Early Humans at the eastern gate of Europe: The discovery and investigation of Oldowan sites in northern Caucasus

This article presents the results of excavations and multidisciplinary investigations of the extraordinary Oldowan site of Muhkai II in the northern Caucasus (Republic of Dagestan, Russia) from 2008 to 2012. Archaeological and palaeontological materials are summarized together with data from palaeomagnetic and palynological analyses, obtained from 34 cultural layers at the site. This gives an opportunity for a new approach to the question of the timing and route of the first human settlement of the middle latitudes of western Eurasian, including south-eastern Europe. Judging by the data obtained, this occurred around 2 million years BP and a route of migration was located along the western shore of the Caspian Sea.     

Planktic foraminiferal biostratigraphy of theMaastrichtian sedimentary beds at Ain Mdeker,northeastern Tunisia

Maastrichtian Foraminifera from the sedimentary beds at Ain Mdeker are recorded and identified. The fauna examined is found to be clearly Tethyan in composition. On the basis of this fauna, four planktic foraminiferal zones, the Globotruncana falsostuarti Zone, the Rugotruncana gansseri Zone, the Abathomphalus mayaroensis Zone and the Globotruncana falsocalcarata Zone are distinguished in the Maastrichtian of the sequence studied. These zones are futher compared with the zones established in equivalent strata in the sequence at El Kef, the most complete sequence in Tunisia. In addition to the index species only the biostratigraphically most important species from the fauna studied are illustrated.     

The Oldowan site Aïn al Fil (El Kowm,Syria) and the first humans of the Syrian Desert

At present, the oldest traces of human cultures are found in Eastern Africa. New discoveries set anew the questions about human and animal dispersal into Eurasia. For over 1.8 million years, humans have been present in the Levant. An extensive program of surveys and excavations in the Syrian Desert showed that this part of the world was a very ancient land of settlement. In Central Syria, the oldest site, Aïn al Fil in the region of El Kowm, was excavated in 2008 and 2010. The lithic industry in the lowest layer can be characterized by numerous unretouched flakes, pebble-tools and core-like artefacts. This assemblage is typical in a broad sense of archaic Palaeolithic the debitage of which corresponds to mode 1. From a techno-typological point of view, this industry tallies quite well with the so-called Oldowan stage. It shows remarkable similarities with the oldest African assemblages. From a chronologic point of view, these levels occur before three positive events in the Matuyama paleomagnetic sequence. It seems consistent to place the Oldowan sequence around 1.8 Ma BP within the Olduvai subchron or just before Olduvai/Matuyama reversal limit. Together with those of the neighbouring site Hummal, these levels would be the oldest traces of human presence ever found in Syria. In the Levant, the first humans not only occupied favourable zones but regularly ventured deep into less welcoming environments suggesting an astonishing flexibility in their behavioural and survival skills.     

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.     

广西田东中山遗址洞外岩厦出土动物骨骼的初步研究

对广西田东中山遗址洞外岩厦出土动物骨骼遗存的研究表明,该批动物遗存至少代表39个属种。中山遗址原始居民以此地作为居住地,会到远处进行狩猎,其生业模式以狩猎为主;对骨骼的利用尚处在初级阶段,未发现精细的加工方式。动物骨骼遗存均来自野生动物,原始居民未开始饲养家畜。当时的中山遗址地处以林缘灌丛、低山森林景观为主的山间盆地中,不远处有成片的草地,并分布着一定面积的水域。这些信息对探讨中国华南地区旧石器时代晚期至新石器时代早期人类的生存行为、生境状况及演化特征等具有重要意义。     

The Oldowan site of Muhkai II,layer 80 (northeastern Caucasus): Spatial structure and cultural and chronological attribution of the lithic assemblage

In 2004–2006 a group of Lower Palaeolithic sites was discovered in the northeastern Caucasus: Ainikab I–VI, Gegalashur I–III and Muhkai I–II. Since then, they have been the subject of comprehensive scientific investigations. One site which is undergoing active research is the multilayered site of Muhkai II. Multiple cultural layers at the site have been found in a 73 m thick sequence of Early Pleistocene sediments. The geological age of the layers encompasses the interval 2.1–0.8 million years ago, or the majority of the Early Pleistocene. Layer 80 of Muhkai II is located in the central part of the section at a depth of −33.6 to −34.0 m. Its significance lies in the fact that the site contains two cultural layers–the upper and the lower (main)–that are preserved in situ or have been subject to minimal fluvial processes. The finds consist of lithic artefacts and osseous faunal remains. According to field observations and microstratigraphic analyses, the cultural layers can be characterised as the ancient surfaces of an occupation area. Two stages of occupation can be defined in the lower cultural layer. Layer 80 of Muhkai II was a periodically visited location at the banks of a waterbody, where the acquisition and butchery of large mammals took place. The faunal collection contains 301 bones, deriving from four carnivorous and six herbivorous species of mammals. The total lithic collection contains 1094 finds. According to typological and technological criteria the lithic assemblage relates to the Oldowan and has analogies with Oldowan sites in Africa (particularly with sites of the Olduvai Gorge as well as others). At the same time, some specifics of the lithic assemblage reflect the uniqueness of the site and its functional type. Layer 80 of the Muhkai II site is estimated to date to within the chronological interval ∼2.1–1.7 mya.     

