A comparative study of adult facial morphology and its ontogeny in the fossil macaque Macaca majori from Capo Figari, Sardinia, Italy

This study examines the morphology of the face in the fossil macaque Macaca majori from Capo Figari (north-eastern Sardinia, Italy) in a comparative ontogenetic context. Thus, a fairly complete face from an adult representative of this fossil species is compared with 3 extant macaque species: Macaca sylvanus (of which species it is questioned whether it is a subspecies, M. sylvanus majori), Macaca mulatta and Macaca fascicularis. Additional incomplete subadult and adult specimens are also examined in order to compare their facial ontogeny with that of the same living species. The comparisons are based on facial landmark data and are undertaken using geometric morphometric methods. These studies indicate that the adult facial morphology and ontogeny of face size and shape in M. majori share much in common with extant macaque species. However, the adult M. majori face displays some unique morphological features, in particular with regard to lateral flaring and relative size of the zygomatic roots. From the study of a limited sample of fossils there is an indication that this flaring arises during postnatal growth, and in consequence the ontogeny of the face of this fossil species may be different from that of M. sylvanus and the other macaque species included in this analysis. From these studies, we conclude that M. majori shows differences in adult facial morphology and possibly in ontogeny from M. sylvanus compatible with a specific rather than subspecific distinction.     

Pleistocene Macaca from Hoxne, Suffolk, England

Pleistocene macaque remains are uncommon in Great Britain. In addition to three specimens previously known from three sites, four teeth from Hoxne, Suffolk are recorded here. Closely resembling teeth of modern Macaca sylvanus (Barbary ape), they were recovered from a Middle Pleistocene stratum containing stone artifacts (including handaxes) and fauna including cold-climate lemmings.     

Systematics,phylogeny and evolutionary pattern of the hystricognath rodent Eumysops (Echimyidae) from the Plio–Pleistocene of southern South America

?Eumysops is a peculiar representative of the currently tropical family Echimyidae, which evolved in increasingly dry and cold Plio–Pleistocene environments of southern South America. The results of a systematic and stratigraphic review of the genus, and of phylogenetic analyses based on both morphology and a combined morphological–molecular dataset in the context of extant representatives, are presented here. Recognised diversity includes four previously described species plus a new one from the late Pliocene. These species form a well-supported monophyletic clade, sister to the late Miocene ?Pampamys and the extant Thrichomys. The position of ?Eumysops–?Pampamys–Thrichomys in a major clade including non-‘eumysopine’ echimyids constrains the traditional taxon Eumysopinae only to these three genera. Phylogeny and stratigraphic distribution of ?Eumysops species suggest an essentially cladogenetic evolutionary pattern. Beyond this, a gradual directional change, involving increase in size and in molar hypsodonty, is shown by ?Eumysops chapalmalensis as part of a late Pliocene faunal turnover interpreted as a local representation of the 2.5-Ma cooling global event. Distinctive skeletal and dental anatomy of ?Eumysops, including large orbits, shortened braincase, marked hypsodonty and postcranial specialisations, would be a result of its southern history related to a particular palaeoclimatic context.     

Craniodental variation in the African macaque, with reference to various Asian species

Based on twenty-seven craniodental measurements and ratios derived from them, the relationship between the African macaque (M. sylvanus) and the others in Asia were examined with principal components analyses (PCA) and Euclidean distance analysis based upon prior discriminant function analyses (DFA). Results based on analyses of raw measurements indicate that the variation between species lies in the first axis of PCA; the species are dispersed according to their differences in size. The variation between sexes (sexual dimorphism) lies in the second axis. In the analyses of ratio variables, though these two patterns of separation remain orthogonal, they lie at approximately forty-five degrees to each axis. Variables relating to anterior teeth were found to play an important role in variation analysis, and this may be related to the special food preferences of these monkeys: more frequent usage of the incisor teeth for processing frugivorous diets than in other primates that are mainly folivorous. The results from Euclidean distance analyses indicate that the average distance of species within the Asian group is shorter than that between Asian and African groups regardless of sex and variable type. In addition the variation between African and Asian groups is larger than that within Asian group. Thus, it is reasonable to suggest that the African macaque has a range of measurements and ratios quite distinct from the species found in Asia (though the greatest separations result from the analyses of ratio data). These results therefore support the view that M. sylvanus may be regarded as an independent species group in the genus Macaca as proposed by Delson [1980].     

