陕西蓝田锡水洞遗址大型哺乳动物保存特征与古人类行为分析

陕西蓝田锡水洞中产出许多中更新世哺乳类化石,这些标本残破者较多。对880件标本作埋藏学分析后发现:其中只有376件较完好,可供分类鉴定;根据身体大小,这些可鉴定的标本可分为较大、中等及较小3类,大个体动物的骨骼保存越破碎;98%的骨骼的风化级别为0—2,只有2%的风化较强,达3—5级;属草食动物的骨骼占97.6%,而食肉类的仅占1.7%;以青羊为例,死亡年龄以中青年为主,为灾变死亡;头骨残破,肢骨近端破碎严重,而远端肢梢几乎完好。种种迹象表明,与古人类活动有关。当时居住在锡水洞中的古人类以草食动物为主要猎取对象,敲骨吸髓,还可用骨作器。     

河南灵井许昌人遗址动物骨骼表面人工改造痕迹

河南灵井许昌人遗址发掘出土了距今约10—8万年前的古人类头骨化石, 与头骨化石同层发现的还有大量哺乳动物化石及石制品等文化遗物。本文是对该遗址2005—2006年出土动物化石骨骼表面人工改造痕迹的观察分析结果。灵井遗址中13%的动物骨骼表面有人工切割痕的产生, 其中切割痕位于长骨骨干部位的约占此类标本总数的98.45%; 同时,在具切割痕的长骨类化石材料中,属于食草动物上部和中部肢骨的分别为34%和41%, 属于下部肢骨的则仅为25%。此外, 灵井动物群中具敲击痕、火烧痕迹、人工使用痕迹的骨骼标本分别占全部观察例数的4.2%、1%、1.32%。总之, 通过对动物骨骼表面保留的上述人工改造痕迹的观察与统计分析, 并与埋藏学实验及其他考古遗址相关属性的对比, 表明古人类是这一遗址中大量脊椎动物肉食资源的初级获取者和利用者, 他们是导致这一动物群聚集形成的主要埋藏学因素。同时, 许昌人遗址中大量破碎动物骨骼的出现可能也与古人类敲骨取髓的取食行为有着非常紧密的联系。     

宁夏鸽子山遗址第10地点出土动物骨骼的埋藏学初步观察

宁夏鸽子山遗址第10地点(QG10)位于青铜峡市西北约20km的贺兰山南麓。2014-2017年,中国科学院古脊椎动物与古人类研究所与宁夏文物考古研究所联合组队对该遗址进行了发掘,出土大量动物化石、近万件石制品以及装饰品、骨制品、结构性火塘等。本项研究基于遗址第4层出土动物化石的埋藏学初步观察认为:晚更新世末期的古人类是遗址中动物骨骼的富集者和改造者;QG10的狩猎-采集人群采取狩猎而非主动食腐的方式获取了遗址附近的大中型食草类动物,并将其完整搬运至遗址内进行后续的肢解、食肉与敲骨取髓等营养性处理过程。相对于上述动物种类而言,遗址内的小型动物则是在其营养物质之外,古人类还利用了它们的骨骼材料以制作器型规整的骨角类工具。     

《解读奥尔杜威——Bed I遗址的埋藏学研究》评述

由西班牙马德里大学史前学系的Manuel Dominguez-Rodrigo、Rebeca Barba及美国印第安纳大学人类学系的Charles P.Egeland三位学者撰写的<解读奥尔杜威——Bed I遗址的埋藏学研究>(Deconstructing Olduvai:A Taphonomic Study of The Bed I Sites)一书于2007年由Springer出版公司正式出版发行.     

泥河湾盆地马圈沟遗址哺乳动物破碎长骨反映的古人类行为

马圈沟遗址是东北亚地区年代最古老的旧石器时代遗址之一,出土了大量石制品及动物化石,现已发现并确认距今1.76～1.26 Ma之间的17个不同阶段的文化层,为探讨早更新世东北亚地区最早人类的扩散与生存适应方式提供了关键材料。本文以距今1.66 Ma的马圈沟遗址第3文化层2001～2003年出土的大、中型哺乳动物长骨为研究材料,开展骨骼破碎方式的分析。研究表明,这批长骨化石以残段及残片为主,通过对它们的断口形态和质地,特别是破裂断口的角度进行测量、统计以及分析,发现大多数长骨是在新鲜状况下破裂的,而古人类很可能是敲碎骨骼和取食骨髓的主体;食肉类动物也造成了一些骨骼的破裂,但应该发生在古人类的行为之后。本文是首次对中国北方早更新世遗址出土动物骨骼的破碎方式进行的系统分析,为讨论早更新世古人类与食肉类的互动关系提供了新的线索。     

