A unique human-fox burial from a pre-Natufian cemetery in the Levant (Jordan)

New human burials from northern Jordan provide important insights into the appearance of cemeteries and the nature of human-animal relationships within mortuary contexts during the Epipalaeolithic period (c. 23,000-11,600 cal BP) in the Levant, reinforcing a socio-ideological relationship that goes beyond predator-prey. Previous work suggests that archaeological features indicative of social complexity occur suddenly during the latest Epipalaeolithic phase, the Natufian (c. 14,500-11,600 cal BP). These features include sedentism, cemeteries, architecture, food production, including animal domestication, and burials with elaborate mortuary treatments. Our findings from the pre-Natufian (Middle Epipalaeolithic) cemetery of 'Uyun al-Hammam demonstrate that joint human-animal mortuary practices appear earlier in the Epipalaeolithic. We describe the earliest human-fox burial in the Near East, where the remains of dogs have been found associated with human burials at a number of Natufian sites. This is the first time that a fox has been documented in association with human interments pre-dating the Natufian and with a particular suite of grave goods. Analysis of the human and animal bones and their associated artefacts provides critical data on the nature and timing of these newly-developing relationships between people and animals prior to the appearance of domesticated dogs in the Natufian.     

Musculoskeletal stress markers in Natufian hunter-gatherers and Neolithic farmers in the Levant: the upper limb

This paper attempts to quantify the changes in activity patterns of early farming populations in the Levant through the musculoskeletal stress markers (MSM) of the upper limb as seen in skeletal remains. The transition to an agricultural way of life resulted in higher loads on the upper limb in Neolithic populations compared to the Natufian hunter-gatherer populations that preceded them. The MSM pattern for males and females indicates a gender-based division of labor both in the Natufian and the Neolithic. It may also suggest that people in the Neolithic period were engaged in different (new) activities and occupations compared to the Natufian.     

Increasing the resolution of the Broad Spectrum Revolution in the Southern Levantine Epipaleolithic (19-12 ka)

We analyze terminal Pleistocene archaeofaunal diversity trends in the Southern Levant by examining eight Epipaleolithic (ca. 19-12 ka) assemblages from the Western Galilee/Mt. Carmel, Israel subregion. We test predictions from a Broad Spectrum Revolution model of the population dynamics of human foragers and their prey. The study emphasizes control over geographic variability and archaeological recovery and recording methods, as we analyze a time series that samples the Epipaleolithic more fully than have previous studies. This provides a new opportunity to examine human population and economic change in the long-term transition to sedentism and agriculture.We use the Mantel test to evaluate the significance of temporal trends in body-size-based big game diversity, as well as in diversity of small game prey types. Results demonstrate a highly significant decline through time in the relative abundance of medium and large big game, measured relative to small big game. This suggests that the apparent “gazelle specialization” by Late Epipaleolithic (Natufian) hunters reflects longer-term anthropogenic overexploitation of the largest prey types in the spectrum. While large and medium big game abundance declined, our results show small game increased in economic importance over time.Considered with associated climate change data, the results provide substantial support for the hypothesis that local human populations expanded rapidly in size after the Last Glacial Maximum (LGM). We suggest that following the post-LGM population pulse, human foragers adopted a shifting series of intensification strategies mediated by changes in residential mobility.     

The pre-Natufian Epipaleolithic: long-term behavioral trends in the Levant

Few cultural developments have taken on as much archeological significance as when people began living in villages and producing their own food. The economic, social, technological, and ideological transformations immediately preceding and following these changes were profound. Early models of culture change associated with pre-agricultural societies of the Levant focused on the sudden, late origin of settled farming villages triggered by climate change. Accompanying this new economic and living situation was durable stone-built architecture; intensified plant and animal use; a flourishing of art and decoration; new mortuary traditions, including marked graves and cemeteries; elaborate ritual and symbolic behavior-a new way of life. This new life style arguably had a slow start, but really took off during the Epipaleolithic period (EP), spanning more than 10,000 years of Levantine prehistory from c. 23,000-11,500 cal BP. The last EP phase, immediately preceding the Neolithic, is by far the best-studied in terms of its cultural and economic contributions to questions on the origins of agriculture.1-4 Recently, archeologists have considered the earlier parts of the EP to be more culturally dynamic and similar to the later phase (Natufian) than was previously thought.3-10 The earlier EP is increasingly seen as demonstrating the behavioral variability and innovations that help us to understand the economic, technological, and social changes associated with complex hunter-gatherers of the Natufian and farmers of the Neolithic. This paper traces the cultural and biological developments of the EP period leading up to the Natufian and considers the long-term trajectory of culture change, social complexity, and village life in the Near East.     