The evolution of Nyctereutes (Carnivora: Canidae) in the Nihewan Basin,Hebei, northern China

The occurrence of Nyctereutes during the Plio-Pleistocene has long been reported in northern China, with the highest abundance in the Nihewan Basin. However, due to site dispersal, the coexistence of different taxa, and lack of a precise stratigraphic constraint, the evolutionary process of this genus remains enigmatic. In this study, we re-examined the available Nyctereutes materials recovered from the Nihewan Basin housed in IVPP and Tianjin Natural History Museum, in addition to a newly recovered specimen from our latest excavation. Furthermore, we compared these materials with Nyctereutes fossils recovered from the Pleistocene Zhoukoudian sites near Beijing and the extant species N. procyonoides. Our analysis of the upper molar morphometry reveals the variations in size and dietary characteristics within different species of Nyctereutes during the late Plio-Pleistocene. The examination of molars indicates an increase in the size of Nyctereutes sinensis compared to early Pliocene N. tingi as well as changes in the molar teeth morphology. Subsequently, changes in diet or environmental factors possibly caused the decrease of body size in the late Pleistocene. We also estimate an age constraint for the fossils of N. sinensis from the Xiashagou section by relocating Licent's localities and referring of updated magnetostratigraphic data.     

Fossil remains of Macaca sylvanus florentina (Cocchi, 1872) (Primates, Cercopithecidae) from the Early Pleistocene of Quibas (Murcia, Spain)

The macaque material from the Early Pleistocene site of Quibas (Albanilla, Murcia, Spain), including dentognathic remains, isolated teeth and some postcranial bone fragments, is described. Both metrically and morphologically, this sample must be attributed to Macaca sylvanus (the Barbary macaque). This species is currently distributed through North Africa and Gibraltar, but was much more widely distributed during the Plio-Pleistocene, being represented by several European fossil subspecies. Metrical comparisons of dental size and proportions between extant M. s. sylvanus and fossil Macaca sylvanus florentina from the type locality and other Italian sites are undertaken, in order to classify the remains from Quibas at the subspecies level. The results show that the Quibas sample not only fits the range of variation of M. s. florentina from the type locality, but also differs from the extant Barbary macaque condition in several regards. This permits us to formally attribute the material from Quibas to M. s. florentina. The material described in this paper therefore significantly improves the knowledge of this fossil taxon, particularly regarding the upper dentition, and further confirms the taxonomic distinctiveness of this extinct taxon at the subspecies rank. Taken as a whole, M. s. florentina largely overlaps in dental dimensions with M. s. sylvanus, but differs from the latter by displaying (on average): (1) absolutely longer upper molars (especially M¹ and M³); (2) relatively wider upper molars (especially M¹ and M²); (3) longer M³ as compared with the M²; (4) absolutely longer M₁ and M₃; and (5) relatively narrower M₃.     

