In 1967 G.G. Simpson described three partial mandibles from early Miocene deposits in Kenya that he interpreted as belonging to a new strepsirrhine primate, Propotto. This interpretation was quickly challenged, with the assertion that Propotto was not a primate, but rather a pteropodid fruit bat. The latter interpretation has not been questioned for almost half a century. Here we re-evaluate the affinities of Propotto, drawing upon diverse lines of evidence to establish that this strange mammal is a strepsirrhine primate as originally suggested by Simpson. Moreover, our phylogenetic analyses support the recognition of Propotto, together with late Eocene Plesiopithecus from Egypt, as African stem chiromyiform lemurs that are exclusively related to the extant aye-aye (Daubentonia) from Madagascar. Our results challenge the long-held view that all lemurs are descended from a single ancient colonization of Madagascar, and present an intriguing alternative scenario in which two lemur lineages dispersed from Africa to Madagascar independently, possibly during the later Cenozoic.
Strepsirrhine or “toothcombed” primates include three ancient clades that diverged early in the Paleogene—Chiromyiformes (represented by one living and one subfossil species of aye-aye, both placed in the genus Daubentonia), Lemuriformes (containing extant lemurids, indriids, cheirogaleids, and lepilemurids, as well as the recently extinct archaeolemurids, palaeopropithecids, and megaladapids1), and Lorisiformes (lorisids and galagids). Recent molecular divergence estimates suggest that Madagascar’s lemurs (the clade containing both chiromyiforms and lemuriforms) split from lorisiforms in the Paleocene or early Eocene1,2,3,4,5, with lemurs colonizing Madagascar and then rapidly splitting into chiromyiform and lemuriform lineages1,2,3. The absence of a terrestrial Paleogene or Neogene fossil record on Madagascar6 has prevented paleontologists from testing this hypothesis. Given its geographic proximity to Madagascar, the adjacent African landmass is currently viewed as the most likely source for ancestral lemurs (and other endemic terrestrial mammals of Madagascar)6,7,8. Indeed, Paleogene ocean currents have been reconstructed as favoring west-to-east dispersal across the Mozambique Channel9, and together with the presence of both stem strepsirrhines and lorisiforms in Africa’s Eocene fossil record10,11,12 support this interpretation.
The primary challenge to the hypothesis of a single colonization of Madagascar by lemurs is the morphological evidence provided by the fossil primate Plesiopithecus teras, represented by a partial cranium and multiple mandibles from a single ~34 Ma (terminal Eocene) site in Egypt13,14. Godinot15 suggested a relationship between Plesiopithecus and extant Daubentonia, noting that “[Plesiopithecus’] lower jaw has exactly the morphology that would be predicted for a daubentoniid ancestor, having already markedly enlarged its anterior tooth and reduced the teeth posterior to it” (p. 457). Although marked enlargement of a single highly procumbent anterior lower tooth occurred more than once in primate evolution (e.g., in Eocene omomyiform haplorhines16), it is nevertheless an exceptionally rare pattern, and among extant primates is now seen only in Daubentonia, a taxon with highly specialized rodent-like anterior teeth. Godinot’s phylogenetic hypothesis linking Daubentonia and Plesiopithecus depends heavily upon their enlarged anterior lower teeth being homologous, as the cheek teeth of Daubentonia are highly modified and bear little resemblance to those of any living or extinct primate; the anterior teeth of Daubentonia are likely incisors17, whereas those of Plesiopithecus could be either canines or incisors18. Although Godinot did not test his hypothesis with an algorithm-driven phylogenetic analysis, it recently gained some support from a Bayesian tip-dating analysis of morphological and molecular data19 that, for some treatments of the morphological data, recovered evidence for a Daubentonia-Plesiopithecus clade within lemurs, despite the fact that, following previous interpretations13,20, the enlarged anterior lower tooth of Plesiopithecus was scored as a canine rather than as an incisor.
Here we present several new lines of evidence suggesting that the purported pteropodid fruit bat Propotto from the early Miocene of western Kenya is not only a strepsirrhine primate as was originally suggested by Simpson21, but represents a close relative of both Plesiopithecus and Daubentonia. Plesiopithecus was first described in 199214, a quarter century after the debate surrounding Propotto’s affinities appeared to have been resolved, hence its significance for interpreting Propotto was not appreciated. Our comparisons indicate that Propotto shares a number of specialized morphological features with Plesiopithecus, including all of the features that originally led Walker22 to doubt Simpson’s proposed lorisid affinities for Propotto. Furthermore, digital reconstruction of the badly damaged upper molars of Plesiopithecus and comparisons with other specimens led us to the identification of two upper molars of Propotto, previously identified as “Lorisidae indet.”23, from the early Miocene site of Chamtwara, Kenya. These specimens offer the first glimpse of Propotto’s upper dentition and further buttress the case for its strepsirrhine primate affinities. Finally, a mandible of Plesiopithecus is here interpreted as retaining a small toothcomb-like canine distal to its enlarged anterior tooth, establishing that the enlarged anterior tooth is probably an incisor, thereby increasing the likelihood that the procumbent anterior lower teeth of Daubentonia, Propotto, and Plesiopithecus are homologous incisors.
Comparative dental morphology of Propotto and Plesiopithecus
Propotto leakeyi was originally described by Simpson as a lorisiform strepsirrhine that might be related to the extant lorisid Perodicticus (commonly known as the potto)21. The hypodigm available to Simpson included the holotype (KNM-SO 508, his specimen “R”; KNM = National Museums of Kenya), a right mandible with P3-M2 and alveoli for P2 and M3 as well as a small portion of the root of an enlarged anterior tooth (Figs. 1g and 2b); KNM-RU 1879 (specimen “S”), a left mandible with a very shallow P2 alveolus, an erupting P3, fully erupted dP4 and M1, alveoli for M2 and an erupting M3 (see M1 and M3 in Fig. 1c, d, respectively; this specimen also exhibits a laterally compressed and forward-facing alveolus for an anterior tooth); and KNM-RU 2084 (specimen “T”), a right mandible with M2–3 that is most likely from Songhor but labeled as being from Rusinga (Fig. 1i). KNM-RU 1879 has “Songhor” written on the specimen despite the fact that the label suggests it might be from Rusinga; we consider it probable that the specimen is, in fact, from Songhor. If all of these specimens are indeed from Songhor, they would originate in the Chamtwara and the “Kapurtay Conglomerates” of Butler24, which Pickford25 put in his “Set I” fauna, and dated at 18.5–20 Ma. This estimate is mainly based on K-Ar dates of Bishop et al.26 published in 1969, so additional work is needed to provide more precise age constraints for these localities using contemporary methodologies. Digital models of all the fossil specimens figured here are available on MorphoSource (Table 1).
