The role of the Y chromosome in human evolutionary studies

Analyses of molecular genetic data have added a new dimension to human evolutionary research. Pioneering studies of variation in human populations were based on analyses of blood groups¹ and electromorphs,² both of which represent qualitative multistate phenotypes. With the development of recombinant DNA methods in the 1970s and 1980s, the focus shifted from gene products to a new and plentiful source of human variability, restriction fragment length polymorphisms (RFLPs).^3,4 Finally, the addition of DNA sequencining survey data to the rapidly growing RFLP data base made it feasible for the first time to determine the exact number of nucleotide substitutions between different alleles, as well as to construct gene trees and reconstruct the phylogenetic history of populations.^5–7     

Maxillary canine microwear in Dryopithecus from Spain

The three functional domains of the upper canines of Dryopithecus from Spain are analysed through microscopic examination. Evidence is presented that shows a food choice in concordance with open woodland habitat.     

Mandible of Ouranopithecus macedoniensis (Hominidae,primates) from a new late Miocene locality of Macedonia (Greece)

In 1990, a new late Miocene locality named “Nikiti 1” or NKT, was discovered near the village of Nikiti (Chalkidiki, Macedonia, Greece) about 100 km east of Thessaloniki City. The locality is situated in the Nikiti Formation, which consists of yellowish sands, gravels and pebbles and has been dated to late Vallesian–early Turolian. Among the initially collected fossils there is a mandible of a hominoid primate, which is described, compared, and attributed to Ouranopithecus macedoniensis. A short review of the species in Macedonia and its phylogenetic relationships are also given. © 1993 Wiley-Liss, Inc.     

Hominine morphology, climatic determinism and an alternative hypothesis

Climatic determinism is an established hypothesis to explain phenotypic selection of hominine physique. Adaptations to heat and cold stress are, however, probably physiological rather than morphological. This paper advances an alternative hypothesis which relegates the influence of the climate to an indirect role only. Athletes select themselves into events for which their physiques are appropriate. ‘Field eventers’ are, in Sheldon's terminology, mesomorphic and ectopenic (muscular and lacking in linearity). ‘Track eventers’ other than sprinters, have balanced physiques and are ectomorphic (linear). Distance runners are usually small and walkers tall. All are endopenic (lacking in the fat component). The physique of the northern (Inuit and Gurkhas) and southern (Bantu and San) study populations had morphological affinities with the physiques of the field and track eveters respectively. Northern populations, hunting megafauna over hilly terrain and sometimes through snow, need physiques of strength in body and leg. Southern populations, running down medium-size game, need the physique of distance runners. The physique of these contemporary populations may therefore be explained in terms of adaptations to the recent demands of hunting a particular range of fauna in a given physicogeographical environment. The pleomorphism and relative endomorphy of the White subjects can be explained by the relative sedentism associated with the adoption of agriculture. The hypothesis also explains the extreme physiques of Pygmies and Nilotics. The thermoregulatory and the alternative ‘task demand’ hypotheses, however, are not incompatible. The small size of the San hunter, for example, whilst having an undoubted biomechanical advantage, will assist rather than hinder thermoregulation.     

New Discoveries of “Opposum-Like” Marsupials from Antarctica (Seymour Island, Medial Eocene)

Five new species of marsupials are described from the middle Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula. Three are derorhynchid didelphimorphians; one species is a prepidolopid polydolopimorphian, and the last is a microbiotheriid australidelphian. Additionally, fragmentary specimens representing an indetermined derorhynchid and a possible marsupial are also described. The prepidolopid and one of the derorhynchids are sufficiently derived as to preclude any close relationship to other members of that family, but the remaining taxa show the closest affinity with species otherwise known only from Itaboraian and older faunas in Patagonia. This differs from the affinity to early Eocene (Casamayoran) taxa shown by the polydolopid marsupials and placental mammals previously known from the La Meseta Formation. The newly described marsupials indicate that the relict La Meseta Fauna is composed of forms that must have dispersed to Antarctica no later than about early late Paleocene, whereas the previously known taxa apparently arrived in the early Eocene. Ecologically, the La Meseta Fauna is composed mostly of small-sized marsupials of likely insectivorous to frugivorous habits and larger-sized placental herbivores. Whereas the ratite bird of the La Meseta Fauna was probably also herbivorous, the phorusrhachoid and falconid birds comprised a large and smaller carnivorous to possibly scavenging component, respectively. Compared to contemporary faunas of Patagonia, the medium- to large-sized marsupial carnivores are lacking in the Antarctic Peninsula. Nevertheless, the La Meseta Fauna is Patagonian in origin and affinity. In conjunction with new faunas of Itaboraian age (early late Paleocene) in Patagonia, the evidence available indicates that from at least Itaboraian time onward the land mammal fauna of Patagonia and northern South America, as well, is a self-contained unit, developing the diversity characteristic of the Paleogene in that continent, including the australidelphian (but South American) microbiotheres. This, in combination with the apparent separation of Australia from Antarctica at ca. 64 Ma, reinforces interpretations that the precursors of the Australian marsupial fauna most likely dispersed from South America to Australia in the late Cretaceous–early Paleocene.     

Early human dispersals into the Iberian Peninsula: a comment on Martínez et al.(2010) and Garcia et al. (2011)

Garcia et al. (2011) recently discussed early human dispersals into the Iberian Peninsula, describing several putative lithic artifacts (Martínez et al., 2010) recovered from layer 7 of the Vallpara díssection (Madurell-Malapeira et al., 2010) in Terrassa (Vallès-Penedès Basin, Catalonia, Spain). According to the authors' opinion, such evidence (1) fills a gap in the chronology of early human occupation in Iberia, (2) indicates that these populations had primary and early access to carcasses, and (3) confirms that early human populations were equipped with advanced cultural traits enabling them to survive in unfavourable climatic conditions. We argue below that the record of human activity at Vallparadís (Martínez et al., 2010;Garcia et al., 2011) is doubtful and even that if confirmed, a chronological gap would remain (contra Garcia et al., 2011). Additional remarks on assertions by these authors on the Vallparadís geology, taphonomy and paleonvironment are also provided.     

