New discoveries of Gigantopithecus blacki teeth from Chuifeng Cave in the Bubing Basin, Guangxi, south China

Ninety two Gigantopithecus blacki teeth have recently been recovered in situ at Chuifeng Cave in the Bubing Basin, Guangxi, south China. The hominoid teeth are associated with a typical early Pleistocene fauna. In comparison with Gigantopithecus of known provenience, for which classification is problematic, the Chuifeng sample can be allocated definitively to G. blacki. The new collection represents the largest sample of this species known, with the exception of the material from Liucheng. Statistical analysis of the mammal fauna indicates that G. blacki is one of the dominant elements, comprising 9% of the fauna. Eleven teeth (12% of the sample) of G. blacki are diagnosed as having caries. In addition, wear on M₃ shows that G. blacki was adapted to consume tough or fibrous food and this wear may potentially imply relative longevity. Further study of this large sample of Gigantopithecus will provide additional insight into the paleobiology of this extinct hominoid.     

Cranial capacity in hominid evolution

We present an analysis of cranial capacity of 118 hominid crania available from the literature. The crania belong to both the genusAustralopithecus andHomo and provide a clear outline of hominid cranial evolution starting at more than 3 million years ago. Beginning withA. afarensis there is a clear increase in both absolute and relative brain size with every successive time period.H.s. neandertal has an absolutely and relatively smaller brain size (1412cc, E.Q.=5.6) than fossil modernH.s. sapiens (1487cc, E.Q.=5.9). Three evolutionary models of hominid brain evolution were tested: gradualism, punctuated equilibrium, and a mixed model using both gradualism and punctuated equilibrium. Both parametric and non-parametric analyses show a clear trend toward increasing brain size withH. erectus and a possible relationship within archaicH. sapiens. An evolutionary stasis in cranial capacity could not be refuted for all other taxa. Consequently, the mixed model appears to more fully explain hominid cranial capacity evolution. However, taxonomic decisions could directly compromise the possibility of testing the evolutionary mechanisms hypothesized to be operating in hominid brain expansion.     

Mandibular postcanine dentition from the Shungura Formation,Ethiopia: Crown morphology,taxonomic allocations,and Plio-Pleistocene hominid evolution

Over 200 hominid specimens were recovered by the International Omo Expedition of 1967–1976. Despite the fragmentary nature of this primarily dental collection, these hominid remains represent a major body of evidence about hominid evolution in eastern Africa during the 2–3 myr time period. Our analysis of the Omo dental collection is based on a large comparative sample of 375 quantifiable mandibular postcanine teeth of A. afarensis, A. africanus, A. aethiopicus, A. boisei, A. robustus, and early Homo. A total of 48 isolated mandibular premolars and molars of the Omo collection spanning the 2–3 myr time period is sufficiently preserved to allow reliable serial allocations and intertaxon comparisons and is the object of study in this paper. We present taxonomic identifications of these teeth and seven other mandibular specimens preserving tooth crowns. Metric analyses of this study include cusp area and crown shape variables taken on occlusal view diagrams. Nonmetric analyses were based on simultaneous observations of all relevant material to ensure accuracy of categorical evaluations. First, a combined metric and morphological evaluation was conducted to allocate each Omo tooth to either robust or nonrobust categories. Further taxonomic affinities were then examined. Our results indicate that nonrobust and robust lineages cooccur by circa 2.7 myr. We consider the Shungura robust specimens from Members C through F to represent A. aethiopicus. A significant phenetic transformation occurs at circa 2.3 myr, with the mosaic emergence of the derived A. boisei morphology across Member G times. Characterization of the East African nonrobust lineage is more difficult because of the comparatively subtle morphological differences seen among the dentitions of A. afarensis, A. africanus, and early Homo. The earlier Members B and C nonrobust specimens are difficult to evaluate and are considered indeterminate to genus or species. Both molars and premolars from Members E through G exhibit phenetic similarities to the early Homo condition and are considered as aff. Homo sp. indet. At present, there is no indication of multiple species in the Omo nonrobust sample at any time horizon. The 2–2.4 myr Omo nonrobust specimens exhibit some similarities to the stated Homo “rudolfensis” condition in size and morphology and are likely to represent the ancestral condition of the genus Homo. The bearing of these results on interpretations of early hominid evolution and diversification is considered. © 1996 Wiley-Liss, Inc.     

