A morphometric analysis of the Late Pleistocene Human Skeleton from the Moh Khiew Cave in Thailand.

Few Late Pleistocene human remains have been found in Southeast Asia and the morphological features of the people of that age are still largely unknown due to the virtual lack of human remains in the area. Recent excavations at the Moh Khiew Cave in Thailand resulted in the discovery of a Late Pleistocene human skeleton in a relatively good state of preservation. An AMS radiocarbon date on the charcoal sample gathered from the burial gave a result of 25,800 +/- 600 BP, implying that the inhabitants of Moh Khiew Cave resided in a part of Sundaland during the last glacial age. In debates on the population history of Southeast Asia, it has been repeatedly advocated that Southeast Asia was occupied by indigenous people akin to present-day Australo-Melanesians prior to an expansion of migrants from Northeast Asia into this area. Morphometric analyses were undertaken to test the validity of this hypothesis. In the present study, cranial and dental measurements recorded from the Moh Khiew remains are compared with those of early and modern samples from Southeast Asia and Australia. These comparisons demonstrate that the Moh Khiew specimen resembles the Late Pleistocene series from Coobool Creek, Australia in both cranial and dental measurements. These results suggest that the Moh Khiew skeleton, as well as other fossil remains from the Tabon, Niah and Gua Gunung sites, represents a member of the Sundaland population during the Late Pleistocene, who may share common ancestry with the present-day Australian Aborigines and Melanesians.     

Early Holocene human skeletal remains from Sumidouro Cave, Lagoa Santa, Brazil: history of discoveries, geological and chronological context, and comparative cranial morphology

In this work, we present new evidence supporting the idea that the first Americans were very distinct from late and recent Native Americans and Asians in terms of cranial morphology. The study is based on 30 early Holocene specimens recovered from Sumidouro Cave (Lagoa Santa region, central Brazil) by Peter Lund in 1843. Sumidouro is the largest known collection of Paleoindian skulls deriving from a single site. Six different multivariate statistical methods were applied to assess the morphological affinities of the Sumidouro skulls in comparison to Howells' worldwide extant series and late archaic Brazilian series (Base Aérea and Tapera). The results show a clear association between Sumidouro and Australo-Melanesians and none with late Asian and Amerindian series. These results are in accordance with those of previous studies of final Pleistocene/early Holocene human skulls from South, Central, and North America, attesting to a colonization of the New World by at least two different, succeeding biological populations: an early one with a cranial morphology similar to that found today in the African and Australian continents, and a later one with a morphology similar to that found today among northeastern Asians.     

Dental perspectives on the population history of Southeast Asia

This article uses metric and nonmetric dental data to test the "two-layer" or immigration hypothesis whereby Southeast Asia was initially occupied by an "Australo-Melanesian" population that later underwent substantial genetic admixture with East Asian immigrants associated with the spread of agriculture from the Neolithic period onwards. We examined teeth from 4,002 individuals comprising 42 prehistoric and historic samples from East Asia, Southeast Asia, Australia, and Melanesia. For the odontometric analysis, dental size proportions were compared using factor analysis and Q-mode correlation coefficients, and overall tooth size was also compared between population samples. Nonmetric population affinities were estimated by Smith's distances, using the frequencies of 16 tooth traits. The results of both the metric and nonmetric analyses demonstrate close affinities between recent Australo-Melanesian samples and samples representing early Southeast Asia, such as the Early to Middle Holocene series from Vietnam, Malaysia, and Flores. In contrast, the dental characteristics of most modern Southeast Asians exhibit a mixture of traits associated with East Asians and Australo-Melanesians, suggesting that these populations were genetically influenced by immigrants from East Asia. East Asian metric and/or nonmetric traits are also found in some prehistoric samples from Southeast Asia such as Ban Kao (Thailand), implying that immigration probably began in the early Neolithic. Much clearer influence of East Asian immigration was found in Early Metal Age Vietnamese and Sulawesi samples. Although the results of this study are consistent with the immigration hypothesis, analysis of additional Neolithic samples is needed to determine the exact timing of population dispersals into Southeast Asia.     