Simpson21 noted the “highly peculiar cheek teeth” (p. 51) of Propotto and the fact that its mandible deepened anteriorly, but nevertheless considered this taxon to be similar enough to the extant lorises Perodicticus and Nycticebus to recognize Propotto as an aberrant lorisid. Walker22 re-examined the hypodigm of Propotto and pointed out that the single-rooted P2 was probably small (though no crown is preserved), and not enlarged and caniniform as in lorisiforms. Further, he interpreted the alveolus of Propotto’s enlarged anterior lower tooth as being for a caniniform canine, and contrasted that with the canine morphology that would be expected in lorisiforms, which incorporate the canine into a toothcomb. Finally, he noted that the mandibular corpus was also unlike those of lorisiforms in deepening anteriorly and having a deep masseteric fossa. Walker concluded that Propotto was a pteropodid fruit bat and not a primate, a conclusion that was accepted by Simpson in correspondence exchanged before the 1969 publication of Walker’s work (Supplementary Fig. 1).
In 1984, Butler24 described a few additional Propotto specimens from the early Miocene sites of Koru, Chamtwara, and Rusinga Island in western Kenya25. The specimens from Rusinga localities located in the Hiwegi Formation would be considerably younger, dated to ~17.9 Ma27. Butler discussed the resemblance of Propotto’s cheek teeth to those of primates such as Cheirogaleus, Perodicticus, and Pithecia, and also with the Neotropical phyllostomid bat Artibeus. He further noted that the enlarged anterior lower tooth of Propotto (which he also interpreted as a canine) is relatively larger than the lower canines of extant pteropodids, having a root that extends posteriorly to at least P3. Despite these observations, Butler ultimately supported the idea that Propotto represented a side-branch of the chiropteran family Pteropodidae, erecting a new subfamily, Propottininae, for the genus.
For the last half-century, discussion of Propotto’s significance as a possible primate has been deterred by the authoritative consensus reached by Simpson, Walker, and Butler that Propotto is a bat. However, it is now clear that the features that Walker cited in his criticism of Simpson’s identification of Propotto as a lorisid are all characteristic of the undoubted strepsirrhine primate Plesiopithecus and so do not necessarily exclude Propotto from Strepsirrhini (Fig. 1j). The laterally compressed and presumably highly procumbent lower anterior tooth of Propotto (Fig. 2d, e; unknown to both Simpson and Walker because this feature is only preserved in specimens described by Butler in 1984) does not occur in fruit bats, or for that matter any known living or extinct chiropteran. This feature is, however, present in Plesiopithecus (Figs. 1j and 2d–f) and Daubentonia.
Despite being very low-crowned, the lower molars of Propotto are fundamentally strepsirrhine in structure, and are very similar to those of Plesiopithecus (Fig. 1a–i). Differences from Plesiopithecus include extension of the oblique cristids to meet the protoconid apices, reduction or elimination of hypoflexids, reduction of metaconids, and presence of a cingulid around the lingual margin of the metaconids. The P3–4 of Propotto and Plesiopithecus are very similar in having mesially shifted protoconids from which two dominant crests run distobuccally and distolingually to enclose well-developed talonids (Fig. 2b, c). An automated geometric morphometric analysis of lower molar morphology in strepsirrhines, pteropodids, Propotto, and various living and extinct euarchontans demonstrates that the shape of Propotto’s M2 is most similar to that of strepsirrhines (and particularly those of cheirogaleids, Daubentonia and Plesiopithecus; Fig. 3). The molar morphology of this set of taxa occupies a morphospace that is distinct from sampled pteropodids. Strepsirrhine lower molars also have low principal component (PC) 1 values that separate them from all non-euarchontans, non-primates, tarsiers, and almost all sampled Paleogene primates. The only fossils that group with modern strepsirrhines on PC1 are Adapis, Propotto, and Plesiopithecus. On PC2, strepsirrhines are divided into a cluster of lemurids, indriids, lorisiforms, and Adapis with high values, and another including cheirogaleids (Microcebus, Cheirogaleus, Mirza, Phaner), Daubentonia, Plesiopithecus, and Propotto with low values. The pteropodid fruit bats Pteropus and Rousettus are well-separated from Propotto in having much higher PC1-2 scores, although they do overlap with the second group of strepsirrhines. Although we only plot PC1 (20% of variance) and PC2 (14% of variance) in Fig. 3, the most important clustering patterns are maintained on PC3 and PC4, as well (Supplementary Data 1–3).
In addition, digital reconstruction of the damaged upper molars of Plesiopithecus (Fig. 4a) reveals similarities with two upper molars from Chamtwara that were previously identified as “Lorisidae indet.” by Harrison23 (Fig. 4b). Manipulation of digital surfaces of these upper molars allowed us to confirm that they occlude perfectly with Propotto lower molars from Chamtwara (Fig. 1e, f), and they are accordingly identified here as the first known upper teeth of Propotto. The morphology of these upper molars also resembles that of the possible stem lorisiform Karanisia from the earliest late Eocene of Egypt (Fig. 4d)10, the stem strepsirrhine Djebelemur from the early or middle Eocene of Tunisia28, and, intriguingly, the enigmatic late Eocene primate Nosmips from Egypt, which has been placed with Plesiopithecus in some phylogenetic analyses20. Among extant primates, Propotto’s upper molars (particularly M1) are most similar to those of the dwarf lemur Cheirogaleus. Similarities to Djebelemur, Karanisia, Nosmips, and Plesiopithecus include the broad lingual and more restricted buccal cingula, absence of a metaconule, and a concave distal margin of M2. Although some of these features may be primitive within Strepsirrhini, this character suite is nevertheless clearly characteristic of early strepsirrhines, and is not found in any living or extinct chiropteran. The upper molars of Propotto differ from those of known Paleogene strepsirrhines in being very low-crowned (matching the pattern seen in the lower molars), and in exhibiting a massive lingual cingulum, flattened lingual surfaces of the buccal cusps, and a reduced protocone.
