The stone tools of capuchins (Cebus apella)

We examined the production of stone took by capuchins (Cebus apella). Eleven subjects used five reduction techniques to produce 346 stone tools (48 cores and 298 flakes). They produced a sharp edge on 83% of the cores and largest flakes. Three monkeys later used a sample of these objects as cutting tools. These results demonstrate that monkeys produce lithic tools analogous to those produced by Oldowan hominids.     

Quantifying Oldowan Stone Tool Production at Olduvai Gorge,Tanzania

Recent research suggests that variation exists among and between Oldowan stone tool assemblages. Oldowan variation might represent differential constraints on raw materials used to produce these stone implements. Alternatively, variation among Oldowan assemblages could represent different methods that Oldowan producing hominins utilized to produce these lithic implements. Identifying differential patterns of stone tool production within the Oldowan has implications for assessing how stone tool technology evolved, how traditions of lithic production might have been culturally transmitted, and for defining the timing and scope of these evolutionary events. At present there is no null model to predict what morphological variation in the Oldowan should look like. Without such a model, quantifying whether Oldowan assemblages vary due to raw material constraints or whether they vary due to differences in production technique is not possible. This research establishes a null model for Oldowan lithic artifact morphological variation. To establish these expectations this research 1) models the expected range of variation through large scale reduction experiments, 2) develops an algorithm to categorize archaeological flakes based on how they are produced, and 3) statistically assesses the methods of production behavior used by Oldowan producing hominins at the site of DK from Olduvai Gorge, Tanzania via the experimental model. Results indicate that a subset of quartzite flakes deviate from the null expectations in a manner that demonstrates efficiency in flake manufacture, while some basalt flakes deviate from null expectations in a manner that demonstrates inefficiency in flake manufacture. The simultaneous presence of efficiency in stone tool production for one raw material (quartzite) and inefficiency in stone tool production for another raw material (basalt) suggests that Oldowan producing hominins at DK were able to mediate the economic costs associated with stone tool procurement by utilizing high-cost materials more efficiently than is expected and low-cost materials in an inefficient manner.     

Oldowayen archaïque et Oldowayen classique de l’Afrique à l’Europe méditerranéenne

Analyzing lithic industries of Lower Pleistocene and beginning of Middle Pleistocene times allows to define three groups not clearly chronological but which reflect the cognitive evolution of prehistoric Men who knapped them and the constraints of the environment: - “Archaic Oldowan” industries in which raw flakes are dominant and no small tools retouched on flakes or debris are present; - “Classical Oldowan” industries in which raw flakes are dominant and small tools retouched on flakes and debris – especially scrapers – are present; - “Acheulean industries”, in which bifaces are present – generally in small proportions – and small retouched tools are increasingly standardized.     

Adaptive Flexibility of Oldowan Hominins: Secondary Use of Flakes at Bizat Ruhama,Israel

The lithic assemblage of the Early Pleistocene site of Bizat Ruhama, Israel demonstrates the earliest evidence for systematic secondary knapping of flakes. The site, dated to the Matuyama chron, is one of the earliest primary context Oldowan occurrences in Eurasia. According to the experimental replication of the stone-tool production sequence, the secondary knapping of flakes was a part of a multi-stage operational sequence targeted at the production of small (<2 cm) flakes. This sequence included four stages: acquisition of chert pebbles, production of flakes, deliberate selection of flakes of specific morphologies, and their secondary knapping by free-hand or bipolar methods. The results suggest that flakes with retouch-like scars that were produced during this sequence and which commonly are interpreted as shaped tools are unintentional waste products of the small flake production. The intentional manufacture of very small flakes at Bizat Ruhama was probably an economic response to the raw material constrains. Systematic secondary knapping of flakes has not yet been reported from other Early Pleistocene sites. Systematic secondary knapping for small flake production became increasingly important only in the lithic industries of the second half of the Middle Pleistocene, almost a million years later. The results from Bizat Ruhama indicate that Oldowan stone-tool production sequence was conceptually more complex than previously suggested and offer a new perspective on the capabilities for invention and the adaptive flexibility of the Oldowan hominins.     