东亚中更新世古人类下颔第二臼齿釉质-齿质连接面三维形状和釉质厚度分布

东亚中更新世古人类在头骨、下颌骨、牙齿等解剖部位表现出不同程度的形态多样性,中期成员代表为直立人,而晚期成员的演化地位具有较大争议。为进一步了解东亚中更新世古人类内部的形态变异特点和为东亚中更新世晚期古人类分类提供依据,本文使用微分同胚的表面匹配（Diffeomorphic Surface Matching, DSM）和形态测量图（Morphometric map）对下颌第二臼齿（M₂）釉质-齿质连接面的形状和齿冠侧面釉质厚度分布模式进行了量化分析。结果显示：1）东亚中更新世古人类与晚期人属成员（尼安德特人和现代人）存在较明显的形态差别;2）该时段晚期的东亚古人类相对中期直立人在侧面釉质厚度分布规律上具有独特性,并在釉质-齿质连接面的三维形状上与晚期人属成员更加接近。本文在以往对东亚中更新世古人类牙齿内外结构单个性状研究的基础上,使用三维形态测量方法进一步量化了M₂釉质-齿质连接面三维形状和侧面釉质厚度分布模式两项重要特征的变异特点,这对未来该时段同类型牙齿的形态鉴定以及解决东亚中更新世晚期古人类的分类地位具有一定意义。     

L’origine des artefacts d’obsidienne de Gua Pawon, Dago et Bukit Karsamanik à Bandung, Indonésie

This paper presents the results of a study to determine whether the obsidian artifacts found in Gua Pawon, Dago and Bukit Karsamanik in Bandung came from the well-known sources of Gunung Kendan in Nagreg, Kampung Rejeng in Garut or elsewhere. Obsidian artifacts for this study were obtained from earlier archaeological excavations at Gua Pawon and survey at the sites of Dago and Bukit Karsamanik in Bandung. Samples of obsidian were also collected from the known obsidian sources in Gunung Kendan in Nagreg and Kampung Rejeng in Garut for comparative purposes. Analyses of these samples were done on a scanning electron microscope using the energy dispersive X-ray spectrometer at the University of Science, Malaysia, Penang and the electron microprobe at the University of Malaya, Kuala Lumpur. Multielement analysis was undertaken, and statistical procedures were performed on data obtained from the artifacts and the sources. The results of the study thus far suggested that the obsidian artifacts from Gua Pawon were made using obsidian obtained from bath Gunung Kendan and Kampung Rejeng sources while those from Dago and Bukit Karsamanik have yet to be determined. More samples from all the known obsidian sources are needed to determine the variability within and between all the different sources. Temporally the study also revealed that prehistoric humans at Gua Pawon exploited or used the same obsidian resources over several thousands of years.     

Ancestry of the Iban is predominantly Southeast Asian: genetic evidence from autosomal, mitochondrial, and Y chromosomes

Humans reached present-day Island Southeast Asia (ISEA) in one of the first major human migrations out of Africa. Population movements in the millennia following this initial settlement are thought to have greatly influenced the genetic makeup of current inhabitants, yet the extent attributed to different events is not clear. Recent studies suggest that south-to-north gene flow largely influenced present-day patterns of genetic variation in Southeast Asian populations and that late Pleistocene and early Holocene migrations from Southeast Asia are responsible for a substantial proportion of ISEA ancestry. Archaeological and linguistic evidence suggests that the ancestors of present-day inhabitants came mainly from north-to-south migrations from Taiwan and throughout ISEA approximately 4,000 years ago. We report a large-scale genetic analysis of human variation in the Iban population from the Malaysian state of Sarawak in northwestern Borneo, located in the center of ISEA. Genome-wide single-nucleotide polymorphism (SNP) markers analyzed here suggest that the Iban exhibit greatest genetic similarity to Indonesian and mainland Southeast Asian populations. The most common non-recombining Y (NRY) and mitochondrial (mt) DNA haplogroups present in the Iban are associated with populations of Southeast Asia. We conclude that migrations from Southeast Asia made a large contribution to Iban ancestry, although evidence of potential gene flow from Taiwan is also seen in uniparentally inherited marker data.     

Lithostratigraphic Context for Kln-1993.05-SNJ,a Fossil Colobine Maxilla from Jokotingkir,Sangiran Dome

Jablonski and Tyler (1999) announced a new subspecies of colobine monkey based on a fossil partial maxilla from the Sangiran dome. The specimen is easily assigned to a living leaf monkey species—most extant Southeast Asian catarrhines differ only subspecifically from their Middle Pleistocene earliest local fossil ancestors. Yet Jablonski and Tyler (1999) reported an improbable provenance for the specimen; a mass-flow volcanic breccia generally considered late Pliocene in age. We show that the Lower Lahar was laid down amidst a range of paludal habitats and that its deposition predates the appearance of all-but-now extinct, water-tolerant mammals on emergent Java. No other catarrhine fossil has been ascribed to the Lower Lahar, not even hominins, which are the most gregarious members of the group. More probable provenance lies in the upper Sangiran or the lower Bapang formations. Either alternative would associate the specimen with other catarrhine fossils in more tenable Pleistocene environments. We also unravel errors and inconsistencies in the contextual report and in the discussion of dome geochronology. The various radiometric, paleomagnetic, and paleontologic studies cited show a discordance of about 300 Ka (thousand years) across the lithostratigraphic sequence. Plio-Pleistocene biogeographic hypotheses for Java must work with short and long chronologies.     

