TL;DR: Forests of Ankarana limestone massif in northern Madagascar support one of the largest and least disturbed populations of Crowned Lemurs, Lemur coronatus, and a preli is reported.
Abstract: Forests of Ankarana limestone massif in northern Madagascar support one of the largest and least disturbed populations of Crowned Lemurs, Lemur coronatus. This paper reports a preli
TL;DR: While investigating ecogeographic size variation in the extant and extinct lemurs of Madagascar, one of us noted the occurrence in the collections of the Academie Malgache of several unusually small demimandibles of Mesopropithecus an extinct “sloth lemur” (or palaeopropheticcid) from southwest Madagascar.
Abstract: While investigating ecogeographic size variation in the extant and extinct lemurs of Madagascar (Albrechtet al.1990; Godfrey et al.1990), one of us (LRG) noted the occurrence in the collections of the Academie Malgache of several unusually small demimandibles of Mesopropithecus an extinct “sloth lemur” (or palaeopropithecid) from southwest Madagascar. The specimens appeared, at first glance, to belong to adults; all of the permanent teeth were fully erupted. But the jaws were little more than two-thirds the size of those of adult Mesopropithecus globiceps from the same localities. They did not appear to belong to a new and smaller species of Mesopropithecus because the teeth were identical in size and morphology to those of M.obiceps.
TL;DR: Various characteristics place M. dolichobrachionphenetically closest to Babakotia radofilai, Archaeoindris, and Palaeopropithecus, and if these similarities are derived specializations rather than primitive for palaeopopithecids, a new generic name will be required.
Abstract: We diagnose new subfossil specimens belonging to the extinct palaeopropithecid, Mesopropithecus,from several caves at the Ankarana massif in northern Madagascar. They include three partial crania with mandibles, and the first vertebrae, ribs, clavicle, pelvis, ulna, and hand and foot bones of Mesopropithecusever found. Several other postcranial elements are known for this northern variant of Mesopropithecusand for previously described species from central and southern Madagascar. The new materials cannot be accommodated in either currently recognized species of this genus and are,hereby, given the name Mesopropithecus dolichobrachion. M. dolichobrachionis the second new species of extinct subfossil lemur to be found in the caves of Ankarana. It is unlike the two previously described species of this genus primarily in its larger size, different limb proportions, and aspects of its long bone morphology. Most notable is the fact that this is the only species of Mesopropithecuswith the forelimb longer than the hind limb— hence the name, the “long-armed” Mesopropithecus.Various characteristics place M. dolichobrachionphenetically closest (of species belonging to Mesopropithecus)to Babakotia radofilai, Archaeoindris,and Palaeopropithecus.If these similarities are derived specializations rather than primitive for palaeopropithecids, a new generic name will be required.
TL;DR: Morphological and statistical re-examination of all known cranial material of the subfossil Malagasy lemurs Mesopropithecus Standing and Neopropheticcus Lamberton indicates that there is no justification for generic separation of these forms.
Abstract: Morphological and statistical re-examination of all known cranial material of the subfossil Malagasy lemurs Mesopropithecus Standing and Neopropithecus Lamberton indicates that there is no justification for generic separation of these forms. Similarly, ‘N.’ globiceps and ‘N.’ platyfrons are considered to be conspecific. Revised diagnoses are provided for the genus Mesopropithecus and for the species M. pithecoides and M. globiceps.
TL;DR: This work performed the first clade‐wide analyses of craniomandibular growth allometries in 359 specimens from 10 lemuroids and 176 specimens from 8 indrioids to probe the ontogenetic bases of size differentiation and morphological diversity across these clades.
Abstract: Lemurs are notable for encompassing the range of body-size variation for all primates past and present-close to four orders of magnitude. Benefiting from the phylogenetic proximity of subfossil lemurs to smaller-bodied living forms, we employ allometric data from the skull to probe the ontogenetic bases of size differentiation and morphological diversity across these clades. Building upon prior pairwise comparisons between sister taxa, we performed the first clade-wide analyses of craniomandibular growth allometries in 359 specimens from 10 lemuroids and 176 specimens from 8 indrioids. Ontogenetic trajectories for extant forms were used as a criterion of subtraction to evaluate morphological variation, and putative adaptations among sister taxa. In other words, do species-level differences in skull form result from the differential extension of common patterns of relative growth?In lemuroids, a pervasive pattern of ontogenetic scaling is observed for facial dimensions in all genera, with three genera also sharing relative growth trajectories for jaw proportions (Lemur, Eulemur, Varecia). Differences in masticatory growth and form characterizing Hapalemur and fossil Pachylemur likely reflect dietary factors. Pervasive ontogenetic scaling characterizes the facial skull in extant Indri, Avahi, and Propithecus, as well as their larger, extinct sister taxa Mesopropithecus and Babakotia. Significant interspecific differences are observed in the allometry of indrioid masticatory proportions, with variation in the mechanical advantage of the jaw adductors and stress-resisting elements correlated with diet. As the growth series and adult data are largely coincidental in each clade, interspecific variation in facial form may result from selection for body-size differentiation among sister taxa. Those cases where trajectories are discordant identify potential dietary adaptations linked to variation in masticatory forces during chewing and biting. Although such dissociations highlight selection to uncouple shared ancestral growth patterns, they occur largely via transpositions and retention of primitive size-shape covariation patterns or relative growth coefficients.