Stratigraphy, artefact industries and hominid associations for Sterkfontein, member 5

A revised stratigraphy for the early hominid site of Sterkfontein (Gauteng Province, South Africa) reveals a complex distribution of infills in the main excavation area between 2.8 and 1.4 m.y.a, as well as deposits dating to the mid to late Pleistocene. New research now shows that the Member 4 australopithecine breccia (2.8-2.6 Ma) extends further west than was previously thought, while a late phase of Member 4 is recognized in a southern area. The artefact-bearing breccias were defined sedimentologically as Member 5, but one supposed part of these younger breccias, the StW 53 infill, lacks in situ stone tools, although it does appear to post-date 2.6 Ma when artefacts first appear in the archaeological record. The StW 53 hominid, previously referred to Homo habilis, is here argued to be Australopithecus. The first artefact-bearing breccia of Member 5 is the Oldowan Infill, estimated at 2-1.7 Ma. It occupies a restricted distribution in Member 5 east and contains an expedient, flake-based tool industry associated with a few fossils of Paranthropos robustus. An enlarged cave opening subsequently admitted one or more Early Acheulean infills associated in Member 5 west with Homo ergaster. The artefacts attest to a larger site accumulation between ca. 1.7 and 1.4 Ma, with more intensive use of quartzite over quartz and a subtle but important shift to large flakes and heavier-duty tools. The available information on palaeoenvironments is summarized, showing an overall change from tropical to sub-tropical gallery forest, forest fringe and woodland conditions in Member 4 to more open woodland and grassland habitats in the later units, but with suggestions of a wet localized topography in the Paranthropus -bearing Oldowan Infill.     

Are the small human-like fossils found on Flores human endemic cretins?

Fossils from Liang Bua (LB) on Flores, Indonesia, including a nearly complete skeleton (LB1) dated to 18kyr BP, were assigned to a new species, Homo floresiensis. We hypothesize that these individuals are myxoedematous endemic (ME) cretins, part of an inland population of (mostly unaffected) Homo sapiens. ME cretins are born without a functioning thyroid; their congenital hypothyroidism leads to severe dwarfism and reduced brain size, but less severe mental retardation and motor disability than neurological endemic cretins. We show that the fossils display many signs of congenital hypothyroidism, including enlarged pituitary fossa, and that distinctive primitive features of LB1 such as the double rooted lower premolar and the primitive wrist morphology are consistent with the hypothesis. We find that the null hypothesis (that LB1 is not a cretin) is rejected by the pituitary fossa size of LB1, and by multivariate analyses of cranial measures. We show that critical environmental factors were potentially present on Flores, how remains of cretins but not of unaffected individuals could be preserved in caves, and that extant oral traditions may provide a record of cretinism.     

L'hominidé du Pléistocène supérieur en Corée

Since the middle of 1970s, one rock-shelter, six caves and one open archaeological site have yielded several hominid fossils. Among them, fossils from Yonggok, Mandal, Sangsi and Hungsu cave sites are useful to reconstruct the general shape of the Upper Pleistocene Hominids in Korea. The main study of this paper is to focus on the reconstruction of the general shape of the upper Pleistocene hominids, and to examine the cause of cranial changes from the late upper Paleolithic to Mesolithic period in Korea. Biomechanical principles are also applied to reconstruct the social activity of the upper Paleolithic man in Korea. In addition, it is assumed that main proponent of Paleolithic cultures in Korea might be Homo sapiens rather than any other species. Based on the anatomical characteristics of skull, the axillary border of the scapular and the midshaft of the femur, general appearance of Homo sapiens during the Pleistocene in Korea could be reconstructed.     