云南虫的埋藏学研究——兼论云南虫的分类位置

云南虫是澄江生物群中最具争议的动物之一,其系统位置目前至少有6种不同的观点,不同研究组曾分别将其解释为分类位置不定的原口动物、头索动物、半索动物、有头类、后口动物的干支类群,或者两侧对称动物的基部类群等.争论的焦点主要集中在一些关键形态特征的解释,如轴部构造、背部分节以及鳃等.澄江生物群不同地区云南虫标本的详细对比显示,相同地点云南虫的保存有明显共性,而不同地点云南虫的保存特征差异很大.云南虫争议的主要根源在于不同研究组所研究标本的产地不同,标本保存特征不同,同时又缺少不同地点云南虫埋藏学的对比研究所致.埋藏学的初步研究表明,目前云南虫许多性状特征(尤其是关键的分类特征)的解释都存有疑问.背部发生叠覆和扭曲的标本显示云南虫的背部分节和肌节特征并不相同;腮腔外囊状突起的发现更对云南虫头部结构的推测提出质疑.进一步的生物学特性分析表明云南虫身体结构的同源性还远没有定论,云南虫系统分类有待于埋藏学、沉积学、地球化学以及分子系统学等多学科的综合研究.     

《解读奥尔杜威——BedⅠ遗址的埋藏学研究》评述

由西班牙马德里大学史前学系的Manuel Dominguez-Rodrigo、Rebeca Barba及美国印第安纳大学人类学系的Charles P．Egeland三位学者撰写的《解读奥尔杜威——BedⅠ遗址的埋藏学研究》（Deconstructing Olduvai：A Taphonomic Study Of The Bed Ⅰ Sites）一书于2007年由Springer出版公司正式出版发行。     

许家窑遗址马科动物的死亡年龄

普氏野马(Equus przewalskii)和野驴(Equus hemionus)是许家窑遗址动物群中的优势属种。本文基于对这两种动物牙齿材料的测量与分析,确定了遗址中马科动物的死亡年龄,并对上、下文化层的死亡年龄分布进行了研究,以期探知古人类获取肉食资源的方式与特点。通过与马科动物在自然生存状态下以及死于不同原因(如疾病或营养衰竭、食肉动物猎杀、现代人类狩猎等)的年龄结构对比,结果表明:古人类在许家窑文化早期(下文化层)可能通过捡拾自然死亡的动物尸体、与食肉类动物抢夺猎物、主动狩猎等多种方式获取马科动物,而在许家窑文化晚期(上文化层)可能以主动狩猎作为获取马科动物的主要方式。此外,古人类在遗址的早期就可能已经具有捕获整个马科动物居群中任意年龄个体的能力,并能做出最优化判断,有选择地去捕猎脂肪和肉量较高的壮年动物群体。     

中国古人类活动遗址形成过程研究的进展与思考

中国境内分布着数千处古人类活动遗址,是早期人类演化与适应行为研究的重要区域.虽然以往的研究一直关注地学手段在解读遗址地貌和地层形成过程中的作用,然而,作为正确鉴别遗址完整性和早期人类生存行为研究的遗址形成过程(或遗址成因)分析,长期以来缺少系统性的研究和关键指标的选择.本文结合古人类活动遗址保存的地貌和主要沉积物类型,...     

泥河湾盆地板井子晚更新世遗址古人类对动物资源的消费策略

本文以泥河湾盆地板井子遗址（约90 kaBP）2015年出土的动物骨骼为材料,通过骨骼表面痕迹分析、骨骼单元出现频率研究及长骨破碎方式的统计,辨识自然作用与人类行为对动物骨骼造成的不同影响,讨论深海氧同位素5阶段(MIS 5)中国北方古人类获取、搬运及处理动物资源的综合性策略。研究结果显示：1)遗址出土的动物遗存为古人类活动所遗留,自然营力对动物骨骼有改造作用,但并未影响我们对古人类行为的辨识;2)古人类在捕获马科动物之后,将其完整地带回了遗址并肢解;3)在处理猎物遗骸时,肌肉和骨髓富集的部位是古人类利用的重点。结合河南许昌灵井遗址的动物遗存研究结果,我们认为,在MIS 5阶段前后,中国北方已经出现了可以高效利用动物资源的人类群体;稳定、充沛的能量来源,或是他们应对北半球中高纬度干旱草原环境气候波动的重要生存策略。     

