combined with a strong bite supported by tooth-like structures of the maxilla, while a more durophagous-omnivorous diet has been suggested for Stupendemys. This difference in diet and feeding strategy would be in accordance with Gause's Law, by which two species competing for the same ecological niche cannot coexist with one another for a long period of time without either differentiating or one dominating over the other in the long run. In addition to the different skull morphology, the two taxa may have also been able to coexist due to the sheer size of the Pebas Mega-Wetlands they inhabited, as this ecosystem stretched over most of northern South America during the Middle Miocene. This reason may also prevent the two taxa from being in direct competition over nesting grounds and basking spaces.[5]

The diet of Stupendemys may have been very diverse and broad, possibly including molluscs and other hard shelled prey as well as vertebrate prey as suggested by Meylan and colleagues for Caninemys. At its size it would have been easily capable of consuming various fish, snakes and small crocodilians. A broad dietary width would have helped Stupendemys in maintaining its large body size. Furthermore, Cadena and colleagues also highlight the role of turtles as seed-dispersers in modern-day Amazonia, consuming fruit of palms for example (Arecaceae), seasonally sometimes in great quantities, even if they are not typically part of their standard diet. With its wide gape, Stupendemys would qualify as a megafaunal frugivore and seed disperser.[4]

Sexual dimorphism

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The absence of horns on most Stupendemys specimens indicates that they were not used as a defense mechanism. However, their forward-facing position on the carapace may indicate that they were used in intraspecific combat. Cadena and colleagues hypothesize that the horns may have been a sexually dimorphic trait exclusively found in males, suggesting them to have been used similar to the horns and antlers found in artiodactyls. Among extant turtles similar behavior can be found in snapping turtles, some of the largest freshwater turtles alive, which are known to fight for dominance in overlapping territories. This hypothesis is supported by the presence of a deep, elongated scar along the left horn of CIAAP-2002-01, which could have been left by the horn of a rival male that engaged it in combat. The authors further suggest that in Stupendemys the males may have been the larger sex, similar to the condition seen in the modern podocnemids. However other traditionally sexually dimorphic traits of the turtle shell, such as a deeper anal notch or a xiphiplastral concavity, have not yet been observed in Stupendemys fossils.[4]

Hypothetical ontogenetic series of Stupendemys geographica

Ontogeny

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Prior to the 2021 study of Cadena and colleagues, only adult specimens of Stupendemys had been described. The discovery of a specimen with a carapace length smaller than 1 meter gives an insight into the changes the animal undergoes while reaching maturity. In addition to its small size, the animal is identified as a juvenile to young adult based on the absence of large horns and shallow anal notch. The inner nuchal notch, anterior expansion of the peripherals 1 and 2, irregular nodular contours, inner contact between the 7th and 8th costals and the relative size of the plastral lobes and their arrangement (except for the pectorals) remains relatively consistent with size.[5]

One of the most significant changes of the carapace of Stupendemys is its height. With age the shell of the turtle grows significantly flatter, while the nuchal region develops a pronounced upturn of its anterior margin and peripheral 1, creating a wide and deep anteromedial embayment of the carapace. The 2nd and 3rd vertebral scutes grow narrower as the animal matures from juvenile to adult, similar to the extant Podocnemis, Erymnochelys and Peltocephalus. The 5th vertebral scute meanwhile belongs the longest and widest of the series in adults while keeping its trapezoid shape. This ontogenetic change of the vertebral scutes means that phylogenetic coding using the width of the vertebral scutes in relation to the pleural scutes should be treated with care due to the variable nature of these features as shown by Stupendemys.[5]

Paleoenvironment

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Middle Miocene South America