广西柳江土博甘前洞的铀系年代

本文报道晚期智人化石地点广西柳江博甘前洞新生碳酸盐岩和骨化石样的铀系测年结果。该地点表层钙板在约94Ka前开始形成,含化石粘土堆积叠压的钙板年代为约20ka,人牙化石应位于二者之间。二个动物化石样的二种铀系法年代范围为85－139ka,表明该地点与含化石堆积与表层钙板间无地层倒序现象,支持人牙化石大于100ka的结论。邻近的柳江晚期智人化石地点和柳州白莲洞人类遗址铀系测年的结果与本文一致。具现代解剖特征智人在中国南方出现的时间,很可能不晚于西非和非洲。在现代人类起源方面,中国不应是远离中心、滞后和被取代的地区。     

贵州毕节发现古人类化石与哺乳动物群

2008年12月在贵州毕节团结乡首次发现麻窝口洞化石点,经2009年、2012年和2013年3次发掘,在麻窝口洞上部砂质黏土地层中共发现了四千余件哺乳动物牙齿化石。2013年7月发现的3枚古人类牙齿,分别为左上犬齿、左上第一臼齿和右上第二臼齿。人类牙齿尺寸偏小,臼齿咬合面沟纹简单,没有复杂的咬合面皱纹和附尖齿带结构,牙根短而不显粗壮,上述特点有别于我国已经发现的直立人和早期智人,可归入解剖学上的现代人。与人类相伴的哺乳动物化石,经初步鉴定共计8目20科43属53种,动物群组合反映出亚热带森林生态环境。根据动物群的时代特点,地貌地层及堆积物的光释光年代测定,指示毕节麻窝口洞古人类的时代可能为中更新世晚期,或者晚更新世早期,毕节古人类牙齿的发现为东亚地区现代人的起源及演化增添了新的证据。     

Gamma-ray spectrometric dating of late Homo erectus skulls from Ngandong and Sambungmacan, Central Java, Indonesia

Hominid fossils from Ngandong and Sambungmacan, Central Java, Indonesia, are considered to be the most anatomically derived and youngest representatives of Homo erectus. Nondestructive gamma-ray spectrometric dating of three of these Homo erectus skulls showed that all samples underwent uranium leaching. Nevertheless, we could establish minimum age estimates of around 40ka, with an upper age limit of around 60 to 70ka. This means that the Homo erectus of Java very likely survived the Toba eruption and may have been contemporaneous with the earliest Homo sapiens in Southeast Asia and Australasia.     

云南西畴仙人洞动物化石铀系年代

本文报道晚期智人地点云南西畴仙人洞动物牙化石的铀系测年结果。4个样品的230Th234U年龄范围为47—105ka,测定了其中2个样品的227Th/230Th年龄,结果与230Th/234U法的一致。在没有进一步的地层和年代证据的情况下,将西畴人牙化石的年代暂定为47—105ka或许是合理的。但洞穴地点骨化石铀系年代总体偏年轻,上述年代范围很可能被低估。本文结果与我们已有研究的广西通天岩、前洞等地点一致,是晚期智人在我国出现比原认为的早得多的又一例证。     

广西崇左木榄山智人洞的鼠科化石

最近在广西崇左木榄山智人洞遗址采集到1件具有现代智人解剖特征初始状态的下颌骨和丰富的哺乳动物化石。啮齿类中的鼠科化石有锡金小鼠(Mus pahari)、中华姬鼠(Apodemus draco)、黑线姬鼠(Apodemus agrarius)、似德氏狨鼠(Hapalomys cf.H.delacouri)、笔尾树鼠(Chiropodomys gliroides)、社鼠(Niviventer confucianus)、针毛鼠(Niviventer fulvescens)、爱氏巨鼠(Leopoldamys edwardsi)、印度板齿鼠(Bandicota indica)、褐家鼠(Rattus norvegicus)和黄毛鼠(Rattus losea)共8属11种。这种全部由当地或邻近地区现生种类构成的组合显然比当地早更新世的三合大洞和川黔地区中更新世歌乐山期的鼠类组合进步, 而与广西田东雾云洞的鼠类组合相似, 其动物群的时代为晚更新世早期, 与不平衡铀系法得到的测年结果(距今约11万年)相吻合。智人洞鼠科动物的组合明显具有东洋界热带-亚热带动物群的特点, 其中林灌和草地型所占比例较大表明当时的森林面积可能减少、林灌和草地面积可能增加, 反映出当时的气候相对干旱。     

贵州兴义猫猫洞出土的人类化石

本文主要是对贵州兴义猫猫洞遗址出土的人化石进行的初步研究,并对哺乳动物化石、地层、堆积物作叙述。该遗址的人类化石包括下颌骨4件,股骨3段,是中国南方洞穴遗址中发现的数量较多,系统分类地位较清楚的晚期智人的化石。人类化石同层的鹿牙作铀系法测年结果为14500±1200 BP,相当于更新世的末期。     