Phyletic diversity and locomotion in primitive European hominids.

A major contribution of previous analyses of Miocene hominoid postcrania is the recognition of a great ape grade of locomotor morphology in the late Miocene. However, in the absence of a consideration of the taxonomic and phylogenetic implications of the specimens concerned, the importance of this conclusion remains unappreciated. This paper presents a revised view of the positional implications of late Miocene hominid fossils and considers some of the taxonomic and phyletic implications of these specimens. The taxonomic status of a number of large catarrhine specimens from Europe (attributed to Dryopithecus, Sivapithecus, Austriacopithecus, Paidopithex, Rudapithecus) is discussed. The functional and phyletic significance of this material reveals a complex pattern of behavioral and phyletic diversity among large-bodied catarrhines in Europe and suggests that this diversity evolved in situ from circum-Mediterranean middle Miocene ancestors.     

A partial hominoid humerus from the middle miocene of Castell de Barberà (Vallès-Penedès Basin, Catalonia, Spain)

The hominoid right partial humerus IPS4334, from the middle Miocene (MN 8) of Castell de Barberà (Vallès-Penedès Basin, Catalonia, Spain), is described. It preserves the mid-distal portion of the shaft until the proximal margins of the radial and coronoid fossae, as well as the proximal portion of the olecranon fossa; the capitulum, the trochlea and the two epicondyles are missing. Although morphological comparisons are restricted, available evidence indicates that IPS4334 is more derived towards the modern hominoid condition than the Klein Hadersdorf specimen attributed to Griphopithecus (ca. 13-14 Ma), thus being most similar (except for its larger size and greater robusticity) to the presumably juvenile specimen of Dryopithecus fontani from Saint Gaudens in France (ca. 11-12 Ma). On the basis of shaft measurements and allometric regressions derived for extant hominoids, a body mass estimate around 50 kg is derived for IPS4334. Morphological similarities with the Saint Gaudens specimen, together with the large body mass estimate, suggest a tentative attribution of IPS4334 to cf. D. fontani, which is the largest hominoid taxon so far recorded from the Vallès-Penedès Basin. The larger size and higher robusticity of IPS4334 as compared to the Saint Gaudens specimen might be explained by the juvenile status of the latter and/or sexual dimorphism. When both specimens are considered together with a partial femur from Abocador de Can Mata, D. fontani emerges as a less suspensory ape than the late Miocene Hispanopithecus, the locomotor repertoire of the former emphasizing climbing, but still displaying a significant quadrupedal component.     

Transberingian dispersal of cestodes in mammals

During Pleistocene glaciations, eustatic lowering of sea-level exposed the continental shelf between northeastern Eurasia and northwestern North America. That land in combination with unglaciated areas on the adjacent continents formed a vast region open to the west but bounded on the east by continental ice. Organisms from Eurasia spread into the unglaciated Beringian refugium, which was biotically an eastward extension of the Palaearctic. With rising sea-levels following glacial periods, the Bering Strait was formed and organisms of Eurasian origin were left within the nearctic sector of Beringia. As the continental ice disappeared, plants and animals spread eastward and southward from Beringia, while organisms from beyond the southern margins of the ice extended their ranges northward. The significance of Beringia is discussed with reference to the dispersal of host-specific cestodes in mammals that attained holarctic status during the late Pleistocene.     

The evolution of the hallucial tarsometatarsal joint in the Anthropoidea

Changes in the hallucial tarsometatarsal joint, which forms the fulcrum for the grasping hallux, have played a significant role in primate evolution. Comparative studies suggest that one of the morphological novelties heralding the attainment of a monkey grade of structure was the incorporation of the prehallux within this joint. Such a joint is found in the extant Ceboidea and, paradoxically, the Hylobatidae. Hallux and prehallux then form a composite distal articular surface; the proximal surface on the medial cuneiform is completed inferomedially by a convex facet for the prehallux. Divergence of the hallux into the attitude of opposition is accompanied by conjunct rotation, screwing these joint components into a stable, close-packed position. Suppression of the prehallux is accompanied by clear osteological indicators — the absence of prehallux facets on the first metatarsal and medial cuneiform. This modification of the joint is a feature of cercopithecoid evolution, and has also occurred in the hominoid line, after divergence of the ancestral gibbons and apparently after the Dryopithecus (Proconsul) stage. The cladistic relationships indicated by these morphological changes are in striking accord with recent results on primate evolution at the molecular level.     

On the early biogeographical history of the African placentals

The Paleocene Adrar Mgorn local fauna recently discovered in the Ouarzazate basin (Morocco) along with several significant Eocene North African faunas, has yielded the oldest known placental mammals of Africa. Contrary to those from the Eocene which are basically endemic, the Adrar Mgorn placentals display affinities with taxa from North‐Tethyan continents and indicate active faunal interchanges between Africa and Europe (and perhaps Asia) during the Cretaceous/Paleogene times. On biogeographical grounds, two dispersal events are suggested as a working hypothesis. The oldest one, exemplified by the presence of paleoryctid and adapisoriculid “insectivores”; in the Moroccan locality, possibly took place by the K/T boundary. The second dispersal event exemplified by the discovery of an omomyid primate and possible hyaenodontid creodonts may have been contemporaneous with the Paleocene/Eocene boundary during which a marine regression is also known.