Negritos, Australian aborigines, and the "proto-sundadont" dental pattern: the basic populations in east Asia, V.

Five evolutionarily significant dental traits were identified from a B-square distance analysis of nine crown characters recorded for several populations of East Asia and Oceania. Intergroup variation in these traits distinguishes three major divisions of the Mongoloid dental complex: sundadonty, sinodonty, and the dental pattern of Australian Aborigines. The Australian crown features may be characterized as having high frequencies of evolutionarily conservative characters. Negritos, one of the probable representatives of indigenous inhabitants of Southeast Asia who may have shared a common ancestor with Australians, possess the more derived sundadont dental pattern. As far as the five crown traits treated here are concerned, Australian dental features may be described as conforming to a "proto-sundadont" dental pattern, applying Turner's terminology. This pattern may represent a microevolutionary step prior to the emergence of the sundadont and sinodont patterns.     

安徽东至华龙洞出土的人类化石

2006年在安徽省东至县华龙洞发现了1枚人类下颌第二臼齿和2件可以拼接在一起的额骨碎片化石。根据华龙洞动物群组成及地层情况,初步确定华龙洞化石层的时代为更新世中期。本文对在华龙洞发现的人类头骨和牙齿化石的形态特征进行了观测,并与相关古人类标本进行了对比。研究发现:华龙洞人额骨和下颌臼齿都呈现出一系列常见于东亚直立人的特征。华龙洞额骨曲度较小,具有粗壮的颞线和较厚的骨壁。此外,华龙洞额骨还具有额中缝结构和扩大的额窦。华龙洞下颌第二臼齿总体显得比较粗壮。齿冠咬合面具有第五尖、第六尖和第七尖。齿冠尺寸明显大于早期现代人、现代人类和欧洲更新世中期人类,位于直立人变异范围。结合对华龙洞人类额骨和牙齿形态对比所揭示的形态特点,在华龙洞发现的人类化石可能代表着生活在更新世中期的直立人。     

鲤鱼墩新石器时代居民头骨的形态学分析

本文对广东省湛江市遂溪县鲤鱼墩新石器时代遗址所出土的5例人类头骨进行了形态学分析。这些个体在种族特征方面较为一致, 应属于蒙古大人种的范畴, 可被视为"古华南类型"群体, 较接近于现代的南亚类型。岭南地区6组史前时期人群的聚类分析(马氏距离)和特征分析结果表明, 鲤鱼墩组、东湾仔北组、鱿鱼岗组与河宕组之间存在相对较近的形态学关系; 柳江人和甑皮岩组关系最为密切。在更为广泛的地理空间范围内, 对18组不同时期人群进行的聚类分析(马氏距离)和因子分析的结果显示, 鲤鱼墩人群与其他人群保持了相对较远的形态学距离。另外, 岭南地区的古人类从晚更新世阶段到新石器时代晚期, 在颅骨的绝对测量值上反映出一个短颅化、狭颅化和高颅化的过程, 而颅指数反映的却是长颅化的趋势, 说明该地区古人类的颅宽值较之颅长值减小得更快, 形成了颅骨尺寸在绝对值上的减小, 在颅指数上却反映出长颅化趋势的现象。由此可以推测, 现代南亚类型居民的典型长颅型特征可能是在全新世之初开始逐渐形成的。     

The perforated stones of the Doi Pha Kan burials (Northern Thailand): A Mesolithic singularity?

