The early history of the Hejaz: a response to Garth Bawden

Despite Dr. Bawden's criticisms - some of which seem to be based on his misunderstanding of previous arguments - the author reaffirms his view that the development of "oasis urbanism" in the Hejaz at the end of the 2nd millennium was at least in part the result of Egyptian trading contacts with the region. The available evidence does not allow us to conclude that this phenomenon survived into the early 1st millennium, however, and it is more likely that the area became nomadized for several centuries, perhaps until the Neo-Babylonian occupation of Tayma in the mid-sixth century.     

谈偃师焦村魏石经《尚书·无逸》残石

1978年,洛阳汉魏太学遗址东南约18公里的偃师焦村之野发现一块刻有古文、小篆、隶书三体之曹魏正始石经残石,6行19字,经文“家……勤劳……不则……昔在……宁……外”,为《尚书·无逸》篇开首,复原后知为正始石经第廿石中心偏左部位残石。     

核磁共振(NMR)T2分布对云冈石窟风化的初步研究

云冈石窟的保护受到我国文物保护工作者的重视。恶劣的自然环境,加上人为的污染,使云冈石窟的保护问题日显严峻,必须综合治理。然而,在这些复杂因素中,岩体的风化治理最为关键。岩石的孔隙尺寸及其分布是表征岩石力学、水理性质的重要参数。同种岩石,其孔隙率越高或者孔隙分布越大,则表示岩石的力学和水理性质越差。由此可见,借助孔隙率及孔隙分布状况,可表征同种岩石的风化情况。核磁共振横向弛豫时间T2与岩石孔径分布具有一定的线性关系。随着石雕风化的加剧,岩石可视孔隙率增大,孔径大小的平均值也将相应增大。基于这一前提,本研究尝试采用核磁共振横向弛豫时间T2分析石雕文物不同深处的孔径分布情况,通过实验室对云冈石窟新鲜岩石样品,结合抗盐风化安定性实验,和对自然风化样品采用便携式核磁进行无损检测,探讨其风化程度和深度,以便深入研究石雕文物的风化状况。研究结果表明, 风化岩石的新鲜层只有一类小孔隙,弛豫时间约为2~6ms,风化层岩石有大孔隙生成,且随着岩石风化程度增强,小孔径孔隙所占孔隙比例降低,大孔径孔隙所占比例增多。根据不同深度岩样的孔径分布情况,及新鲜岩石的孔径分布情况,可以得出岩石的风化深度为5mm左右。本研究可为后续的现场保护措施提供有价值的信息。     

LASER ARGON DATING AND GEOLOGICAL PROVENANCING OF A STONE AXE FROM THE STONEHENGE ENVIRONS*

The recently-developed laser microprobe ⁴⁰argon-³⁹ argon technique has been used to give a geological date for a rhyolitic tuff stone axe fragment from the Stonehenge environs. The method requires only milligramme-sized samples and gives dates of sufficient accuracy to aid in provenancing artefacts to sources, as well as information on the heating history of samples. The axe sample is of Lower Carboniferous date (341 ± 5 Ma) and this limits possible sources to outcrops within the Scottish Midland Valley and small altered exposures in Dartmoor. X-ray fluorescence analysis of the axe suggests the Scottish Midland Valley as the more likely source. The laser argon analysis also shows that the implement had not been heated in antiquity. Laser argon-argon dating can, therefore, be a useful tool in artefact study.     

汉画像石麒麟图像考略

汉画像石上的麒麟图像因其旁注榜题"騏驎"而成为比较可信的研究资料,其图像以鹿为原型、头部有"山"形角、个别身腹部刻饰羽翼等纹饰。这一图像拓展了鹿图像引魂升天的主题,在鹿的头部加上"山"形角,提升了鹿图像的神格地位,使之成为王者风范的象征。其身腹部刻饰羽翼则是中西文化交流成果的体现。     

宋代多层墓葬研究

多层墓葬是指在墓葬中构造出多个立体空间的墓葬形制。从层次结构上看,可分为三层和双层两类,以双层结构为主。这种多层构造最早出现在北宋中期,作为一种御赐的"地下石藏"来使用。在北宋晚至南宋初期,多层墓葬的形制和构造均发生一定的变化,隔层的功能也发生改变,但总体上仍可以看作是"地下石藏"的变形。到了南宋中期,多层构造的使用方式也发生了很大的变化,上层空间的实用性明显增强,出现葬人或密封防潮等利用方式。多层墓葬的结构和功能随着时代发展,其目的大多离不开对棺椁和尸体的保存。     