During the Middle Miocene, the area inhabited by Stupendemys was part of an interconnected series of lakes, rivers, swamps and marshes that drained into the Caribbean known as the Pebas Mega-Wetlands, which included the Colombian La Victoria Formation.[7] The Wetlands provided favorable conditions to the native reptilian fauna, with several lineages of crocodilians reaching enormous sizes during the Mid to Late Miocene and also diversifying in ecology. Some of the enormous crocodilians that coexisted with Stupendemys included the enormous caimain Purussaurus, the bizarre Mourasuchus and large-bodied gharials of the genus Gryposuchus, some species of which reaching lengths of over 10 meters. Some of these crocodilians may have played a role in the evolution of Stupendemys' large body-size, putting pressure on the animal through predation. Bite marks have been found on Colombian and Venezuelan specimens and an isolated tooth was found attached to the ventral surface of CIAAP-2002-01.[4]

As the Pebas System began to disappear with the onset of the transcontinental Amazon Drainage, Stupendemys persisted in the wetlands of the northern Urumaco Formation and the Solimões Formation in Acre State, Brazil, into the Late Miocene before eventually dying out during the Early Pliocene like much of the large crocodilian fauna of the Miocene wetlands. Besides the aforementioned reptiles the waterways of Late Miocene South America were also inhabited by fish, including catfish such as Phractocephalus and Callichthyidae, characids such as Acregoliath rancii and the tambaqui (Colossoma macropomum), the South American lungfish (Lepidosiren paradoxa), trahiras (e.g. Paleohoplias assisbrasiliensis) and freshwater rays and sharks. Other turtles and tortoises found in the same deposits are Chelus columbiana[8] (a fossil relative of the mata mata) and Chelonoidis. Further aquatic vertebrates included river dolphins and the large darter "Anhinga" fraileyi.[3] At least within the Solimões Formation Stupendemys would have inhabited a floodplain or lacustrine environment with savannahs and gallery forests.[3]

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Stupendemys is an extinct of giant freshwater side-necked belonging to the Podocnemididae, known for being the largest non-marine ever discovered. The comprises two : the S. geographicus and S. souzai. S. geographicus possessed a massive measuring up to 2.4 meters in length and weighing approximately 1,145 kg, making it comparable in size to a small . These s inhabited the riverine and ecosystems of the northern Neotropics during the Middle Miocene to early epochs, approximately 13 to 5 million years ago, with fossils primarily recovered from regions in present-day , , , and , including a new specimen from Acre in 2025. First described in 1976 based on shell fragments from the Urumaco Formation in , Stupendemys was initially recognized for its extraordinary dimensions, earning it the name meaning "marvelous " in Latin. Subsequent discoveries, including nearly complete shells and the first associated skull in 2020, have revealed : males featured prominent anterolateral horns on their carapaces, likely used for display or , while females had smoother shells. Bite marks on fossils indicate interactions with large predators such as caimans, suggesting a complex ecological role in aquatic environments. Paleobiological studies suggest Stupendemys was a durophagous or , capable of crushing hard-shelled prey or dispersing seeds through its diet, with individuals potentially living up to 110 years based on bone histology. Phylogenetically, it forms a to other erymnochelyine within the , highlighting its position as a specialized giant among side-necked that retracted their necks sideways rather than vertically. These findings underscore Stupendemys as a key species for understanding and diversification in prehistoric freshwater reptiles.