Mid-Tertiary elapid snakes (Squamata, Colubroidea) from Riversleigh, northern Australia: early steps in a continent-wide adaptive radiation

Vertebral and cranial remains of elapid snakes have been collected from fossil assemblages at Riversleigh, north-west Queensland, Australia; most are Miocene but one may be late Oligocene and another as young as Pliocene. The oldest specimen (probably the oldest elapid yet known anywhere) is a vertebra that can be referred provisionally to the extant taxon Laticauda (Hydrophiinae, sensu Slowinski and Keogh, 2000), implying that the basal divergences among Australasian hydrophiine lineages had occurred by the early Miocene, in contrast to most previous estimates for the age of this geographically isolated adaptive radiation. Associated vertebrae and jaw elements from a Late Miocene deposit are described as Incongruelaps iteratus nov. gen. et sp., which has a unique combination of unusual derived characters otherwise found separately in several extant hydrophiine taxa that are only distantly related. Associated vertebrae from other sites, and two parietals from a possibly Pliocene deposit, suggest the presence of several other taxa distinct from extant forms, but the amount of material (and knowledge of variation in extant taxa) is currently insufficient to diagnose these forms. The Tertiary elapids of Riversleigh thus appear to be relatively diverse taxonomically, but low in abundance and, with one exception, not referable to extant taxa below the level of Hydrophiinae. This implies that the present diversity of hydrophiine elapids (31 recognized terrestrial genera, and approximately 16 marine) represents the result of substantial extinction as well as the “cone of increasing diversity” that could be inferred from phylogenetic studies on extant forms.     

Seroprevalence of SV40-like polyomavirus infections in captive and free-ranging macaque species

BACKGROUND AND METHODS: To investigate the seroprevalence of polyomavirus infections in macaques, we analyzed 1579 sera from nine different species for antibodies cross-reactive with simian virus 40 (SV40) in an enzyme-linked immunosorbent assay. Most samples were collected from captive animals, but we also investigated a colony of free-ranging Barbary macaques (Macaca sylvanus). RESULTS: High seropositive rates were found in rhesus macaques (Macaca mulatta; 74.7%), cynomolgus macaques (Macaca fascicularis; 44.8%) and Tonkean macaques (Macaca tonkeana; 41.7%), especially in animals imported from China. Low rates were measured in cynomolgus macaques from Mauritius (8.8%), and in Barbary macaques (1.4%). Seropositivity was age-dependent increasing to >70% in animals of 5 years and older. CONCLUSIONS: High seroprevalence rates were found in different species of macaques, dependent on their origin. Very low infection rates found in Barbary macaques and cynomolgus macaques from Mauritius suggest that these animals in the wild are not commonly infected by SV40-like viruses.     

Orycteropus (Tubulidentata, Mammalia) from Langebaanweg and Baard's Quarry, Early Pliocene of South Africa

Fossil teeth and bones of aardvarks are relatively common at Langebaanweg, an Early Pliocene site in western Cape Province, South Africa. The remains are compatible in size and most details of morphology to extant Orycteropus afer, and are the earliest fossils attributed to this species. Other Late Miocene to Early Pliocene localities in Africa have yielded smaller species of aardvarks, suggesting that the extant lineage evolved in southern Africa. Morphologically the genus Orycteropus has been remarkably conservative since at least the Early Miocene but it witnessed an overall increase in size through the Neogene. The species O. afer has been morphometrically stable since the Early Pliocene. These observations indicate that the evolutionary process in aardvarks is extremely bradytelic. To cite this article: M. Pickford, C. R. Palevol 4 (2005).     

Trichoepithelioma in a Barbary ape (Macaca sylvanus): review of cutaneous tumors in nonhuman primates and case report

A cutaneous tumor was surgically removed from a 10-year-old, male Barbary ape (Macaca sylvanus). Histologically, the tumor was primarily adnexoid in nature and contained structures that resembled abortive hair follicles. The tumor was diagnosed as a trichoepithelioma.     

Dolichopithecus balcanicus sp. nov., a new Colobinae (Primates, Cercopithecidae) from the early Pliocene of southeastern Europe, with a discussion on the taxonomy of the genus

We describe a new species of Dolichopithecus, D. balcanicus sp. nov., from the Pliocene (late Ruscinian) of the Balkans. Although known by mandibular remains only, it is readily distinguished from the common European species, D. ruscinensis, by its smaller size, much shallower mandibular corpus, and crowding of the premolars. Ukrainian finds of "Adelopithecus" can be accommodated within D. ruscinensis as a separate, smaller subspecies, D. ruscinensis hypsilophus, but the specimens reported from Asia are more distinct, and they probably represent a separate subgenus of Dolichopithecus, the valid name of which is D. (Parapresbytis) Kalmykov and Mashchenko.     