Geomorphology to paleoecology: Gigantopithecus reappraised

Critical evaluation of the geomorphological circumstances leading to the formation of and deposition within the Gigantopithecus blacki cave near Liucheng, South China is undertaken on the basis of the available data. Models for the evolution of the Liucheng tower karst and the mode of deposition of the fossiliferous Quaternary sediments are presented. Analyses concerning the behavioural, phylogenetic and taxonomic placements of G. blacki are examined in the light of the proposed models. Hominid affinity or parallel in terms of behaviour or savannah provenance are questioned.     

Hominid Ichnotaxonomy: An Exploration of a Neglected Discipline

Although more than 60 ancient hominid track sites ranging in age from 3.7 million to less than 500 B. P. are recorded from all continents except Antarctica, no ichnotaxonomic names have ever been formally proposed for hominid tracks. There is no prohibition to the naming of fossil footprints of species that created tracks and trackways similar to those of living species. On the contrary, there is precedent for the naming of ichnotaxa corresponding to the dominant extant vertebrates classes: mammals = Mammalipedia and birds = Avipeda. The hominid track site sample includes only about a dozen sites where footprint preservation is good enough to show details of diagnostic foot morphology and typical trackway morphology. We infer that the Acahualinca Footprint Museum site in Nicaragua represents the most important ancient hominid track site that combines accessibility, a large sample of well-preserved trackways and reliable dating. For this reason, we select the Nicaraguan tracks as the type sample for the new ichnotaxon Hominipes modernus ichnogen., and ichnsp. et ichnosp. nov., which we infer to represent fully modern Homo sapiens. Our preliminary investigations of other track sites suggest that the majority also yield H. modernus. However, at many sites preservation is insufficient to make an ichnotaxonomic designation at the species level or to infer that the trackmaker was H. sapiens. Thus, at many sites including the famous Laetoli site, we apply the more general label of Hominipes isp. indet.     

Morphology and molecular characterization of Acanthogyrus (Acanthosentis) bilaspurensis Chowhan,Gupta & Khera, 1987 (Acanthocephala: Gyracanthocephala: Quadrigyridae) from the common carp Cyprinus carpio Linnaeus (Cypriniformes: Cyprinidae) in Pakistan

Acanthogyrus (Acanthosentis) bilaspurensis Chowhan, Gupta & Khera, 1987 is a poorly known acanthocephalan species reported from the reba carp Cirrhinus reba (Hamilton) (Cypriniformes: Cyprinidae) in India. In the present study, the detailed morphology of A. (Acanthosentis) bilaspurensis were studied using light microscopy and, for the first time, scanning electron microscopy (SEM), based on newly collected specimens from the common carp Cyprinus carpio Linnaeus (Cypriniformes: Cyprinidae) in Pakistan. The SEM observations revealed the outer shell of eggs with numerous remarkable protuberances and the gonopore of female located at a discoid protrusion surrounded by some very small spines. This is the first time that A. (Acanthosentis) bilaspurensis was reported in Pakistan, and the common carp represents a new host for this species. In addition, the molecular characterization of the 18S and 28S rDNA of A. (Acanthosentis) bilaspurensis is provided for the first time. There was no intraspecific genetic variation detected in the 18S and 28S regions between different individuals of A. (Acanthosentis) bilaspurensis, but high level of interspecific nucleotide divergence was found in the 18S (4.15–16.7%) and 28S regions (3.60–15.4%). Phylogenetic results based on the 18S, 28S and 18S + 28S sequence data, respectively, all revealed the Quadrigyridae, Pallisentinae and the genus Neoechinorhynchus are not monophyletic groups, and the genera Acanthogyrus and Pallisentis have far relationship. The systematic status of the genus Acanthogyrus and some species of Neoechinorhynchus need further clarify based on different mtDNA and nuclear DNA data including broader representatives of the class Eoacanthocephala.     