Discovery and Taxonomy

History of Discovery

The genus Stupendemys was established in 1976 when paleontologist C. Wood described the S. based on shell fragments collected from the Middle to Late Miocene Urumaco Formation in northwestern Venezuela. These initial fossils, including the holotype (MCNC-244), represented a remarkably large podocnemidid and marked the first recognition of such a giant freshwater in South American deposits. In 2006, a second species, S. souzai, was named by J. Bocquentin-Villa and J. Melo from an incomplete humerus and associated peripheral bone discovered in the Miocene-Pliocene Solimões Formation of Acre State, western Brazil. This material suggested morphological distinctions from S. geographica, expanding the known range of the genus into the southwestern Amazon Basin. However, subsequent analysis in 2020 by E.A. Cadena and colleagues synonymized S. souzai with S. geographica after comparing it to new specimens, attributing earlier differences to intraspecific variation rather than a separate taxon. The same 2020 study introduced significant new finds, including the allotype CIAAP-2002-01—a nearly complete 2.86-meter-long carapace—from the Middle Miocene Tatacoa Desert in Colombia's Huila Department, as well as Venezuelan material from the Urumaco Formation; these revealed previously unknown features such as robust marginal horns on males and healed shell injuries interpreted as combat damage. Further advancements came in 2021 with the description by Cadena and coauthors of the first Stupendemys geographica specimen preserving an associated skull and shell (VPPLT-1337), a juvenile to early adult individual under 1 meter in shell length, from the Middle Miocene La Victoria Formation in Colombia's Tatacoa Desert—this formation forms part of the broader Pebas Mega-Wetland System that extended into Peru. The associated elements provided critical insights into cranial anatomy and early ontogeny, confirming the turtle's pleurodiran affinities. Fossils attributable to Stupendemys have also been reported from Peruvian deposits, including the late Miocene Contamana Group in the Amazon Basin, underscoring the genus's wide distribution across northern South America. In 2025, Brazilian paleontologists announced two major discoveries enhancing understanding of Stupendemys' temporal and geographic context. A partial shell from the Miocene Solimões Formation in Acre State was added to the Universidade Federal do Acre (UFAC) collection, representing one of the largest known specimens from Brazil. Additionally, during a July expedition to the Amazon triple border region (Brazil-Peru-Bolivia) led by researchers from the University of Campinas (Unicamp) and University of São Paulo (USP) as part of the Amazon+10 Initiative, a well-preserved shell was unearthed near the Javari River, dated to approximately 9-10 million years ago via associated biostratigraphy; the fossil was transported to Unicamp for detailed preparation and analysis. These finds reaffirm the Miocene age of the genus and its prevalence in ancient Amazonian wetlands.

Etymology and Species

The genus name Stupendemys is derived from the Latin stupendus, meaning "marvelous" or "stupendous," combined with emys, meaning "," in reference to the extraordinary size of its fossils. The species epithet was originally geographicus honoring the , which funded the 1973 expedition leading to the discovery of the type material in , but was emended to geographica in to agree with the feminine gender of the genus name. The sole valid species is S. geographica, established as the in and diagnosed by its massive body size ( up to 2.4 m long), low-domed and nodular , prominent nuchal emargination, fused gular scutes, well-developed anal notch, and unique features such as inflated maxillae and a tridentate triturating surface. The , MCNC-244, consists of a partial and associated left from the Urumaco Formation in . A second species, S. souzai, was proposed in 2006 based on fragmentary material from the Miocene-Pliocene Solimões Formation in but was later recognized as a junior synonym of S. geographica due to substantial morphological overlap, particularly in and limb proportions, as detailed in a 2020 taxonomic revision. An emended in 2021 further refined S. geographica by incorporating new associated skull-shell specimens, emphasizing pleurodiran traits like sutural pelvis-shell articulation and saddle-shaped cervical centra, while distinguishing it from related podocnemidids.

Synonymy and Classification

Stupendemys was originally described by in 1976 and placed within the family Podocnemididae, a group of side-necked turtles known for their freshwater habitats in and . Early assessments positioned the genus close to the extant genus Podocnemis due to superficial similarities in shell morphology and geographic distribution, but subsequent analyses revealed more derived features aligning it with basal pleurodires. By 2020, phylogenetic revisions confirmed its placement in the subfamily Erymnochelyinae within Podocnemididae, identifying Stupendemys as a basal member based on cladistic analyses of carapace and cranial traits. A significant taxonomic revision occurred in 2020 when Stupendemys souzai, originally described in from Brazilian fossils, was synonymized with the type species . This decision stemmed from the recognition of shared features, such as the presence of prominent horns on the anterior peripherals and overall nuchal morphology, coupled with a lack of consistent distinguishing traits in the limited S. souzai material. New specimens from and further supported this monospecific interpretation, as mandibular and shell elements across sites showed uniform proportions and ornamentation without diagnostic differences. Historical misclassifications extended to related taxa, including the Caninemys, whose C. tridentata was initially synonymized with S. geographica in 2020 due to overlapping stratigraphic ranges and preliminary cranial similarities. However, a 2021 re-examination of associated skull-shell material re-established Caninemys as a distinct , justified by unique cranial differences such as tridentate mandibular symphyses and broader temporal regions not observed in Stupendemys. These clarifications refined the , emphasizing Stupendemys' basal position in Erymnochelyinae while distinguishing sympatric giant pleurodires in .