Hominin occupations at the Dmanisi site, Georgia, Southern Caucasus: raw materials and technical behaviours of Europe's first hominins

Dmanisi is the oldest site outside of Africa that records unquestioned hominin occupations as well as the dispersal of hominins in Europe and Asia. The site has yielded large numbers of artefacts from several periods of hominin occupation. This analysis of Dmanisi stone tool technology includes a review of all the pieces recovered during the last 15 years of excavations. This lithic assemblage gives insights into the hominin behaviour at 1.7-1.8 Ma in Eurasia. Dmanisi hominins exploited local rocks derived from either nearby riverbeds or outcrops, and petrographic study provides data on patterns of stone procurement. Recent geological surveys and technological studies of the artefacts illustrate the roles of hominins in composing the assemblage. Dmanisi hominins selected two types of blanks, including cobbles and angular blocks, of basalt, andesite, and tuffs. Many complete cobbles, pebbles, and rolled blocks in basalt were unmodified, and geological analyses and surveys indicate that hominins brought manuports back to the site, suggesting a complex procurement strategy. Cores, flakes and debris show that all stages of flaking activity took place at the site. Numerous unifacial cores suggest that knapping was not very elaborate. Centripetal knapping is observed on some flake-cores. Knapping was influenced by the blank shape and natural angles. Most flaked objects were either cores or chopper-cores. Flakes predominate while flake tools are rare. The Dmanisi lithic assemblage is comparable to Oldowan sites in Africa in terms of reduction sequence, organisation of the removals, platform types, and the lack of retouched flakes. Dmanisi artefacts and may have been produced by the original hominins in Europe and Asia.     

Tool-using strategies by early hominids at bed II, Olduvai Gorge, Tanzania

This study examines the current prevailing model of Oldowan technology-the opportunistic, least-effort strategy of stone tool making and using by early hominids. The sample includes the MNK chert factory site and three contemporaneous assemblages from Olduvai Gorge, all dated between 1.65 and 1.53 m.y.a. The analysis suggests that early hominids at Olduvai may have been selective, applying distinctive strategies in making and using tools depending on the different types of raw materials available to them. The preponderance of lava cores and near absence of flakes associated with the cores suggest that lava cores at Olduvai did not provide a source of flakes. They were primarily heavy-duty core tools, despite the fact that the majority of Olduvai lava is of excellent quality for flaking. Contrary to this pattern, the abundance of chert flakes and the lack of large chert cores suggest that the production of flakes was the most important strategy applied to chert. Original forms and flaking mechanics of the raw materials may have been important factors in the simultaneous application of the different, complementary strategies. The Oldowan tool-using strategy was dynamic and flexible, in response to changes in raw material availability. The use of chert between 1.65 and 1.53 m.y.a. was apparently related to the drastic decrease in flake production in lava and quartz. Finally, lack of initial reduction episodes of lava material challenges the idea of the stone cache strategy at Olduvai between 1.65 to 1.53 m.y.a.     

Late Paleo-Indian Activity At The Lubbock Lake Site

Abstract

Excavations at Lubbock Lake (41 LU1), Southern High Plains of Texas, revealed the presence of a complex, late Paleo-Indian feature containing a camping area and bison (Bison antiquus) kill/butchering locale. The feature is found within a cienega or marsh deposit and dates from 8300 to 8600 years. At least two camping episodes are indicated, separated by the kill/butchering event. Camp debris consists of a projectile point midsection, unifacial and bifacial tools, and flakes. Faunal debris includes remains of butchered pronghorn antelope, rabbits, ducks, grouse, and turtles. The kill/butchering locale contains remains of four bison and three fetuses, a bone expediency tool, a reworked projectile point base, unifacial butchering tools, and flakes. Projectile points, other lithic tools, and age of the feature indicate a Firstview occupation. From faunal and geologic data, site environs are reconstructed as a marshlands rimmed by a narrow border of wet meadows grading into a mixed grass prairie. Although several late Paleo-Indian kill/butchering locales are known on the Southern High Plains, this feature is the first late Paleo-Indian camp.     