The Smiling Abbot: Rediscovering a Unique Medieval Effigial Slab

The article reports on a newly re-discovered fragment of a recumbent effigial slab commemorating Abbot Hywel (‘Howel’), most likely an abbot of the Cistercian house of Valle Crucis, near Llangollen (Denbighs.). The slab was probably carved very early in the fourteenth century, and could have covered the abbot’s burial place. The stone was dislocated and fragmented at an unknown point in the abbey’s history, and most likely removed from the site during the nineteenth-century clearance of the abbey ruins. It was briefly reported on in 1895 and has been lost to scholarship subsequently.

If indeed from Valle Crucis, the stone is the only known effigial slab commemorating a Cistercian abbot from Wales, and a rare example from Britain. Given that few similar Cistercian abbatial monuments have been identified from elsewhere, the ‘Smiling Abbot’, although only a fragment, is a significant addition to the known corpus of later medieval mortuary monuments. The article discusses the provenance, dating, identification and significance of the monument, including the abbot’s distinctive smile. The stone sheds new light on mortuary and commemorative practice at Valle Crucis Abbey in the early fourteenth century.     

DNA AND PROTEIN RECOVERY FROM WASHED EXPERIMENTAL STONE TOOLS*

Traces of protein and DNA are preserved on stone tools used to process animals. Previous research documents the identification of protein residues from tools sonicated in 5% ammonium hydroxide, but it remains untested whether the same treatment yields useable DNA. In this study we report both DNA and protein recovery using 5% ammonium hydroxide from residues on stone tools. We extracted 13‐year‐old residues from experimentally manufactured stone tools used to butcher a single animal. We also show that surface washing procedures typically used to curate stone tools remove only a small fraction of the DNA and protein deposited during animal butchery.     

A Cut‐marked and Fractured Mesolithic Human Bone from Kent's Cavern,Devon, UK

An isolated adult human ulna fragment recovered from the ‘black mould’ layer of Kent's Cavern by William Pengelly in 1866 exhibits a series of stone tool cut marks. The specimen has been directly AMS ¹⁴C‐dated to 7314–7075 cal bc (OxA‐20588: 8185 ± 38 bp ) and may be from the same individual as a maxilla fragment dated to the same period. The cut marks are located on the olecranon process, in a position indicative of dismemberment, whereas the fracture characteristics of the bone furthermore suggest peri‐mortem breakage, typical of butchery for the extraction of marrow. We here present and discuss the specimen and consider both ritual mortuary treatment and anthropophagy as possible explanations. Although it is difficult to interpret a single element in isolation, the latter scenario seems to be better supported and is not without parallel in prehistoric Europe, as indicated by a review of the available literature. Copyright © 2012 John Wiley & Sons, Ltd.     

Developing FTIR Microspectroscopy for the Analysis of Animal-Tissue Residues on Stone Tools

The analysis of microscopic residues on stone tools provides one of the most direct ways to reconstruct the functions of such artifacts. However, new methods are needed to strengthen residue identifications based upon visible-light microscopy. In this work, we establish that reflectance Fourier-transform infrared microspectroscopy (FTIRM) can be used to document IR spectra of animal-tissue residues on experimental stone tools. First, we present a set of reflectance FTIRM standards for the most commonly identified animal-tissue residues on stone tools: skin, meat, fat, hair, blood, feather barbules, fish scales, and bone. We provide spectral peak assignments for each residue and demonstrate that high-quality reflectance FTIRM spectra can be generated under ideal circumstances. Second, we document the spectra for these residues when they are located on a stone substrate such as flint or obsidian. We discuss procedures for correcting spectra that are affected by specular reflection and explain the effects of spectral interference from the stone. Our results show that reflectance FTIRM is sensitive to small intra-sample differences in composition. This means that it will record the effects of decomposition in ancient residues. The methodological developments we present here will help lithic residue analysts incorporate in situ reflectance FTIRM into their analysis protocols to strengthen identifications.     