Description

Carapace and Shell Features

The of Stupendemys geographicus is characterized by a low-arched, shape exceeding 2 meters in straight midline length, with irregular nodular contours on the surface and a thickened, upturned anterior border. It features a typical of 24 marginal scutes (12 pairs), including a large first marginal that covers much of the and the first peripheral, and a deep nuchal emargination formed by a median notch at the frontal margin. The five vertebral scutes are arranged such that the first is restricted to the nuchal, while the fifth becomes the longest and widest in adults, and four pairs of pleural scutes extend to the peripherals without significant ontogenetic changes despite prolonged growth. The plastron is broad, flat, and shorter than the carapace, with equal-length anterior and posterior lobes and a solid, diamond-shaped entoplastron that contacts the hyoplastra convexly, lacking a fontanelle in adult specimens. The pectoral-abdominal sulcus lies anterior to the mesoplastra, aligning with the lateral notch of the hyoplastra. A distinctive sexual dimorphism is evident in the shell, with males exhibiting paired, massive bony horns projecting anterolaterally from the expanded first and second peripherals near the frontal margin, slightly ventrally directed and absent or reduced in females. These horns bear a smooth to slightly pitted or striated surface texture, with evidence of growth annuli visible in the underlying bone histology that indicate age through lines of arrested growth, and some 2020 specimens show deep, elongated scars suggestive of intraspecific interactions.

Skull and Appendages

The of Stupendemys geographicus is roughly triangular in dorsal view, with converging lateral margins that form a straight anterior edge at the . This morphology was first detailed from an associated skull-shell specimen in , marking the initial complete cranial description for the . The jaws are edentulous, lacking teeth, and feature broad, deep triturating surfaces formed by the premaxillae, maxillae, and , which create an oval concavity suited for crushing food items. Additionally, the skull exhibits greatly inflated maxillae and large temporal fenestrae, with reduced temporal emargination contributing to a robust cranial structure. The neck of Stupendemys comprises eight , a standard pleurodiran condition that facilitates side-neck retraction, where the head is folded laterally alongside the body for protection. Preserved elements, such as 2, 7, and 8 from multiple specimens, show high neural arches and acute postzygapophyseal angles (less than 90°), supporting this retractile mechanism typical of side-necked turtles (). The forelimbs of Stupendemys are paddle-like, adapted for aquatic , with a squat, massive exhibiting a triangular cross-section and webbed digits inferred from the robust pectoral girdle. In contrast, the hindlimbs are robust and dorsoventrally flattened, featuring a squat indicative of bottom-walking in shallow freshwater environments. These limb adaptations highlight Stupendemys' semi-aquatic lifestyle, balancing efficiency with substrate interaction. Juvenile skulls of Stupendemys, identified from fossils, display proportionally larger orbits relative to the overall cranium and softer, less ossified margins compared to adults, suggesting ontogenetic changes in cranial robustness.

Size Estimates

The largest known of Stupendemys geographicus measures 2.86 m in straight parasagittal length, represented by specimen CIAAP-2002-01 from the of . This surpasses the carapace length of 2.20 m reported for ischyros, the largest known marine turtle. Weight estimates for S. geographicus derive from volumetric modeling of complete and partial specimens, yielding a maximum of 1,145 kg for CIAAP-2002-01 based on averaged midline and parasagittal reconstructions. Adult individuals generally ranged from 1.8 to 2.4 m in carapace length, with juveniles exhibiting carapaces of approximately 0.5 to 1.0 m. Total body length for the largest adults reached approximately 3.3 m when accounting for head and tail extensions beyond the shell. These dimensions highlight S. geographicus as the largest non-marine turtle on record, with a mass approximately 100 times that of its closest living relative, the big-headed Amazon River turtle (Peltocephalus dumerilianus), and roughly 1.3 times that of the largest modern marine turtles, such as the leatherback sea turtle (Dermochelys coriacea).

