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Dryopithecus

Dryopithecus is an extinct genus of great apes () that lived during the to epoch, approximately 13 to 9 million years ago, with fossils known primarily from sites across including , , , , , and . The genus is characterized by a medium to large body size ranging from 20 to 45 kg, an orthograde posture adapted for arboreal suspensory locomotion such as vertical climbing and below-branch suspension, and a mosaic of primitive and derived cranial and postcranial features. First described by paleontologist Édouard Lartet in 1856 based on dental remains from Saint-Gaudens, , Dryopithecus played a pivotal role in early discussions of , with proposing it as a potential ancestor to modern apes. Taxonomically, Dryopithecus is often placed in the subfamily Dryopithecinae within , though its exact position is debated, encompassing several species such as the D. fontani (from ), D. laietanus (from , sometimes classified under the Hispanopithecus), and D. crusafonti (from , sometimes classified under Hispanopithecus). Key fossils include partial crania, mandibles, and postcranial elements like humeri, femora, and phalanges, which reveal in body size and dental morphology adapted for a soft-fruit diet with thin and low-crowned molars. Locomotor adaptations, including a broad range of elbow mobility and elongated forelimbs, indicate a shift toward more versatile arboreal behaviors compared to earlier hominoids, bridging proconsulids and crown hominids. In terms of evolutionary significance, Dryopithecus is viewed as a hominine, potentially ancestral to the ( apes and s), with evidence suggesting an origin followed by dispersal to around 16–14 million years ago and possible back-migration to by the ; however, its precise affinities to pongines (orangutans) and other dryopithecines like Pierolapithecus and Anoiapithecus remain debated. Its discovery challenged early 19th-century views of uniqueness and highlighted as a center of hominoid diversification during the radiation, influencing modern understandings of great phylogeny.

Etymology and History

Etymology

The genus name Dryopithecus was coined by paleontologist Édouard Lartet in to describe a new based on a fragmentary discovered in deposits at Saint-Gaudens in the French Pyrenees. The name derives from the words dryos (referring to an oak tree or wood, implying arboreal ) and pithekos (), translating to "wood " or "oak-tree ," reflecting Lartet's inference of tree-dwelling adaptations from the limited remains. Lartet chose the name to emphasize the fossil's affinities with modern apes while highlighting its presumed lifestyle in forested environments, a drawn from the dental suggesting a frugivorous, arboreal form. This nomenclature captured early 19th-century paleontological interest in linking fossil primates to living species, predating Charles Darwin's On the Origin of Species by three years and underscoring emerging ideas about primate in European contexts.

Discovery History

The genus Dryopithecus was first established based on fossil discoveries in the mid-19th century. In 1856, French paleontologist Édouard Lartet described the D. fontani from mandibular fragments and a unearthed in deposits at Saint-Gaudens in the , marking the initial recognition of this extinct great ape. These finds, collected from lignite mine workings, provided early evidence of a European hominoid with dental features suggestive of frugivory, influencing contemporary debates on evolution. Earlier fossils from German localities, such as the complete discovered in the 1820s at Eppelsheim near , were later recognized as belonging to an extinct hominoid under the name Paidopithex rhenanus, highlighting the region's role in pre-Lartet hominoid paleontology. These specimens from the Dinotheriensande formation contributed to the foundational understanding of Eurasian diversity. Significant 20th-century discoveries expanded the geographic and anatomical scope of Dryopithecus. In the , excavations at Rudabánya in northeastern , initiated after geologist Gábor Hernyák identified promising fossils in 1965, yielded extensive remains including cranial, dental, and postcranial elements attributed to D. brancoi (later re-evaluated as Rudapithecus). These finds, from (Vallesian) coal mine deposits, revealed suspensory locomotor adaptations and enriched interpretations of social and dietary behaviors among European great apes. Further major contributions came from the in the and , particularly at sites in the Vallès-Penedès Basin, , . Systematic fieldwork at localities like Can Pons and Can Llobateres uncovered partial skeletons and of D. laietanus (synonymized with Hispanopithecus), providing insights into orthogrady and through well-preserved postcrania. These discoveries, dated to approximately 11.9–9.7 million years ago, solidified the basin as a key European hotspot for dryopithecine evolution. Post-2010 research has focused on advanced analyses of existing fossils rather than new major sites, with no significant discoveries reported after 2020. In , micro-CT scans and geometric morphometric studies of Vallès-Penedès specimens have enabled virtual reconstructions of enamel-dentine junctions and tali, refining assessments of taxonomic diversity and phylogenetic affinities among Iberian dryopithecines. Similarly, endocast analyses from and material have illuminated locomotor and sensory , bridging gaps in the genus's .