泥河湾盆地南山边遗址发现的旧石器

南山边遗址位于泥河湾盆地东缘、大田洼台地北缘,于2013年的旧石器调查中发现。随后的试掘中,出土石制品38件,动物化石3件,石制品包括石核、石片、刮削器、残片、断块等,属于中国北方以小石制品为主的主工业类型。石制品位于泥河湾层中下部,根据地层对比,与大长梁地点、小长梁遗址、照坡遗址、葡萄园遗址等属于同一层位,时代相同,由此在台地北缘形成一处面积广阔、时代接近、分布集中的遗址区,为探讨早更新世古人类的活动范围、栖居模式、遗址功能分析等提供有益线索。     

Geological summary of the Busidima Formation (Plio-Pleistocene) at the Hadar paleoanthropological site, Afar Depression, Ethiopia

The Hadar paleoanthropological site in Ethiopia preserves a record of hominin evolution spanning from approximately 3.45 Ma to 0.8 Ma. An angular unconformity just above the ca. 2.95 Ma BKT-2 complex divides the sediments into the Hadar Formation (ca. 3.8-2.9 Ma) and the Busidima Formation (ca. 2.7-0.15 Ma). The unconformity is likely a response to a major tectonic reorganization in the Afar Depression, and activation of the As Duma fault near the Ethiopian Escarpment (west of Hadar) created a half-graben in which the Busidima Formation was deposited. The pattern and character of sedimentation in the region changed dramatically above the unconformity, as cut-and-fill channel conglomerates and silt-dominated paleosols that comprise the Busidima Formation stand in sharp contrast to the underlying deposits of the Hadar Formation. Conglomerate deposition has been related to both the perennial, axial paleo-Awash and ephemeral, escarpment-draining tributaries. Overbank silts have yielded fossils attributed to early Homo and Oldowan stone tools. Numerous tuffaceous deposits exist within the Busidima Formation, but they are often spatially limited, fine-grained, and reworked. Recent work on the tephrostratigraphic framework of the Busidima Formation at Hadar has identified at least 12 distinct vitric tephras and established the first geochemical-based correlations between Hadar and the neighboring project areas of Gona and Dikika. Compared to Gona and Dikika, where Busidima Formation sediments are exposed over large areas, the highly discontinuous sediments at Hadar comprise less than 40 m in composite section and are exposed over an area of <20 km², providing only snapshots into the 2.7-0.15 Ma window. The stratigraphic record at Hadar confirms the complex depositional history of the Busidima Formation, and also provides important details on regional stratigraphic correlations and the pattern of deposition and erosion in the lower Awash Valley reflective of its tectonic history.     

History of American paleoanthropological research on early Hominidae, 1925–1980

Understanding of the early stages of hominid evolution prior to 1925 was based primarily on comparative morphological evidence derived from extant primates. With the publication of Australopithecus by Dart in 1925 and subsequent research in South Africa, new possibilities for empirical assessment of early hominid evolutionary history were opened. It was Gregory's work, with Hellman, reported at the first meeting of the AAPA in 1930, that convinced many workers of the hominid status of Australopithecus. The debunking of Eoanthropus as a Pliocene hominid, far from having a totally negative effect, showed that cranial expansion had occurred after bipedalism in hominid evolution, demonstrated that chemical dating had come of age, and in a broader sense, had underlined that phylogenetic hypotheses are falsifiable by recourse to the evidence. The input of biological sciences into early hominid studies, as exemplified by Washburn's “new physical anthropology,” reduced taxonomic diversity and focused attention on paleoecology and behavior. The development of the multidisciplinary approach to field research, pioneered by L. Leakey and brought to fruition by Howell, was of fundamental importance in accurately dating and understanding the context of early hominids. Archaeology, primatology, comparative and functional morphology, and morphometrics have contributed substantially in recent years to a fuller understanding of early hominid evolution. American granting agencies have heavily supported early hominid research but patterns of funding have not kept pace with the change from research based largely on individualistic enterprise to multidisciplinary research projects. Future early hominid research, if funding is available, will likely be directed toward investigating temporal and geographic gaps now known in the fossil record and in more rigorous and multidisciplinary investigations of early hominid behavior.     

