Investigations into cut-marks on fossil bones of Lower Pleistocene age from Venta Micena (Orce,Granada province,Spain)

Fossil bones from the Lower Pleistocene site of Venta Micena bear cut-marks in a small proportion of specimens, similar to that of bones with cut-marks at East African sites at Olduvai and East Lake Turkana. Cut-marks are distinguishable from other surface marks on bone cortex in terms of metrical characteristics, anatomical location, grouping, and microscopical characteristics, particularly those such as microstriations which may be observed with the scanning electron microscope.     

The first human dispersal to Europe: Remarks on the archaeological and palaeoanthropological record from Orce (Guadix-Baza basin, southeastern Spain)

The chronology of the first arrival ofHomo in Europe is a rather controversial issue, with most scholars claiming until very recently that there were no permanent human settlements before the middle Pleistocene. However, new findings at Atapuerca, Dmanisi and Orce, as well as the re-evaluation of the evidence from Java, Israel and China indicate a protracted chronology for the arrival of hominids in Eurasia, during late Pliocene/lower Pleistocene times. The systematic study of the macrovertebrate assemblages from circummediterranean sites such as Orce and Dmanisi has shown a faunal replacement at the Plio-Pleistocene boundary, marked by the arrival in Europe of African immigrants such as the hippopotamus, an equid similar to modern grevy’s zebra, a large cercopithecoid and several carnivores, including a giant hyaena, a sabre-tooth and a wild dog. An analysis of the relative frequency of bones and teeth for those species of large mammals preserved in Venta Micena indicates the improbability thatHomo sp. is represented in the fossil assemblage by several bones and no tooth remain. Finally, new data on the stratigraphy of Barranco León are offered, with remarks on the discovery in this locality of lithic artefacts and molar tooth fragment BL5-0.     

Radiographical study of skull fragment of Venta Micena (VM-0) (Orce, Granada Spain)

Since 1983, the Orce skull has been a polemic piece. The last article which refuses the human affinity of VM-0 is based on the presence of a supposed coronalis suture in VM-0 situated at 40mm of lambda point (Moyà-Solà &; Khöler 1997). This would imply that VM-0 belonged to a very small skull not possible in human genus. The present detailed x-ray study which includes: “classic x-ray”, digital x-ray, macro x-ray and computerized tomography, proves definitively the not presence of coronalis suture in VM-0 and demonstrate that all interpretations based on the presence of coronalis suture are a great mistake. Also this study shows different characters which prove the human affinity of VM-0: presence of a wide sulcus sagittalis (9mm), the print of the superior sinus sagittalis where drained venous blood of a big brain is not possible in a colt whose brain size is similar to that of sheep. We consider that the visual inspection is not enough in human Palaeontology and it is incorrect to not apply the different tests which permit proving or refusing the different subjective impressions.     

Spanish late Pliocene and early Pleistocene hominid, palaeolithic and faunal finds from Orce (Granada) and Cueva Victoria (Murcia)

In SE Spain, recent excavations in the Orce basin and at Cueva Victoria indicate presence of both hominids and hominid activity from the Plio-Pleistocene boundary and early Lower Pleistocene.     

Some fossil woods from the palaeogene of northern Kyushu,III

Petrified woods obtained from the Oligocene of Tsuyazaki, Fukuoka Prefecture have been studied, and four new species ofPrunus (Rosaceae) are described:Prunus palaeozippeliana, P. ascendentiporulosa, P. uviporulosa andP. polyporulosa. These four species are very similar to each other in gross anatomical features and are characterized by the diffuse porosity, exclusively simple perforation plates, spiral thickenings on vessel walls, heterogeneous rays and the presence of traumatic gum canals. The petrified woods ofPrunus are new records from the Tetiary of Japan.     

The oldest human fossil in Europe,from Orce (Spain)

The Orce region has one of the best late Pliocene and early Pleistocene continental paleobiological records of Europe. It is situated in the northeastern sector of the intramontane Guadix-Baza Basin (Granada, Andalusia, southern Spain). Here we describe a new fossil hominin tooth from the site of Barranco León, dated between 1.02 and 1.73 Ma (millions of years ago) by Electron Spin Resonance (ESR), which, in combination with paleomagnetic and biochronologic data, is estimated to be close to 1.4 Ma. While the range of dates obtained from these various methods overlaps with those published for the Sima del Elefante hominin locality (1.2 Ma), the overwhelming majority of evidence points to an older age. Thus, at the moment, the Barranco León hominin is the oldest from Western Europe.     

