Apparent Competition Structures Ecological Assemblages

Total Page:16

File Type:pdf, Size:1020Kb

Apparent Competition Structures Ecological Assemblages letters to nature 20. Leakey, R. E. & Leakey, M. G. A new Miocene hominoid from Kenya. Nature 342, 143–146 (1986). 21. Leakey, M. G., Leakey, R. E., Richtsmeier, J. T., Simons, E. L. & Walker, A. C. Similarities in Aegyptopithecus and Afropithecus facial morphology. Folia Primatol. 56, 65–85 (1991). 22. Delson, E. & Andrews, P.in Phylogeny of the Primates: A Multidisciplinary Approach (eds Luckett, W. P. & Szalay, F. S.) 405–446 (Plenum, New York, 1975). 23. Strasser, E. & Delson, E. Cladistic analysis of cercopithecid relationships. J. Hum. Evol. 16, 81–99 (1987). Acknowledgements. Excavations at Maboko were conducted with permission of the Office of the President, Republic of Kenya and in collaboration with the National Museums of Kenya. We thank the field crew (especially B. Onyango, V. Oluoch and S. Gitau) and M. G. Leakey for assistance, and E. Delson, M. Kohler, S. Moya-Sola and D. Pilbeam for comments and advice. This work was supported by NSF, L. S. B. Leakey Foundation, National Geographic Society, Wenner Gren Foundation for Anthropological Research, Fulbright, and Boise Fund. Correspondence and requests for materials should be addressed to B.R.B. (e-mail: bbenefi[email protected]). Apparent competition structures ecological assemblages M. B. Bonsall & M. P. Hassell Department of Biology and the NERC Centre for Population Biology, Imperial College at Silwood Park, Ascot, Berkshire SL5 7PY, UK ......................................................................................................................... Competition is a major force in structuring ecological com- munities1. It acts directly2 or indirectly, in which case it may be mediated by shared natural enemies and is known as ‘apparent 3–6 Figure 3 Bivariate plot of log10-transformed mean brain and body weight data for competition’ . The effects of apparent competition on species extant hominoids (H), cercopithecoids (C), platyrrhines (P), tarsiers (T), lemuroids coexistence are well known theoretically7,8 but have not previously and lorisoids (L)14, Victoriapithecus and Aegyptopithecus. Superimposed best fit been demonstrated empirically in controlled multigenerational lines for extant anthropoids (higher) and strepsirhines (lower) are based on least- experiments. Here we report on the population dynamic conse- squares linear regression equations. quences of apparent competition in a laboratory insect system with two host species and a common parasitoid attacking them. We find that whereas the two separate, single host–single para- catarrhine features, rather than derived indicators of affinity with sitoid interactions are persistent, the three-species system with the great ape and human clade. In this way, the Victoriapithecus skull the parasitoid attacking both hosts species (which are not allowed shows that the anatomy of fossil cercopithecoids is as important as to compete directly) is unstable, and that one of the host species is that of hominoids for deciphering the evolutionary history of Old eliminated from the interaction owing to the effects of apparent World higher primates. M competition. Received 21 November 1996; accepted 30 May 1997 Classical ecological theory predicts that simple interactions in 1. Pilbeam, D. R. New hominoid skull material from the Miocene of Pakistan. Nature 295, 232–234 which species share common natural enemies are unstable, leading 9 (1982). to one species being eliminated from the interaction . This effect 2. Brown, B. & Ward, S. in Orang-utan Biology (ed. Schwartz, J. H.) 247–260 (Oxford Univ. Press, New arises through competitive interactions mediated by the natural York, 1988). 7,8 3. Moya-Sola, S. & Kohler, M. Recent discoveries of Dryopithecus shed new light on evolution of great enemy in ‘apparent competition’ . As the two host species are not apes. Nature 365, 543–545 (1993). directly competing for resources, the loss of one of the species results 4. Moya-Sola, S. & Kohler, M. New partial cranium of Dryopithecus Lartet, 1863 (Hominoidea, Primates) from the upper Miocene of Can Llobateres, Barcelona, Spain. J. Hum. Evol. 29, 101–139 solely from the dynamic consequences of the natural enemy (1995). becoming more abundant as a consequence of having an alternative 5. Von Koenigswald, G. H. R. Miocene Cercopithecoidea and Oreopithecoidea from the Miocene of East host species. The species that persists in the interaction is the one Africa. Foss. Vert. Afr. 1, 39–51 (1969). 