Examining time trends in the Oldowan technology at Beds I and II,Olduvai Gorge

The lithic analysis of the Bed I and II assemblages from Olduvai Gorge reveals both static and dynamic time trends in early hominids' technology from 1.8 to 1.2 m.y.a. The Bed I Oldowan (1.87-1.75 m.y.a.) is characterized by the least effort strategy in terms of raw material exploitation and tool production. The inclusion of new raw material, chert, for toolmaking in the following Developed Oldowan A (DOA, 1.65-1.53 m.y.a.) facilitated more distinctive and variable flaking strategies depending on the kind of raw materials. The unique characters of DOA are explainable by this raw material factor, rather than technological development of hominids. The disappearance of chert in the subsequent Developed Oldowan B and Acheulian (1.53-1.2 m.y.a.) necessitated a shift in tool production strategy more similar to that of Bed I Oldowan than DOA. However, the evidence suggests that Bed II hominids might have been more skillful toolmakers, intensive tool-users, and engaged in more active transport of stone tools than the Bed I predecessors. Koobi Fora hominids maintained a more static tool-using behavior than their Olduvai counterparts due mainly to a stable supply of raw materials. They differed from Olduvai hominids in terms of less battering of cores, consistent transport behavior, and few productions of side-struck flakes, indicating a regional variation of toolmaking and using practice. However, they shared with Olduvai hominids a temporal trend toward the production of larger flakes from larger cores after 1.6 m.y.a. Increased intake of animal resources and the expansion of ranging area of Homo ergaster would have led to the development of technological organization. Technological changes in the Oldowan industry are attested at Olduvai Gorge, Koobi Fora, and Sterkfontein, suggesting that it was a pan-African synchronous phenomenon, beginning at 1.5 m.y.a.     

安徽省宁国市安友庄旧石器遗址调查及发掘简报

2003-2004年,安徽省文物考古研究所对地处水阳江流域的宁国安友庄遗址开展野外调查及考古发掘,发掘面积250 m²,调查采集石制品3件,发掘出土石制品49件。石制品原料以中津河（水阳江一级支流）二级阶地底部砾石层中产出的石英岩砾石为主,少量为石英。石制品类型包括石核、石片和石器。石制品均为使用硬锤直接剥片。石制品主要出自中国南方地区常见的网纹红土和均质红土中,根据长江中下游地区第四纪红土风化壳的相关研究结果,初步推断安友庄遗址古人类生存与活动的年代延续中更新世中、晚期一段时间。虽然安友庄遗址发现石制品数量不多,但其中存在模式2技术产品,如剥取大石片的大石核、长度大于或等于10 cm的大石片,以及以手斧、大型石刀等为代表的大型切割石器,特别是比较典型的两面加工手斧在水阳江流域尚不多见。安友庄遗址的发现,为进一步讨论早期人类在长江下游地区的扩散与技术发展具有重要的科学意义。     

Going big versus going small: Lithic miniaturization in hominin lithic technology

Lithic miniaturization was one of our Pleistocene ancestors' more pervasive stone tool production strategies and it marks a key difference between human and non‐human tool use. Frequently equated with “microlith” production, lithic miniaturization is a more complex, variable, and evolutionarily consequential phenomenon involving small backed tools, bladelets, small retouched tools, flakes, and small cores. In this review, we evaluate lithic miniaturization's various technological and functional elements. We examine archeological assumptions about why prehistoric stoneworkers engaged in processes of lithic miniaturization by making small stone tools, small elongated tools, and small retouched and backed tools. We point to functional differences that motivate different aspects of lithic miniaturization and several instances where archeological systematics have possibly led archeologists to false negative findings about lithic miniaturization. Finally, we suggest productive avenues by which archeologists can move closer to understanding the complex evolutionary forces driving variability in lithic miniaturization.     