Miocene marmosets: First fossil evidence

The first fossil remains of marmosets, an isolated incisor, premolar, and molar, all similar in size toCallithrix species, have been discovered in the middle Miocene La Venta fauna of Colombia. The M¹ is referred to a new genus and species,Micodon kiotensis, characterized by a fully developed hypocone and low occlusal relief. The P₄ and I¹ resemble those ofCallithrix, suggesting a close affinity with callitrichin marmosets. In combining small size with a four-cusped morphology,Micodon demonstrates the shortcomings of typological definitions of platyrrhine families and suggests that small body size may have preceded the tricuspid molar pattern in marmoset evolution. The 14- to 15-Ma date for the La Venta suggests that marmosets are an at least moderately ancient radiation, contrary to estimates based upon the molecular clock.     

Two new fossil woods ofAcer and a new combination ofPrunus from the Tertiary of Japan

Two new species ofAcer fossil woods,A. momijiyamense andA. Watarianum, are described and a short review of fossil wood of this genus from the Tertiary of Japan is given. In the course of a study on three fossil wood species which have been described asAcer andAcernium from Japan, it is noticed thatAcernium iwatense Watari does not belong toAcer but toPrunus of the Rosaceae, and is therafore transferred intoPrunus asPrunus iwatense comb. nov.     

Tetracentron Wood from the Miocene of Noto Peninsula,Central Japan,with a short revision of homoxylic fossil woods

A vesselless fossil wood was discovered in the Miocene Yanagida Formation in the Noto Peninsula, central Japan. This fossil has distinct growth rings with gradual transition from the early- to the latewood ; tracheids, which are called 'usual traeheids' here, constitute the ground mass of the wood and have typical scalariform bordered pits on radial walls in the earlywood and circular sparse pits on those in the latewood ; rays are 1\2-4 cells wide and heterogeneous with low to high uniseriate wings; axial parenchyma strands are scattered in the latewood. This wood has a peculiar feature; sporadic radial files of broad tracheids whose tangential walls have crowded alternate bordered pits. The radial walls have crowded half-bordered pits to ray cells, but no pits to the usual tracheids. Among all of the extant and extinct angiosperms and gymnosperms, these unusual tracheids occur only in Tetracentron. From these features, we refer the fossil to the extant genus Tetracentron, and name it T. japonoxylum. A revision of homoxylic woods is made for comparision with the present fossil. Tetracentron japonoxylum is the only fossil wood of Tetracentron.     

Hemiptelea mikii sp. nov. (Ulmaceae), fossil fruits and woods from the pleistocene of central Japan

A new fossil species,Hemiptelea mikii, is described on the basis of fruits from the Pleistocene of central Japan. It is distinguished fromH. davidii, the only extant species of the genus restricted to Korea and China, in having shorter fruits. Fossil woods discovered from the same horizon differ from the extant one in some anatomical characteristics, and are assigned to the new fossil species. Taken together with earlier records of fossil fruit occurrence in the early and the middle Pleistocene of central Japan, the latest finding of fossil fruits and woods from the last glacial sediments (ca. 50,000 years ago) at Kita-egota site of Tokyo suggests thatH. mikii was widespread in central Japan throughout the Pleistocene and survived until as late as the Last Glacial age.     

Stature estimation from complete long bones in the Middle Pleistocene humans from the Sima de los Huesos, Sierra de Atapuerca (Spain)

Systematic excavations at the site of the Sima de los Huesos (SH) in the Sierra de Atapuerca (Burgos, Spain) have allowed us to reconstruct 27 complete long bones of the human species Homo heidelbergensis. The SH sample is used here, together with a sample of 39 complete Homo neanderthalensis long bones and 17 complete early Homo sapiens (Skhul/Qafzeh) long bones, to compare the stature of these three different human species. Stature is estimated for each bone using race- and sex-independent regression formulae, yielding an average stature for each bone within each taxon. The mean length of each long bone from SH is significantly greater (p < 0.05) than the corresponding mean values in the Neandertal sample. The stature has been calculated for male and female specimens separately, averaging both means to calculate a general mean. This general mean stature for the entire sample of long bones is 163.6 cm for the SH hominins, 160.6 cm for Neandertals and 177.4 cm for early modern humans. Despite some overlap in the ranges of variation, all mean values in the SH sample (whether considering isolated bones, the upper or lower limb, males or females or more complete individuals) are larger than those of Neandertals. Given the strong relationship between long bone length and stature, we conclude that SH hominins represent a slightly taller population or species than the Neandertals. However, compared with living European Mediterranean populations, neither the Sima de los Huesos hominins nor the Neandertals should be considered ‘short’ people. In fact, the average stature within the genus Homo seems to have changed little over the course of the last two million years, since the appearance of Homo ergaster in East Africa. It is only with the emergence of H. sapiens, whose earliest representatives were ‘very tall’, that a significant increase in stature can be documented.     

