ESR dating of the Neanderthal site, Kebara Cave, Israel

In 1985 a Neanderthal skeleton was found in the cave of Kebara in southern Mt. Carmel. Electron spin resonance (ESR) dates have been obtained on tooth enamel of gazelles found in layer X, just overlying the layer in which the skeleton was found. Assuming early uptake of uranium by the teeth, they yield an age of 60 ± 6 ka; assuming gradual, linear uptake of uranium yields an age of 64 ± 6 ka. Both age estimates are consistent with a previous estimate for the skeleton, based on TL dating of burnt flint, of 60 ± 4 ka.     

The Chinese Upper Paleolithic: Geography, Chronology, and Techno-typology

This article reviews the archaeology and chronology of the Chinese Upper Paleolithic and the human fossils attributed to this period. The onset of the Upper Paleolithic in China dates to ca. 35,000–30,000 years ago and is marked by the appearance of a few body decorations and well-shaped bone tools that were added to stone tool assemblages, including core-and-flake tools in North China and cobble tools in South China. The proliferation of blade assemblages in northwest China is interpreted as the cultural impact or the physical presence of bearers of blade industries from western Eurasia. The ensuing appearance of microblade assemblages in North China by 23,000–22,000 years ago reflects the use of local siliceous crystalline nodules by a population that recognized the advantages of this raw material. At that time in South China, prehistoric artisans continued to shape their stone objects from the available flat river cobbles. During the later part of the Chinese Upper Paleolithic (ca. 21,000–10,000 BP), foragers also made bone tools, antler objects, pottery, and shell tools, which laid the technological foundations for the early Neolithic period. One difficulty in this research is that human fossils are rare. Few are well dated and morphological, cultural, and biological interpretations are hotly debated. Our review attempts to facilitate the understanding of a poorly known period in Chinese archaeology and its place in human cultural evolution.     

Hayonim Cave: a TL-based chronology for this Levantine Mousterian sequence

The thermoluminescence dating method was applied to 77 heated flints from the Mousterian layers of Hayonim Cave in order to provide a precise TL-based chronology for this important Levantine sequence. A detailed dosimetric study was performed by using 76 dosimeter capsules and revealed strong spatial dose-rate variations. In parallel, Fourier transform infrared spectrometry enabled the identification of various mineral assemblages in the sediments of the cave and to localize the boundaries of these assemblages. By comparing these two data sets, it is shown that low dose-rate values (∼500 μGy/a) are systematically recorded in areas where the calcite-dahllite (CD) assemblage is preserved, whereas higher values (up to 1300 μGy/a) are associated with the leucophosphite, montgomeryite, variscite and siliceous aggregates (LMVS) assemblage. The dosimetric and mineralogical information was combined in order to assess, where possible, the dose-rate experienced by each flint during its burial. Some of the flint samples analyzed were too close to mineral assemblage boundaries and were therefore discarded. This rigorous selection led to TL ages ranging from 230 to 140 ka for the lower part of the Mousterian sequence (layers F and Lower E), which contains lithic industries characterized by blade production using the laminar method.     

The Body–Power Relationship and Immanent Philosophy: A Question of Life and Death

According to Foucault, the human body is the targeted object of modern power systems. In his genealogical studies, Foucault describes the manner in which these power systems leave an imprint on the body and utilize knowledge of the body as an indirect means of exercising subtle forms of control. In recent years, several researchers have claimed that the status of the body, subsumed as it is by modern power networks, has become a means for conducting a unique political critique in which the human being is viewed as an agent of oppression and freedom. This article takes a fresh look at Foucault’s notions of life and death that underpin the critical understanding the body–power relationship. While this approach recognizes the completeness of subjective structuring processes, it also enables the formulation of new insights regarding the status of the modern individual as the subject of separate and independent modes of speech and action.     

Together in the field: interdisciplinary work in Kebara and Hayonim caves (Israel)

The authors present an example of close field collaboration among prehistorians and researchers from different disciplines (particularly the geosciences), within the context of a long program of interdisciplinary research at the caves of Kebara and Hayonim (Israel). We outline the benefits brought about by the presence of different specialists being in the field during the excavation over long periods. Specifically, daily collaboration in the field during the excavation brings about: (1) A consensus of choice of strategic areas to excavate, either at the beginning of the project or during successive field campaigns, while taking into account the needs and goals of different specialists and their needs in taking samples; (2) A meeting of different points of view with many discussions of stratigraphy and site formation processes, which in caves are quite complex; (3) A unification of specialized vocabulary and jargon specific to each discipline by constant interaction in the field, which in turn facilitates communication among specialists; (4) A positive didactic element in training doctoral students in the field. This interdisciplinary strategy is more or less widespread now, but it was not the case in the early 1980s, and actual integration of results from the sciences (particularly the geosciences) came about only fairly recently. Without doubt, the awareness of the importance of such interdisciplinary archaeological data for discussing archaeological issues has ultimately paved the way for active interdisciplinary collaboration sprouting from the fieldwork, and has led to the generation of more robust and accurate interpretations.     