Systematics

Phylogenetic Relationships

Phylogenetic analyses position Stupendemys as a member of the Erymnochelyinae subfamily within the Podocnemididae family, based on a modified matrix from Joyce et al. (2021) that incorporates cranial and postcranial characters. In this cladistic framework, Stupendemys geographica (emended from geographicus in to match the feminine genus name) is placed as the sister taxon to Peltocephalus dumerilianus within Erymnochelyinae (Clade 2), distinct from Cerrejonemys wayuunaiki in Podocnemidinae and basal Caninemys tridentata. This placement is supported by a parsimony analysis in TNT 1.5, yielding a single most with a tree of 464, consistency index of 0.772, and retention index of 0.971. Key synapomorphies diagnosing this position include interparietal scutes that do not meet medially and a cranial pit on the premaxillae. Additional cranial features, such as the posterior positioned at the -pterygoid suture, further corroborate its erymnochelyine affinities. These traits distinguish Stupendemys from more derived podocnemidids while aligning it with early-diverging lineages in the . The genus is known from middle to fossils (approximately 13.5 to 7 Ma), including from the La Victoria Formation in (13.651 ± 0.107 Ma), reflecting an adaptive expansion of pleurodiran turtles in Neotropical freshwater environments during this period. This temporal context aligns with the broader radiation of podocnemidids in northern . The inclusion of the first associated skull and shell specimen (VPPLT-1337, a juvenile or early adult female) in the 2021 analysis significantly refines pleurodiran interrelationships by resolving ambiguities in podocnemidoid topology, particularly in distinguishing Stupendemys geographica from sympatric taxa like Caninemys tridentata, which is reestablished as a valid, distinct species. This data, revealing a robust but generalized cranial morphology, strengthens the erymnochelyine placement and highlights the role of integrated datasets in clarifying evolutionary branching patterns among side-necked turtles.

Comparisons to Extant and Extinct Turtles

Stupendemys geographica, as a pleurodiran turtle, shares the characteristic side-neck retraction mechanism with extant relatives in the genus Podocnemis, including a long parietal-quadratojugal contact and reduced cheek emargination that facilitate tucking the head sideways into the shell. However, Stupendemys far exceeded Podocnemis in size, with a carapace length reaching up to 2.40 meters compared to the much smaller dimensions of species like Podocnemis dumerilianus, which is approximately 100 times less massive. Additionally, while Podocnemis exhibits an omnivorous diet incorporating fruits and softer vegetation, Stupendemys displayed pronounced durophagous adaptations, such as robust triturating surfaces suited for crushing hard-shelled prey like mollusks and possibly crocodylian eggs. In contrast to the extinct marine protostegid , which inhabited open-ocean environments, Stupendemys occupied freshwater wetland habitats during the , reflecting divergent ecological niches within giant chelonian evolution. Stupendemys also possessed prominent anterolateral horn-like projections on its —absent in the streamlined, hornless shell of —that likely served defensive or display functions in its riverine setting. Although both taxa achieved enormous sizes, with 's measuring around 2.20 meters, Stupendemys was marginally larger overall, emphasizing its status as the largest known nonmarine . Among related fossil pleurodires, Stupendemys differed markedly from the podocnemidoid Caninemys tridentata in scale and horn morphology, as Caninemys skulls exhibit tridentate triturating surfaces similar to those in Stupendemys but on a much smaller body frame, with estimated lengths far below 2 meters. These shared cranial features have led to suggestions that Caninemys may represent a junior synonym of Stupendemys, highlighting close evolutionary ties within podocnemidids, though Stupendemys' exaggerated horns and overall distinguish it as a specialized form. The of Stupendemys exemplifies broader evolutionary trends in northern South American , where expansive aquatic habitats supported extreme body sizes not only in but also in contemporaneous crocodylians like caimans, likely driven by abundant resources and predation pressures from large predators. This parallel underscores how ecosystems facilitated the convergence of massive body plans across vertebrate lineages during the .