Insights into the evolution of child growth from Lower Pleistocene humeri at Venta Micena (Orce, Granada province, Spain)

Well-defined human anatomical characteristics are present on humeral fragments of a child (VM-1960) and an adult (VM-3691) from early Lower Pleistocene sediments at Venta Micena: both have narrower medullary cavities than in AfricanHomo erectus/ergaster (KNM-ER 1808), and the child’s humeral shaft is longer than in recent 8-to-9-year-olds even though its muscle markings are less pronounced than theirs. We infer that exposure of growing children to high mechanical loading favoured Plio-Pleistocene skeletal evolution inHomo of humeral robusticity and elongation. Precocious childhood arm-bone development, occurring before pubertal growth-spurt increments in shoulder and arm muscularity, implies a different balance from today between prepubertal hormonal influences exerted on ossification (growth hormone and somatomedin C) and the adolescent gonadal hormones of our modern growth spurt which may have still been in the process of evolution by natural selection.     

New details on the morphology of fossil onagraceous pollen grains

Fossil onagraceous pollen grains from two Upper Miocene localities in E. Austria were investigated by LM and EM. Exine structure and sculpture as well as viscin threads suggest affinities with the extant genusCircea.     

Poor fossil record and major changes around 1 MaBP

The abundance of early fossil humans in African sites ceases at dates around 1.3MaBP; there is almost none until nearly 0.8MaBP. Again these are scarce until less than 0.5 Ma. Most of Homo erectus fossils in Java are dated between c.1.3 and 0.70Ma; just a few fossil humans are known in Eurasia for this time span. Questions arise on eventual environmental constraints, that may have influenced evolutionary crises of human populations, but also on geographic conditions adverse to fossilization processes and/or site formation. Records on climate variables, vegetation, sea level, sedimentary conditions and tectonic behavior in regions of the Old World are collected, and correlation traced back in time slices. Continental accretion is related to end of sedimentation in African basins; repeated compressive tectonic activity negatively affected preservation of both fossils and occupation sites widely, before and immediately after the M/B reversal. Lithic artefact assemblages, although derived, are understood as evidence of human occupation in the studied interval. Human populations are exspected to be affected by environmental changes, small, and scattered. Origin of Homo sapeins and divergence of preneandertalians are driven back to those times. Ancestorship to the latter is found probably in African fossils of that time span. Modern traits found in the Atapuerca-TD6 sample and the preceeding considerations urge research on humans and their movements intra- and intercontinental around 1 MaBP.     

A fossil hominoid proximal femur from Kikorongo Crater, southwestern Uganda

The external morphology of a fragmentary right proximal femur from southwestern Uganda is described here. Discovered in the Kikorongo Crater of Queen Elizabeth National Park in 1961, this specimen was informally assigned to Homo sapiens (although never described) and tentatively dated to the late Pleistocene. However, because aspects of the external morphology of the femur align the fossil with the African great apes, we suggest that the Kikorongo femur may be the first postcranial fossil of the genus Pan. Like the African apes, the Kikorongo specimen lacks both an obturator externus groove and an intertrochanteric line. It has a short femoral neck with a circular cross section, and a narrow and deep superior notch. Using resampling statistics and discriminant function analysis, the Kikorongo femur clustered with the genus Pan, as opposed to Gorilla or Homo. However, if the specimen is from Pan, it would be large for this taxon. Furthermore, features that clearly distinguish the external morphology of Plio-Pleistocene hominin proximal femora from African ape femora, such as the shape of the femoral neck in cross section and femoral neck length, have converged in Holocene humans and African apes. Unfortunately, the internal morphology of the femoral neck of the Kikorongo fossil was not discernable. Although we hypothesize that the Kikorongo femur is from the genus Pan, there is such variability in the proximal femora of modern humans that, although it would be an unusual human, it remains possible that this fossil represents H. sapiens.