6 6. Benefit, B. R. & McCrossin, M. L. Ancestral facial morphology of Old World higher primates. Proc. that can support the higher parasitoid density . Natl Acad. Sci. USA 88, 5267–5271 (1991). These indirect competitive interactions have received little atten- 7. Benefit, B. R. The permanent dentition and phylogenetic position of Victoriapithecus from Maboko Island, Kenya. J. Hum. Evol. 25, 83–172 (1993). tion from natural or laboratory systems, although they are likely to 8. Benefit, B. R. Phylogenetic, paleodemographic and taphonomic implications of Victoriapithecus be as important, if not more so, than direct competitive interac- deciduous teeth from Maboko, Kenya. Am. J. Phys. Antropol. 95, 277–331 (1994). tions. Empirical work so far has focused mainly on short-term, 9. Feibel, C. S. & Brown, F. H. Age of the primate-bearing deposits on Maboko Island, Kenya. J. Hum. Evol. 21, 221–225 (1991). behaviourally orientated studies in which natural enemy responses 10. Andrews, P., Meyer, G., Pilbeam, D. R., Van Couvering, J. A. & Van Couvering, J. A. H. The Miocene are recorded within a single field season of the interaction10–15.No fossil beds of Maboko Island, Kenya: Geology, age, taphonomy and paleontology. J. Hum. Evol. 10, 35–48 (1981). empirical studies have addressed directly the long-term effects of 11. Stromer, E. Mitteilungen uber die Wirbeltierreste aus dem Mittelpliocan des Natrontales (Agypten). apparent competition on the population dynamics of the interact- 1. Affen. Z. Deutsch. Geol. Gesell. Abh. 65, 349–361 (1913). ing organisms. We now report on the temporal consequences of 12. Harrison, T. New postcranial remains of Victoriapithecus from the middle Miocene of Kenya. J. Hum. Evol. 18, 3–54 (1989). such apparent competition (Figs 1, 2). A series of long-term 13. Radinsky, L. The fossil evidence of anthropoid brain evolution. Am.J.Phys.Anthropol.41, 15–28 (1974). laboratory experiments were used to explore the interaction 14. Martin, R. D. Primate Origins and Evolution (Princeton Univ. Press, Princeton, NJ, 1990). 15. Benefit, B. R. & McCrossin, M. L. The facial anatomy of Victoriapithecus and its relevance to the between the ichneumonid parasitic wasp Venturia canescens ancestral cranial morphology of Old World monkeys and apes. Am.J.Phys.Anthropol.92, 329–370 (1993). (Gravenhorst) and two of its moth hosts, Plodia interpunctella 16. Vogel, C. Morphologische studien am gesichtschadel Catarrhiner primaten. Biblio Primatol. 4, 1–226 (Hubner) and Ephestia kuehniella Zeller, over a period of several (1966). 17. Harrison, T. The phylogenetic relationships of the early catarrhine primates: A review of the current generations. The direct competitive effects between the host evidence. J. Hum. Evol. 16, 41–80 (1987). species were fully excluded by a vertical barrier of nylon mesh 18. Simons, E. L. The earliest apes. Sci. Am. 217, 28–35 (1967). 19. Simons, E. L. New faces of Aegyptopithecus from the Oligocene of Egypt. J. Hum. Evol. 16, 273–289 dividing each cage in half. The mesh size was large enough to (1987). allow free access for the searching parasitoids between the two NATURE | VOL 388 | 24 JULY 1997 Nature © Macmillan Publishers Ltd 1997 371 letters to nature Figure 1 Representative examples of the population dynamics of the single host-single parasitoid interac- tions: a, b, P.interpunctella (dotted line)–V. canescens (dashed line); c, d, E. kuehniella (unbroken line)–V. canescens (dashed line). Experiments were carried in cages (30 3 30 3 30 cm) under standard environmen- tal conditions (25 6 2 8C; 70 6 5% R.H. 16 : 8 h light– dark cycle). Linear time series analysis indicates an underlying tendency for oscillations dampening towards a stable equilibrium. Figure 2 Representative examples of the population dynamics of the three species system of two hosts and a single parasitoid: P. interpunctella (dotted line)–E. kuehniella (unbroken line)–V. canescens (dashed line). In all these cases, E. kuehniella is eliminated from the interaction by the action of the shared natural enemy, V. canescens. Time series analysis now indicates damped oscillations for the interaction between P. interpunctella and V. canescens and diverging oscillations for E. kuehniella. halves, but was too small to let the hosts pass through. The between the two apparently competing host species (P. interpunc- interactions with a single host and single parasitoid, and the more tella and E. kuehniella) is amensal: the effect of P. interpunctella on E. complex three-species interactions of two hosts and a single kuehniella is strong whereas the reciprocal effects of E. kuehniella on parasitoid, were each replicated eight times and monitored over P. interpunctella is negligible (Fig. 3). P. interpunctella is dominant 15 generations by weekly census counts of dead adults16. because it has a larger intrinsic rate of increase and shorter In all the two-species systems, the two populations persisted in development time16. relatively stable interactions (Fig. 1). Time-series statistics show that Such asymmetric relationships in the interaction strengths have the dynamics in these cases