Taxonomy and Phylogeny

Classification

Dryopithecus is classified within the superfamily Hominoidea, the family , and the Dryopithecinae, encompassing a group of extinct apes primarily known from Eurasian fossils. This placement reflects its status as an early great ape, with Dryopithecinae often treated as a distinct or tribe () of stem hominids, including genera such as Dryopithecus, Hispanopithecus, and Rudapithecus. Historically, Dryopithecus was initially described in the mid-19th century and grouped with other apes in the now-obsolete family , which included all non-human great apes. By the 1960s, extinct apes like Dryopithecus were often segregated into a separate family, Dryopithecidae, distinct from both and . Subsequent revisions in the late 20th century, driven by morphological comparisons, shifted Dryopithecus into , initially as a potential to pongines (orangutans) or hominines (African apes and humans), but increasingly as a stem hominid outside these crown clades. The current consensus, informed by post-2015 cladistic analyses incorporating dental, cranial, and postcranial data, positions Dryopithecinae as a clade of middle to Eurasian apes that diverged early within , distinct from both and . These studies, using and Bayesian methods on extensive character matrices, consistently recover Dryopithecus and related taxa as stem hominids, outside the ape-human , highlighting their role in early great ape diversification in rather than direct ancestry to modern groups. Recent reviews (as of ) suggest Dryopithecus may be paraphyletic, with some taxa better placed in distinct genera. This view underscores the origin of key hominid adaptations during the , with Dryopithecinae representing a basal separate from later dispersals.

Included Species

The genus Dryopithecus currently encompasses primarily one uncontested valid , distinguished by shared cranial and dental characteristics such as thin and a sectorial lower third (P3) that hones against the upper , features typical of Miocene hominoids adapted to arboreal lifestyles. The , D. fontani, was originally described from a discovered in 1856 at Saint-Gaudens, , with fossils dating to approximately 10–12 million years ago (Ma) during the middle ; this is represented by multiple dental and partial cranial specimens exhibiting the diagnostic thin (mean relative thickness of about 10.6) and sectorial P3 morphology. Material from St. Stefan, , originally described as D. carinthiacus (dated to ~12.5 Ma), is now often considered a junior synonym of D. fontani based on shared dental traits. D. brancoi, described in 1901 from isolated teeth and jaw fragments found at Eppelsheim, , dating to the late middle Miocene (approximately 11–12 Ma), is sometimes included in the genus; its assignment is justified by comparable dental features, including the thin cap and honing P3, despite limited material and ongoing debate about its distinction from D. fontani. Several taxa originally assigned to Dryopithecus have been synonymized or reclassified into separate genera based on distinct morphological differences. For instance, D. laietanus, known from multiple skeletons and dentition from late Miocene sites in (such as Can Llobateres, dated to about 9.9–9.8 Ma), was reclassified as Hispanopithecus laietanus in a 2004 taxonomic revision due to unique postcranial adaptations for suspensory locomotion that differ from the core Dryopithecus . Similarly, D. crusafonti from (originally described in 1992) is now classified as Hispanopithecus crusafonti, though its distinction from H. laietanus remains debated. Material from the late Miocene Rudabánya site in , initially referred to as Dryopithecus (including specimens like RUD 77), was reassigned to Rudapithecus hungaricus following analyses highlighting differences in cranial robusticity and dental proportions, such as relatively thicker paraconid on lower molars, separating it from the thinner-enamelled D. fontani group. The reference to D. wimani from in some older sources likely refers to material now attributed to D. brancoi or D. fontani, with no current recognition as a distinct . These reclassifications emphasize the importance of integrated dental, cranial, and postcranial evidence in delineating boundaries within dryopithecins. Taxonomic debates persist, with recent analyses (as of 2023) supporting the distinction of related genera like Pierolapithecus and Anoiapithecus from based on enamel-dentine junction , while underscoring the limited material for some proposed taxa.