Hominin-carnivore interactions during the Chinese Early Paleolithic: taphonomic perspectives from Xujiayao

The ability of archaic Homo sapiens to survive in more northerly latitudes was contingent on securing a regular source of animal fat and protein. We present a taphonomic study that examines how successful these hominins were at acquiring these food sources during the latter part of the Early Paleolithic in Northeast Asia. This study focuses on the long bone midshaft surface modifications observed on the faunal remains from Xujiayao, a middle-late Pleistocene open-air site located at 40 degrees latitude in the western Nihewan Basin, northern China. The faunal assemblage is dominated by equid remains. Analysis of the percussion, tooth, and cut mark frequencies on the long bone midshafts demonstrates that the Xujiayao hominins had primary access to high utility (meat-bearing and marrow-rich) long bones. Investigation of the dual-patterned (tooth-marked and butchery-marked) bone fragments suggests that hominins were under little pressure from competing carnivores to abandon their kills. The lack of significant differences between the size of fragments with only percussion-marks and those with only tooth-marks supports these findings. Fragmentation ratios indicate that forelimbs were more intensively processed than hind limbs. Based on the water rounding and abrasion data, the Xujiayao assemblage is likely of autochthonous origin. Since the age of Xujiayao is still in question, we can only conclude that archaic Homo sapiens were successful predators of large game in Northeast Asia some time during the latter part of the Early Paleolithic.     

Beyond leopards: tooth marks and the contribution of multiple carnivore taxa to the accumulation of the Swartkrans Member 3 fossil assemblage

The ca. 1.0 myr old fauna from Swartkrans Member 3 (South Africa) preserves abundant indication of carnivore activity in the form of tooth marks (including pits) on many bone surfaces. This direct paleontological evidence is used to test a recent suggestion that leopards, regardless of prey body size, may have been almost solely responsible for the accumulation of the majority of bones in multiple deposits (including Swartkrans Member 3) from various Sterkfontein Valley cave sites. Our results falsify that hypothesis and corroborate an earlier hypothesis that, while the carcasses of smaller animals may have been deposited in Swartkrans by leopards, other kinds of carnivores (and hominids) were mostly responsible for the deposition of large animal remains. These results demonstrate the importance of choosing appropriate classes of actualistic data for constructing taphonomic inferences of assemblage formation. In addition, they stress that an all-encompassing model of assemblage formation for the hominid-bearing deposits of the Sterkfontein Valley is inadequate and that each must be evaluated individually using not just analogical reasoning but also incorporating empirical data generated in the preserved fossil samples.     

A brief note on the resemblance between relatives in the presence of population stratification

Population stratification occurs when a study population is comprised of several sub-populations, and can result in increased false positive findings in genomewide-association studies. Recently published work shows that sub-population-specific positive assortative mating at the genotypic level results in population stratification. We show that if the allele frequency of a single nucleotide polymorphism responsible for a trait varies between sub-populations and there is no dominance variance, then the heritability of the trait increases, primarily due to an increase in the additive genetic variance of the trait.     

Taphonomic study of a pleurosternid turtle shell from the Early Cretaceous of Angeac‐Charente,southwest France

The feeding behaviour of crocodilians leads to the formation of particular assemblages by accumulation of carcasses on the bottom or at the edge of water points, in addition to the characteristic marks it leaves on bones, making crocodilians important taphonomic agents. We report here the case of a Pleurosternidae turtle shell, Pleurosternon bullockii (Owen 1842 ), discovered in 2014 in Angeac‐Charente in south‐western France. The shell shows a range of tooth marks left by a crocodyliform. Several elements designate Goniopholis as the most likely author of the marks and support the use of the ‘nutcracker’ technique. Some marks appear to have healed, while others suggest that this P. bullockii individual suffered from shell diseases. Many turtle remains and some ornithomimosaur dinosaur bones from Angeac‐Charente bear marks of a crocodyliform attack.     