The anterior dentition of Plesiopithecus
The holotype of Plesiopithecus teras (CGM 42291; CGM = Egyptian Geological Museum) preserves a single enlarged and procumbent tooth mesial to P2-M3. A different mandibular specimen, DPC 11636 (DPC = Duke Lemur Center Division of Fossil Primates), was figured and discussed by Simons and Rasmussen13 (their Fig. 3) and preserves a small tooth (which the authors interpreted as a P1) between the enlarged anterior tooth and the P2. They did note, however, that the tooth “might also be the lateral canine derived from a toothcomb” (p. 9949). At some point after the description of this specimen in 1994, the crown of the tooth was broken and glued back onto the root, although rotated into an incorrect orientation. We have reconstructed the tooth using digital models and provide additional views of the specimen for the first time (Figs. 2c and 5). The tooth differs markedly in morphology and orientation from the adjacent P2, and has several features that are more consistent with it being a vestigial canine. The evolution of Daubentonia’s rodent-like incisor morphology from a toothcombed ancestor would likely involve topographically shifting the canine out of the toothcomb to accommodate an enlarged incisor. Indeed, in Plesiopithecus, this canine is strongly procumbent relative to its root, has a flattened surface (corresponding to the mesial face of a typical toothcomb canine, but more appropriately described as topographically lingual in DPC 11636) demarcated by a distinct ridge from the surface best exposed in occlusal view (lingual in a typical toothcomb canine, better described as topographically distal in Plesiopithecus), which has a gently curving and apically convex buccal margin. Morphological evidence supporting identification of this tooth as a lower canine rather than as a first premolar is supplemented by the dental formulae of all known living and extinct crown strepsirrhines, which unequivocally indicates that the loss of the upper and lower first premolar occurred along that clade’s stem lineage, and therefore before the appearance of both the strepsirrhine crown group and the split between the chiromyiform and lemuriform lineages. Indeed, no African strepsirrhine, living or extinct, is known to retain a P1. In light of this, it is more parsimonious to interpret this tooth of Plesiopithecus as a reduced lower canine, requiring the enlarged anterior tooth of Plesiopithecus to be an incisor, and therefore more likely homologous with the anterior tooth of Daubentonia. This enlarged anterior tooth also shows some thinning of the lingual enamel (relative to that on the buccal surface), though not to the extent seen in Daubentonia. The Plesiopithecus mandible DPC 13607 has also been digitally reconstructed, revealing a tiny canine alvelous anterior to the P2 (Fig. 1j); therefore the holotype is unlike the two other known specimens in lacking a canine.
Phylogenetic placement of Propotto and Plesiopithecus
Phylogenetic analysis (see Methods) of our combined molecular and morphological data matrix using the Bayesian tip-dating method with fossilized-birth-death parameterization recovered Propotto as exclusively related to Daubentonia, and Plesiopithecus as the sister taxon to this Daubentonia-Propotto clade (Fig. 6). Standard Bayesian (“non-clock”) analysis recovered an exclusive Propotto-Plesiopithecus clade that is sister to Daubentonia. In both analyses, Propotto and Plesiopithecus are strongly supported as crown lemurs (posterior probability = 0.9) and are situated as stem chiromyiforms. Importantly, this result emerged despite controlling for two scoring biases that could have provided additional support for a Daubentonia-Plesiopithecus-Propotto clade. First, though there are sound reasons to consider Propotto’s enlarged anterior lower tooth to be homologous with that of Plesiopithecus, Propotto was conservatively not scored for either canine or incisor characters (i.e., only premolar and molar characters were scored). Second, Plesiopithecus’ enlarged anterior upper teeth were scored as canines and not incisors, although they could conceivably be enlarged incisors homologous with those of Daubentonia. To further avoid bias, we did not create any new characters or character states to capture novel observations of derived dental features shared by Daubentonia and Propotto to the exclusion of Plesiopithecus (see discussion below).
Bayesian stepping-stone estimation of marginal likelihoods for alternative placements of Plesiopithecus and Propotto, using the morphology matrix and constraining these two taxa to fall in different positions within the optimal time-scaled tree derived from the tip-dating analysis of molecular and morphological data, reveals that there is “strong” evidence (based on a Bayes factor of 15.64) for favoring a (Plesiopithecus (Daubentonia, Propotto)) topology over the (Daubentonia (Plesiopithecus, Propotto)) topology derived from the non-clock analysis. Other alternative constraints, such as situating Plesiopithecus and Propotto as advanced stem strepsirrhines or as stem lemurs, were decisively rejected by stepping-stone analyses (based on Bayes factors of 572.49 and 651.97, respectively). Bayesian reconstruction of ancestral morphological character states on the optimal clock topology identified 15 character state changes along the chiromyiform stem leading to the (Plesiopithecus (Daubentonia, Propotto)) clade, and 18 character state changes along the lineage leading to the Daubentonia-Propotto clade. The monophyly of Eocene-Recent chiromyiforms is supported by character changes relating to the modification of the anterior dentition to include only a single enlarged and procumbent incisor, as well as numerous details of premolar and molar crest and cusp development/placement, and increased depth of the mandibular corpus (see supporting data files held in the Dryad Digital Repository associated with this study (https://doi.org/10.5061/dryad.gb182)).
Biogeographic history of lemurs
Bayesian reconstruction of strepsirrhine biogeographic history strongly supports (posterior probability = 1) African origins for both Chiromyiformes and Lemuriformes, implying independent dispersals across the Mozambique Channel. Our analyses place the last common ancestor of Daubentonia and Propotto on the African continent at 27.9 Ma (near the early-late Oligocene boundary), suggesting that the dispersal to Madagascar that ultimately gave rise to Daubentonia likely occurred some time after the early Oligocene. The continental divergence of the chiromyiform and lemuriform lineages is estimated at 41.1 Ma (late middle Eocene) and the island origin of crown lemuriforms is estimated at 19.9 Ma (early Miocene).