Bioarchaeological analysis of cultural transition in the southern Levant using dental nonmetric traits

To many Near Eastern archaeologists, the Late Bronze Age-Early Iron Age transition in the southern Levant indicates the emergence of a new ethnicity. The question remains, however, whether changes in the material culture are the result of an invasion of foreigners, or instead arose from shifting cultural and technical practices by indigenous peoples. This study utilized dental morphological traits to assess phenetic relationships between the Late Bronze Age site of Dothan (1500-1100 BC) and the Iron Age II site of Lachish (Tell ed-Duweir, 701 BC). Information on 30 dental crown and root traits was collected for 4,412 teeth, representing 392 individuals from Lachish and a minimum of 121 individuals from Dothan, using the Arizona State University Dental Anthropology System. Seventeen traits from Dothan and Lachish were compared with dentitions from a Byzantine Jerusalem monastery, Iron Age Italy, a Natufian group (early agrarians from the Levant), and a Middle Kingdom Egyptian site using C.A.B. Smith's mean measure of divergence statistic. The findings suggest that there are more similarities between Dothan and Lachish than either of them and other sites. This analysis indicates that the material culture changes were not the result of a foreign invasion. Rather, the Iron Age people of the southern Levant were related to their Bronze Age predecessors.     

Tooth wear and dental pathology at the advent of agriculture: new evidence from the Levant

Differences in patterns of diet and subsistence through the analysis of dental pathology and tooth wear were studied in skeletal populations of Natufian hunter-gatherers (10,500-8300 BC) and Neolithic populations (8300-5500 BC, noncalibrated) from the southern Levant. 1,160 Natufians and 804 Neolithic teeth were examined for rate of attrition, caries, antemortem tooth loss, calculus, periapical lesions, and periodontal processes. While the Natufian people manifest a higher rate of dental attrition and periodontal disease (36.4% vs. 19%), Neolithic people show a higher rate of calculus. Both populations manifested low and similar rates of caries (6.4% in the Natufian vs. 6.7% in the Neolithic), periapical lesions (not over 1.5%), and antemortem tooth loss (3.7% vs. 4.5%, respectively). Molar wear pattern in the Neolithic is different than in the Natufian. The current study shows that the dental picture obtained from the two populations is multifactorial in nature, and not exclusively of dietary origin, i.e., the higher rate and unique pattern of attrition seen in the Natufian could result from a greater consumption of fibrous plants, the use of pestles and mortars (which introduce large quantities of stone-dust to the food), and/or the use of teeth as a "third hand." The two major conclusions of this study are: 1) The transition from hunting and gathering to a food-producing economy in the Levant did not promote changes in dental health, as previously believed. This generally indicates that the Natufians and Neolithic people of the Levant may have differed in their ecosystem management (i.e., gathering vs. growing grains), but not in the type of food consumed. 2) Changes in food-preparation techniques and nondietary usage of the teeth explain much of the variation in tooth condition in populations before and after the agricultural revolution.     

Epipaleolithic human appendicular remains from Ein Gev I,Israel

The Upper Paleolithic (Early Epipaleolithic/Kebaran; ∼ 19,000 cal BP) human skeleton, from Layer 3 of Ein Gev I on the western flanks of the Golan Heights adjacent to the Sea of Galilee, retains sufficient limb remains to permit assessment of its body size and proportions, as well as diaphyseal reflections of skeletal hypertrophy. The individual was of modest stature but average mass for a later Upper Paleolithic individual, providing it with the body mass-to-stature body proportions characteristic of later Upper Paleolithic and more recent circum-Mediterranean humans. The humeri exhibit unexceptional diaphyseal asymmetry and robustness for an Upper Paleolithic human, and the femur exhibits similar relative diaphyseal hypertrophy. The humeral midshafts are relatively round, but the femoral and tibial midshafts are pronounced anteroposteriorly. As such, Ein Gev 1 provides additional paleobiological data on the appendicular remains of these Southwest Asian humans prior to the increasing sedentism of the terminal Pleistocene.     