Phylogenetic Position

is generally regarded as a basal great within , frequently positioned as a stem hominid in comprehensive phylogenetic analyses of Miocene fossils, though some interpretations favor it as a stem hominine more closely allied with the African and human clade () than with orangutans (). This placement stems from parsimony and Bayesian analyses incorporating cranial, dental, and postcranial characters, where clusters outside the crown hominine radiation but shares derived traits with later , such as reduced canine honing and thin-enameled molars. For instance, in related dryopithecines like Hispanopithecus and Rudapithecus exhibits semicircular canal proportions akin to those of and , distinguishing them from the more divergent pongine condition and supporting a closer affinity to . A key line of evidence for Dryopithecus's phylogenetic ties to involves its wrist , which displays features adapted for suspensory locomotion, including a proximodistally elongated capitate and modifications in the scaphoid-lunate articulation that parallel those in extant African apes. These adaptations, indicative of orthograde and bridging behaviors, suggest parallel evolutionary pathways from an ancestral hominoid condition toward in both hominines and pongines, but with Dryopithecus retaining a more aligned with the former's locomotor repertoire than the highly specialized below-branch of . Such postcranial evidence underscores Dryopithecus's role as a transitional form bridging early proconsulids and crown hominids, rather than a direct pongine precursor. The evolutionary position of Dryopithecus has fueled ongoing debates regarding the origins of great apes, particularly the contrast between an cradle as hypothesized by and an emerging model. Proponents of the European origin, including revisions by de Bonis and colleagues, argue that Dryopithecus and allied taxa represent the basal radiation of the hominid clade in , with subsequent dispersal to giving rise to modern around 9-7 million years ago. This view challenges Darwin's African-centric hypothesis by highlighting the absence of hominine fossils in and the abundance of dryopithecine remains in dating to 12.5-9.5 million years ago. Recent studies from 2010 to 2023 have refined this debate through integrated fossil and genetic approaches. estimates, calibrated against fossil divergences, align the initial Eurasian radiation of hominids—including Dryopithecus—with approximately 13 million years ago, coinciding with a shift in hominoid diversity from to amid climatic cooling and forest fragmentation. Phylogenetic analyses incorporating new Anatolian and specimens further support a Eurasian cradle for hominines, positioning Dryopithecus as part of a western Eurasian that dispersed eastward and southward. The analysis by de Bonis et al. emphasizes postcranial and dental synapomorphies linking Dryopithecus to early hominines, reinforcing the European origin of the while acknowledging gaps in the record.

Physical Description

Cranial and Dental Features

The cranium of Dryopithecus is characterized by a small braincase with an endocranial volume estimated at 300–330 cm³, comparable to that of extant small-bodied apes. The face exhibits moderate , featuring a long muzzle and a large, triangular pyriform that is widest at its base and vertically oriented relative to the facial plane. The nasal region includes a fused nasoalveolar clivus without a septal groove, and the , where preserved, are thin and contribute to a steep nasomaxillary suture. Dental remains reveal low-crowned molars with thin , a condition shared with African great apes and contrasting with the thicker of some contemporaneous Asian hominoids. The molars display a Y-5 cusp pattern, consisting of five main cusps arranged in a characteristic configuration typical of hominoids. Upper premolars and molars are wide with inflated bases and slightly peripheralized cusps, while canines are moderately compressed and high-crowned, particularly in males, with a honing complex evident on associated mandibular specimens. Sexual dimorphism is pronounced in the cranium and dentition, with males exhibiting more robust features such as larger canines and overall greater craniofacial size compared to gracile females. This dimorphism aligns Dryopithecus with modern great apes in displaying significant intraspecific variation in head morphology. In comparison to Sivapithecus, Dryopithecus shares some dental traits like robust premolars but differs in having a longer midface, greater nasal margin length, and reduced facial height; notably, it lacks the airorhynchy (upward tilt of the nasal region) diagnostic of pongine apes.