Our analyses suggest that Propotto and Plesiopithecus are stem chiromyiform lemurs that are closely related to the extant aye-aye Daubentonia from Madagascar, and that stem chiromyiforms were present in Africa from at least the late Eocene through the early Miocene. Our time-scaled tree, when combined with Bayesian biogeographic analyses, strongly supports an African origin for the common ancestor of lemuriforms and chiromyiforms, and independent dispersals of these groups across the Mozambique Channel to Madagascar. Although independent African origins for two closely related Madagascan lineages might appear overly coincidental, recent molecular phylogenies of chameleons indicate that there were two independent colonizations of Madagascar by African lineages in the Cenozoic29, establishing an independent precedent for the feasibility of such a pattern. Our results suggest that the chiromyiform dispersal to Madagascar occurred no earlier than the Oligocene (based on the divergence date of Propotto and Daubentonia), while the lemuriform dispersal could have occurred no later than the early Miocene (based on the time of origin of the crown lemuriform clade). Our results do not allow us to address the question of when the lemuriform dispersal to Madagascar occurred within the ~41 to ~20 Ma dispersal window provided by our analyses, but it is noteworthy that the combined phylogenetic and biogeographic evidence can now accommodate a scenario in which lemuriforms dispersed to Madagascar quite late in the Cenozoic (i.e., as late as the earliest Miocene), where they then underwent an adaptive radiation. Because our results do not require lemuriforms to have been present on Madagascar until the early Miocene, they render the recently proposed hypothesis of a mass extinction of lemuriforms on Madagascar near the Eocene–Oligocene boundary1 less likely, but not impossible.
Previously, lemurs have been regarded as the first placental mammals to colonize Madagascar (with the possible exception of the enigmatic subfossil mammal Plesiorycteropus, whose affinities are uncertain). However, our results suggest much later dispersal windows for lemuriforms and chiromyiforms which overlap with those that have been recently estimated for Madagascar’s other endemic terrestrial mammals—i.e., euplerid carnivorans30,31, nesomyine rodents31, and tenrecids31,32. The Oligocene to early Miocene interval also overlaps with recently proposed dispersal windows for hyperoliid frogs8,33, lamprophiid snakes8,34, zonosaurine lizards8,35, as well as multiple scincids and gekkonids8. Importantly, this interval was also characterized by the lowest sea levels in the Cenozoic36, prior to the onset of middle Miocene cooling.
Several additional derived dental features shared by Propotto and Daubentonia (to the exclusion of Plesiopithecus) would be consistent with a close relationship of the former two genera, but were not captured by the morphological matrix used here. In the upper dentition, both taxa have particularly well-developed parastyle and metastyle cusps that are close in height to the paracone and metacone, respectively; flat (as opposed to convex) lingual surfaces of the buccal cusps; and low molar protocones. In the lower dentition, Daubentonia and Propotto share very shallow talonid basins; tall and wall-like oblique cristids; and highly reduced (Propotto) or absent (Daubentonia) metaconid and entoconid cusps, protocristid crests, and hypoflexids on M1–2. The Propotto specimen KNM-RU 3690 shows that the mesial aspect of P3 was much closer to the alveolus for the enlarged anterior lower tooth than in Plesiopithecus, suggesting that the P2 of Propotto was smaller than that of Plesiopithecus and that there was no room for a canine as in Plesiopithecus; this pattern is derived toward the total loss of the lower premolars seen in Daubentonia.
From a functional perspective, the distally oriented postprotocrista and mesiodistally aligned lingual cingulum on the M1 of Propotto, combined with the low M1–2 protocones, flattening of the talonid basins and reduction of the hypoflexids, protocristids, and metaconids on the lower molars (features not present in Plesiopithecus) reflects increased emphasis on propalinal mastication and associated development of predominantly mesiodistally aligned upper and lower molar wear facets, as in Daubentonia. If Propotto is indeed a close relative of Daubentonia, the former’s massive lingual cingula and reduced protocone and metaconid cusps might even help to explain the strange lingual region of M1–2 in Daubentonia. These teeth superficially appear to lack a lingual cingulum, but nevertheless bear hypocone cusps, structures that are always derived from the distolingual cingulum in crown strepsirrhines. The fact that the M1–2 hypocones in Daubentonia are connected buccally to the postmetacristae by what appear to be tall and thick postcingula, and are continuous mesiolingually with similarly tall and thick elongate ridges, hints at the possibility that the latter features might be derived from the lingual cingulum and not the protocone, and that the protocones (which are highly reduced in Propotto) are effectively absent in Daubentonia. A possible mechanism for this transformation is provided by the occlusal morphology of the Propotto molars from Chamtwara, the M1 of which bears a cingulid lingual to the very reduced metaconid that occludes with the lingual cingulum of M1. Digital manipulation of these surfaces indicates that the gutter between the mesial aspect of the M1 lingual cingulum and the protocone occludes on top of the reduced M1 metaconid, which is a remarkably odd arrangement, but one that, taken to an extreme, would yield a morphology like that seen in Daubentonia (Fig. 2a). The morphological similarity of Daubentonia and Propotto M2 surfaces, as supported by our automated geometry analyses, lends further credibility to this hypothesis. Again, these novel interpretations of the cusp/crest homologies of Daubentonia were not scored as characters in our phylogenetic analyses to avoid circularity in our assessment of phylogenetic relationships of the taxa in question.
Marked restructuring of interpretations of strepsirrhine biogeographic history suggested by our analyses presently depends almost exclusively on dental morphology, hence more rigorous tests of these hypotheses will only be possible as new and more complete fossils are discovered. An obvious challenge to the hypothesis that chiromyiforms and lemuriforms independently dispersed to Madagascar is the current lack of diagnostic stem lemuriforms in the African fossil record. Notably, the Paleogene fossil record of Afro-Arabia is notoriously poor and geographically biased toward northern Africa37. Nonetheless, a handful of fragmentary fossils provide tantalizing evidence of possible lemuriform-like strepsirrhines from other parts of Afro-Arabia, such as Notnamaia from Namibia38, and Omanodon and Shizarodon from Oman39. Furthermore, an early Miocene origin for the crown lemuriform clade does not necessarily require that the Africa-to-Madagascar dispersal event be coincident with, or even close in age to, the origin of that clade—that dispersal could have occurred at any point along the long lemuriform stem lineage. Therefore, absence of lemuriform fossils from the Paleogene of Afro-Arabia might be explained by an early dispersal to Madagascar closer to the chiromyiform–lemuriform split, followed by the extinction of basal stem lemuriforms in Africa. An analogous pattern is seen in the fossil record of platyrrhine anthropoid primates that likely also originated in Afro-Arabia and then dispersed to South America, from an as-yet unsampled stem lineage in Afro-Arabia.