Twenty thousand-year-old huts at a hunter-gatherer settlement in eastern Jordan

Ten thousand years before Neolithic farmers settled in permanent villages, hunter-gatherer groups of the Epipalaeolithic period (c. 22-11,600 cal BP) inhabited much of southwest Asia. The latest Epipalaeolithic phase (Natufian) is well-known for the appearance of stone-built houses, complex site organization, a sedentary lifestyle and social complexity--precursors for a Neolithic way of life. In contrast, pre-Natufian sites are much less well known and generally considered as campsites for small groups of seasonally-mobile hunter-gatherers. Work at the Early and Middle Epipalaeolithic aggregation site of Kharaneh IV in eastern Jordan highlights that some of these earlier sites were large aggregation base camps not unlike those of the Natufian and contributes to ongoing debates on their duration of occupation. Here we discuss the excavation of two 20,000-year-old hut structures at Kharaneh IV that pre-date the renowned stone houses of the Natufian. Exceptionally dense and extensive occupational deposits exhibit repeated habitation over prolonged periods, and contain structural remains associated with exotic and potentially symbolic caches of objects (shell, red ochre, and burnt horn cores) that indicate substantial settlement of the site pre-dating the Natufian and outside of the Natufian homeland as currently understood.     

New age constraints on the Middle Stone Age occupations of Kharga Oasis, Western Desert, Egypt

Spring-deposited carbonate rocks, or tufas, exposed along the flanks of the Libyan Plateau near Kharga Oasis, Western Desert, Egypt, can provide a directly datable stratigraphic context for Middle Stone Age/Middle Paleolithic (MSA/MP) archaeological material, if such material can be found in situ within tufa strata. Two such localities (Mata'na Site G and Bulaq Wadi 3 Locus 1) described by Caton-Thompson were revisited and sampled for uranium-series analysis. At Mata'na Site G (KH/MT-02), Middle Stone Age ("Upper Levalloisian") material is underlain by tufa with a uranium-series age of 127.9+/-1.3 ka, and overlain by tufa with an age of 103+/-14 ka. At Bulaq Wadi 3 Locus 1, a uranium-series age of 114.4+/-4.2 ka on tufa capping a small collection of Middle Stone Age artifacts also provides a minimum age constraint on that material. Tufa underlying an MSA workshop (KH/MD-10) indicates that this assemblage, characterized by use of several Levallois reduction methods, was deposited after approximately 124 ka. Furthermore, uranium-series ages averaging approximately 133 ka on a Wadi Midauwara tufa (WME-10) without associated archaeological material suggest that one period of spring flow in the region began during the Marine Isotope Stage 6/5e transition, prior to the warmest portion of the last interglacial period. The dated archaeological material suggests that the distinction that has been identified between Nubian and non-Nubian complexes in the Nile Valley may hold for the Western Desert, although local complexity has yet to be fully described.     

8000 year-old human remains on the sea floor near Atlit,Israel

Our knowledge of prehistoric fishermen in the Eastern Mediterranean area is very scanty since most of the ancient coastal settlements are today inundated by the sea. The present paper describes and analyzes the human remains revealed and excavated in the 8,000 year-old submerged site at Atlit-Yam, Israel. The skeletal material indicates extensivce marine activities among the inhabitants of the village, including deep sea fishing, diving and fishnet production. The morphological similarity to the nearby Natufian population (Nahal Oren) points to population continuity in the region. The possibility of seafaring and relationships to pupulations of major mediterranean islands is also discussed.     

Sex determination of adolescent skeletons using the distal humerus

Accurate determination of the sex of immature skeletal remains is difficult in the absence of DNA, due to the fact that most sexually dimorphic features of the human skeleton develop as secondary sex characteristics during adolescence. Methods of assessment of adult skeletons cannot reliably be applied to adolescent skeletons because of the transitional nature of the skeleton at puberty and the variability of the adolescent growth spurt. The purpose of this work was to evaluate the accuracy of Rogers's method of morphological sex determination using the distal humerus (Rogers: J Forensic Sci 44 ( 1999 ) 55–59) to assess the sex of adolescent skeletons. The sample consists of 7 documented adolescent skeletons from the Christ Church Spitalfields collection at the British Museum of Natural History and 35 from the Luis Lopes skeletal collection housed in the National History Museum (Museu Bocage) of the University of Lisbon, Portugal. Ages range from 11 to 20 years. The technique achieved an accuracy of 81% on the combined sample of 42. This method can be applied to adolescent skeletons once the trochlea begins fusing to the humeral diaphysis, which occurred by age 11 years in the test samples. Am J Phys Anthropol 2009. © 2009 Wiley‐Liss, Inc.     