Depositional environments, archeological occurrences and hominids from Members E and F of the Shungura Formation (Omo basin, Ethiopia)

The several known archeological occurrences from the Shungura Formation (Members E and F) are discussed within the context of their particular depositional and paleoenvironmental settings, and the broader context of the Pliocene of the Turkana Basin. These assemblages date from 2·3–2·4 Ma, and are among the oldest yet known in Africa. In situ archeological assemblages are restricted to the distal edge of fluviatile levees, behind gallery forests and at the edge of open savanna. Extensive and rather dense scatters of slightly disturbed quartz artifacts are linked to large expanses of braided stream situations. Lag components are derived from stream beds. There is no available evidence of occupation either under riverine or deltaic forest settings or on dryland. Hominid skeletal remains from this interval, none of which occur at or are directly associated with such archeological occurrences, are attributed to two hominid taxa. Most specimens represent a “robust” australopithecine and are attributed here to A. aethiopicus. A few hominid teeth are attributed to aff. Homo sp.     

百色盆地六林岭旧石器遗址试掘报告

本文是对2018年广西百色六林岭旧石器遗址试掘结果的报道。试掘共开7个探方（面积28 m²）和1条探沟,可见9层堆积,从两个层位共获得石制品182件（其中地层出土40件,采集142件）。虽然两个文化层石制品在埋藏和保存状况上存在明显差异,但属于同一个技术传统。石制品分为备料、石锤、石核、石片、断块和石器;石器包括砍砸器、手镐和刮削器。在第一文化层发现了与石制品伴生的玻璃陨石碎片,初步推测其年代为803 kaBP,尚不排除二次堆积的可能;第二文化层在第一文化层之下,年代要早于第一文化层,表明古人类在百色盆地持续活动了相当长的一段时间;两个文化层显示出不同的沉积环境,表明古人类在百色盆地生存环境的复杂性和多样性。     

The fauna and associated artefacts from the Lower Pleistocene site of Mansourah (Constantine, Algeria)

The site of Mansourah (Constantine, Algeria) had yielded to the early authors, and more recently to the late G. Laplace, a lithic industry associated with a fauna of large Mammals, which looks contemporaneous with that of Aïn Hanech, although it is well-distinct ecologically, and might even be slightly older. The lithic assemblage is completely devoid of any bifacial artefact or cleaver and can only be referred to the Oldowan. Thus, the Mansourah site documents a very early human occupation of North Africa, and perhaps one of the earliest. To cite this article: Y. Chaid-Saoudi et al., C. R. Palevol 5 (2006).     

河北阳原泥河湾盆地籍箕滩遗址发现的新材料

河北阳原泥河湾盆地的籍箕滩旧石器时代晚期旷野遗址群于上世纪80年代被发现并系统发掘,目前,曾出土了丰富的细石叶制品及动物碎骨的第2地点(T2)由于后期工程建设的原因已不复存在,原记录中的第1地点(T1)、第3地点(T3)也均受到了不同程度的人为破坏或自然力侵蚀。为探明遗址堆积保存状况,工作队对遗址第1、3地点进行了复查及剖面清理,分别发现了密度较大的石制品遗存。对第1地点和第3地点的光释光和¹⁴C测年结果表明,该地有人类活动遗迹的堆积物形成年代为距今16000余年至全新世初期,与河对岸虎头梁遗址群中的马鞍山、于家沟相当,表明了当时古人类的活动范围同时覆盖了桑干河南北两岸。     

Emergence pattern,site selection,and seasonal regulation of Onychogomphus costae Selys, 1885 (Odonata: Gomphidae) in northeastern Algeria

Emergence and seasonal regulation of the dragonfly Onychogomphus costae Selys, 1885, were surveyed thoroughly during two consecutive years from two nearby stretches upstream the Seybouse River, northeastern Algeria. The emergence season started in mid-May and lasted 68 and 58 days showing a peak in late May and early June in 2011 and 2012, respectively. During the two years 2011 and 2012, 50% of annual emergence occurred after 25 and 22 days, respectively. Sex ratio was slightly but not significantly male biased. Female exuviae were recorded at higher height than males. Height of the exuviae fixation was positively correlated to support height and head width. Percentage mortality at emergence was mainly due to deformity and predation counting from 7.9% to 9.15% of the total emergent population. The species seasonal regulation is inferred and discussed based on the emergence temporal pattern and larval development.     

周口店第一地点西剖面2009-2010年发掘报告

周口店第一地点再次发掘的主要目的在于提升遗址西剖面的保护状态与水平,同时也为东亚直立人演化方面某些焦点问题的研究与解决提供机遇与可能。2009-2010年,在西剖面最顶部堆积(即第三层)的野外发掘中共计出土大中型动物化石材料约800件。埋藏学研究表明,西剖面第三层中葛氏斑鹿(Cervus(Sika)grayi)等动物属种的骨骼富集并非古人类生存行为的结果;石制品以及古人类化石材料的缺失也在一定程度上印证了这一结论。结合发掘过程中揭露出来的一系列洞穴坍塌事件的证据,我们初步认为,至少在第三层堆积形成时期,第一地点西剖面位置处的洞穴形态并不适合于古人类的栖居活动;葛氏斑鹿等骨骼材料则是当时在遗址附近活动的各种动物因意外因素陷落于其中而得以聚集的。