Regardless of the phylogenetic and biogeographic history of Daubentonia, it is of great paleoecological significance that Cenozoic African primate communities gave rise to a somewhat Daubentonia-like (and presumably tree gouging) primate lineage, as occurred in various non-primate mammalian radiations on other continents, such as Apatemyidae and various plesiadapiform euarchontans on northern continents, and the marsupial groups Petauridae and Yalkaparidontia in Australasia40,41. It is also significant that the strepsirrhine lineage represented by Plesiopithecus and Propotto persisted in Africa well into the Miocene, long after major perturbations in Earth climate history such as global cooling at the Eocene–Oligocene boundary and biotic events in Africa such as the immigration of multiple mammalian lineages in the late Oligocene or early Miocene. These patterns add to the evidence that equatorial Africa likely had a key role as a relatively temperate refugium for primate communities at a time of marked mid-Cenozoic ecological restructuring42,43.
We tested Simpson’s original hypothesis of Propotto-lorisid affinities, and Godinot’s hypothesis of a Daubentonia-Plesiopithecus clade within Strepsirrhini, by adding Daubentonia and Propotto to an augmented version of Seiffert et al.’s44 morphological character matrix, rescoring the anterior lower dentition of Plesiopithecus (taking into account the observations detailed above), and combining those morphological data with the molecular dataset of Springer et al.4. The dermopteran Galeopterus was also added to the matrix and scored for morphological characters, so that two extant euarchontan outgroup taxa were scored for both molecular and morphological data; the augmented morphological dataset now includes 102 fossil and 23 living euarchontans and 395 characters. To maximize phylogenetic signal, 264 ordered characters were constructed using intermediate states to code for polymorphic observations45. However, MrBayes currently imposes a six-state limit for ordered transformation series, necessitating that 39 of these characters be recoded using standard polymorphic scoring.
The DNA supermatrix of Springer et al.4 consists of 69 nuclear and 10 mitochondrial gene segments totaling 61,119 positions. To optimize data completeness, molecular sequences for Lepilemur ruficaudatus and Propithecus verreauxi were selected to accompany morphological character scores for their respective genera. All other taxa were scored for both molecular and morphological data at the species level, and species present in the DNA supermatrix but absent from the morphological dataset were removed. PartitionFinder v2.1.146 was used to select a DNA subset scheme and nucleotide substitution models. Each gene segment was assigned as an input block and testing included all models available in MrBayes. The best parameterization was assessed using the Bayesian Information Criterion (BIC), which recommended a scheme with 13 subsets and a combination of General Time Reversible (GTR + G and GTR + I + G) models.
The molecular and morphological datasets were concatenated with Mesquite v3.2047. We used the parallel (MPI) version of MrBayes v3.2.648 to conduct two total-evidence Bayesian phylogenetic analyses. The first was a standard “non-clock” analysis. The second was a time-scaled “clock” analysis which implemented the tip-dating method with fossilized-birth-death (FBD) parameterization. For the molecular portion of the matrix, settings for partitions and models were assigned based on the PartitionFinder results. The morphological portion of the matrix was set as a single partition using a gamma-distributed Markov k model and variable coding to accommodate ascertainment bias. Parameters for models across all 14 partitions were set as unlinked. Two hard topological constraints were applied—one enforced monophyly for primates and the other constrained scandentians as an outgroup. Metropolis coupled Markov chain Monte Carlo (MCMCMC) parameters were set for 2 runs with 4 chains each and to sample in 1000 generation increments. To promote chain swapping, the heating temperature was set to 0.02.
Run length was assessed and chosen using built-in MrBayes diagnostics for convergence and sampling sufficiency. First, we targeted run lengths yielding an average standard deviation of split frequencies (ASDSF)≤0.01. The value of this diagnostic should approach zero as individual runs converge on topological distributions. Second, we targeted run lengths in which the minimum estimated sampling size (minESS) of all parameters was ≥ 100. Burn-in settings were selected to optimize these two diagnostics. We explored absolute burn-in generation values in increments of 5 M, ranging from 5 M up to 50% of run lengths. At each increment, tree and parameter summarizations were run and diagnostic data were collected. The final burn-in value for each analysis was selected by identifying all values that yielded the ASDSF target (≤0.01), and then from this group, choosing the one which yielded the minESS set whose least sampled parameter most exceeded the minESS target (≥100). Under this run-length strategy, the non-clock analysis was run for 92 M generations of which 5 M were discarded as burn-in. The resulting ASDSF was 0.00995 and the smallest minESS in the parameter set was 532.5906. The tree distribution was summarized using the “allcompat” (majority-rule plus compatible groups) option.
Our clock analysis included several additional settings. (1) The node age prior was set as calibrated with living taxa fixed to zero (=present day) and fossil taxa constrained to an age range. Age ranges were estimated using (when possible) the currently recognized upper and lower bounds of magnetochrons, “land mammal ages”, and/or other radiometric constraints in which each fossil taxon may be reasonably placed44. Fossil-tip ages were set to sample from uniform distributions across these ranges. (2) For the clock variance prior, we used the independent gamma rates (IGR) model to estimate relaxed clock rates. For the associated IGR variance prior, we used the default MrBayes setting (exponential distribution, λ = 10). (3) We applied the FBD model for the prior probability distribution of branch lengths and used the fossil-tip sampling strategy. The FBD extinction and fossilization priors were set as flat (beta distributions, α = 1, β = 1) and the FBD speciation prior was set to the MrBayes default (exponential distribution, λ = 10). The FBD model also requires a sampling probability prior which is an estimate for the proportion of extant taxa included in the study. With about 450 living primate species4, 2 currently recognized living dermopteran species49 (though it should be noted that there is now strong evidence for cryptic diversity within Demoptera50), and 20 living scandentian species51, the 23 extant taxa in our matrix constitute ~0.0487 of living euarchontan diversity. (4) The clock rate prior is an initial estimate for a distribution describing the number of substitutions per site per million years. To derive this prior, we used novel R code that utilizes the non-clock tree, age estimates for each taxon and an age estimate for the tree root. First, the dist.nodes function from the R package APE v3.452 was used to extract path lengths from each tree tip to the tree root. Next, each path length was scaled by the difference between the root age estimate and a tip age estimate. For the root age, we used 65.2 Ma that corresponds to the earliest bound for Purgatorius, the oldest fossil taxon in the dataset. For tip ages, we used zero for living taxa and age range midpoints for fossil taxa. Finally, the fitdist function from the R package fitdistrplus v1.0-653 was used to fit normal, lognormal and gamma distributions to the set of scaled path lengths. The best model was assessed using the BIC, in this case a lognormal distrbution with a mean of −3.983465721 and a standard deviation of 0.564231504. This model and its parameter values were used directly for the MrBayes clock rate prior. (5) Age calibrations were applied to both the Primates and Euarchonta nodes. Calibration settings specified truncated normal distributions with minimum and mean ages corresponding to the earliest bound of the oldest fossil taxon in the group (Primates: Teilhardina = 55.8 Ma, Euarchonta: Purgatorius = 65.2 Ma). Pre-Eocene ghost lineages were penalized by setting 1 Ma standard deviations on these distributions. The clock analysis was run for 150 M generations, of which 20 M were discarded as burn-in. The resulting ASDSF was 0.009053 and the smallest minESS in the parameter set was 138.0835. The tree distribution was summarized using the “allcompat” option.