Book reviews

Selwyn Ilan Troen and Benjamin Pinkus, eds., Organizing Rescue: National Jewish Solidarity in the Modern Period, London, Frank Cass, 1992, pp. xi, 424.

Idith Zertal, From Catastrophe to Power: Jewish Illegal Immigration to Palestine 1945–1948 (Hebrew). Tel Aviv: Am Oved Publishers, 1996. 674 pp.; notes; bibliography; index.

Yoav Gelber, Jewish‐Transjordanian Relations, 1921–48, London: Frank Cass, 1997. 320 pp., glossary, sources and bibliography, index.

Moshe Shemesh, The Palestinian Entity, 1959–1974; Arab Politics and the PLO, Second (Revised) Edition, London: Frank Cass, 1996. xxiii, 433pp., bibliography, index.

Yeshayahu A. Jelinek, ed., Zwischen Moral und Realpolitik: Deutsch‐israelisch Bezeihungen 1945–1965: Eine Doku‐mentensammlung. Gelingen: Bleicher Verlag, 1997. 687 pp.

Angelika Timm, Jewish Claims Against East Germany: Moral Obligations and Pragmatic Policy. Budapest: Central European University Press, 1997, xi + 291pp.     

ESR Dating of the Last Interglacial Mousterian at Karaïn Cave, Southern Turkey

We have obtained ESR ages on 18 teeth from archaeological levels AH16-AH27 exposed at the east profile in compartment E at Karaïn Cave. This sequence exhibits a transition in lithic assemblage from a Classic Charentian to a Karaïn (Zagros-type) Mousterian between levels AH27 and AH25, and two calcite-cemented soils at levels AH22 and AH16 which have been interpreted as climatic warm phases. Since we found no systematic increase in tooth ages with depth, we assigned this sequence a mean early uptake (EU) age of 108 ± 23 ka and mean linear uptake (LU) age of 121 ± 27 ka, on the basis of 37 subsamples from 16 teeth. In this site, the precision of individual tooth ages suffered little from the problems associated with uranium uptake. However, this advantage was offset due to uncertainties arising from the rather inhomogeneous nature of the enclosing strata which contained various sizes of limestone blocks with intervening sediment. This led to difficulties in ascribing a precise annual gamma radiation dose to individual teeth in such a "lumpy" gamma radiation field. Considerable scattering of the individual tooth ages occurred mainly because the annual gamma dose comprised greater than 50% of the total annual dose to the individual teeth. On the basis of the ESR dating results, we infer that deposition of the two different lithic assemblages and both the penultimate and the final climatic warm phases at Karaïn probably occurred during oxygen isotope stage 5. We also conclude that these lithic assemblages are significantly different than contemporaneous Levantine Mousterian industries which occur about 700 km to the southeast.     

New radiocarbon dating of the transition from the Middle to the Upper Paleolithic in Kebara Cave,Israel

The Middle to Upper Paleolithic transition (MP-UP transition) is considered a major technological and cultural threshold, at the time when modern humans spread “out of Africa”, expanded from the Levant into Europe and possibly into central and northern Asia. The dating of this techno-cultural transition has proved to be extremely difficult because it occurred sometime before 40,000 radiocarbon years before present (¹⁴C years BP), which is close to the end of the effective dating range of radiocarbon. Other dating methods such as Thermoluminescence (TL) or Electron Spin Resonance (ESR) are not sufficiently precise to date the recorded archaeological MP-UP transition in the Levant. Here we report a consistent set of stratified radiocarbon ages on freshly excavated charcoal from Kebara Cave, Mt. Carmel (Israel), that span the late Middle Paleolithic (MP) and Early Upper Paleolithic (EUP) This study applied novel strategies to improve sample preparation techniques and data analysis to obtain high-resolution radiocarbon models. From this study it is proposed that the MP-UP transition for this site can be placed immediately after 45,200 ± 700 ¹⁴C years BP and before 43,600 ± 600 ¹⁴C years BP or from 49/48 to 47/46 radiocarbon calibrated years before present (years Cal BP).