Paleobiology

Diet and Feeding Adaptations

Stupendemys exhibited adaptations indicative of a generalist omnivorous diet with pronounced durophagous capabilities, allowing it to process a variety of food items including hard-shelled , , and plant matter. The robust featured inflated maxillae, a tridentate upper triturating surface, and a deep lower concavity equipped with powerful adductor musculature, enabling efficient crushing of tough prey such as mollusks and bivalves. These features supported a broad dietary niche that likely included both aquatic and terrestrial resources, distinguishing it from more specialized herbivores among its relatives. A detailed of the first associated and shell specimen of S. geographicus in revealed cranial morphology consistent with omnivory and durophagy, including a secondary formed by medial contact between the maxillae and , as well as deep premaxillary concavities. The triturating surfaces showed structural adaptations for grinding and crushing, with inferred wear patterns suggesting regular consumption of hard-shelled prey like bivalves prevalent in its . This morphology implies a versatile feeding strategy involving both suction-based capture and forceful mastication, capable of handling diverse prey sizes. Inferences from the Pebas mega-wetland system sediments, where Stupendemys fossils occur, support a diet incorporating from local and such as mollusks, reflecting the wetland's rich . These environmental associations indicate opportunistic on available resources, including fruits that could serve as a significant source during seasonal peaks. Compared to modern podocnemidids like Podocnemis, which are predominantly herbivorous with limited durophagy, Stupendemys demonstrated greater dietary versatility, potentially including more animal matter to sustain its massive body size.

Behavior and Sexual Dimorphism

Sexual dimorphism in Stupendemys geographicus is evidenced by distinct shell morphotypes, with males possessing prominent anterolateral horns protruding from the front edges of the , while s exhibit hornless shells. These horns, formed by robust bony projections covered in a keratinous sheath, are absent in specimens, suggesting a sexually selected trait primarily in males. Male shells also appear relatively longer and narrower compared to the broader, more rounded form of shells, potentially adapted for and laying, akin to patterns observed in some extant pleurodire . Fossil evidence from Miocene deposits in and reveals deep scars and healed bite marks on the horns of specimens, interpreted as injuries from intraspecific . These pathologies, including grooves and punctures consistent with conspecific , indicate aggressive male-male interactions likely over access, with the horns functioning as weapons similar to those in modern vertebrates exhibiting . No such combat-related injuries are reported on female shells, supporting the role of dimorphism in reproductive rivalry. Mating behaviors in Stupendemys are inferred to have occurred in aquatic environments, mirroring displays in modern pleurodires such as chelids and podocnemidids, where males perform territorial head-bobbing or circling to attract females. The pronounced size difference, with males potentially exceeding females in length, may have facilitated such displays or physical contests without direct evidence of forced copulation. However, no fossils directly documenting —such as eggs, nests, or embryonic remains—have been recovered, leaving these inferences based on dimorphic traits and phylogenetic comparisons. The presence of strongly implies selection pressures driven by mate competition and female choice.