Comparing likelihoods of alternative topologies
Both the clock and non-clock analyses recovered stem chiromyiform positions for Plesiopithecus and Propotto, but with different placements relative to Daubentonia. As time is a fundamental factor in estimating branch lengths of phylogenetic trees, and statistical methods such as Bayesian inference inseparably consider branch lengths and topology in likelihood calculations, we regard the result of the clock analysis as optimal. To compare the estimated marginal likelihood of the clock result to those of alternate topologies, we conducted a set of post hoc analyses using MrBayes. To do so, Plesiopithecus and Propotto were pruned from the time-scaled clock tree, and the remaining tree was used as a soft constraint for reanalysis of the morphological partition with stepping-stone sampling. (A) The first reanalysis allowed Plesiopithecus and Propotto to be placed anywhere in the tree. The result was identical to the clock analysis—specifically that Plesiopithecus is positioned as sister to a Propotto-Daubentonia clade [H1, optimal]. (B) The second reanalysis disallowed a Propotto-Daubentonia group. The resultant topology for Chiromyiformes was identical to the non-clock analysis—specifically that a Propotto-Plesiopithecus clade is positioned as sister to Daubentonia [H2]. Comparison of the estimated marginal likelihood of H1 to that of H2 yielded a Bayes factor of 15.6. (C) The third reanalysis disallowed placements of Plesiopithecus and Propotto as stem chiromyiforms. Given this constraint, a Propotto-Plesiopithecus clade was instead positioned as the immediate sister clade of crown strepsirrhines [H3]. Comparison of the estimated marginal likelihood of H1 to that of H3 yielded a Bayes factor of 572.5. (D) The fourth reanalysis also disallowed placements of Plesiopithecus and Propotto as stem chiromyiforms, but forced these taxa to be placed within crown Strepsirrhini. Given these constraints, a Propotto-Plesiopithecus clade is positioned as the immediate sister group of the chiromyiform–lemuriform clade [H4]. Comparison of the estimated marginal likelihood of H1 to that of H4 yielded a Bayes factor of 652.0. We interpret Bayes factors >10 as strong evidence, and >100 as decisive evidence, in favor of the optimal hypothesis versus alternate hypotheses54,55.
Morphological character state transformations
MrBayes was used to conduct ancestral state reconstructions (ASR) for all morphological characters that were scored for either Plesiopithecus or Propotto (n = 166). Given the topology and branch lengths of the “allcompat” tree derived from the clock analysis, ASR provides the probabilities of all states of all characters for each ancestral node. For each character, we considered the state with the highest probability to be the best estimate at an ancestral node, provided that the probability of that state exceeded all others by >10%. If the probability of a runner-up state was ≤10% of the highest, we considered the best ancestral estimate to be inclusively polymorphic.
Geographic distribution for each taxon in the dataset was coded as one of the following six land masses: North America, South America, Europe, Asia, Afro-Arabia, Madagascar. For both the optimal [H1] and first runner-up [H2] trees, MrBayes was used to conduct ASR of biogeography; both analyses support independent dispersals of the chiromyiform and lemuriform lineages from Afro-Arabia to Madagascar. A concise summary of ancestral biogeography on the optimal tree is presented in Fig. 6.
Auto3dgm analysis of tooth shape
To assess the phenetic affinities of the molar teeth of Propotto in an objective and quantitative way, we used an automated three dimensional (3D) geometric morphometric analysis. Our sample consists of lower second molars of 222 individuals representing 42 genera (Supplementary Data 1). Digital models of these specimens were created by micro-CT scanning physical specimens (either casts or originals); Avizo versions 6-8.156 were used to fit and crop surfaces, followed in some cases by further processing (patching and smoothing) in Geomagic57. Euarchonta is comprehensively represented (with the exception of anthropoids), including a diversity of early fossil prosimians. We also include molars of two pteropodid genera, as a test of the hypothesis that Propotto is a primitive fruit bat. Automated analyses allow an objective and comprehensive representation of shape. The software evenly spreads a user-specified number of “pseudolandmarks” over the surface of a 3D object and then algorithmically determines the correspondence among landmarks on different bones58. We used the MATLAB version of auto3dgm, the most recent version of which can be accessed by contacting the authors or through the github address: https://github.com/trgao10/PuenteAlignment/. We used the following parameters in our analysis: 300 initial pseudolandmarks, 1100 final pseudolandmarks, 3000 iterations of iterative closest points, and reflections allowed. The analysis was run on the mathematics computing cluster at Duke University. The Procrustes transformed pseudolandmark coordinates are available (Supplementary Data 1). The aligned coordinates of the pseudolandmarks from Table S1 were then analyzed using principal components analysis of tangent space in morphologika2.5 (Supplementary Data 2 and 3). We decided to remove Prolemur from the analysis post hoc given the small sample (n = 2), and problems with breakage on one tooth and heavy wear on the other. Additionally, we identified seven outlier specimens (in the sense that they plotted far from other individuals of their species) in an early version of the analysis. These seven outliers turned out to have mesh or alignment issues as noted in the footnote of Supplementary Data 1.