Throughout continental Southeast Asia, the Hoabinhian techno-complex stands out in clear contrast with the universal chrono-cultural model essentially established on the basis of western prehistory. Following this model, early authors considered perforated stones and associated lithic artefacts as markers of what was then believed to pertain to a Southeast Asian Mesolithic. However, Southeast Asian Mesolitithic has progressively been abandoned in favour of a ubiquitous Hoabinhian spanning from 30,000 to 3000 BP. Here, we present and discuss the discovery of perforated stones at the Doi Pha Kan site in northern Thailand. Perforated stones have almost never been found in undisturbed stratigraphic conditions nor dated with any sufficient degree of certainty. At Doi Pha Kan site, such a kind of artefacts was found in burials intersecting sedimentary layers that could be ascertained as Hoabinhian. In contrast with similar perforated stones described in the literature, that found at Doi Pha Kan are well-dated (13,000 BP), thus providing a time-reference for a putative Southeast Asian Mesolithic. We therefore advocate that such non-Hoabinhian artefacts support the early authors’ hypothesis of the existence of a Southeast Asian Mesolithic. Finally, the funerary practices, the unusually high stature of individuals found at Doi Pha Kan in conjunction with the particular lithic assemblages further contributes to raise the question of the co-occurrence of several cultures or populations at the Pleistocene–Holocene interface in continental Southeast Asia.     

Limb bone proportions and body mass of the cave bear (Ursus spelaeus)

The European cave bear evolved during the Middle Pleistocene and adapted to mountain environments. Earlier workers have described the cave bear as a robust bear. In this study the cave bears limb bone morphology is compared to the limb bone morphology of extant bears. Body mass estimates for the cave bear are made both based on different limb bone characters and based on dental and cranial characters. The shafts are wider in the cave bear limb bones than in the extant bear limb bones, and consequently the shaft widths give higher weight estimates to the cave bear than the other dimensions. The widened shafts are suggested to be a special adaptation (of presently unknown significance) rather than an indicator of an increased body mass.     

Nacurrie 1: Mark of ancient Java, or a caring mother’s hands, in terminal Pleistocene Australia?

There has been a protracted debate over the evidence for intentional cranial modification in the terminal Pleistocene Australian crania from Kow Swamp and Coobool Creek. Resolution of this debate is crucial to interpretations of the significance of morphological variation within terminal Pleistocene-early Holocene Australian skeletal materials and claims of a regional evolutionary sequence linking Javan Homo erectus and Australian Homo sapiens. However, morphological comparisons of terminal Pleistocene and recent Australian crania are complicated by the significantly greater average body mass in the former. Raw and size-adjusted metric comparisons of the terminal Pleistocene skeleton from Nacurrie, south-eastern Australia, with modified and unmodified H. sapiens and H. erectus, identified a suite of traits in the frontal, parietal, and occipital bones associated with intentional modification of a neonate’s skull. These traits are also present in some of the crania from Kow Swamp and Coobool Creek, which are in close geographic proximity to Nacurrie, but not in unmodified H. sapiens or Javan H. erectus. Frontal bone morphology in H. erectus was distinct from all of the Australian H. sapiens samples. During the first six months of life, Nacurrie’s vault may have been shaped by his mother’s hands, rather than though the application of fixed bandages. Whether this behaviour persisted only for several generations, or hundreds of years, remains unknown. The reasons behind the shaping of Nacurrie’s head, aesthetics or otherwise, and why this cultural practice was adopted and subsequently discontinued, will always remain a matter of speculation.     

Vegetation history from archaeological charcoals in central Australia: The late Quaternary record from Puritjarra rock shelter

Archaeological charcoals from Puritjarra rock shelter provide the first direct information about the vegetation of central Australia during the late Pleistocene and early Holocene. During the late Pleistocene there appears to have been a more open vegetation than today with fewer trees and shrubs, though with many of the taxa that are important in the modern central Australian flora. The persistence of species such as Acacia macdonnelliensis, Callitris glaucophylla and Eucalyptus opaca throughout the time of the last glacial maximum and the presence of appreciable quantities of wood charcoal in the archaeological deposits at this time indicate that the region was not a tree-less steppe even during full glacial aridity. From 13,000 B.P. onwards, acacias are strongly represented in the charcoal assemblage both quantitatively and in terms of the number of species present. Acacia aneura is for the first time a major component of the assemblage indicating that it had by this time become a significant element of the local vegetation. These changes coincide with evidence elsewhere in the Australian arid zone for the onset of wetter conditions in the early Holocene.     