Growth and Ontogeny

The discovery of a juvenile to subadult specimen (VPPLT-1337) in 2021 provided the first associated and shell for Stupendemys geographicus, revealing key early developmental traits. This individual, from the middle La Victoria Formation in , had a measuring 86.2 cm along the midline and a moderately domed shell profile, contrasting with the flatter, low-arched structure observed in adults. The measured 15.2 cm in length, representing the initial stages of growth before reaching subadulthood at under 1 m length. Ontogenetic changes in Stupendemys included progressive flattening of the and narrowing of vertebral scutes 2 and 3 with maturity, alongside the development of pronounced shell features such as an upturned nuchal margin in adults. Males exhibited post-maturity development of massive anterolateral horns on the first two peripheral bones, absent in juveniles and females. These shifts, documented through comparisons of the 2021 specimen with adult fossils, indicate a prolonged developmental period adapting the shell for increased body mass and potential sexual roles. Bone histology from carapace elements reveals cyclical growth marks, with 2–4 lines of arrested growth (LAGs) in costals and up to 8 in neurals, suggesting annual deposition patterns similar to those in extant . Estimated growth was rapid in early , allowing subadults to reach approximately 1 m length, but overall rates were slow at 3–5 cm per year based on comparisons to large podocnemidids, with individuals potentially taking 60–110 years to attain maximum sizes exceeding 2.4 m. Growth lines in the 2021 juvenile's costals further support episodic early expansion before deceleration. Developmental shifts in feeding heightened juvenile vulnerability, with skull morphology consistent with omnivory and durophagy as in adults, potentially suited for a range of prey including softer items early on. This ontogenetic pattern, evident in skull proportions and inferred from the 2021 specimen, likely influenced early-life predation risks in aquatic environments.

Distribution and Paleo

Geographic Distribution

Fossils of Stupendemys are restricted to northern , with no records reported from outside the continent. The genus is known from deposits dating between approximately 13 and 5 million years ago, though the majority of specimens derive from Middle horizons around 11 to 10 Ma. This temporal range aligns with the peak of the Pebas Mega-Wetland System, a vast interconnected fluvial network that facilitated widespread dispersal across the region. Key fossil localities include the Urumaco Formation in Falcón State, , where multiple specimens of S. geographicus have been recovered since the 1990s. In , remains occur in the La Tatacoa Desert and Villavieja area of , also attributed to S. geographicus. Peruvian sites are centered in the Loretto region, particularly the Pebas Formation, yielding fossils from the middle wetlands. Brazilian occurrences are documented in the Solimões Formation of the Acre and Amazonas basins, including material from near Sena Madureira previously described as the species S. souzai (though its attribution to Stupendemys remains debated). Recent discoveries in 2025 have expanded the known Brazilian distribution, with new S. geographicus specimens unearthed in the western Amazon near the triple border of Brazil, Peru, and Bolivia, as well as additional finds in Acre State from Solimões Formation outcrops. These extensions underscore a broader occupation of Amazonian wetland habitats during the Miocene, likely enabled by proto-Amazonian river systems connecting the Pebas and Acre basins.

Interactions with Contemporaneous Species

Stupendemys coexisted with giant caimans such as in the Pebas Mega-Wetlands of the Middle Miocene, sharing a hyperdiverse aquatic environment that included other crocodylians, fishes, and mammals. specimens from and preserve clear evidence of biotic interactions, including multiple bite marks and punctured bones on carapaces and plastrons, attributed to attacks by these large predators. One notable example features an embedded crocodylian tooth on the ventral surface of a shell, demonstrating direct physical contact likely during predation attempts on adults or defensive encounters. These traces highlight the vulnerability of even the largest Stupendemys individuals to apex crocodylians capable of exerting immense bite forces. In the same wetland system, Stupendemys shared habitats with other podocnemidid turtles, including smaller species like Podocnemis bassleri, suggesting potential competition for durophagous resources such as mollusks abundant in the shallow lakes and swamps. Niche partitioning likely occurred based on body size disparities, with the gigantic Stupendemys accessing larger or harder-shelled prey through its robust jaws and greater crushing capability, while smaller congeners exploited finer or more accessible food items. This size-based differentiation would have facilitated coexistence amid resource limitations in the nutrient-rich but contested mega-wetland . As a mid-level omnivore in the Pebas food web, Stupendemys functioned as both predator and prey, contributing to trophic dynamics by consuming hard-shelled invertebrates, fishes, and possibly soft vegetation or fruits, while facing predation primarily from giant caimans. Its durophagous adaptations positioned it within a layered community where smaller herbivores and invertivores formed the base, escalating to larger carnivores and omnivores like Stupendemys, and culminating in top predators such as Purussaurus. This structure underscores the intense interspecies pressures shaping the evolution of Miocene Neotropical vertebrates in a biodiversity hotspot.