Input data files, settings, and results from phylogenetic, stepping stone, ASR, and biogeographic analyses are available on the Dryad Digital Repository (https://doi.org/10.5061/dryad.gb182). Digital surface models for all of the figured fossil specimens are available on MorphoSource (www.morphosource.org, see Table 1 for digital object identifiers).
Kistler, L. et al. Comparative and population mitogenomic analyses of Madagascar’s extinct, giant ‘subfossil’ lemurs. J. Hum. Evol. 79, 45–54 (2015).
Yoder, A. D. Back to the future: a synthesis of strepsirrhine systematics. Evol. Anthropol. 6, 11–22 (1997).
Yoder, A. D., Cartmill, M., Ruvolo, M., Smith, K. & Vilgalys, R. Ancient single origin for Malagasy primates. Proc. Natl Acad. Sci. USA 93, 5122–5126 (1996).
Springer, M. S. et al. Macroevolutionary dynamics and historical biogeography of primate diversification inferred from a species supermatrix. PLoS ONE 7, e49521 (2012).
Steiper, M. E. & Seiffert, E. R. Evidence for a convergent slowdown in primate molecular rates and its implications for the timing of early primate evolution. Proc. Natl Acad. Sci. USA 109, 6006–6011 (2012).
Samonds, K. E. et al. Spatial and temporal arrival patterns of Madagascar’s vertebrate fauna explained by distance, ocean currents, and ancestor type. Proc. Natl Acad. Sci. USA 109, 5352–5357 (2012).
Yoder, A. D. & Nowak, M. D. Has vicariance or dispersal been the predominant biogeographic force in Madagascar? Only time will tell. Annu. Rev. Ecol. Evol. Syst. 37, 405–431 (2006).
Crottini, A., Madsen, O., Strauß, A., Vieites, D. R. & Vences, M. Vertebrate time-tree elucidates the biogeographic pattern of a major biotic change around the K–T boundary in Madagascar. Proc. Natl Acad. Sci. USA 109, 5358–5363 (2012).
Ali, J. R. & Huber, M. Mammalian biodiversity on Madagascar controlled by ocean currents. Nature 463, 653–657 (2010).
Seiffert, E. R., Simons, E. L. & Attia, Y. Fossil evidence for an ancient divergence of lorises and galagos. Nature 422, 421–424 (2003).
Seiffert, E. R., Simons, E. L., Ryan, T. M. & Attia, Y. Additional remains of Wadilemur elegans, a primitive stem galagid from the late Eocene of Egypt. Proc. Natl Acad. Sci. USA 102, 11396–11401 (2005).
Seiffert, E. R. Early primate evolution in Afro-Arabia. Evol. Anthropol. 21, 239–253 (2012).
Simons, E. L. & Rasmussen, D. T. A remarkable cranium of Plesiopithecus teras (Primates, Prosimii) from the Eocene of Egypt. Proc. Natl Acad. Sci. USA 91, 9946–9950 (1994).
Simons, E. L. Diversity in the early tertiary anthropoidean radiation in Africa. Proc. Natl Acad. Sci. USA 89, 10743–10747 (1992).
Godinot, M. Lemuriform origins as viewed from the fossil record. Folia Primatol. 77, 446–464 (2006).
Gunnell, G. F. & Rose, K. D. in The Primate Fossil Record (ed. Hartwig, W. C.) Ch. 5 (Cambridge University Press, Cambridge, 2002).
Ankel-Simons, F. Deciduous dentition of the aye-aye, Daubentonia madagascariensis. Am. J. Phys. Anthropol. 39, 87–97 (1996).
Simons, E. L., Rasmussen, D. T., Bown, T. M. & Chatrath, P. in Anthropoid Origins (eds Fleagle, J. G. & Kay, R. F.) 179-201 (Plenum Press, New York, 1994).
Herrera, J. P. & Dávalos, L. M. Phylogeny and divergence times of lemurs inferred with recent and ancient fossils in the tree. Syst. Biol. 65, 772–791 (2016).
Seiffert, E. R. et al. A fossil primate of uncertain affinities from the earliest late Eocene of Egypt. Proc. Natl Acad. Sci. USA 107, 9712–9717 (2010).
Simpson, G. G. The tertiary lorisiform primates of Africa. Bull. Mus. Comp. Zool. 136, 39–62 (1967).
Walker, A. True affinities of Propotto leakeyi Simpson 1967. Nature 223, 647–648 (1969).
Harrison, T. in Cenozoic Mammals of Africa (eds Werdelin, L. & Sanders, W. J.) Ch. 20 (University of California Press, Berkeley, 2010).
Butler, P. M. Macroscelidea, Insectivora and Chiroptera from the Miocene of east Africa. Palaeovertebrata 14, 117–200 (1984).
Pickford, M. Preliminary Miocene mammalian biostratigraphy for western Kenya. J. Hum. Evol. 10, 73–97 (1981).
Bishop, W. W., Miller, J. A., & Fitch, F. J. New potassium-argon age determinations relevant to the Miocene fossil mammal sequence in East Africa. Am. J. Sci. 267, 669–699 (1969).
Drake, R., Van Couvering, J. A., Pickford, M., Curtis, G. & Harris, J. A. New chronology for the early Miocene mammalian faunas of Kisingiri, western Kenya. J. Geol. Soc. Lond. 145, 479–491 (1988).
Marivaux, L. et al. Djebelemur, a tiny pre-tooth-combed primate from the Eocene of Tunisia: a glimpse into the origin of crown strepsirhines. PLoS ONE 8, e80778 (2013).
Tolley, K. A., Townsend, T. M. & Vences, M. Large-scale phylogeny of chameleons suggests African origins and Eocene diversification. Proc. R. Soc. B 280, 20130184 (2013).
Zhou, Y., Wang, S.-R. & Ma, J.-Z. Comprehensive species set revealing the phylogeny and biogeography of Feliformia (Mammalia, Carnivora) based on mitochondrial DNA. PLoS ONE 12, e0174902 (2017).
Poux, C. et al. Asynchronous colonization of Madagascar by the four endemic clades of primates, tenrecs, carnivores, and rodents as inferred from nuclear genes. Syst. Biol. 54, 719–730 (2005).
Everson, K. M., Soarimalala, V., Goodman, S. M. & Olson, L. E. Multiple loci and complete taxonomic sampling resolve the phylogeny and biogeographic history of tenrecs (Mammalia: Tenrecidae) and reveal higher speciation rates in Madagascar’s humid forests. Syst. Biol. 65, 890–909 (2016).