The Unknown Oldowan: ~1.7-Million-Year-Old Standardized Obsidian Small Tools from Garba IV,Melka Kunture,Ethiopia

The Oldowan Industrial Complex has long been thought to have been static, with limited internal variability, embracing techno-complexes essentially focused on small-to-medium flake production. The flakes were rarely modified by retouch to produce small tools, which do not show any standardized pattern. Usually, the manufacture of small standardized tools has been interpreted as a more complex behavior emerging with the Acheulean technology. Here we report on the ~1.7 Ma Oldowan assemblages from Garba IVE-F at Melka Kunture in the Ethiopian highland. This industry is structured by technical criteria shared by the other East African Oldowan assemblages. However, there is also evidence of a specific technical process never recorded before, i.e. the systematic production of standardized small pointed tools strictly linked to the obsidian exploitation. Standardization and raw material selection in the manufacture of small tools disappear at Melka Kunture during the Lower Pleistocene Acheulean. This proves that 1) the emergence of a certain degree of standardization in tool-kits does not reflect in itself a major step in cultural evolution; and that 2) the Oldowan knappers, when driven by functional needs and supported by a highly suitable raw material, were occasionally able to develop specific technical solutions. The small tool production at ~1.7 Ma, at a time when the Acheulean was already emerging elsewhere in East Africa, adds to the growing amount of evidence of Oldowan techno-economic variability and flexibility, further challenging the view that early stone knapping was static over hundreds of thousands of years.     

The Lower Palaeolithic assemblage of Layers 15–18 (Unit G) at Hummal. An exemplary case addressing the problems placing undated,archaic-looking stone tool assemblages in the Early and Lower Palaeolithic record by techno-typological classification

The site of Hummal is situated in the region of El Kowm in central Syria. The site comprises an archaeological sequence covering the entire Pleistocene epoch, and encompasses all major Palaeolithic complexes currently known in the Middle East. At the base of the site, 14 m below today's ground level, several layers with a lithic assemblage attributed to the Lower Palaeolithic have been excavated over the past years. At present, the collection recovered from this lowest succession at Hummal contains more than 700 stone artefacts and more than 3000 bone fragments. The lithic assemblage is characterized by a simple flaking technique and the presence of different pebble tools, such as choppers, hammerstones and sphaeroids. Additionally four handaxes were recovered, which have a symmetric shape, are clearly bifacial and rather flat. The lithic assemblage from the lowermost layers of the Hummal excavation largely resembles an Archaic, Lower Palaeolithic assemblage, belonging to the so-called Oldowan or Mode 1 stage. However, the presence of well-shaped and symmetric handaxes sheds doubt on the validity of this attribution to a Mode 1, Oldowan or the Early Acheulean Stage. It can, therefore, be debated, whether the common classifications of lithic industries are adequate for describing the archaeological record from the period in question in the Middle East.     

The TD6 level lithic industry from Gran Dolina, Atapuerca (Burgos, Spain): production and use.

Technological analysis of lithic artefacts recovered at the Aurora stratum of Atapuerca-TD6 shows that this Lower Pleistocene assemblage is similar to Mode I Technology (=Oldowan tradition) documented at many African sites. Diachronic comparison of the different levels of Gran Dolina allows us to conclude that this particular form of early European technology lacks the production of big flakes to manufacture large tools such as bifaces and cleavers. Rather, it is characterized by the presence of small artefacts, including flakes, denticulates, notches, and side-scrapers, many of which bear use-wear traces of butchery and woodworking. The dominant production technique is orthogonal, which is also reflected in the core recovered at the slightly older level of TD4. The raw materials also found in the Middle Pleistocene occupations at Atapuerca, though with significant proportion differences, have a local origin and include varieties of flint, quartzite and sandstone as well as limestone and quartz. TD6 small artefacts were made from most of these, although the retouched pieces seem to have been preferentially made of the best quality flint, i.e., Cretaceous flint, pointing to the existence of differential use of lithic material, and therefore, some degree of planned knapping behaviour. Most of the "cha?nes opératoires" or reduction sequences took place inside the cave, although some artefacts, elaborated on Cretaceous flint, seem to have been retouched off site, possibly near the supply sources.     