Paleoenvironment

Depositional Settings

Fossils of Stupendemys are primarily preserved in middle to deposits of the Urumaco Formation in , the Pebas Formation in , and the Solimões Formation in , all representing fluvial-lacustrine environments characterized by river channels, , swamps, and shallow lakes. The Urumaco Formation consists of fine-grained sandstones, organic-rich mudstones, and coquinoid limestones deposited in low-energy and delta plain settings, with some estuarine influences. Similarly, the Pebas Formation reflects a vast mega-wetland system with mixed fluvial and lacustrine , including mudstones and silty deposits formed under tectonic and Andean sediment input. The Solimões Formation features mudstones, silty mudstones, and clayey siltstones in a chaotic fluvial system influenced by tectonic pulses, encompassing permanent water bodies like swamps and lakes. Preservation of Stupendemys fossils typically involves articulated shells embedded in fine-grained silts and mudstones, pointing to rapid burial in low-energy aquatic environments that limited post-mortem disturbance and promoted anaerobic conditions. For instance, exceptionally complete carapaces up to 2.4 meters long have been recovered from such sediments in the Urumaco and Pebas systems, where early helped maintain structural integrity. In the Solimões Formation, similar fine sediments facilitated the preservation of partial shells, though exposure along riverbanks can lead to fragmentation if not excavated promptly. Recent discoveries in from the Acre region of , near the triple border with and along the Acre River, come from floodplain sediments equivalent to the Solimões Formation, yielding a well-preserved shell approximately 1.7 meters wide. These triple-border finds, including specimens from overbank deposits in the Pebas/Solimões system around the Peruvian-Colombian-Brazilian junction, highlight deposition in meandering fluvial settings with periodic flooding. Taphonomic biases in Stupendemys assemblages often include disarticulated limbs and scattered peripheral bones, indicative of post-mortem in fluvial currents before final in low-energy overbank or lacustrine . Such patterns are evident across the Urumaco, Pebas, and Solimões formations, where articulated central elements like plastra contrast with transported appendages, reflecting the dynamic yet ultimately protective nature of these depositional contexts.

Climatic and Ecological Context

During the Middle Miocene, northern experienced a warm and humid climate, characterized by the Middle Miocene Climatic Optimum (MMCO), which supported expansive aquatic habitats conducive to the evolution of large-bodied vertebrates like Stupendemys. This period featured high precipitation and temperatures warmer than today, fostering the development of the Pebas Mega-Wetland System, a vast network of lakes, swamps, and rivers spanning over 1 million km² across western Amazonia from approximately 23 to 8 million years ago. The Pebas system acted as a megafaunal hotspot, with elevated primary productivity from nutrient-rich fluvial inputs and periodic marine influences, enabling in taxa such as , crocodylians, and by providing abundant food resources and stable aquatic refugia. Stupendemys thrived in this environment, occupying freshwater to brackish littoral zones within the system. Isotopic analyses of fossil shells from the Pebas Formation, including those of mollusks associated with turtle-bearing deposits, reveal δ¹⁸O values that reflect warm, low-evaporation conditions in a predominantly freshwater setting with salinity gradients due to episodic marine incursions. These data indicate a dynamic hydrological regime, where δ¹⁸O and δ¹³C signatures in shells document shifts from lacustrine to more estuarine environments, supporting diverse aquatic communities that sustained Stupendemys' herbivorous or omnivorous diet. The high productivity of the wetlands, driven by and sediment cyclicity, further amplified ecological niches for giant reptiles, as evidenced by hyperdiverse faunas in coeval deposits. The decline of Stupendemys coincided with environmental changes around 10–5 million years ago, marked by regional drying and the transition of the Pebas system to a fluvial-dominated Acre system, which reduced extent through Andean uplift and during the Climatic Transition. This and decreased aquatic connectivity favored smaller-bodied podocnemidid turtles, which adapted better to narrower riverine corridors, ultimately contributing to the extinction of Stupendemys by the early .

References

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