华北人欧洲人和澳洲土著人的头骨厚度

The thickness of the cranial vault at the midline on the mid-frontal squama, pre-bregmatic einence, frontal at bregma, parietal at vertex, occipital at lambda and the external occipita1 protuberance was recorded in 40 male and 7 female Northern Chinese crania, 47 male and 52 female Australian Aboriginal crania and 13 male European crania using specially nodified vernier calipers. Comparison of vault thickness data obtained through direct measurement with those obtained fron lateral radiographs indicated that direct measurenent provided consistently more accurate results.
Male and fermale samples were processed separately so that the extent of sexbased variation could be examined.Student's t test was used to compare the sample means and the percentage of sexual dimorphism for each dimension was calculated according to Garn et al, (1964).The possibility of an allometric association between the thickness of the bones within the cranial vault, size of the cranial vault and stature was examined using Spearman's rank correlation coefficient and the Australian Aboriginal sample.
All but one of the mean thickness dimensions in the Australian Aboriginal male sample is significantly greater than the Northern Chinese and European means. The female results support those obtained with the males.In both males and females thickness at the external occipital protuberance, in all of the populations examined,did not correlate highly with that obtained from other parts of the cranial vault.This reflects the high degree of morphological variation in the position of the internal occipital protuberance and its influence on cranial vault thickness dimensions recorded at the external occipital protuberance.The European and Northern Chinese samples have similar cranial vault thickness dimensions. The Spearman's rank correlation coefficient matrix scores provide sone support for a biological association between vault thickness and overall cranial size. However, there appears to be little support for an association between stature and cranial vault thickness. The difference between the male and female mean vault thickness dimensions were significant at bregma, vertex and the external occipital protuberance in Australian Aboriginals and lambda and the external occipital protuberance in Northern Chinese. Some caution is needed in the interpretation of the Northern Chinese female data as the sample is extremely small.
Evidence of trauma, supressed fractures, is extremely common on the vaults of Australian Aboriginal crania from southern and central Australia. Traditionally Australian Aboriginals, males and females, involved in agressive dispute will use a substantial wooden implement and strike to the head of thir opponent(Meggitt 1962).The injuries that result from this are more common in females than in male. This form of social interaction must have rigorously selected against those individuals with thinner bones in their cranial vaults. To a large degree this may explain the greatly thickened vaults in Australian Aboriginals relative to Europeans and Northern Chines.This may also provide a clue to the factors resulting in the development of marked cranial vault thickness in Homo erectus.
     

A new pleistocene hominid-bearing locality at Hoedjiespunt,South Africa

HDP1 is an archaeological and faunal site located on the Hoedjiespunt peninsula at Saldanha Bay, South Africa, that has recently yielded fossil human remains. Artefacts from the associated archaeological deposits are identified as being Middle Stone Age. U series analysis of capping calcretes and analysis of the foraminifera and fauna associated with the human fossils indicate an age for the deposit in excess of 74,000 years before present, and it most probably dates to around 300,000 years before present. The fossil human teeth from in situ deposits at Hoedjiespunt are described and found to be large by comparison with modern humans but smaller than the known upper dentitions of southern African “archaic” Homo sapiens. The Hoedjiespunt molars are found to be morphologically within the range of variation observed in the teeth of modern Homo sapiens. © 1995 Wiley-Liss, Inc.     

Determination of cranial capacity in fossil men

The cranial capacity of a skull of unknown origin can be determined by assuming that the product of the chief dimensions corresponds to a part of the endocranial volume. We start with formulas for present day man and determine their validity for fossil man. The equivalence differs in fossil men according to their taxonomic position. This method is useful even for damaged skulls, with porion and basion missing.     

Upper pleistocene human remains from Vindija cave,Croatia, Yugoslavia

Human remains excavated from Vindija cave include a large although fragmentary sample of late Mousterian-associated specimens and a few additional individuals from the overlying early Upper Paleolithic levels. The Mousterian-associated sample is similar to European Neandertals from other regions. Compared with earlier Neandertals from south central Europe, this sample evinces evolutionary trends in the direction of Upper Paleolithic Europeans. Compared with the western European Neandertals, the same trends can be demonstrated, although the magnitude of difference is less, and there is a potential for confusing temporal with regional sources of variation. The early Upper Paleolithic-associated sample cannot be distinguished from the Mousterian-associated hominids. We believe that this site provides support for Hrdli?ka's “Neandertal phase” of human evolution, as it was originally applied in Europe.     