The Early Middle Palaeolithic lithic industry of Dederiyeh Cave,Northwest Syria

The Lower-to-Middle Paleolithic transition of the Levant has attracted much attention, particularly because the early Middle Paleolithic is the period when the earliest anatomically modern humans fossils known to date in Eurasia have been attested in that part of Asia . The associated lithic assemblages are a significant source of information for investigating the cultural landscape of this important transition. This paper presents a new dataset from the 2003–2009 excavations at Dederiyeh Cave, northwest of Syria. A techno-typological analysis of the lithic industry reveals a common practice of blade blank production, which corroborates the other known early Middle Paleolithic assemblages of the Levant. However, its strong emphasis on Levallois core reduction and sidescraper manufacturing is noteworthy. The significance of this finding deserves further research from multiple viewpoints, including the functional and spatio-temporal variability of hominin activities in this period. It will be also important to interpret the techno-typological diagnostics of the early Middle Paleolithic assemblage of Dederiyeh considering its geographic location at the northern end of the Levant, distant from the previously known sites in the central and southern Levant.     

A historic biogeography of the aquatic fauna of the Levant

The historic biogeography of the aquatic fauna of the Levant is reconstructed upon evidence of the gastropod groups with a well-established taxonomy and a rich fossil record. Faunal origins include ancient northern elements coming from an Anatolian–Iberian faunal province that, in the early Miocene, bypassed mainland Italy. This scenario is more plausible than the current 'Lago Mare' biogeographical theory. Palaeotropical elements represent either an Oriental or an African source; in either case these elements could have first reached Anatolia, from where they eventually spread southwards into the Levant, perhaps broadly coinciding in time with the invasion of the northern elements. Within the Levant, the faunas of the Euphrates, Orontes, and Jordan formed at first one common pool, but by 2 Mya the fauna of the Jordan had diverged from that of the Orontes; later, the Orontes fauna diverged from that of the Euphrates. By 1.4 Mya the fauna of the Levant consisted of both ancient survivors and new species. Some 780 000 years ago there was an exceptionally diversified fauna with many new, northern elements. Many of these elements did not survive to recent times. The fossil record suggests that the fauna of the Jordan Valley was separate from that of the Orontes throughout the Pliocene–Pleistocene. Taxa common today to the Jordan Valley and coastal sites may reflect an ancient system of rivers that drained westwards to the Mediterranean Sea, across the Jordan Valley of today.  © 2007 The Linnean Society of London, Biological Journal of the Linnean Society , 2007, 92 , 625–639.     

The role of western Asia in modern human origins.

Western Asia provides the best collection of human skeletal remains relevant to the two basic models for the emergence of modern humans, namely the 'rapid replacement' and the 'regional continuity' models. Regardless of the taxonomies of particular hominids, their chronology is of crucial importance. Thermoluminescence (TL) and electron spin resonance (ESR) dates demonstrate that the Acheulo-Yabrudian and Mousterian entities and their associated fossils (Zuttiyeh, Tabun, Skhul, Qafzeh, Kebara, Shanidar, Amud) span the late Middle and Upper Pleistocene period. These new dates initiated major chronological revisions and renewed discussion of the cultural-archaeological implications. One of the most important conclusions is that the Middle to Upper Palaeolithic transition (or Revolution) 45-40 ka ago has nothing to do with the appearance of anatomically early modern humans in western Asia, which occurred some 100 ka ago or more. The Levant, the coastal region of the eastern Mediterranean, was both a corridor for movement of humans and animals as well as a refugium during climatically harsh periods. The mixture of morphological characteristics among the available Middle Palaeolithic human fossils is interpreted as reflecting the presence of immigrant and local populations. Archaeologically observable behavioural changes are taken as hints to the pre-adaptations of the Middle to Upper Palaeolithic revolution. The archaeological record of western Asia can contribute significantly to explaining the Middle to Upper Palaeolithic revolution. This region was the core area where the 'Neolithic Revolution' took place. The shift to systematic cultivation and the domestication of animals occurred within a short time.(ABSTRACT TRUNCATED AT 250 WORDS)     

Paleopathology and the origin of agriculture in the Levant

This study addresses changes in health which were consequential to the Neolithic transition in the southern Levant, judged on the basis of the study of specific and nonspecific stress indicators, trauma, and degenerative joint disease in 200 Natufian (hunter‐gatherer) skeletons (10,500–8300 BC) and 205 Neolithic (agricultural) skeletons (8300–5500 BC) from the southern Levant. The comparison of the health profiles of pre‐Neolithic (Natufian) and Neolithic populations reveals a higher prevalence of lesions indicative of infectious diseases among the Neolithic population, and an overall reduction in the prevalence of skull trauma among males. No change over time was observed in the prevalence of degenerative joint disease. These results indicate that in the southern Levant the Neolithic transition did not simply lead to an overall deterioration in health but rather resulted in a complex health profile which was shaped by 1) an increase exposure to disease agents, 2) changes in diet, 3) population aggregation in larger and denser settlements, 4) changes in activity patterns and the division of labor, and possibly 5) a higher resistant immunological system and response capacity to environmental aggressions (mainly infections). Am J Phys Anthropol 143:121–133, 2010. © 2010 Wiley‐Liss, Inc.     

