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R F Kay

Publications and source records attributed to R F Kay.

30 records · Page 2Linked to original sources
PubMed1982

Sexual dimorphism in Ramapithecinae.

The Ramapithecinae are an extinct, mainly Miocene group of hominoids comprising the genera Sivapithecus and Gigantopithecus. Ouranopithecus and Ramapithecus are other included genera, here regarded as invalid. Cladistically, ramapithecines are hominid, although, in most aspects of their anatomy, they remain very primitive or ape-like. Miocene ramapithecines show reduced sexual dimorphism in canine size. In this respect they resemble Pliocene/Recent hominids, not extant great apes (which have highly dimorphic canines). Reduced dimorphism in canine size is an important shared derived feature indicating the hominid status of ramapithecines. Among living anthropoids, a significant association has been observed between a monogamous social structure and low canine dimorphism. This supports the inference that ramapithecines may have been monogamous.

Journal Article↗
PubMed1980

Sexual dimorphism in early anthropoids.

Sexual dimorphism in canine/premolar tooth size and in body size is found among many species of living primates and has been shown to be correlated with social organization. Among extant higher primate species that normally live in the nuclear families consisting of a mated pair with their offspring, adult males and females are similar in body size and in the size of canine and anterior premolar teeth. In contrast, higher primate species living in more 'complex' polygynous groups (either single-male harems or multi-male groups) are characterized by sexual dimorphism in the size of canine/premolar teeth and frequently by body size dimorphism as well. We provide here the first evidence for sexual dimorphism in three species of primates from the Oligocene of Egypt--Aegyptopithecus zeuxis, Propliopithecus chirobates, and Apidium phiomense. This is the earliest record of sexual dimorphism among higher primates and suggests, by analogy with living species, that the earliest known fossil Old World anthropoids lived in polygynous (either single-male harems or multi-male groups) rather than monogamous social groups.

Animals↗
PubMed1978

Dietary and dental variations in the genus Lemur, with comments concerning dietary-dental correlations among Malagasy primates.

Field studies of feeding in the lemur subspecies Lemur fulvus rufus and L. f. mayottensis have revealed that feeding patterns within a single species can be markedly different, both regionally and seasonally. Thus L. f. rufus is a dietary specialist (3 plant species accounting for 80-90% of feeding time), and is highly folivorous, especially during the dry season (90% of feeding time spent eating leaves during the dry season, and 53% during the wet season). On the other hand, L. f. mayottensis is more generalized dietarily (the parts of 12 plant species accounting for 90% of feeding time), and is primarily frugivorous (64% of feeding time spent eating fruit, with a monthly maximum during the wet season of 79%. In both these respects, L. f. mayottensis resembles L. catta are more closely thant it does L. f. rufus. When size differences are corrected for, Lemur fulvus rufus has significantly longer second lower molar shearing crests than does L. f. mayottensis. Other folivorous Malagasy strepsirhines also tend to have long shearing crests than frugivorous forms. Some data on cheirogaleines also suggest that the more insectivorous species have better developed molar crests than frugivorous species. Some apparent exceptions to this pattern are noted, especially for Lemur catta, which in certain functional respects dentally more closely resembles L. f. rufus than L. f. mayottensis. The problems of dietary classifications are discussed.

Animals↗
PubMed1977

The evolution of molar occlusion in the Cercopithecidae and early Catarrhines.

Those Eocene prosimians which are possible catarrhine ancestors have four blade-like crests on each lower molar. Each crest shears in sequence across two upper molar crests. Occluding crests are concavely curved to hold the foods being sheared. Each of two medial lower molar crests bordering the principal crushing surface shear past single upper molar crests at about the same time the lateral lower molar crests contact the second rank of upper molar crests. Grinding and crushing areas are restricted to hypoconid, trigonid, and protocone surfaces. Oligocene catarrhine molars have increased crushing-grinding capacities and maintained but modify their shearing. As the crushing surface of the protocone expands and a crushing hypocone is added, the "second rank" upper molar shearing crests are functionally reduced. At the same time medial crests are increasingly emphasized so that the total shearing capacity remains virtually unchanged. Marginal shearing blades are straight edged; leading edges of occluding blades are set at different angles to the occlusal plane so that blades contact at only one point at any given time. Early Primates have separate crushing basins surrounded by shearing blades. Catarrhines tend to link explanding crushing surfaces anteroposteriorly into a continuous surface between all molars. A cladistic analysis based on both new and previously recognized characters indicates that: 1. Apidium may be more closely related to Aegyptopithecus than to Parapithecus; 2. cercopithecids are derived from a Parapithecus-related stock; 3. Oreopithecus could equally well have come from an Apidium or Aegyptopithecus stock.

Animals↗
PubMed1975

The functional adaptations of primate molar teeth.

Measurements were taken on the upper and lower molars of 37 species of primates and one tupaiid to assess the relative importance of shearing, crushing and grinding features. Significant correlations were found between pairs of allometrically standardized dimensions which measure the same molar function (shearing, crushing, or grinding). Correlations between pairs of dimensions which do not measure the same function are not significant. Second molar adaptations for shearing, crushing, and grinding, as well as the length of the second lower molar, and the total surface of the post-canine dentition are negatively allometric with respect to metabolic rate. Species which take different proportions of fruit, leaves, and insects in their diets have different molar structure. Frugivores have small teeth for their adult body size with poorly developed shearing, crushing, and grinding features on their molars. By contrast, leaf-eating species tend to have large teeth for their adult body size with well developed shearing, crushing, and grinding. The second molars of insectivorous species were found to parallel closely those of leaf-eating species. The two groups are clearly distinguishable from the former on the basis of body size alone: the smallest living primate leaf-eater is on order of magnitude larger than the largest living primate insectivore.

Adaptation, Physiological↗
PubMedDate not supplied

Mammals and rainfall: paleoecology of the middle Miocene at La Venta (Colombia, South America).

A comparison of the species richness and macroniche composition of diet, locomotor and body-size classes among 16 nonvolant mammalian faunas in tropical South America reveals numerous significant positive correlations with rainfall. In particular, significant and strong positive correlations with rainfall are found in 18 attributes, including the number of nonvolant mammal species, number of primate species, number of frugivores, primary consumers, arborealists, and the number of species between 100 g to 10 kg in body weight. Estimates of annual rainfall derived from least-squares and polynomial regressions and principal components analysis yield a modal estimate of between 1500 and 2000 mm annual rainfall for the Monkey Beds assemblage at La Venta. This level of rainfall is associated today with the transition between savanna and forest environments in lowland equatorial South America. Paleontological evidence strongly suggests the presence of forest biotopes at La Venta. Paleontologic and sedimentologic evidence together indicate a dynamic and heterogeneous riparian mosaic associated with the shifting course of meandering rivers. Faunal evidence also suggests that habitat heterogeneity and canopy discontinuity extended into the interfluvial area. Seasonal rainfall was probably only of secondary importance in shaping the structural and spatial configuration of the dominantly forested mosaic habitat at La Venta. The fossil record is not consistent with the presence of extensive primary or undisturbed, continuous-canopy, evergreen tropical rainforest. The reconstructed middle Miocene environment at La Venta differs significantly from modern environments of similar geography on the piedmont east of the Andes at the same latitude. This in turn suggests that the extensive evergreen rainforests of the upper Amazonian piedmont that today receive more than 4000 mm of rainfall may post-date the initiation of Andean uplift.

Animals↗