中国古人类颅容量的推算方法比较

古人类的体质特征和现代人不同,依据现代人头骨测量数据计算出来的公式往往不适于古人类颅容量的推算。获取古人类颅容量最准确的方法是复原出其内部的颅内模;然而,由于颅内模的复原工艺复杂,加上古人类头骨化石数量稀少且多数残破,如何准确地推算其颅容量,成为古人学者研究的难点问题之一。本文通过对中国境内发现的不同演化阶段的古人类颅容量推算方法的对比和验证,试图找出推算古人类颅容量的最适合的公式法。研究结果显示：1）早期现代人解剖特征同现代人基本接近,依据现代人头骨推算出来的回归方程可以用来推算其颅容量;2）直立人头骨厚重、脑颅低矮,体质特征不同于现代人,其颅容量的推算不能使用现代人公式法。依据本文中国直立人头骨测量数据推导出来的回程方程（C=-1301.944+60606L+0.718b+9.936h）适合其颅容量的推算。采用此直立人公式法,推算出蓝田直立人的颅容量为918 mL;3）古老型智人的体质特征位于直立人和现代人之间,对其颅容量的推算不能一概而论：体质特征接近直立人的,如大荔人、华龙洞6号,可采用直立人公式法;体质特征接近早期现代人的,如许昌1号,可采用现代人公式法;体质特征位于直立人和早期现代人中间位置的,如马坝人、金牛山人,其颅容量约等于采用现代人公式法和采用直立人公式法获得的颅容量的平均值。     

《人类演化》评介

《人类演化》一书,作者是美国密歇根大学古人类学教授沃尔波夫,大13开本,厚达900多面。初次看到如此又大又厚的书时,着实使人吃惊。16午前,沃尔波夫曾出版过一部《古人类学》教科书,在学术界颇有影响。现在出版的虽然书名为《人类演化》,但在编写材料的安排次序上,与前者并无二致,而在内容上却大大扩充了。全书内容分四大部分。第一部分是有关人类演化的基础知识,分三章,分别论述年代测定、演化理     

Contrasting signatures of population growth for mitochondrial DNA and Y chromosomes among human populations in Africa

A history of Pleistocene population expansion has been inferred from the frequency spectrum of polymorphism in the mitochondrial DNA (mtDNA) of many human populations. Similar patterns are not typically observed for autosomal and X-linked loci. One explanation for this discrepancy is a recent population bottleneck, with different rates of recovery for haploid and autosomal loci as a result of their different effective population sizes. This hypothesis predicts that mitochondrial and Y chromosomal DNA will show a similar skew in the frequency spectrum in populations that have experienced a recent increase in effective population size. We test this hypothesis by resequencing 6.6 kb of noncoding Y chromosomal DNA and 780 basepairs of the mtDNA cytochrome c oxidase subunit III (COIII) gene in 172 males from 5 African populations. Four tests of population expansion are employed for each locus in each population: Fu's Fs statistic, the R(2) statistic, coalescent simulations, and the mismatch distribution. Consistent with previous results, patterns of mtDNA polymorphism better fit a model of constant population size for food-gathering populations and a model of population expansion for food-producing populations. In contrast, none of the tests reveal evidence of Y chromosome growth for either food-gatherers or food-producers. The distinct mtDNA and Y chromosome polymorphism patterns most likely reflect sex-biased demographic processes in the recent history of African populations. We hypothesize that males experienced smaller effective population sizes and/or lower rates of migration during the Bantu expansion, which occurred over the last 5,000 years.     

现代中国人颞骨乳突后部的形态变异

人类颞骨因其复杂的表面及内部结构成为演化研究的重要解剖部位之一,然而由于缺乏对现代人颞骨形态与变异的细致研究及对比数据,对颞骨一些特征的定义和鉴定价值还存在争议。迄今为止,尚无学者对现代中国人群颞骨形态与变异做过专门研究。有鉴于此,本文对颞骨乳突后部一些典型性状的形态变异在现代中国人及部分古人类的表现情况进行了研究。研究结果表明:1)除乳突旁隆起的发育水平存在性别差异外(不受地区差异影响),乳突切迹、枕乳嵴、枕动脉沟的出现率和发育水平既不受地区差异影响,又无性别差异。2)现代中国人乳突后部形态总体表现为窄而深的乳突切迹、明显的乳突旁隆起、以及发育程度较弱的枕动脉沟和枕乳嵴;3)在本文所研究的性状中,乳突切迹、乳突切迹前端隆起、乳突旁隆起、枕乳嵴和枕动脉沟均呈现不同程度的个体变异;4)一些被认为属于尼安德特人衍生特征的性状在中国古人类和现代中国人的乳突后部都有出现;5)本文研究的颞骨乳突后部形态特征在中国更新世晚期人类的表现与现代中国人接近。     

Human molars from later Pleistocene deposits of Witkrans Cave,Gaap Escarpment,Kalahari Margin