Comparative ossification sequence and skeletal development of the postcranium of palaeognathous birds (Aves: Palaeognathae)

Palaeognaths constitute one of the most basal lineages of extant birds, and are also one of the most morphologically diverse avian orders. Their skeletal development is relatively unknown, in spite of their important phylogenetic position. Here, we compare the development of the postcranial skeleton in the emu (Dromaius novaehollandiae), ostrich (Struthio camelus), greater rhea (Rhea americana) and elegant crested‐tinamou (Eudromia elegans), focusing on ossification. All of these taxa are characterized by element loss in the appendicular skeleton, but there are several developmental mechanisms through which this loss occurs, including failure to chondrify, failure to ossify and fusion of cartilages prior to ossification. Further evidence is presented here to support a reduction in size of skeletal elements resulting in a delay in the timing of ossification. This study provides an important first look at the timing and sequence of postcranial ossification in palaeognathous birds, and discusses the influence of changes in the pattern of skeletal development on morphological evolution.     

A reconsideration of “Races” and their impact on the origins of the Chalcolithic in the Levant using available anthropological and archaeological data

Populations of the Chalcolithic Levant as defined by archaeological excavations has in many cases reinforced the traditional scheme that a number of “races” are present. This scheme is usually based not only on differential cultural traditions as identified by archeologists, but also on the available skeletal evidence as discussed by physical anthropologists. Recently this view has been challenged and it has been suggested that the metrical and anatomical range of variability as identified within Chalcolithic populations can be subsumed into a single population or “racial” range. This paper examines both the available biological and archaeological evidence from the Chalcolithic Levant and concludes that there is no strong archaeological or biological evidence to support a multiple “racial” origin for the Chalcolithic of the Levant.     

Has the transition to agriculture reshaped the demographic structure of prehistoric populations? New evidence from the Levant

This paper presents the demographic changes that followed the transition from a hunting-gathering way of life (Natufian) to an agricultural, food-producing economy (Neolithic) in the southern Levant. The study is based on 217 Natufian (10,500-8,300 BC) skeletons and 262 Neolithic (8,300-5,500 BC) skeletons. Age and sex identification were carried out, and life tables were constructed. A five-parameter competing hazard model developed by Siler ([1979] Ecology 60:750-757) was used to smooth life-table data. No indication of increased mortality with the advent of agriculture was noted. On the contrary, both life expectancy at birth (24.6 vs. 25.5 years) and adults' mean age at death (31.2 vs. 32.1 years) increased slightly from the Natufian to the Neolithic period (assuming stationary populations). Yet the transition to agriculture affected males and females differently: mean age at death in the Natufian was higher for adult females compared to adult males, while in the Neolithic, it was the reverse. One interpretation given to the distribution of female ages at death is that with the onset of the Neolithic period, maternal mortality increased as a result of a concomitant increase in fertility. If the adoption of agriculture in the Levant increased the rate of population growth at the beginning of the Neolithic, expectation of life may have increased dramatically.     

Observations of the tissue-skeleton interface in the scleractinian coral <Emphasis Type="Italic">Stylophora pistillata</Emphasis>

Recent micro-analytical studies of coral skeletons have led to the discovery that the effects of biology on the skeletal chemical and isotopic composition are not uniform over the skeleton. The aim of the present work was to provide histological observations of the coral tissue at the interface with the skeleton, using Stylophora pistillata as a model, and to discuss these observations in the context of skeletal ultra-structural organization and composition. Several important observations are reported: (1) At all scales of observation, there was a precise morphological correspondence between the tissues and the skeleton. The morphological features of the calicoblastic ectoderm correspond exactly to the shape of individual crystal fiber bundles in the underlying skeleton, indicating that the calicoblastic cell layer is in direct physical contact with the skeletal surface. This is consistent with the previously observed chemical and isotopic composition of the ultra-structural components in the skeleton. (2) The distribution and density of desmocyte cells, which anchor the calicoblastic ectoderm to the skeletal surface, vary spatially and temporally during skeletal growth. (3) The tissue above the coenosteal spines lack endoderm and consists only of ectodermal cell-layers separated by mesoglea. These findings have important implications for models of vital effects in coral skeletal chemistry and isotope composition.