A history of shifting fortunes for African penguins

Africa is home today to only a single breeding species of penguin, Spheniscus demersus (black‐footed penguin), which is endangered with extinction. Spheniscus demersus has been the only breeding species of penguin to share African coastlines with humans over the last 400 000 years. Interestingly, African penguin diversity was substantially higher before the evolution of archaic humans. The fossil record indicates that a diverse assemblage of penguin species inhabited the southern African coasts for much of the Neogene. Previous excavations have identified four distinct species in Early Pliocene coastal marine deposits. Here we extend this pattern of high diversity and report the oldest record of penguins from Africa. Seventeen penguin specimens were identified from the Saldanha Steel locality, revealing the presence of at least four distinct species in South Africa during the Miocene. The largest of these species reached the size of the extant Aptenodytes patagonicus (king penguin), whereas the smallest was approximately the size of the smallest extant penguin Eudyptula minor (little blue penguin). Recovery of Miocene penguin remains is in accordance with earlier predictions of multiple pre‐Pliocene colonizations of Africa and supports a higher level of ecological diversity amongst African penguins in the past. © 2013 The Linnean Society of London     

A twinning event in Macaca sylvanus of Gibraltar.

Linear measurements and body proportions for a set of free-ranging Macaca sylvanus twins are presented. Their measurements are compared to a full-term perinatal dead female. The twins are dizygous and probably 28 days premature.     

New small mammals from the Hasnot–Tatrot area of the Potwar Plateau,northern Pakistan

New rodent and lagomorph fossils from the Hasnot–Tatrot area of northern Pakistan are presented here to complement knowledge of stratigraphic ranges and morphology of key late Neogene Siwalik taxa. Most of the material is from two sites near the village of Bhandar in strata of the late Miocene age Dhok Pathan Formation; one specimen comes from the Pliocene Tatrot beds. We apply previously established magnetostratigraphy to date the fossils, the Bhandar sites dating to 6.6–6.7 Ma. In describing the fossils, we emphasize new morphological information represented by the material. As surface finds, these fossils represent relatively large body size species: three bamboo rat relatives, a porcupine, and a rabbit. The bamboo rats (Rhizomyinae) are an endemic group, and both the porcupine (Hystrix) and the rabbit (Alilepus) represent late Miocene immigrants into the Indian subcontinent.     

Geographic and stratigraphic distributions of the Caribbean species of Cladocora (Scleractinia, Faviidae)

A complete account of the faviid genus Cladocora within the Caribbean is presented. In the Caribbean this genus represents an extant group that had its earliest occurrence during the Campanian-Maastrichtian of Jamaica. Recent forms have been reported throughout the Caribbean. The following forms were found (with stratigraphic ranges in the Caribbean): C. arbuscula (Pliocene-Recent), C. debilis (Pleistocene-Recent), C. gracilis (Middle-Upper Maastrichtian), C. jamaicaensis (Campanian-Maastrichtian and Eocene), C. johnsoni (Pliocene), and C. recrescens (Middle-Upper Oligocene). The occurrence of the genus Cladocora in the Caribbean is largely continuous from the Campanian to Recent, during the majority of the Caribbean species show affinities to European assemblages. For the time intervals Paleocene, Lower Oligocene, and Miocene the taxon has not been reported from the Caribbean.     