The Early Stone Age lithic assemblages of Gadeb (Ethiopia) and the Developed Oldowan/early Acheulean in East Africa

The Early Stone Age sites of Gadeb (Ethiopian South-East Plateau) were excavated under the direction of Desmond Clark in the 1970s. Dated to between 1.45 and 0.7 Ma, Gadeb proved that humans had already occupied high altitude areas in the Lower Pleistocene. Despite the importance of the Gadeb sites, their lithic assemblages were never published in detail, and no review of the stone tools has ever been reported since the original 1970s study. This paper updates the information available on Gadeb by presenting a systematic review of the lithic technology of several assemblages. The objectives are to evaluate the technological skills of Gadeb knappers and to contextualize them into the current discussion of the origins of the Acheulean and its possible coexistence with the so-called Developed Oldowan in East Africa.     

阿舍利大石片的生产方式与策略

阿舍利技术的两个核心要素在于剥取大石片以及制作手斧等定型化大型工具。目前,国内有关手斧工业的研究中,关注较多的是大型工具的加工与制作,而对于大石片生产的方式与策略则缺乏系统的研究和介绍。本文重点介绍和综述了目前国外发现和报道的大石片生产技术,并对每种技术的具体特点进行了分析和阐释。根据剥片复杂程度的不同,阿舍利大石片生产技术可细分为三类;第一类指砾石初级剥片技术,是利用原料的自然特征,选择合适台面和剥片角度进行单次剥片;第二类包括两面剥片技术、板状石核剥片技术和昆比哇技术,是在了解原料特征的基础上,对石核进行有计划的剥片,以便连续生产出多个大石片;第三类包括奇尔基技术、塔拜勒巴拉-塔奇恩基特技术和西维多利亚技术,是在较为复杂的剥片流程引导下,通过对石核的预制,获取具有相对稳定形态的大石片。在此基础上,初步分析了广西百色盆地发现的大型石核和大石片标本,探讨其在深入认识该地区石器工业面貌方面的作用和意义。     

湖北郧县肖沟旧石器时代遗址发掘简报

肖沟遗址位于湖北省郧阳区安阳镇钟家河村,埋藏于丹江口库区汉江左岸第二级堆积阶地,遗址所在地三面环水,北靠低山。2010年10月-12月对该地点进行抢救性发掘,揭露面积近1500 m~2,出土石制品413件。石制品类型包括石器、石核、石片、断块断片和碎块碎片等。古人类利用河流砾石,就地取材加工石制品;硬锤锤击是主要剥片方法;石制品总体以小型居多,石器主要以石片为毛坯,边刮器为主要类型。石制品特点显示石片工业特点。石制品类型以石片类和断块类为主体,石制品拼合率近10%,是一处原地埋藏的古人类遗址。通过与丹江口库区相关旧石器遗址的比较,结合地貌地层特点,推测该遗址形成于旧石器时代晚期。     

洛南花石浪龙牙洞1995年出土石制品研究

1995─1997年,经过连续3年对洛南盆地花石浪龙牙洞遗址的发掘,获得20余种哺乳动物、鸟类和水生动物化石以及包括人类生活踩踏面、灰烬层、烧石、烧骨和77000余件石制品在内的大量的人类文化遗迹和遗物。本文是1995年度龙牙洞内顶部扰动层及第4层上部出土的18608件各类石制品的阶段性研究成果。研究结果显示石制品是以中小型石片和简单的石片工具为代表的旧石器时代早期文化,而龙牙洞是一处内涵丰富的早期人类居住类型遗址。     