Recommended publications
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • Closest Relatives of Primates Earliest True Primates Share
    Closest relatives of Primates Earliest true primates share: • Archonta • Inner ear morphology – Scandentia (tree shrews) • Postorbital bar, orbital convergence – Dermoptera (flying lemurs) • Large brain case with large orbits – Chiroptera (bats) • Modifications of the elbow • Plesiadapiformes • Elongation of the heel, opposable thumb – Paleocene radiation of unusual critters and nails (instead of claws) – Replaced by rodents – Put in and out of Primate order Eocene Oligocene • Lots of fossils from N America and Europe; little • Continents mostly in present positions from Africa or Asia; • S America and Australia separate from • Prosimians anatomically and likely behaviorally Antarctica • Adapoids and Omomyoids, ecologically diverse; • Best site is Fayum, Egypt 28-32 my very similar early so likely monophyly Lemurs, Lorises • Adapoids like higher primates with large size, • , early anthropoid primates diurnality, frugivory and folivory (feet like lemurs) • Propliopithecus and Aegyptopithecus • Omomyoids more similar to galagos but • Dental apes but New World monkey bodies increase in size and folivorous late • Late Oligocene settling of S. America by • Where are prosimians lately? anthropoid primates Relationships based on fossils and Monkey Evolution molecular evidence • Hominoid and cercopithecoid apomorphies • New World Monkeys (Platyrrhini) show up in Oligocene, primitive versions by Miocene and at 20 and 18 my thereafter look very much like modern forms • Gibbons and Siamangs at 17 my • Old World Monkeys (Catarrhini) show up in Miocene (after apes); Victoriapithecus and then • Orang utans at 12 my split between colobines and cercopithecines; lots of evolutionary change late and lots of • Gorillas at 9 my convergences make systematics challenging • Pan troglodytes and Pan paniscus at 6 my • Also absence of fossils from many lineages • Very successful lately; out competing most apes • Putting chimp vs.
    [Show full text]
  • A Unique Middle Miocene European Hominoid and the Origins of the Great Ape and Human Clade Salvador Moya` -Sola` A,1, David M
    A unique Middle Miocene European hominoid and the origins of the great ape and human clade Salvador Moya` -Sola` a,1, David M. Albab,c, Sergio Alme´ cijac, Isaac Casanovas-Vilarc, Meike Ko¨ hlera, Soledad De Esteban-Trivignoc, Josep M. Roblesc,d, Jordi Galindoc, and Josep Fortunyc aInstitucio´Catalana de Recerca i Estudis Avanc¸ats at Institut Catala`de Paleontologia (ICP) and Unitat d’Antropologia Biolo`gica (Dipartimento de Biologia Animal, Biologia Vegetal, i Ecologia), Universitat Auto`noma de Barcelona, Edifici ICP, Campus de Bellaterra s/n, 08193 Cerdanyola del Valle`s, Barcelona, Spain; bDipartimento di Scienze della Terra, Universita`degli Studi di Firenze, Via G. La Pira 4, 50121 Florence, Italy; cInstitut Catala`de Paleontologia, Universitat Auto`noma de Barcelona, Edifici ICP, Campus de Bellaterra s/n, 08193 Cerdanyola del Valle`s, Barcelona, Spain; and dFOSSILIA Serveis Paleontolo`gics i Geolo`gics, S.L. c/ Jaume I nu´m 87, 1er 5a, 08470 Sant Celoni, Barcelona, Spain Edited by David Pilbeam, Harvard University, Cambridge, MA, and approved March 4, 2009 (received for review November 20, 2008) The great ape and human clade (Primates: Hominidae) currently sediments by the diggers and bulldozers. After 6 years of includes orangutans, gorillas, chimpanzees, bonobos, and humans. fieldwork, 150 fossiliferous localities have been sampled from the When, where, and from which taxon hominids evolved are among 300-m-thick local stratigraphic series of ACM, which spans an the most exciting questions yet to be resolved. Within the Afro- interval of 1 million years (Ϸ12.5–11.3 Ma, Late Aragonian, pithecidae, the Kenyapithecinae (Kenyapithecini ؉ Equatorini) Middle Miocene).