Evolutionary significance of cranial variation in Asian Homo erectus

Homo erectus inhabited a wide geographic area of Asia, ranging from 40 degrees north latitude in China to 8 degrees south latitude in island Southeast Asia. Yet variation within Asian H. erectus and its relation to ecological and temporal parameters have been little studied. I synthesize the revised radiometric chronologies for hominid sites in Asia and their relation to new oxygen isotope curves (proxies for climatic fluctuations and landbridge connections). These data suggest substantial opportunities in the later Pleistocene for both regional isolation and gene flow between hominids in mainland and Southeast Asia. They also suggest that the most northerly located Chinese sites (Zhoukoudian and Nanjing) may have been occupied during sequential, interglacial periods. Probably reflecting these periods of isolation, nonmetric features and principal components analysis (PCA) of calvarial shape suggest regional differentiation between northern Asian and Southeast Asian H. erectus. The most recent Southeast Asian fossils (e.g., Ngandong) conform to the Southeast Asian pattern. Except perhaps in brain size, there is no evidence that the temporally intermediate Chinese fossils are intermediate in morphology between older and younger Indonesian fossils. In fact, northern Chinese calvaria are easier to exclude from the larger Asian H. erectus hypodigm than are the Ngandong fossils. The Chinese specimens differ from the others based on their narrower occipitals and frontals for their cranial size. The Chinese sample from Zhoukoudian alone is thus not a good proxy for the morphology and variation seen within Asian H. erectus. Both the Chinese and late Indonesian samples exhibit less variation than does the early Indonesian sample; this along with their shared morphological bauplan suggests a common origin and no more than subspecific differentiation. This shared morphology, despite regional differences, was likely maintained by the increasing intensity of multiple glaciations (and longer-lasting land bridge connections) between mainland and island Southeast Asia during the last million years.     

Major features of Sundadonty and Sinodonty, including suggestions about East Asian microevolution, population history, and late Pleistocene relationships with Australian aboriginals

The eight diagnostic morphological traits of the Sundadont and Sinodont divisions of the Mongoloid dental complex are identified. Intra- and intergroup variation for these crown and root features is plotted. The univariate frequency distributions provide useful evidence for several suggestions about East Asian prehistory, dental microevolution, and intergroup relationships. The case for local evolution of Sundadonty is strengthened by finding Australian teeth to be very similar to this pattern. Australian Aboriginal teeth are also generally like those of Jomonese and some Ainus, suggesting that members of the late Pleistocene Sundaland population could have initially colonized Sahulland as well as the continental shelf of East Asia northward to Hokkaido.     

Theloderma licin McLeod and Ahmad, 2007 （Lissamphibia： Anura： Rhacophoridae）, a New Frog Record for Borneo

A new record of the rhacophorid frog, Theloderma licin is reported from Gunung Serambu, in the Bau region of western Sarawak, East Malaysia, which comprises the first published record of the species from the Sundaic island of Borneo. The species was previously known from the Malay Peninsula （southern Peninsular Thailand and Peninsular Malaysia）. Species of Theloderma are widespread in mainland and insular Southeast Asia, their arboreal habits perhaps contributing to our perception of rarity.     

福建漳平奇和洞发现的新石器时代早期人类头骨

2011年在福建漳平奇和洞发现的距今1万年左右的新石器时代早期人类遗骸"奇和洞III号",是迄今在福建地区发现的最早、最完整的古人类头骨,为探讨华南更新世晚期向全新世过渡阶段人类的体质特征及现代人群的形成与分化提供了重要的研究材料。本文对这件头骨进行了研究,奇和洞III号为35岁左右的男性个体,牙齿龋病严重,推测当时人类的经济模式主要以农耕为主。通过与更新世晚期柳江、山顶洞101号及14组新石器时代人类头骨的比较,发现奇和洞III号头骨兼有更新世晚期人类及新石器南、北方居民的混合体质特征:奇和洞III号头骨长而脑量大,似更新世晚期人类;其高而狭窄的面部、宽阔而低矮的鼻部,呈现出不同于南、北方人群的特殊体质特征。主成分分析显示,奇和洞III号与对比的新石器时代各组在头骨的测量数据上没有表现为明显的南、北地区间差异,但在头骨的测量指数或形状上存在时代和地区间的不同。本文研究为新旧石器过渡阶段人类体质特征的变异提供了进一步证据。     

Cranial thickening in an Australian hominid as a possible palaeoepidemiological indicator

This paper describes the cranial thickening of a late Pleistocene hominid (Willandra Lakes Hominid 50) from Australia. The unusual development of the vault structures in this individual has few, if any, equals among other hominids or more recent populations from around the world. The vault morphology is, therefore, described in terms of a pathologically related condition associated with the modern haemolytic blood dyscrasias, typical of sickle cell anamia and thalassemia. A possible palaeoepidemiology for these genetic adaptations among early Australasian populations is proposed together with a discussion of similar changes observed in the vault of the Singa calvarium from the Sudan. It is tentatively suggested that the cranial thickening of the Australian hominid has its origins in some form of genetic blood disease and that if this diagnosis is correct, this individual provides a rare glimpse of human biological adaptation in the late Upper Pleistocene.