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Christy G. Turner Ⅱ 《人类学学报》2000,19(4)
在近 10年里 ,有许多文章涉及解剖学上现代东亚人及其衍生人群起源问题 (Akazawa,Aoki and Kimura,1992 ;Brown,1998,1999?;Hanihara,1994;Howells,1995 ;Neves,19 98;Omoto,1995 ;Pope,1992 ;Turner,1992 a,1992 b;Wu,1998)。在许多论文中关注了周口店山顶洞的晚更新世化石 (Black,1934 ;Pei,1934 ;Weidenreich,1938— 39)。尽管原来的标本在战时失踪 ,但直接从 30年代制作模型上已经进行过许多考察和分析 ,或者利用了 Weidenreich的对原标本的测量和观察资料进行分析 ,或者兼而用之 (Brown,19 98;Howells,1995 ;Kaminga and Wrigh… 相似文献
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The human remains recovered from Upper Cave at Zhoukoudian are the richest and best preserved late Pleistocene human fossils ever found in east Asia. For decades, as the representative of the late Pleistocene human in east Asia, the Upper Cave skulls have played an important role in research on the origins of modern Mongoloids and American Indians. Recently, more attention has been paid to the details and mechanisms for late Pleistocene human evolution and the formation of modern human populations. Both the origin and diversification of modern humans have been stressed in research. Some studies further the debates on the evolutionary position of Upper Cave Man and this group’s role in the formation of modern human populations in east Asia. To further explore these problems, we examined and compared 12 non-metric features on three Upper Cave skulls and modern Chinese unearthed from two archaeological sites in North China. Our results indicate that 8 features are expressed differently between Upper Cave Man and modern Chinese. We believe that more primitive characteristics define Upper Cave Man when compared to modern Chinese populations. These findings and some problems on late Pleistocene human evolution including intra2group variation and the standard for modern human populations, are discussed. 相似文献
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LIU Wu; WU Xian-zhu; WU Xiu-jie 《人类学学报》2009,28(02):113
The morphological and metrical features of seven late Pleistocene human teeth found in Huanglong Cave, Yunxi County, Hubei Province, were compared with relevant fossil and recent human samples. Our work indicates that most of the dental features of the Huanglong Cave teeth resemble those of modern humans, with a few features also identified in the late Pleistocene humans. The occurrence of shoveling and double shoveling on the upper incisors , and enamel extension on the upper molar from the Huanglong Cave suggest that these humans already had typical dental morphological features of East Asian populations. This study also found a greater size and more pronounced robustness in the Huanglong Cave anterior teeth as compared to modern humans. Obvious damage and chipping caused by non-masticatory utilization of teeth was also recognized. 相似文献
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周口店田园洞古人类化石点地层学研究及与山顶洞的对比 总被引:7,自引:1,他引:7
田园洞主体堆积厚度约2.5m,其动物群可分为上、下两个组合:上部组合物种多样性丰富,化石被啮齿类严重啮咬;下部组合化石种类单调,以鹿类和绵羊类为主,但化石丰富,极少有啮齿类咬痕。人类化石发现于下部组合;东洋界动物主要出现在上部组合,例如猕猴、猪獾、果子狸和鬣羚等。而马鹿和绵羊只出现于下部组合。沟齿鼯鼠和豪猪在下部组合开始出现,但主要发现于上部组合。梅花鹿是田园洞的优势种,在各个阶段都出现。通过统计比较,发现山顶洞3个地层单元(上室、下室和下窨)中所含化石属种基本一致,代表同一个动物群。尽管田园洞动物群中尚未发现可靠绝灭种类,但却有10种地区绝灭种,它与现生动物群有一定差异;而在堆积物特征及化石组合方面,与周口店山顶洞的更为接近。在田园洞和山顶洞出现的沟齿鼯鼠、猪獾、果子狸及鬣羚等是各自在华北地区的最早记录,可能代表了更新世末期自南而北的动物迁徙事件。 相似文献
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TONG Haowen 《人类学学报》2006,25(01):68
The fauna in Tianyuan Cave can be divided into two assemblages. The Upper Assemblage is typical of rodent gnawing marks, and contains more oriental elements. The Lower Assemblage contains the human fossils and almost completely free of gnawing. <br>The main deposits in Tianyuan Cave are composed of breccia with mild clay, which resembles that of Upper Cave in Zhoukoudian. <br>The Upper Cave deposits were composed of three units: Upper room , Lower Room and the Lower recess. Based on the analysis of the fauna, it seems that there is no difference among these three units. That’s to say, the Upper Cave Fauna is a uniform fauna. But the most interesting elements are without horizon record, such as Hystrix and Paguma as well as Elephas. <br>AMS 14C dating on mammalian bones gave the results: 34 —24 ka BP (Chen et al. , 1992). In chronology, they are correlated with the lower portion of the Tianyuan Cave deposits , which dated to 30 500—39 430 a B. P. <br>In the composition of fauna, Tianyuan Cave has 27 species in common with the Upper Cave fauna, which accounts for 6912 % of the total fauna. Additionally, both the Tianyuan Cave and Upper Cave are dominated by Cervus nippon; and they contain the earliest records of Aeretes melanopterus, as well as the latest