    [Show full text]
  • 8. Primate Evolution
    8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America.
    [Show full text]
  • Fossil Primates
    AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates.
    [Show full text]
  • The Cleveland Museum of Natural History
    The Cleveland Museum of Natural History December 2007 Number 56:72–85 A NEW LATE MIOCENE SPECIES OF PARACOLOBUS AND OTHER CERCOPITHECOIDEA (MAMMALIA: PRIMATES) FOSSILS FROM LEMUDONG’O, KENYA LESLEA J. HLUSKO Department of Integrative Biology University of California, 3060 Valley Life Sciences Building Berkeley, California 94720-3140 [email protected] ABSTRACT The Colobinae (Mammalia: Primates) are relatively unknown from the middle to late Miocene of eastern Africa. When they appear in the Pliocene fossil record they are unambiguous and fairly diverse taxonomically, geographically, and ecologically. The primate fauna from the late Miocene of Lemudong’o is dominated by colobines and therefore represents one of the richest fossil assemblages yet published of this subfamily at 6 Ma. At least three species of colobine, including a new species of Paracolobus, are represented in this collection. Given the paleoecological reconstruction for Lemudong’o Locality 1, and the postcranial morphology of the cercopithecids, colobines in this area of Africa were occupying a relatively closed or forested habitat, and exhibiting a primarily arboreal habitus, which contrasts with previous hypotheses suggesting that colobines prior to the Pliocene were terrestrial and occupying more open habitats. Introduction The early evolutionary history of the Cercopithecidae remains The cercopithecoids (Old World Monkeys) are commonly relatively unknown. The Colobinae are particularly enigmatic in thought to have split molecularly from the homininoids (apes) 25– Africa until the Pliocene when they appear to have undergone 23 Ma, presumably in Africa (Kumar and Hedges, 1998), a radiation of large-bodied forms. The earliest known African although a recent analysis suggests that it may have been 34–29 colobine specimens are Microcolobus tugenensis from Ngeringer- Ma (Steiper et al., 2004).
    [Show full text]
  • Old World Monkey Had Tiny, Complex Brain 3 July 2015
    Old World monkey had tiny, complex brain 3 July 2015 and created a three-dimensional computer model of what the animal's brain likely looked like. Micro-CT scans of the creature's skull show that Victoriapithecus had a tiny brain relative to its body. Co-authors Fred Spoor of the Max Planck Institute for Evolutionary Anthropology and Lauren Gonzales of Duke University calculated its brain volume to be about 36 cubic centimeters, which is less than half the volume of monkeys of the same body size living today. If similar-sized monkeys have brains the size of The brain hidden inside the oldest known Old World oranges, the brain of this particular male was more monkey skull has been visualized for the first time. The akin to a plum. ancient monkey, known as Victoriapithecus, first made headlines in 1997 when its 15 million-year-old skull was "When Lauren finished analyzing the scans she discovered on an island in Kenya's Lake Victoria. Now, thanks to high-resolution X-ray imaging, researchers called me and said, 'You won't believe what the have peered inside its cranial cavity and created a three- brain looks like,'" said co-author Brenda Benefit of dimensional computer model of what the animal's brain New Mexico State University, who first discovered likely looked like. Its tiny but remarkably wrinkled brain the skull with NMSU co-author Monte McCrossin. supports the idea that brain complexity can evolve before brain size in the primate family tree. The Despite its puny proportions, the animal's brain was creature's fossilized skull is now part of the permanent surprisingly complex.