Postcranial Skeleton

The postcranial skeleton of Dryopithecus is known primarily from fragmentary remains, with the most complete evidence coming from the partial IPS 18800 of D. laietanus (also referred to as Hispanopithecus laietanus) recovered from the site of Can Llobateres 2 in , dated to approximately 9.6 million years ago. This assemblage includes elements of the , , forelimbs, and hindlimbs, revealing a with orthograde adaptations intermediate between those of cercopithecoids and extant hominoids. The overall proportions are gibbon-like, with elongated forelimbs relative to hindlimbs, supporting a body mass estimate of 20–30 kg for adults. The torso exhibits features indicative of a broad, shallow chest suited for suspensory postures, as evidenced by preserved and vertebral fragments from 18800. The first , for instance, displays a craniocaudally compressed shaft similar to that in modern great apes, combined with a protuberant more akin to monkeys, suggesting a transitional . Vertebrae from the same , including thoracic and elements, further indicate a wide and flexible spinal column, with dimensions comparable to those in small hominoids like . These axial elements collectively point to enhanced mobility in the and regions without fully committing to the derived orthogrady of later apes. Forelimbs in D. laietanus are characterized by elongated arms and highly mobile shoulders, as seen in the scapular fragments, , and remains from Can Llobateres. The shows a hominoid-like distal morphology with a reduced lateral supracondylar ridge, while the proximal features a broad trochlear notch and short process, facilitating extension during suspension; however, a posteromedially tilted retains some quadrupedal capabilities. The radial is mediolaterally compressed, resembling cercopithecoid patterns, and hand phalanges are long and curved, with proximal phalanges exhibiting dorsally concave articular surfaces for hyperextension. These traits align with proportions yielding an intermembral index of around 110–120, akin to . Hindlimbs are shorter than forelimbs, with evidence from femoral, , and pedal elements emphasizing grasping capabilities over propulsion. The distal from IPS 18800 displays a robust talar facet and medial oriented for dorsiflexion, supporting foot inversion during arboreal activities, while phalanges—particularly proximal pedal ones—are elongated and curved, indicative of a prehensile foot with opposable hallux. Femoral remains suggest a relatively short bone compared to the , reinforcing the gibbon-like limb and a body mass scaling around 22–25 kg for the Can Llobateres individual. Additional isolated postcranials, such as a from older European sites attributed to D. fontani, show similar robusticity but larger estimated mass up to 44 kg, highlighting intraspecific variation.

Paleobiology

Locomotion and Behavior

Dryopithecus primarily engaged in arboreal locomotion, relying on suspensory climbing and arm-swinging to navigate forest canopies, as indicated by postcranial adaptations such as a mobile elbow joint with a strongly marked brachialis insertion for powerful flexion and a wrist with reduced stylo-triquetral contact enabling extensive pronation and supination. These features, observed in partial skeletons like that of Hispanopithecus laietanus (synonymous with Dryopithecus laietanus), suggest a locomotor repertoire similar to that of modern orangutans, emphasizing orthograde clambering and below-branch suspension on flexible branches rather than rapid quadrupedalism. The long forelimbs relative to hindlimbs further supported above-branch progression and grasping during movement, reflecting an adaptation to small-branch foraging environments. Terrestrial capabilities appear limited in Dryopithecus, with no morphological evidence for habitual or , distinguishing it from later hominoids and implying a predominantly arboreal confined to forested habitats. The postcranial , including a broad shallow and dorsally positioned , reinforces this arboreal specialization without indications of significant ground-based locomotion. Behavioral inferences from high levels of in body size observed in Dryopithecus s suggest a involving male competition, potentially with fission-fusion grouping, though the exact nature remains speculative due to limited . There is no direct evidence for tool use or constructed nesting, consistent with the lack of such behaviors in early hominoids. isotope analyses from the Rudabánya site, where D. brancoi is found, indicate seasonal variations in forest resources, implying potential seasonal movements within wooded environments to track available arboreal niches.