An archaic character in the Broken Hill innominate E. 719

The additional hominid material from Broken Hill, Kabwe, Zambia, is only dubiously associated with the hominid cranium from the site and is often considered to be anatomically modern in morphology. This study identifies an archaic feature, previously recognised in Pliocene and earlier Pleistocene innominates, in the Broken Hill innominate E. 719. An acetabulo-cristal buttress of cortical bone 10 mm thick is present, and this can be clearly distinguished from the morphology present in a comparative sample of large recent Homo sapiens innominates. This observation increases the likelihood that some of the additional specimens from Broken Hill are indeed of comparable antiquity to the hominid cranium and extends the range of hominids in which the feature has been recognised.     

The recent New Zealand species of Triforis (Gastropoda: Triforidae)

Paramendax apicina Powell and Mendax attenuatispira Powell are referred to genus Triforis Deshayes; T. antepallaxa, T. blacki, and T. tui are described as new; and a species close to the South Australian Triforis epallaxa (Verco) is recorded from New Zealand waters. Paramendax Powell is transferred from the Cerithiopsidae to the Triforidae as a subgenus of Triforis. It is suggested that the Recent South African Cerithiella nonnitens Barnard is referable to Triforis.     

Bipedal behavior of olive baboons (Papio anubis) and its relevance to an understanding of the evolution of human bipedalism

The bipedal behavior of a troop of olive baboons (Papio anubis) is described. Bipedalism is relatively rare but nevertheless occurs in a wide variety of situations, although bipedalism during feeding occurs much more frequently than in other situations. The incidence of bipedalism varies between different age-sex classes and between individuals within age-sex classes. This pattern of bipedalism occurred within an overall adaptive response, particularly in feeding behavior, which was similar to that of the gelada baboon (Theropithecus gelada). The data on bipedalism is used together with an existing model of early hominid differentiation based on T. gelada to indicate the types of bipedal behavior which might have occurred in early hominid small object feeders and to suggest how a bipedal pattern of this type might have served as a basis for the action of selection for a more committedly bipedal pattern at later stages of hominid evolution.     

Several cranial indices and their relevance to fossil man

An evaluation of three cranial indices proposed by Le Gros Clark ('50) is presented in light of hominid fossil material not previously considered. The data analysis suggests that the supra-orbital height index is an important contribution to cranial analysis and elaborations of it may prove valuable. From the results, the authors suggest that the two australopithecine types be separated on the genus level, i.e., Australopithecus africanus and Paranthropus robustus. It is also proposed that Skhūl V be considered Homo sapiens sapiens. The authors generally conclude that a more dynamic approach in primate cranial analysis is needed. This approach should incorporate non-morphological variables.     

Forward from Taung

The hominine grade of organization should preferably be defined by those morphological characters of the braincase and face which are first recognizable in Homo erectus. Provisionally, then, Olduvai hominid 24 and East Rudolf 1470 are regarded as protanthropine, irrespective of whether they both belong to “Homo habilis” or not. It is possible that either or both of these hominids can be considered directly prehominine, while A. africanus reflects an earlier prehominine stage.     

Laetoli toes andAustralopithecus afarensis

The probable misfit between feet, particularly toes II–V, of 3.0-million-year-oldAustralopithecus afarensis from Hadar, Ethiopia, and the 3.5-million-year-old hominid footprints at Site G, Laetoli, Tanzania, casts doubt thatA. Afarensis made the Laetoli trails. We suggest that another species ofAustralopithecus or an anonymous genus of the Hominidae, with remarkably humanoid feet, walked at Laetoli. It would be imprudent to declare thatHomo was present at Laetoli 3.5 million years ago (my) because there is no evidence of brain expansion, advanced tool manufacture, or other non-locomotor hallmarks of the human condition at Site G.     