New dates for the Fontéchevade (Charente, France) Homo remains

Homo I from the site of Fontéchevade, France, has long been an anomaly in the European fossil record. The specimen is a fragment of human frontal bone that lacks a supraorbital torus and appears to belong to an anatomically modern Homo sapiens. However, the level from which it was recovered in 1947 was dated on the basis of associated faunal and lithic material to the last interglacial or earlier. As a result, Homo I has been interpreted, among other things, as a representative of a pre-sapiens lineage in Europe. This paper reports on recent ESR and radiocarbon dates that indicate that the specimen almost certainly dates to oxygen isotope stage 3, which brings it in line with other evidence for the entry of modern Homo sapiens into Europe.     

郧县人类头骨化石与周口店直立人头骨的形态比较

对郧县人类头骨化石与周口店直立人头骨作了形态上的比较以检验直立人特征在郧县头骨化石上的表现情况．比较项目包括眶上圆枕、枕骨圆枕、枕平面与项平面之间的转折情况、眶后收缩、颅骨最大宽位置、颅盖低平情况、前额后倾情况和颅容量．结果表明,在郧县人类头骨化石的这些特征项目中,有的因头骨破损和变形而难以肯定．其余的则应是早期智人的特征．从形态上讲,郧县人类头骨化石目前还难肯定是属于直立人,而有可能属于智人,如果认为“直立人”和“智人”是两个不同的物种的话．     

The femur in early human evolution.

Uni- and multivariate analyses of 5 fossil and 215 extant hominoid femora show that two morphological patterns of hominid femora existed about two million years ago. Femora classified as Homo sp. indet. (KNMER 1472 and 1481) are more like Homo sapiens although not identical.Those classified as Australopithecus robustus (SK 82 and 97) and A. boisei (KNM-ER 1503) are similar to one another but uniquely different from any living hominoid. The strong mophological constrasts imply biomechanical and possible locomotor differences, although these are as yet unknown.     

Hominid cranial remains from upper Pleistocene deposits at Aduma, Middle Awash, Ethiopia

The Upper Pleistocene localities of Aduma and Bouri have yielded hominid fossils and extensive Middle Stone Age (MSA) archaeological assemblages. The vertebrate fossils recovered include parts of four hominid crania from Aduma and a complete right parietal from Bouri. Archaeological associations and radiometric techniques suggest an Upper Pleistocene age for these hominids. The more complete cranium from Aduma (ADU-VP-1/3) comprises most of the parietals, the occipital, and part of the frontal. This cranium is compared to late Middle and Upper Pleistocene hominid crania from Africa and the Middle East. The Aduma cranium shows a mosaic of cranial features shared with "premodern" and anatomically modern Homo sapiens. However, the posterior and lateral cranial dimensions, and most of its anatomy, are centered among modern humans and resemble specimens from Omo, Skhul, and Qafzeh. As a result, the Aduma and Bouri Upper Pleistocene hominids are assigned to anatomically modern Homo sapiens.     

贵州毕节麻窝口洞与智人伴生的长鼻类化石

最近在贵州毕节麻窝口洞发现了3枚古人类牙齿化石和伴生的哺乳动物群。其中,古人类牙齿经初步研究可归入解剖学上的现代人,而与古人类相伴的大、小哺乳动物化石,经初步鉴定共计8目20科43属53种。本文系统记述了该动物群中大哺乳动物的典型代表——长鼻类化石,共2属2种:东方剑齿象(Stegodon orientalis)和亚洲象(Elephas maximus)。麻窝口洞的长鼻类缺失我国南方早更新世的典型种类——中华乳齿象(Sinomastodon)和华南剑齿象(Stegodon huananensis),具有从典型的中更新世大熊猫-剑齿象动物群(Ailuropoda-Stegodon fauna)向晚更新世亚洲象动物群(Asian elephant fauna)过渡的特征。依动物群的性质和地貌地层的特征,毕节麻窝口洞的智人及伴生动物群的地质时代很可能为中更新世晚期或晚更新世早期,这与堆积物的光释光年代测定的初步结果(距今约11.2-17.8万年)基本吻合。麻窝口洞东方剑齿象与亚洲象的组合明显具有东洋界亚热带动物群的特点,指示温暖潮湿的气候,这些长鼻类与智人等生存于近水的森林和灌丛中,并镶嵌了一些草地。     