Diet and Social Structure

Dryopithecus species are inferred to have been primarily frugivorous, consuming soft fruits and leaves, as indicated by their low-cusped molars with thin suited for processing ripe, sugary produce rather than hard or abrasive items. Dental microwear analyses further support this, showing patterns consistent with a rich in fruits, including evidence of caries lesions in specimens like D. carinthiacus that suggest frequent intake of high-sugar foods such as ripe fruits and possibly . Microwear on buccal enamel surfaces reveals additional variability, with scratches and pits indicating occasional folivory or consumption of tougher vegetation, resembling patterns seen in modern folivores like gorillas that process abrasive plant matter. Post-2015 studies, including texture analyses of related dryopithecins such as Rudapithecus hungaricus, confirm intermediate complexity in microwear suggestive of mixed feeding that includes harder foods alongside fruits, potentially reflecting seasonal shifts toward more folivorous habits. Fine-scale pits in some specimens hint at minor insectivory, though this remains supplementary to the dominant frugivorous signal. The social structure of Dryopithecus is not directly evidenced by fossils but inferred from pronounced in body and canine size, which parallels that in extant apes with high dimorphism such as or orangutans. This high dimorphism suggests a structure potentially involving or solitary male dispersal with male competition for mates, aligning with the ecological demands of a fruit-based requiring ranging in forested habitats, though direct behavioral traces are absent and inferences remain tentative.

Paleoecology

Habitat and Environment

Dryopithecus inhabited subtropical woodlands and forests across during the mid- to epoch, spanning approximately 12.5 to 11.1 million years ago. These environments consisted of a heterogeneous mix of and trees, forming dense canopies with occasional clearings that supported arboreal lifestyles. evidence from associated sites indicates that these forests were characterized by high diversity, including fruit-bearing trees and vegetation suitable for . The climate during this period was predominantly warm and humid, with seasonal rainfall patterns that promoted lush vegetation growth. Pollen records from Miocene deposits associated with Dryopithecus remains reveal a prevalence of thermophilous (warm-loving) plant species, such as oaks, laurels, and figs, underscoring the subtropical conditions. These wetter phases aligned with the broader Climatic Optimum, where elevated atmospheric CO₂ levels and global temperatures fostered expansive forested biomes. However, subtle seasonal variations in precipitation likely influenced resource availability, as evidenced by isotopic analyses of associated sediments. Dryopithecus coexisted with a diverse array of large herbivores, including rhinoceroses like Plesiaceratherium and proboscideans such as Gomphotherium and Deinotherium, which grazed and browsed in the understory and forest edges. This faunal assemblage points to transitional habitats blending closed-canopy woodlands with open savanna-like margins, where mixed feeders thrived on browse and grasses. Such associations highlight the ecological role of Dryopithecus within a balanced ecosystem supporting both arboreal and terrestrial mammals. Toward the late Miocene, around 11 million years ago, environmental shifts driven by global cooling and increased aridity began to alter these habitats. Progressive retreat of warm, humid forests into more fragmented, open woodlands reduced suitable arboreal niches, contributing to the restricted distribution and eventual extinction of Dryopithecus in . This climatic transition, marked by declining temperatures and expanding C4 grasslands, disrupted the subtropical refugia that had sustained hominoid diversity.

Geographic Distribution

Fossils attributed to Dryopithecus are primarily known from Western and , with key discoveries in , , , and . These sites document the genus's distribution during the middle to , reflecting its adaptation to forested environments across the continent. In , early specimens were recovered from Saint-Gaudens in the region, where a and other remains indicate a late middle Miocene age of approximately 11.5 million years ago (mya). Additional French localities, such as La Grive-Saint-Alban, have yielded dental and cranial fragments from the Vallesian stage (11.2–9.7 mya). In , the richest assemblages come from the Vallès-Penedès Basin in , including sites like Abocador de Can Mata and Can Llobateres, dated to 12.0–11.8 mya, encompassing the middle boundary and early Vallesian. These Iberian finds include partial faces, dentition, and postcranial elements, highlighting D. fontani as a prominent species. German sites, such as Eppelsheim in , have produced isolated teeth from the late Vallesian, around 10 , contributing to understanding Dryopithecus's eastern extent in . Austrian records include dental remains of D. carinthiacus from Mariathal and St. Stefan, also from the late middle , approximately 12–11 . Collectively, these European localities span 12.5–11.1 , aligning with the Vallesian mammalian stage. The genus's range shows possible extensions beyond core , with questionable links to populations via Miocene migration routes across the Tethys Sea, though no definitive Dryopithecus fossils have been confirmed on the African continent. There are no verified Asian records, distinguishing Dryopithecus from contemporaneous pongine apes like in . Potential eastern extensions include isolated Balkan finds, such as tentative attributions from (typically classified as the related dryopithecine ) and , but these remain debated as of 2025 and not conclusively assigned to the genus.

