The earliest hominin occupation of Europe is one of the most debated topics in palaeoanthropology. However, the purportedly oldest of the Early Pleistocene sites in Eurasia lack precise age control and contain stone tools rather than human fossil remains. Here we report the discovery of a human mandible associated with an assemblage of Mode 1 lithic tools and faunal remains bearing traces of hominin processing, in stratigraphic level TE9 at the site of the Sima del Elefante, Atapuerca, Spain. Level TE9 has been dated to the Early Pleistocene (approximately 1.2-1.1 Myr), based on a combination of palaeomagnetism, cosmogenic nuclides and biostratigraphy. The Sima del Elefante site thus emerges as the oldest, most accurately dated record of human occupation in Europe, to our knowledge. The study of the human mandible suggests that the first settlement of Western Europe could be related to an early demographic expansion out of Africa. The new evidence, with previous findings in other Atapuerca sites (level TD6 from Gran Dolina), also suggests that a speciation event occurred in this extreme area of the Eurasian continent during the Early Pleistocene, initiating the hominin lineage represented by the TE9 and TD6 hominins.

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etween 1994 and 1996, during the excavation of a 7-m 2 test pit, a sample of Ϸ100 hominin fossil remains was found in the so-called Aurora Stratum of the stratigraphic unit TD6 of the Gran Dolina site in Sierra de Atapuerca, Burgos, northern Spain (1). The hominin remains were associated with 268 lithic artifacts made of flint, quartzite, sandstone, limestone, and quartz. This sample is characterized by the presence of small artifacts, and includes flakes, denticulates, notches, and side-scrapers and can be characterized as Mode 1 technology (2). The excavation of the Aurora Stratum also yielded a rich small mammal assemblage (26 species, including the water vole Mimomys savini) as well as Ϸ1,000 large mammal fossil remains. The study of the arvicolids suggests that the TD6 level can be referred to the Biharian biochron (3). The macromammal assemblage is biochronologically consistent with the end of the Early Pleistocene or early Cromerian (4, 5). Paleomagnetic dating places TD6 in the Matuyama reversed Chron, hence, before 780 thousand years ago (6, 7). These paleomagnetic data combined with electron spin resonance and uranium series results give an age range of between 780 and 857 thousand years for TD6 (8). Pollen analysis suggests that the Aurora Stratum was deposited under wet, temperate conditions (9); thus, the Aurora Stratum possibly correlates to oxygen isotope stages 21 or 19.In 1997, the TD6 hominins were attributed to Homo antecessor, a new European Lower Pleistocene species (10). On the basis of cranial and dental features, it was suggested that this species could be the common ancestor of modern humans (Homo sapiens) and Neandertals (Homo neanderthalensis). The new taxon was defined in part by using facial and mandibular traits observed in immature individuals. Although the TD6 remains were compared with those of individuals of the same dental age (e.g., KNM-WT 15000), it was clear that the credibility of the species would improve if new specimens corresponding to adult individuals were found. In 2003, we obtained in the Aurora Stratum an excellently preserved mandible, whose description and comparative analysis is the subject of the present study. Mandible ATD6-96Preservation and Age at Death. The specimen catalogued as ATD6-96 was recovered in a planar section of Ͻ1 m 2 , near the area excavated during the 1994-1997 field seasons (1). ATD6-96 is a left half of a gracile mandible of an adult individual (Hominid 7) with the premolars and molars in place (Fig. 1). The specimen is broken at the level of the lateral incisor-canine septum, and the left genial apophysis is preserved. Some postmortem fractures are observed at the region between the corpus and ramus and near the neck of the condyle, but there is no noticeable distortion. Molar (M)3 is fully erupted and exhibits a minimal wear facet at the mesial marginal ridge. During restoration, the corpus and ramus were separated, and the roots of the M3 were observed directly. These roots are at stage Rc of tooth formation (11). Thus, according to mo...

East Africa has provided the earliest known evidence for Oldowan stone artifacts and hominin-induced stone tool cutmarks dated to ~2.6 million years (Ma) ago. The ~1.8-million-year-old stone artifacts from Ain Hanech (Algeria) were considered to represent the oldest archaeological materials in North Africa. Here we report older stone artifacts and cutmarked bones excavated from two nearby deposits at Ain Boucherit estimated to ~1.9 Ma ago, and the older to ~2.4 Ma ago. Hence, the Ain Boucherit evidence shows that ancestral hominins inhabited the Mediterranean fringe in northern Africa much earlier than previously thought. The evidence strongly argues for early dispersal of stone tool manufacture and use from East Africa or a possible multiple-origin scenario of stone technology in both East and North Africa.

The Resource Dependence Institutional Cooperation (RDIC) model was constructed from four combined theories: network, organizational behavior, resource dependence, and new institutional. The authors developed the model in an effort to better understand cooperation in public health settings, and tested its validity in two different types of networks related to occupational health. Two qualitative studies were performed in the Netherlands. The first study included 11 respondents dealing with the sickness absence of 4 employees. The second study included 11 respondents from 5 organizations involved in developing sickness absence policy. Document analyses and semistructured interviews were performed. The results indicate that the RDIC model coincided with empirical patterns of cooperation in both types of networks. Though they recommend further empirical research, the authors conclude that the model appears to be a valid instrument for understanding cooperation. They assert that the RDIC model can facilitate the management of cooperation in various public health settings.

Over the last two decades, the Pleistocene sites of the Sierra de Atapuerca (Spain) have provided two extraordinary assemblages of hominin fossils that have helped refine the evolutionary story of the genus Homo in Europe. The TD6 level of the Gran Dolina site has yielded about one hundred remains belonging to a minimum of six individuals of the species Homo antecessor. These fossils, dated to the end of the Lower Pleistocene (800 kyr), provide the earliest evidence of hominin presence in Western Europe. The origin of these hominins is unknown, but they may represent a speciation event from Homo ergaster/Homo erectus. The TD6 fossils are characterized by a significant increase in cranial capacity as well as the appearance of a “sapiens” pattern of craniofacial architecture. At the Sima de los Huesos site, more than 4,000 human fossils belonging to a minimum of 28 individuals of a Middle Pleistocene population (ca. 500–400 kyr) have been recovered. These hominins document some of the oldest evidence of the European roots of Neanderthals deep in the Middle Pleistocene. Their origin would be the dispersal out of Africa of a hominin group carrying Mode 2 technologies to Europe. Comparative study of the TD6 and Sima de la Huesos hominins suggests a replacement model for the European Lower Pleistocene population of Europe or interbreeding between this population and the new African emigrants.

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