Australopithecus afarensis and the single species hypothesis

Ferguson (1989) has recently argued that the variability seen in the fossils assigned toA. afarensis is far more than expected for a single hominid species, and therefore proposes they represent multiple taxa. In particular, he utilizes data on variation in dental metrics and in premolar morphology in support of this hypothesis. A re-evaluation of these data finds the above conclusion to be unwarranted. Variation in dental metrics providesno basis for separating this sample into multiple taxa, regardless of the analog that is used (i.e. modern primate species or fossil hominid species). Additionally, data on P₃ morphology indicate that thepattern of variation seen in the Laetoli/Hadar sample is comparable to the sexual variation seenwithin a single hominoid species. Overall, the balance of the evidence at present indicates that the fossils from Laetoli and Hadar represent a single hominid species,A. afarensis.     

Carrying, Sharing, and Hand Preference in Tufted Capuchins (Cebus apella)

We examined the relationship among carrying, food-sharing, and hand preference in tufted capuchins (Cebus apella). The rationale was to evaluate further the use of Cebus as an alternative primate model to Pan for behavior relevant to early hominid evolution. We first examined bipedalism and food-sharing within an established social group, and then examined the direction and strength of hand preference for food carrying in an expanded sample. Several aspects of capuchin behavior warrant discussion. First, bipedal carrying and food-sharing occurred more frequently when we provided bulky foods than when we provided smaller foods. Second, food-sharing was characterized by passive tolerance, rather than active giving, between subjects. Third, subjects shared food primarily with immatures and followed a pattern of reciprocal exchange. Finally, we found no evidence for population-level hand preference for carrying. We posit that an array of behavioral similarities among Cebus, Pan, and Homo evolved through convergent processes, and in this regard capuchins can be seen as an alternative primate model to chimpanzees for the evolution of early hominid behavior.     

History of American paleoanthropological research on early Hominidae, 1925–1980

Understanding of the early stages of hominid evolution prior to 1925 was based primarily on comparative morphological evidence derived from extant primates. With the publication of Australopithecus by Dart in 1925 and subsequent research in South Africa, new possibilities for empirical assessment of early hominid evolutionary history were opened. It was Gregory's work, with Hellman, reported at the first meeting of the AAPA in 1930, that convinced many workers of the hominid status of Australopithecus. The debunking of Eoanthropus as a Pliocene hominid, far from having a totally negative effect, showed that cranial expansion had occurred after bipedalism in hominid evolution, demonstrated that chemical dating had come of age, and in a broader sense, had underlined that phylogenetic hypotheses are falsifiable by recourse to the evidence. The input of biological sciences into early hominid studies, as exemplified by Washburn's “new physical anthropology,” reduced taxonomic diversity and focused attention on paleoecology and behavior. The development of the multidisciplinary approach to field research, pioneered by L. Leakey and brought to fruition by Howell, was of fundamental importance in accurately dating and understanding the context of early hominids. Archaeology, primatology, comparative and functional morphology, and morphometrics have contributed substantially in recent years to a fuller understanding of early hominid evolution. American granting agencies have heavily supported early hominid research but patterns of funding have not kept pace with the change from research based largely on individualistic enterprise to multidisciplinary research projects. Future early hominid research, if funding is available, will likely be directed toward investigating temporal and geographic gaps now known in the fossil record and in more rigorous and multidisciplinary investigations of early hominid behavior.     

The genus Neilo in New Zealand (Mollusca: Bivalvia)

Abstract

The phylogenetic history, paleontological implications, and ecology of larger New Zealand Recent species of Neilo (sensu stricto) are discussed. N. wairoana delli, N. blacki, and N. (Pseudomalletia) aoteana are described as new. The following taxa are reduced to chronosubspecies: N. jugifera Marwick - of N. australis (Quoy & Gaimard); N. annectens Powell and N. rugata Dell - of N. sublaevis Marwick; N. sinangula Finlay - of N. awamoana Finlay.     