Perineal swellings: a social and endocrine advantage for Barbary macaque females (Macaca sylvanus)

This study focuses the relationship between social rank, intersexual behavior, age, fecal cortisol equivalent excretion rates and perineal swelling size in contraceptive-treated Macaca sylvanus females. Behavioral data and fecal samples were collected during a twenty-week period from 24 females. Females were categorized with regard to perineal swelling (enlarged or reduced), and to their dominance rank (high or low); we found that swelling size was not associated with it. However, females with an enlarged perineum received more male grooming interactions, had closer spatial relations to males, and received significantly more interventions from males than did the others. Endocrinologically, females with enlarged swelling showed decreased fecal cortisol equivalent excretion rates. Multiple regression models showed a positive relationship between the extent of the swelling size and grooming, inspection and spatial relation. There was a negative relationship between the extent of swelling size and fecal cortisol equivalents. These results imply that enlarged perineal swellings among implanted Barbary macaque females have a greater impact on intersexual contact and adrenocortical activity than does social rank or age.     

Neogene phasianids (Aves: Phasianidae) of Central Asia: 3. Genera <Emphasis Type="Italic">Lophogallus</Emphasis> gen. nov. and <Emphasis Type="Italic">Syrmaticus</Emphasis>

Large phasianids from four Miocene and Pliocene localities of Mongolia are reviewed. Lophogallus naranbulakensis gen. et sp. nov. from the Middle Miocene of the Naran Bulak locality is described. It resembles extant Gallus, Lophura, and partially Pavo. The fossil pheasant Syrmaticus kozlovae Kurochkin is compared in detail with other Neogene and living pheasants. The stratigraphic position of phasianids from Neogene localities of Central Asia is discussed.     

The Iberian record of the puma-like cat Puma pardoides (Owen, 1846) (Carnivora,Felidae)

Fossil puma-like cats (Puma pardoides) are recorded from several Late Pliocene to Early Pleistocene Eurasian localities, but the interpretation of the phylogenetic relationships between them and the extant puma (Puma concolor) remains controversial. In the past, extinct puma-like cats have been classified into several genera and species, and a close relationship with both pumas (Puma concolor) and snow leopards (Uncia uncia) has been suggested. Here, we describe the fossil remains of puma-like cats from the Iberian Peninsula. These remains (from the localities of La Puebla de Valverde, Cueva Victoria and Vallparadís) cover the whole known chronological distribution of this species in Eurasia. Although there are dentognathic similarities with U. uncia, the Iberian remains of P. pardoides most closely resemble the extant P. concolor. It is concluded that P. pardoides is closely related to living pumas, which supports a likely Eurasian origin of the puma lineage.     

Galling: the prevalent form of insect folivory in the latest Neogene monsoon-influenced tropical forests of the Chotanagpur Plateau,eastern India

Indian Cenozoic deposits contain well-preserved diverse angiosperm leaf assemblages, but galling, a common form of angiosperm leaf damage in modern tropical forests, has not been well-documented. Here we report insect herbivory on diverse angiosperm fossil leaf specimens from Pliocene (Rajdanda Formation) sediments of the Chotanagpur Plateau, eastern India, revealing that galling was the most common form of folivory in the latest Neogene monsoon-adapted tropical forests of eastern India. Diverse well-preserved galls are described on the basis of their size, shape and position on the host angiosperm leaf remains. Nine gall damage types (DT 32, DT 33, DT 34, DT 80, DT 83, DT 85, DT 110, DT 120, and DT 144) are identified. They are compared with extant galls and the probable gall inducers making morphologically similar galls on related host tropical plant species of Ficus, Mangifera, Albizia, Galactia, Ziziphus, Hylodesmum, Adina, and Psidium. The gall producers belong to the insect orders Orthoptera, Hemiptera, Hymenoptera, Coleoptera, Lepidoptera, and Diptera (Cecidomyiidae). Although the detailed morphology of the phytophagous insects associated with the recovered fossil leaves is unknown, our findings indicate that many modern plant-insect relationships were likely established by the Pliocene. The reconstructed warm, humid Pliocene climate with a weak monsoon seasonality was conducive to extensive galling activity during this time.