Optically stimulated luminescence dating of the city wall system of ancient Tayma (NW Saudi Arabia)

In addition to a series of chronological markers (artefacts, pottery) in the archaeological contexts of ancient Tayma (NW Saudi Arabia), optically stimulated luminescence (OSL) and radiocarbon dating techniques were applied to generate reliable ages for the city wall system of the oasis. A massive aeolian sand deposit burying the oldest part of the outer wall of Tayma was sampled to obtain a minimum age for the construction of this wall. The sequence of OSL ages from the inactive dune (ID) (4900 ± 300 a, 5100 ± 400 a, 4400 ± 300 a, 3900 ± 200 a, 4000 ± 200 a) is in full accordance with ¹⁴C-AMS ages of charcoal embedded into the same dune (4190–4420 cal BP, 3870–4080 cal BP). Underlying alluvial samples from the inactive gravel sheet (IGS) in contrast give maximum ages for the construction which scatter between 6600 ± 300 a and 4900 ± 400 a. The new dating sequence provides evidence that the oldest part of the ancient city wall system already existed in the 2nd half of the 3rd mill. BC which is earlier than expected thus far from archaeological and architectural interpretation.     

The origins of lithic projectile point technology: evidence from Africa,the Levant,and Europe

Projectile weaponry is a human cultural universal, but its origins and antiquity remain poorly understood. Stone- and bone-tipped projectile weapons have long been treated as emergent features of the "Upper Paleolithic" behavioral revolution. Recently it has been proposed that projectile technology was in widespread use among Homo sapiens populations in Africa during Middle Stone Age (MSA) times. One obstacle to researching the origins of projectile point technology is that the criteria archaeologists employ for recognizing plausible and implausible stone projectile points are largely subjective (overall tool shape, microwear traces). Tip cross-sectional area (TCSA) is a ballistically significant dimension that works well at discriminating North American stone projectile points (spearthrower dart tips and arrowheads) from spear points. This paper compares the TCSA values of ethnographic North American stone projectile points to hypothetical Middle and Upper Paleolithic stone projectile points from Africa, the Levant, and Europe. The results of this comparison do not support the hypothesis of widespread use of stone-tipped projectiles in Africa, the Levant, or Europe prior to 40 Ka. In the New World and in Australia, where we have the richest ethnographic record of stone projectile point use, these implements are largely employed in big-game hunting and in warfare. One or both of these factors may have played a role in the widespread adoption of stone projectile point technology after 40 Ka.     

A geometric morphometric relationship predicts stone flake shape and size variability

The archaeological record represents a window onto the complex relationship between stone artefact variance and hominin behaviour. Differences in the shapes and sizes of stone flakes—the most abundant remains of past behaviours for much of human evolutionary history—may be underpinned by variation in a range of different environmental and behavioural factors. Controlled flake production experiments have drawn inferences between flake platform preparation behaviours, which have thus far been approximated by linear measurements, and different aspects of overall stone flake variability (Dibble and Rezek J Archaeol Sci 36:1945–1954, 2009; Lin et al. Am Antiq 724–745, 2013; Magnani et al. J Archaeol Sci 46:37–49, 2014; Rezek et al. J Archaeol Sci 38:1346–1359, 2011). However, when the results are applied to archaeological assemblages, there remains a substantial amount of unexplained variability. It is unclear whether this disparity between explanatory models and archaeological data is a result of measurement error on certain key variables, whether traditional analyses are somehow a general limiting factor, or whether there are additional flake shape and size drivers that remain unaccounted for. To try and circumvent these issues, here, we describe a shape analysis approach to assessing stone flake variability including a newly developed three-dimensional geometric morphometric method (‘3DGM’). We use 3DGM to demonstrate that a relationship between platform and flake body governs flake shape and size variability. Contingently, we show that by using this 3DGM approach, we can use flake platform attributes to both (1) make fairly accurate stone flake size predictions and (2) make relatively detailed predictions of stone flake shape. Whether conscious or instinctive, an understanding of this geometric relationship would have been critical to past knappers effectively controlling the production of desired stone flakes. However, despite being able to holistically and accurately incorporate three-dimensional flake variance into our analyses, the behavioural drivers of this variance remain elusive.     