    [Show full text]
  • Ancestral Facial Morphology of Old World Higher Primates (Anthropoidea/Catarrhini/Miocene/Cranium/Anatomy) BRENDA R
    Proc. Natl. Acad. Sci. USA Vol. 88, pp. 5267-5271, June 1991 Evolution Ancestral facial morphology of Old World higher primates (Anthropoidea/Catarrhini/Miocene/cranium/anatomy) BRENDA R. BENEFIT* AND MONTE L. MCCROSSINt *Department of Anthropology, Southern Illinois University, Carbondale, IL 62901; and tDepartment of Anthropology, University of California, Berkeley, CA 94720 Communicated by F. Clark Howell, March 11, 1991 ABSTRACT Fossil remains of the cercopithecoid Victoia- (1, 5, 6). Contrasting craniofacial configurations of cercopithe- pithecus recently recovered from middle Miocene deposits of cines and great apes are, in consequence, held to be indepen- Maboko Island (Kenya) provide evidence ofthe cranial anatomy dently derived with regard to the ancestral catarrhine condition of Old World monkeys prior to the evolutionary divergence of (1, 5, 6). This reconstruction has formed the basis of influential the extant subfamilies Colobinae and Cercopithecinae. Victoria- cladistic assessments ofthe phylogenetic relationships between pithecus shares a suite ofcraniofacial features with the Oligocene extant and extinct catarrhines (1, 2). catarrhine Aegyptopithecus and early Miocene hominoid Afro- Reconstructions of the ancestral catarrhine morphotype pithecus. AU three genera manifest supraorbital costae, anteri- are based on commonalities of subordinate morphotypes for orly convergent temporal lines, the absence of a postglabellar Cercopithecoidea and Hominoidea (1, 5, 6). Broadly distrib- fossa, a moderate to long snout, great facial
    [Show full text]
  • Fleagle and Lieberman 2015F.Pdf
    15 Major Transformations in the Evolution of Primate Locomotion John G. Fleagle* and Daniel E. Lieberman† Introduction Compared to other mammalian orders, Primates use an extraordinary diversity of locomotor behaviors, which are made possible by a complementary diversity of musculoskeletal adaptations. Primate locomotor repertoires include various kinds of suspension, bipedalism, leaping, and quadrupedalism using multiple pronograde and orthograde postures and employing numerous gaits such as walking, trotting, galloping, and brachiation. In addition to using different locomotor modes, pri- mates regularly climb, leap, run, swing, and more in extremely diverse ways. As one might expect, the expansion of the field of primatology in the 1960s stimulated efforts to make sense of this diversity by classifying the locomotor behavior of living primates and identifying major evolutionary trends in primate locomotion. The most notable and enduring of these efforts were by the British physician and comparative anatomist John Napier (e.g., Napier 1963, 1967b; Napier and Napier 1967; Napier and Walker 1967). Napier’s seminal 1967 paper, “Evolutionary Aspects of Primate Locomotion,” drew on the work of earlier comparative anatomists such as LeGros Clark, Wood Jones, Straus, and Washburn. By synthesizing the anatomy and behavior of extant primates with the primate fossil record, Napier argued that * Department of Anatomical Sciences, Health Sciences Center, Stony Brook University † Department of Human Evolutionary Biology, Harvard University 257 You are reading copyrighted material published by University of Chicago Press. Unauthorized posting, copying, or distributing of this work except as permitted under U.S. copyright law is illegal and injures the author and publisher. fig. 15.1 Trends in the evolution of primate locomotion.
    [Show full text]
  • 1 Old World Monkeys
    2003. 5. 23 Dr. Toshio MOURI Old World monkey Although Old World monkey, as a word, corresponds to New World monkey, its taxonomic rank is much lower than that of the New World Monkey. Therefore, it is speculated that the last common ancestor of Old World monkeys is newer compared to that of New World monkeys. While New World monkey is the vernacular name for infraorder Platyrrhini, Old World Monkey is the vernacular name for superfamily Cercopithecoidea (family Cercopithecidae is limited to living species). As a side note, the taxon including Old World Monkey at the same taxonomic level as New World Monkey is infraorder Catarrhini. Catarrhini includes Hominoidea (humans and apes), as well as Cercopithecoidea. Cercopithecoidea comprises the families Victoriapithecidae and Cercopithecidae. Victoriapithecidae is fossil primates from the early to middle Miocene (15-20 Ma; Ma = megannum = 1 million years ago), with known genera Prohylobates and Victoriapithecus. The characteristic that defines the Old World Monkey (as synapomorphy – a derived character shared by two or more groups – defines a monophyletic taxon), is the bilophodonty of the molars, but the development of biphilophodonty in Victoriapithecidae is still imperfect, and crista obliqua is observed in many maxillary molars (as well as primary molars). (Benefit, 1999; Fleagle, 1999) Recently, there is an opinion that Prohylobates should be combined with Victoriapithecus. Living Old World Monkeys are all classified in the family Cercopithecidae. Cercopithecidae comprises the subfamilies Cercopithecinae and Colobinae. Cercopithecinae has a buccal pouch, and Colobinae has a complex, or sacculated, stomach. It is thought that the buccal pouch is an adaptation for quickly putting rare food like fruit into the mouth, and the complex stomach is an adaptation for eating leaves.