Vences, M. et al. Multiple overseas dispersal in amphibians. Proc. R. Soc. B 270, 2435–2442 (2003).
Nagy, Z. T., Joger, U., Wink, M., Glaw, F. & Vences, M. Multiple colonizations of Madagascar and Socotra by colubrid snakes: evidence from nuclear and mitochondrial gene phylogenies. Proc. R. Soc. B 270, 2613–2621 (2003).
Blair, C. et al. Multilocus phylogenetic and geospatial analyses illuminate diversification patterns and the biogeographic history of Malagasy endemic plated lizards (Gerrhosauridae: Zonosaurinae). J. Evol. Biol. 28, 481–492 (2015).
Miller, K. G. et al. The Phanerozoic record of global sea-level change. Science 310, 1293–1298 (2005).
Seiffert, E. R. in Cenozoic Mammals of Africa (eds Werdelin, L. & Sanders, W. J.) Ch. 2 (University of California Press, Berkeley, 2010).
Pickford, M., Senut, B., Morales, J., Mein, P. & Sánchez, I. M. Mammalia from the Lutetian of Namibia. Mem. Geol. Surv. Namib. 20, 465–514 (2008).
Gheerbrant, E., Thomas, H., Roger, J., Sen, S. & Al-Sulaimani, Z. Deux nouveaux primates dans l’Oligocene inferieur de Taqah (Sultanat d’Oman): premiers adapiformes (?Anchomomyini) de la peninsule arabique? Palaeovertebrata 22, 141–196 (1993).
Cartmill, M. in Prosimian Biology (eds Martin, R. D., Doyle, G. A. & Walker, A. C.) Daubentonia, Dactylopsila, woodpeckers, and klinorhynch (Duckworth, London, 1974).
Beck, R. M. D. Was the Oligo-Miocene Australian metatherian Yalkaparidon a ‘mammalian woodpecker’? Biol. J. Linn. Soc. 97, 1–17 (2009).
Stevens, N. J. et al. Palaeontological evidence for an Oligocene divergence between Old World monkeys and apes. Nature 497, 611–614 (2013).
Seiffert, E. R. Evolution and extinction of Afro-Arabian primates near the Eocene-Oligocene boundary. Folia Primatol. 78, 314–327 (2007).
Seiffert, E. R. et al. New adapiform primate fossils from the late Eocene of Egypt. Hist. Biol. 30, 204–226 (2018).
Wiens, J. J. in Phylogenetic Analysis of Morphological Data (ed. Wiens, J. J.) Coding morphological variation within species and higher taxa for phylogenetic analysis (Smithsonian Institution Press, Washington, DC, 2000).
Lanfear, R. F. P., Wright, A. M., Senfeld, T. & Calcott, B. PartitionFinder 2: new methods for selecting partitioned models of evolution for molecular and morphological phylogenetic analyses. Mol. Biol. Evol. 34, 772–773 (2016).
Maddison, W. P. & Maddison, D. R. Mesquite: a modular system for evolutionary analysis v3.20 (2017)
Ronquist, F. et al. MrBayes 3.2: efficient Bayesian phylogenetic inference and model choice across a large model space. Syst. Biol. 61, 539–542 (2012).
Stafford, B. J. & Szalay, F. S. Craniodental functional morphology and taxonomy of dermopterans. J. Mammal. 81, 360–385 (2000).
Mason, V. C. et al. Genomic analysis reveals hidden biodiversity within colugos, the sister group to primates. Sci. Adv. 2, e1600633 (2016).
Roberts, T. E., Lanier, H. C., Sargis, E. J. & Olson, L. E. Molecular phylogeny of treeshrews (Mammalia: Scandentia) and the timescale of diversification in Southeast Asia. Mol. Phylogenet. Evol. 60, 358–372 (2011).
Paradis, E., Claude, J. & Strimmer, K. APE: analyses of phylogenetics and evolution in R language. Bioinformatics 20, 289–290 (2004).
Delignette-Muller, M. L. & Dutang, C. fitdistrplus: an R package for fitting distributions. J. Stat. Softw. 64, 1–34 (2015).
Jarosz, A. F. & Wiley, J. What are the odds? A practical guide to computing and reporting Bayes factors. J. Probl. Solving 7, 1–9 (2014).
Jeffreys, H. Theory of Probability 3rd edn (Oxford University Press, New York, 1961).
Visualization Sciences Group. AVIZO v6.0 (Mercury Computer Systems, Burlington, 2009).
3D Systems Inc. Geomagic Studio (3D Systems Inc, Rock Hill, 2013).
Boyer, D. M. et al. A new fully automated approach for aligning and comparing shapes. Anat. Rec. 298, 249–276 (2015).
We thank the National Museums of Kenya for access to the Propotto specimens figured and discussed here, and the Egyptian Mineral Resources Authority, the Egyptian Geological Museum, and the Egyptian Environmental Affairs Agency for supporting paleontological fieldwork in the Fayum area of Egypt that led to the recovery of the Plesiopithecus specimens figured and described here. The late Alan Walker graciously provided copies of his correspondence with George G. Simpson. This research was funded by Leakey Foundation grants to N.J.S.; National Science Foundation grants BCS-0416164 and BCS-0819186 to Elwyn L. Simons and E.R.S.; BCS-1231288 to E.R.S., D.M.B., G.F.G., and John G. Fleagle; BCS-1440742 to D.M.B. and G.F.G.; DBI-1458192 to GFG; BCS-1552848 to D.M.B.; and BCS-1127164 and BCS-1638796 to N.J.S; and DDIG 0925793 to Lynn Lucas and Lynn Copes. This is Duke Lemur Center publication #1400.
The authors declare no competing interests.
Publisher's note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
About this article
Cite this article
Gunnell, G.F., Boyer, D.M., Friscia, A.R. et al. Fossil lemurs from Egypt and Kenya suggest an African origin for Madagascar’s aye-aye. Nat Commun 9, 3193 (2018). https://doi.org/10.1038/s41467-018-05648-w
Journal of Vertebrate Paleontology (2020)
Revision of Oligocene ‘Paraphiomys’ and an origin for crown Thryonomyoidea (Rodentia: Hystricognathi: Phiomorpha) near the Oligocene–Miocene boundary in Africa
Zoological Journal of the Linnean Society (2020)