The environmental contexts of early human occupation of Georgia (Transcaucasia)

The hominid mandible and a third metatarsal found in Dmanisi (Republic of Georgia) are accompanied by a rich faunal assemblage and a core-chopper stone tool industry. The mandible represents a somewhat isolated morphological type of Homo erectus that appears, given the combination of its primitive and advanced traits and specific dental morphology, to be a forerunner of both late H. erectus and early archaic H. sapiens. The faunal assemblage mostly consists of Villafranchian mammals, with the majority of the species assigned to an early phase of the Upper Villafranchian (Late Villanian and Early Biharian). Faunal and paleobotanical evidence as well as the depositional nature of the site indicate that hominid occupation took place in a mosaic environment of open steppe and gallery forests. Both the concentration of resources and the warm climatic conditions in the Dmanisi region at the beginning of the early Pleistocene were favorable for hominid occupation. It is possible that hominids reached the Caucasus through the Levantine corridor, and that the environment of this region allowed them to establish a stronghold and later colonize adjacent areas.     

Paleoanthropology of the Kibish Formation, southern Ethiopia: Introduction

Cranial and skeletal remains of modern humans, Homo sapiens, were discovered in the Kibish Formation in 1967 by a team from the Kenya National Museums directed by Richard Leakey. Omo I, from Kamoya's Hominid Site (KHS), consists of much of a skeleton, including most of the cranial vault, parts of the face and mandible, and many postcranial elements. Omo II, from Paul's Hominid Site (PHS), is a virtually complete calvaria. Only a limited fauna and a few stone artifacts attributed to the Middle Stone Age were recovered in conjunction with the fossil hominids. The available dating techniques suggested a very early age, over 100 ka, for Member I, from which the Omo I and Omo II fossils were recovered. However, in subsequent decades, the reliability of the dates and the provenance of the Kibish hominids were repeatedly questioned. The papers in this volume provide a detailed stratigraphic analysis of the Kibish Formation and a series of new radiometric dates that indicate an age of 196 +/- 2 ka for Member I and 104 +/- 1 for Member III, confirming the antiquity of the lower parts of the Kibish Formation and, in turn, the fossils from Member I. Studies of the postcranial remains of Omo I indicate an overall modern human morphology with a number of primitive features. Studies of an extensive lithic record from Members I and III indicate a Middle Stone Age technology comparable to assemblages of similar age elsewhere in Ethiopia. Studies of the mammalian, avian, and fish faunas indicate overall similarities to those found in the region today, with a few distinctive differences.     

中国直立人与早期智人的牙齿形态鉴别

对直立人与早期智人的上颌牙齿特征的比较表明 :直立人牙齿的长宽尺寸 ,除中门齿唇舌径外 ,与早期智人的相应值很难区分 -早期智人的长宽尺寸多在直立人相应值的变异范围之内 ;直立人牙齿的观察性特征几乎都能在早期智人某些成员中见到。这意味着直立人与早期智人可能并无“种”而只有“亚种”这一分类级别上的差异 ,把直立人并入智人种这一建议是可取的。对若干化石地点的单个牙齿进行的重新鉴定表明 :桐梓、沂源、郧县梅铺、洛南和淅川的人类牙齿不一定是代表直立人的 ,有可能是代表早期智人的。     

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.     

Position chronologique des sites de l’Homme moderne en Chine d’après la datation U-Th

The origin and evolution of modern Homo sapiens has been the subject of an intensive debate between exponents of two competing hypotheses, multiregional origins and “recent out of Africa”. This paper presents a synthesis of the chronological studies on seven hominid sites in China based on the U-series dating, five of them of intercalated speleothem calcites and other two of fossil materials. The results show that modern humans were present in China about 100 ka ago, much earlier than previously estimated, and that the so-called “temporal gap” of human presence in China between 40 and 100 ka is most probably nothing but an artifact caused by systematic errors of the dating methods. Further multidisciplinary studies on hominid sites in China may provide important evidence for resolving the hotly debated issues concerning the origin of modern humans.