Hystrix in North China. The fossils from the afore mentioned two sites are less fossilized. <br>Felis tigris, Lepus and Pseudaxis are the most abundant ones in the Upper Cave fauna. Paguma and Acinonyx jubatus are the rarest ones. <br>The Upper Cave fauna is characterized by complete skeletons. In the Lower recess complete skeletons of deer and bear were all piled together ( twenty-five deers). <br>Aeretes melanopterus, Arctonyx collaris, Paguma larvata and Capricornis represent the earliest appearance in North China. <br>Ochotona dauurica, Cricetinus ( Cricetulus) varians, Hystrix subcristata, Ursus thibetanus, Acinonyx jubatus, Cervus elaphus and Ovis in Tianyuan Cave and Upper Cave represent the latest record of these species in Beijing area. <br>The Tianyuan Cave and the Upper Cave faunas should be named after Cervus nippon-Hystrix- Aeretes. 相似文献
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Chen Tiemei;R. E. M. Hedges;Yuan Zhenxin 《人类学学报》1992,11(02):112
Altogether 12 fossil bone samples in two batches were dated with accelerator mass spectro-metry radiocarbon ( AMS-C14) technique. In comparison with the first batch of AMS-Cl4 da-tes, new combined dating results push the age for the cultural phase further back to 29- -24ka before present, while the time of filling of the Lower Recess remains unchanged, which hadstarted at about 34--33 ka ago (see table 1).<br>This new age assignment is much older than coinmonly accepted conventional radiocarbonages of 10470 a for the cultural phase and 18340 a for the deposits in the Lower Recess. Wethink the AMS-C14 dates are more compatible with geological and archaeological evidences.(1) Human skulls found in this site were unanimously classified as late Homo sapiens.Mor phologically these skulls show more primitive features than other members of Later Homo sapiens like Ziyang Man and Chuandong Man of Puding, and are different in species levelfrom that of Chinese early neolithics. It must have taken quite a long time for the evolutionprocess when Upper Cave Men gradually transformed into Homo sapiens, which would contra-dict the conception that the Upper Cave Men lived at the very end of Late Pleistocene.<br>(2) 19-11 ka was an extremely cold period, while 34--24 ka was a relatively warm in-terstadial during the Wurm Glacial. Upper Cave fauna contained tropic animals like Pugumalarvata and Acinonyx cf. jubatus, but no Coelodonta antiquitatis nor mammuthus which werevery popular during cold glacial time in North China. AMS -Cl4 age determination of 34--24ka would better fit the composition of the fauna.<br>No difference in culture nor fauna between upper and lower parts of the cultural depo-sits has been reported, still as no samples from the uppermost layers of this site has been datedyet, the possibility that the Upper Cave Culture had lasted somewhat later than 24 ka can notbe completely excluded. 相似文献
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山顶洞人与现代华北人头骨非测量性特征比较及中国更新世晚期人类演化的一些问题 总被引:3,自引:1,他引:3
山顶洞人化石是迄今在东亚地区发现的数量最为丰富、保存状态最为完好的更新世晚期人类化石。多年来,山顶洞人作为东亚地区更新世晚期人类的代表,在研究东亚地区现代蒙古人种及美洲印第安人起源方面发挥着重要作用。随着对现代人起源与演化研究的深入,学术界对更新世晚期人类演化及现代人群形成过程的许多细节及演化机制予以了越来越多的注意,提出了现代人群出现时间及现代人群分化时间的概念。一些研究对山顶洞人的演化程度及其在东亚地区现代人群形成上的作用也提出了不同看法。为了深入探讨这些问题,本文对12项颅骨非测量特征在山顶洞人与现代中国人的表现情况进行了对比研究。发现有8项特征在山顶洞人与现代中国人之间具有不同的表现,作者认为山顶洞人在颅骨特征表现上较现代中国人具有更多的原始性。在此基础上,作者就更新世晚期人群内部变异、现代人群特征标准等问题进行了讨论。 相似文献
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Chen Tiemei 《人类学学报》1989,8(03):216
Five accelerator-mass spectrometry radiocarbon dates of bone samples collected from Upper Cave, Zhoukoudian are given in this paper. Instead of collagen, amino acid was extracted from the bone for dating purpose. The measurements were carried out at the AMS facility of Oxford University. 10 ka and 20-23 ka of ages are suggested for the upper and lower limits of the Palaeolithic Culture of Upper Cave, respectively. 相似文献
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Katerina Harvati 《Journal of human evolution》2009,(6):751-762