Small carnivores from a Late Neolithic burial chamber at Çatalhöyük,Turkey: pelts,rituals, and rodents

Results derived from the analysis of small carnivores from a burial chamber at the Late Neolithic Çatalhöyük (TP Area) shed light on the socioeconomic significance of stone martens (Martes foina), red foxes (Vulpes vulpes), and common weasels (Mustela nivalis). All of these are fur-bearing animals, though only the stone marten remains to show evidence that this animal was exploited for its pelt. The evidence consists of the observed skeletal bias (only the head parts and foot bones were present) and skinning marks. Two of five sets of articulated feet are most likely linked with an almost completely preserved human infant skeleton, one of two well-preserved skeletons that were interred on the burial chamber floor. In contrast to these, other human skeletons were found mostly incompletely preserved, though with evidence of articulation. It seems that the articulated forepaws were deliberately incorporated into the structure, most likely as a part of burial practice and ritual behavior. These distinctive deposits, along with rich grave goods, emphasize the uniqueness in the entire Anatolian Neolithic of the assemblage from the burial chamber, which is decorated by a panel incised with spiral motifs.     

德国多孔隙石质古迹化学增强保护新材料和新施工工艺

介绍了20世纪90年代德国石质古迹化学增强保护的新材料和新的施工工艺,提出呈皮壳状风化石雕保护的建议。     

Bairaki–a lower paleolithic site on the lower dniester

Findings of excavations at a Lower Paleolithic site, discovered in 2010 near Dubasari on the Lower Dniester, are described. Earlier, two sites with Lower Paleolithic fl int tools – Dubasari-1 (Bolshoi Fontan) and Pogrebya – were found nearby. The cultural layer, located in the top of the lower buried soil overlying the alluvial deposits of the sixth or seventh terrace of the Dniester, included a few stone artifacts and a fragment of an animal bone. The likely age of this buried soil is estimated at ca 500 ka by geological methods. In the alluvium gravel of the same terrace downstream, three pebble tools including two choppers made of a strong Cos?u?i sandstone, and four fl int pieces were found. Geological observations suggest that this alluvium is more than 800 ka old. So far these are the earliest stone tools discovered in a stratified context in the Russian, Moldavian, and Ukrainian parts of the Russian Plain.     

How flakes shatter: a critical evaluation of quartz fracture analysis

Despite its worldwide use as a stone tool raw material, quartz is known to be a difficult material for archaeologists. The main reason for this is the tendency of quartz flakes to fragment during detachment, which complicates the use of traditional lithic analyses. In this article we present an experimental study of quartz flake fragmentation. We evaluate the method called fracture analysis that has been developed and used explicitly for the study of quartz assemblages. The method assumes high predictability of quartz flake fragmentation, but our experiments show that there is significant variation in fragmentation that fracture analysis does not take into account. Our results indicate that this variation is partly explained by indenter hardness, the relative thickness of the detached flake, as well as individual knapper-related factors. These results undermine the applicability of quartz fracture analysis in its current form. In addition, we discuss the effects of flake fragmentation on the technological organisation of prehistoric quartz users and suggest that it has affected reduction strategies as well as blank and tool dimensions. We also suggest that there should be mobility-related differences in archaeological assemblages in terms of the quality of the quartz raw material and that the curation of quartz should be low in relation to better quality raw materials used parallel with it.     

Vein quartz in lithic traditions: an analysis based on experimental archaeology

Worldwide, vein quartz was a commonly used raw material for stone tools but this material has proved difficult for archaeologists to analyse because many quartz assemblages appear to be comprised of amorphous pieces, not easily recognised as humanly modified or forming ‘tools’. This paper discusses the analysis of the debitage – focusing on the debitage fragmentation rate, the debitage, break, and fragment types, and the quantitative analysis of the complete flakes – resulting from experimental knapping of quartz, which formed part of a project which investigated the use of quartz in Irish prehistoric lithic traditions. The results have highlighted the complexity involved in analysing quartz assemblages, and the significant differences between the debitage products of quartz and chert knapping assemblages. While bipolar knapping is generally easy to differentiate from direct percussion, it is harder to differentiate between soft and hard hammer percussion.