    [Show full text]
  • Supporting Information
    Supporting Information Moya` -Sola` et al. 10.1073/pnas.0811730106 SI Text netic relationships between all these taxa by classifying them all Systematic Framework. In Table S1 we provide a systematic into a single family Afropithecidae with 2 subfamilies (Keny- classification of living and fossil Hominoidea to the tribe level, apithecinae and Afropithecinae). by further including extant taxa and extinct genera discussed in The systematic scheme used here requires several nomencla- this paper. Hominoidea are defined as the group constituted by tural decisions, which deserve further explanation. The nomina Hylobatidae and Hominidae, plus all extinct taxa more closely Kenyapithecini and Kenyapithecinae are adopted instead of related to them than to Cercopithecoidea. Hominidae, in turn, Griphopithecinae and Griphopithecini (see also ref. 25) merely are defined as the group containing Ponginae and Homininae, because the former have priority. It is unclear why neither Begun plus all extinct forms more closely related to them than to (1) nor Kelley (2) specify the authorship of Griphopithecinae (or Hylobatidae. While this broad concept of Hominidae is currently Griphopithecidae), but, to our knowledge, the authorship of the used by many paleoprimatologists (e.g., refs. 1–2), the systematic latter nomina must be attributed to Begun (ref. 4, p. 232: Table position of primitive (or archaic) putative hominoids is far from 10.1), which therefore do not have priority over Kenyapithecinae clear (see below). Begun (3–5) employs the terms ‘‘Eohomi- Andrews, 1992. Griphopithecinae thus remains potentially valid noidea’’ and ‘‘Euhominoidea’’ to informally refer to hominoids only if Kenyapithecus (and Afropithecus, see below) are excluded of primitive and modern aspect, respectively.
    [Show full text]
  • Harrison CV June 2021
    June 1, 2021 Terry Harrison CURRICULUM VITAE CONTACT INFORMATION * Center for the Study of Human Origins Department of Anthropology 25 Waverly Place New York University New York, NY 10003-6790, USA 8 [email protected] ) 212-998-8581 WEB LINKS http://as.nyu.edu/faculty/terry-harrison.html https://wp.nyu.edu/csho/people/faculty/terry_harrison/ https://nyu.academia.edu/TerryHarrison http://orcid.org/0000-0003-4224-0152 zoobank.org:author:43DA2256-CF4D-476F-8EA8-FBCE96317505 ACADEMIC BACKGROUND Graduate: 1978–1982: Doctor of Philosophy. Department of Anthropology, University College London, London. Doctoral dissertation: Small-bodied Apes from the Miocene of East Africa. 1981–1982: Postgraduate Certificate of Education. Institute of Education, London University, London. Awarded with Distinction. Undergraduate: 1975–1978: Bachelor of Science. Department of Anthropology, University College London, London. First Class Honours. POSITIONS 2014- Silver Professor, Department of Anthropology, New York University. 2003- Director, Center for the Study of Human Origins, New York University. 1995- Professor, Department of Anthropology, New York University. 2010-2016 Chair, Department of Anthropology, New York University. 1995-2010 Associate Chair, Department of Anthropology, New York University. 1990-1995 Associate Professor, Department of Anthropology, New York University. 1984-1990 Assistant Professor, Department of Anthropology, New York University. HONORS & AWARDS 1977 Rosa Morison Memorial Medal and Prize, University College London. 1978 Daryll Forde Award, University College London. 1989 Golden Dozen Award for excellence in teaching, New York University. 1996 Golden Dozen Award for excellence in teaching, New York University. 2002 Distinguished Teacher Award, New York University. 2006 Fellow, American Association for the Advancement of Science.
    [Show full text]