Since the discovery of the human remains from the Upper Cave of Zhoukoudian in the 1930s there has been speculation over their affinities. In particular, the degree to which the three adult crania exhibit recent East Asian morphology, as well as their degree of within-group variability, has long been debated. Several early researchers described a resemblance to East Asian populations, but these findings have been for the most part rejected by more recent metric and non-metric analyses. Nevertheless, the Upper Cave specimens have not been classified conclusively into any recent modern human population to which they have been compared, and classification results differ for each cranium. Here, the question of the affinities of Upper Cave 101 and 103, the two better-preserved crania, is examined from the perspective of the Late Pleistocene human fossil record using the methodology of 3-D geometric morphometrics. The degree of morphological variation between the two specimens is also evaluated within the context of recent population variability. Neurocranial and facial morphology are analyzed separately so as to maximize comparative samples. Results show a morphological resemblance of the Upper Cave material to Upper Paleolithic Europeans. It is proposed that the Upper Cave specimens retain important aspects of modern human ancestral morphology, and possibly share a recent common ancestral population with Upper Paleolithic Europeans, in accordance with the Single Origin model of modern human origins. 相似文献
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Since the discovery of the Homo sapiens crania from the Upper Cave of Zhoukoudian in northern China (UC 101, UC 102, and UC 103), no clear consensus has arisen regarding their affinities with modern populations. We use linear craniofacial measurements to compare UC 101 and UC 103 to a worldwide sample of H. sapiens that includes Paleoamericans and Archaic Indians, and employ Mahalanobis distance analysis and associated unweighted, unrestricted canonical variate analysis for the comparisons. Analyses indicate that UC 101 has consistent affinities with Easter Island and European populations, whereas UC 103 has more tenuous similarities with Australo-Melanesian groups. Both fossils exhibit some similarities to certain Paleoamerican and Archaic Indian individuals, but rarely cluster together. Upper Cave 103 is more of an outlier to modern populations than is UC 101. The fossils are not representative of any group to which they have been compared, but may be part of the generalized population that was ancestral to Paleoamericans. 相似文献
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Cioclovina (Romania): affinities of an early modern European 总被引:1,自引:0,他引:1
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对近代—现代非洲和中国人群26项颅骨特征的观测和分析显示非洲人具有一些显示其特异性的颅骨特征,但多数特征的表现与东亚人类非常接近,提示现代人群体质特征的趋同性。作者认为非洲人在多数颅骨特征的表现方式上较中国人更为多样化,表明现代非洲人群在体质特征的表现上较东亚人类具有更宽广的形态变异谱。作者基于许多东亚、欧洲及澳洲人类的颅骨特征在非洲人群具有较高的出现率或明显的表现等现象提出一些未来研究中有待解决的问题。 相似文献
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Nancy Minugh-Purvis 《American journal of physical anthropology》1993,92(4):449-461
Reexamination of the immature Upper Pleistocene hominid maxilla from Mugharet el-'Aliya (Tangier), Morocco is undertaken in light of new evidence on the growth and development of Upper Pleistocene hominids. Metric and qualitative comparisons were made with 17 immature Upper Pleistocene maxillae, and with a recent Homo sapiens sapiens sample. No unambiguous criteria for aligning the maxilla with Neandertals were found, although one character, the degree of maxillary flexion on the zygoma, strongly suggests that this child could be a representative of H. s. sapiens. The probable lack of a canine fossa in Mugharet el-'Aliya 1, the primary criterion used previously to align it with Neandertals, cannot be accurately extrapolated to its adult form from this juvenile. The present evidence suggests that it is inappropriate to refer to this fossil as “Neandertal-like” or as a North African “neandertaloid.” Thus, the Tangier maxilla should not be cited as evidence for the presence of Neandertal facial features in North Africa during the Upper Pleistocene. © 1993 Wiley-Liss, Inc. 相似文献
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TONG Hao-wen; LIU Jin-yi; ZHANG Shuang-quan 《人类学学报》2004,23(03):213
Tianyuan Cave is a human fossil-bearing site found recently outside of the core area of prehistoric localitiesin Zhoukoudian area. The newly discovered site is also very rich in large mammal fos-sils, most of which are cervids. Until now, all the mammal fossils recovered here can be included into the living forms except a broken tooth of Crocuta. The geologic age of the new site can be correlated with that of the Upper Cave at Zhoukoudian. Some elements of the mammal fauna have become disap-peared from this region nowadays, they are Martes sp., Ursus thibetanus, Moschus moschiferus, Cervus nippon, Bos sp. and Capricornis sp. The fossil evidence of all these mammal species mentioned above may represent the latest records of their existence in Beijing area. But some elements are the first records of their appearance in Beijing area, such as Arctonyx collaris and Capricornis sp., both of them are oriental animals. 相似文献