Species-specific albumin in fossil bones from Orce, Granada, Spain

A skull fragment (VM-0) from Orce, Granada, Spain, dated palaeomagnetically at about 1.6 Myr, is thought by some palaeontologist to be hominid, while others maintain it is equid. If hominid, it would be by far the oldest evidence ofHomo in Europe. Immunological studies on residual albumin in this fossil were carried out independently, and with different immunological methods, at the University of California, San Francisco (radioimmunoassay), and at the University of Granada, Spain (enzyme immunoassay). Other fossils attributed to hominids also studied wereVM1960 from Venta Micena, andCV-1 from Cueva Victoria, Murcia, Spain. Undisputed equid and bovid fossils from the same deposits and dated to a similar period as the Orce skull were also analyzed. Our results showed that species-specific albumin can be detected in 1.6 Myr-old hominid, equid and bovid fossils. The albumin from the Orce skull fragment and fromVM-1960 was immunologically closer to human albumin. These findings support the contention that theVM-0 andVM-1960 are hominid and that members of the genusHomo occupied southern Spain 1.6 Myr ago.     

Hominid cranial capacity versus time: A regression approach

The application of a linear regression approach to hominid data shows that there is more regularity in hominid cranial capacity over time than has been supposed. Two outcomes of this analysis are: (1) the possibility that the South African Australopithecus africanus sites are older than the presently accepted estimates of perhaps around 2·5 million years and (2) the suggestion that the Ngandong (Solo) cranial material is also considerably older than generally assumed; probably, in excess of approximately 250,000 years B.P.     

The “Phoca standard”: An external molecular reference for calibrating recent evolutionary divergences

Comparison of the complete mitochondrial DNA (mtDNA) of the high-Arctic ringed seal (Phoca hispida) and the sub-Arctic harbour (P. vitulina) and grey (Halichoerus grypus) seals shows that they are genetically equidistant from one another. We relate the evolutionary divergence of the three species to expanding glaciation in the Arctic Basin and establish, in conjunction with mtDNA data, a standard reference for calibration of recent divergence events among mammalian taxa. In the present study, we apply the “Phoca standard” to the dating of divergences within the hominid phylogenetic tree. After determining the relative rates of substitution over all mitochondrial protein-coding genes in the different evolutionary lineages, we estimate that humans and chimpanzees diverged from each other 6.1 Mya (95% confidence limits: 5.2–6.9 Mya). The corresponding lower-limit divergence between common chimpanzee,Pan troglodytes, and pygmy chimpanzee,P. paniscus, occurred 3 (2.4–3.6) Mya, and the primary split within theP. troglodytes complex 1.6 (1.3–2.0) Mya. The analyses suggest that the split betweenGorilla andPan/Homo occurred 8.4 (7.3–9.4) Mya. They also suggest thatPongo (orangutan) and the lineage leading to gorillas, chimpanzees, and humans diverged 18.1 (16.5–19.6) Mya. The present analysis is independent of the hominid paleontological record and inferential morphological interpretations and thus is a novel approach to the lower-limit dating of recent divergences. Correspondence to: U. Arnason     

The identity and typification of Pimia Seem. (Sterculiaceae)

The unispecific Fijian genus Pimia Seem. (Sterculiaceae) has long been considered to be related to genera that are now included in the Byttneriaceae (also known as Malvaceae-Byttnerioideae). Morphological characters, however, indicate that Pimia is a mixture of Commersonia J. R. Forst. & G. Forst. (Byttneriaceae) and Diospyros L. (Ebenaceae). The name of the sole species, P. rhamnoides Seem., is lectotypified with an element that is determined to be C. bartramia (L.) Merr. and thus Pimia becomes a synonym of Commersonia. An epitype for P. rhamnoides is also selected because the lectotype now lacks flowers, which were an important element of the protologue.