浅谈WHO国家疫苗监管体系评估及其上市许可板块要求

通过卫生组织国家疫苗监管体系(National Regulatory Authority)评估是一个国家疫苗具备参与联合国全球采购资格的必要条件。本文对WHO国家疫苗监管体系评估整体加以简述,重点对上市许可板块指标进行归纳,通过探讨WHO国家疫苗监管体系评估上市许可部分的管理理念,以期为疫苗监管相关部门加强自身管理提升监管质量和效率有所提示。     

Open questions on the 3D structures of collagen containing vertebrate mineralized tissues: A perspective

Our current understanding of the structures of vertebrate mineralized tissues is largely based on light microscopy/histology and projections of 3D structures onto 2D planes using electron microscopy. We know little about the fine details of these structures in 3D at the length scales of their basic building blocks, the inherent variations of structure within a tissue and the cell-extracellular tissue interfaces. This limits progress in understanding tissue formation, relating structure to mechanical and metabolic functions, and obtaining deeper insights into pathologies and the evolution of these tissues. In this perspective we identify and discuss a series of open questions pertaining to collagen containing vertebrate mineralized tissues that can be addressed using appropriate 3D structural determination methods. By so doing we hope to encourage more research into the 3D structures of mineralized vertebrate tissues.     

A review of recent advances in the study of early angiosperms from northeastern China

The last 10 years (1998–2007) were very productive and important in the study of early angiosperms in northeastern China. The new discoveries of the earliest well-documented records of angiosperms such as Archaefructus, as well as Hyrcantha decussata (= Sinocarpus decussatus), provided fresh knowledge for better understanding the primitive characters of the ancient angiosperms and also their aquatic (or wet) habitat and their herbaceous nature. Some new approaches such as the combination of molecular and morphological characters joined together to place Archaefructus in the angiosperm phylogenetic framework. These fossils demonstrate that we should expect more ancient angiosperms to be found in the pre-Cretaceous which will continue to add important new understanding to the nature of the origin and evolution of the angiosperms.     

A Suite of Dermestid Beetle Traces on Dinosaur Bone from the Upper Jurassic Morrison Formation,Wyoming, USA

Most studies of insect traces on fossil bone deal with one or two trace morphs found on isolated bone fragments, making it difficult to identify the trace-maker and its behavior. We report the discovery of a suite of insect traces on an articulated Camptosaurus dinosaur skeleton that permits the identification of the trace-maker and interpretations of its behavior. The traces include mandible marks, pits, and shallow bores on cortical bone, and deep, meandering furrows and tunnels (borings) on articular surfaces. The interiors of bones are intensely mined, and the cavities and borings are filled with fine bone fragments (insect frass). The distinctive mandible marks consist of opposing sets of parallel grooves, indicating the maker had two apical teeth set on symmetrical mandibles and that all of the traces were made by a single taxon. Comparison of the fossils with the mandible morphology and bone traces of extant insects indicates dermestid beetles made the traces. Based on extant dermestid behavior, soft tissues were likely absent and the bones were lipid-laden when the traces were made. Examination of more than 5,000 bones from the Morrison and Cedar Mountain formations shows insect traces on bone are common but overlooked and that many bones are substantially damaged by insect mining. The key to the recognition of these important yet subtle traces is a search model and an intense, oblique light source.     

Dark bands on pyritic internal moulds of the Early Jurassic ammonites Oxynoticeras and Cheltonia from Gloucestershire,England: interpretation and significance to ammonite growth analysis

Abstract: Thin, radiating, darker bands occur on pyritic internal moulds of the Early Jurassic ammonites Oxynoticeras and Cheltonia from Bishop’s Cleeve, Gloucestershire. They closely resemble true colour patterns preserved in Early Jurassic Calliphylloceras from Kutch, India, and false colour patterns reported in Carboniferous and Triassic ammonoids. Up to five dark bands occur within the body chamber, suggesting that they do not represent serially repeated anatomical structures, but the same feature repeatedly formed during growth. Dark bands are interpreted as traces of black bands deposited on the inside of the shell at the aperture during pauses in growth. The angles between dark bands and between septa correlate strongly in Cheltonia, suggesting that pauses in growth coincided with septal secretion during the chamber formation cycle. There are, however, no other indications that growth was episodic in either genus.