Evolutionary Significance

Relation to Modern Apes

Dryopithecus shares several morphological traits with modern , particularly in postcranial and dental features that suggest a close affinity within the great ape lineage. The facial morphology of Dryopithecus exhibits derived hominid characteristics reminiscent of , including robust jaw structure and overall cranial proportions adapted for powerful mastication. Additionally, dental features such as elongated shearing crests on the molars reflect traits shared with African apes, consistent with a mixed of soft fruits and leaves, though distinguished from the specialized folivory of modern by its thin enamel. Morphometric analyses of postcranial elements support this resemblance, with similarities in limb proportions and configurations based on shared traits in and pelvic morphology. In contrast, Dryopithecus differs markedly from orangutans in key dental and adaptations. Its thickness is notably thin, averaging relative enamel thickness (RET) values around 10.6, which contrasts with the moderately thicker enamel in (RET ~15-20), reflecting dietary divergences where Dryopithecus relied more on soft fruits and leaves rather than harder, abrasive foods. morphology in Dryopithecus also aligns more closely with hominines than pongines; the , including the scaphoid and capitate, show configurations supporting compressive loading and grasping during arboreal , akin to African apes, rather than the enhanced midcarpal mobility specialized for suspension in orangutans. Relative to humans, Dryopithecus retains basal great ape traits, such as a small estimated at 300-330 cm³, comparable to modern apes but far below the average of 1,200-1,400 cm³, indicating limited . However, its suspensory limb adaptations, evidenced by elongated forelimbs, flexible shoulder joints, and orthograde postural capabilities in the partial skeleton from , represent an early stage in great ape locomotion that prefigures the locomotor shifts toward in later hominins.

Role in Hominid Evolution

Dryopithecus plays a pivotal role in hypotheses regarding the Eurasian origin of the family, providing evidence that supports a biogeographic model in which early hominoids migrated around 17–13 million years ago (), diversified in , and subsequently dispersed back to . Fossils of Dryopithecus, dating to approximately 12.5–9.5 from sites across , exhibit key derived traits such as enhanced suspensory locomotion adaptations and thin-enameled molars suited to Eurasian forest environments, which align with the emergence of crown hominids in this region from more primitive ancestors like Kenyapithecus. This "out of Africa then back" scenario posits that hominine lineages, including precursors to apes and humans, re-entered around 9–8 , challenging earlier Africa-centric views of great origins. As a representative of the Dryopithecinae , Dryopithecus is considered a key precursor to the hominine radiation, bridging the divergence of great ape lineages and the subsequent African ape split around 8–7 . Its postcranial skeleton, including elongated forelimbs and a flexible , reflects an arboreal lifestyle that likely facilitated the ecological shifts enabling the separation of and chimpanzee-human clades in . Recent analyses of Dryopithecus specimens from and underscore its position as an early hominid that contributed to the diversification of suspensory behaviors, setting the stage for the hominine 's adaptation to varied forested habitats before the . This radiation is evidenced by the temporal overlap with related taxa like Rudapithecus, highlighting Dryopithecus's influence on the evolutionary trajectory toward modern great apes. However, its exact phylogenetic position remains debated, with some studies suggesting it as a stem hominine ancestral to the Pan-Homo , while others view it as a more basal or evolutionary side branch due to mosaic traits and . Debates surrounding Dryopithecus emphasize its status as a stem taxon rather than a direct of humans, serving instead as a close to the ape and human . Phylogenetic studies position it outside the immediate human lineage, with shared traits like reduced dimorphism informing broader hominid ancestry but not specific bipedal origins. Its locomotor features, primarily suspensory and orthograde, have influenced hypotheses on the transition to by suggesting that early hominins retained arboreal capabilities before terrestrial adaptations, countering models of immediate . Analyses integrating and dental data continue to support a emphasis in hominid models, though debates on versus Eurasian origins persist.

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