Human molars from travertine deposits of Witkrans Cave (Gaap Escarpment, northern Cape Province, South Africa) are described. The Witkrans molars were discovered in direct association with later Pleistocene faunal remains and a sample of Middle Stone Age artifacts (Peabody, 1954; Clark, 1971; Sampson, 1974; Klein, 1984; Volman, 1984). The morphology and dimensions of the Witkrans molars resemble remains from other localities of similar age in southern Africa (Singer & Wymer, 1982; Grine & Klein, 1985; Grine et al., 1991; Rightmire & Deacon 1991) but exhibit differences from later Pleistocene occurrences in northern Africa (McBurney et al. 1953; Vallois & Roche, 1958; Ennouchi, 1969; Hublin & Tillier, 1981). These results offer further support for the existence of later Pleistocene human populations south of the Sahara which were distinct from contemporaneous peoples of Mediterranean Africa (Howell, 1978; Brauer, 1984; Rightmire, 1984; Klein 1992).     

Homo erectus—who,when and where: A survey

The state of information bearing on Homo erectus as developed since about 1960 is surveyed, with the resulting effects on problems. Definitions of H. erectus still rest on the Far Eastern samples (Chou-k'ou-tien/Java), and thus relate to late Lower to middle Middle Pleistocene material. Numerous important individual finds, however, have expanded the total: extension of the early and very early Sangiran material; very early to later in Africa, and relatively late in Europe. Datings remain uncertain or controversial within broad limits, but with some important successes and revisions. Discussion by authors of problems concerns degree of divergence among H. erectus populations and rate of evolutionary change; both appear relatively slight, but the data are inadequate for much present judgment. The apparent zone of transition to more advanced morphology (H. sapiens, sensu lato) by the late Middle Pleistocene better reflects signs of regional divergence. Some writers—not all—believe that even the earliest European fossils known (e.g., Petralona) had already advanced to a H. sapiens basic level, with later change in the direction of Neanderthals. A separate African phylum, from OH 9, is also suggested; recent Chinese finds may provide a third different post-erectus population before the Upper Pleistocene. Taxonomic expression of all this gives some problems.     

从中国晚期智人颅牙特征看中国现代人起源

本文提供或援引了中国晚期智人头骨的额骨鳞部最突出点位置、颊部骨骼下缘的形状、头骨最宽处位置等特征和铲形门齿等牙齿特征的出现率等的有关数据,并探讨了这些特征系来源于非洲“夏娃”的后裔,还是中国当地更早的人群。所得结论更倾向于后者而不利于前者。中国旧石器时代中期和晚期的文化之间缺乏显然的反差,没有中断的迹象,也是不利于中国现代人起源的替代说的有力佐证。     

Where are inion and endinion? Variations of the exo- and endocranial morphology of the occipital bone during hominin evolution

The occipital bone is frequently investigated in paleoanthropological studies because it has several features that help to differentiate various fossil hominin species. Among these features is the separation between inion and endinion, which has been proposed to be an autapomorphic trait in (Asian) Homo erectus. Methodologies are developed here to quantify for the first time the location of these anatomical points, and to interpret their variation due to the complex interactions between exocranial and endocranial size and shape of the occipital and nuchal planes, as well as the occipital lobes and cerebellum. On the basis of our analysis, neither ‘the separation between inion and endinion’ nor ‘endinion below inion’ can be considered as an autapomorphic trait in H. erectus, since this feature is a condition shared by extant African great apes and fossil hominins. Moreover, our results show that the exo- and endocranial anatomy of the occipital bone differs between hominins (except Paranthropus boisei specimens and KNM-ER 1805) and great apes. For example, chimpanzees and bonobos are characterized by a very high position of inion and their occipital bone shows an antero-posterior compression. However, these features are partly correlated with their small size when compared with hominins. Asian H. erectus specimens have a thick occipital torus, but do not differ from other robust specimens, neither in this feature nor in the analysed exo- and endocranial proportions of the occipital bone. Finally, the apparent brain size reduction during the Late Pleistocene and variation between the sexes in anatomically modern humans (AMH) reflect that specimens with smaller brains have a relatively larger posterior height of the cerebellum. However, this trend is not the sole explanation for the ‘vertical shift’ of endinion above inion that appears occasionally and exclusively in AMH.     

贵州普定穿洞出土的一化石智人颅盖骨

1976年南京大学地理系俞锦标教授等在贵州省普定县进行野外调查时,在穿洞发现骨化石、烧骨、灰烬等。后于1979年,在有关方面的配合下,在洞口进行试掘,掘到1.5米深处,获得了一个破碎的智人颅盖骨化石。颅盖骨附近还有右上颌骨半块、单独的右上中门齿一枚。与头骨化石共生的有一些骨角器、烧骨和少量石器。这些材料俞教授等已作过报道和初步研究(俞锦标等,1983;俞锦标,1984)。不久前,俞教授把头盖骨化石供本人作古人类学研究之用,现报告如下。