Barogali et l’Oued Doure. Deux gisements représentatifs du Paléolithique ancien en République de Djibouti

In the Republic of Djibouti, surveys and excavations, carried out from 1985 to 1992, confirmed the presence of the pre-Acheulean (Oldowan) and Acheulean sites in the country. Three seasons of excavations (1985-1987 in the Gobaad Basin, have unearthed in a hardened compact clay strata of an ancient marshland dating to the Lower Pleistocene, the fossilized skeletal remains of an Elephas recki ileretensis. Numerous stone tools have been gathered with the bones. The E.S.R. dating the elephant’s lower third molar gave a date between 1,.6 and 1,.3 MY that would confirm its paleontological grouping and the membership of this butchery site to the Oldowan period. The animal appeared to have been lying on its left side. The cranial roof had been separated from the calvarium, perhaps to get at the brain; but the skull remains in anatomic connection with the tusks. The jaw (mandible) seems to have been broken to extract the tongue. Hominids, perhaps Homo ergaster, knapped tools from a nearly outcrop of poor quality lava. The tools were specifically adapted to their needs, such as scraping, chopping and scattering the bones. The site has yielded 569 artifacts: utilized material and hammerstones (121); pebble tools (32); cores (14); “debitage” products (366); retouched flakes (36). Artifacts are rarely retouched and often broken. Five different types of choppers have been classified. The polyedrons and one bola make up 22% of the pebble tools. The cores are divided into unipolar, centripetal and polyhedrical types. In another site, Haïdalo, an almost complete skeleton of an Elephas recki recki in anatomical connection and without any sign of predation, has been found at eight kilometers from Barogali. During surveys in the Ali Sabîh region (1990-1992) seven sectors have been discovered and prospected in the Oued Doure Basin. On the surface area and also in situ into some little pits, 345 rhiolitic Acheulean artifacts have been found, near rhyolitic outcrop. These artifacts are generally large. The choppers (18) can be dividended into 2 sets : side choppers (55%) and end choppers (27%), often with a bifacial cutting edge. There is only one polyedron, but we have found eight heavy scrapers. The Acheulean group is important (43 tools). The bifaces are varied and there are also a few cleavers and picks. Cores are numerous (92) and Levallois cores are preponderant (45%). We find also centripetal cores (27%) and so unipolar, bipolar and polyhedral cores. Tools made of flakes (118) are numerous: scrapers are typologically diversified. Some of them have a double utilization. Notch tools, denticulate tools are presents but also end scrapers, burin, borer, back knifes and scantily retouched flakes. The characters of this lithic material, large cores and big flakes, large bifaces of various types, cleavers and retouched flakes, indicates that they are Acheulean products. So, the Doure Site can be placed in the Middle / Upper Acheulean transition.     

Further evidence of a lower pleistocene arrival of early humans in northern Europe--the Untermassfeld site (Germany)

The discovery of 24 stone artifacts and two bone tools at the German fluvial site of Untermassfeld associated with a rich vertebrate fauna of the Epivillafranchian provide further evidence of a Lower Pleistocene arrival of early Homo in northern Europe, since results of geological, paleomagnetic and biostratigraphic investigations point to an absolute age of approximately 1.07 million years (ma). The typological study of the lithic artifacts is accompanied by the analysis of the mineralogical structure of the raw materials and use wear traces of simple flakes and retouched lithic fragments. Signs of thermal alteration on the surface of a stone tool may denote former exposure to fire. Hominin processing of animal resources is indicated by at least one knapped bone tool and bone surface modifications considered to be of cultural origin. Finally, lithic material from further archeological find sites of the Werra Valley associated with assumed Lower Pleistocene river sediments are discussed.