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 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.     

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.     

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.     

Making time: ‘Living floors’, ‘palimpsests’ and site formation processes – A perspective from the open-air Lower Paleolithic site of Revadim Quarry, Israel

The recognition of the dynamic role of site formation processes led archaeologists to recognize a behavioral dichotomy between ‘living floors’ and palimpsests’, Yet the archaeological proxies of ‘living floor’ and ‘palimpsest’ were never defined formally, and therefore have been used variably. We use archaeological criteria mentioned in the archaeological literature to model types of formation processes. The case study of the Lower Paleolithic open-air site of Revadim Quarry, Israel is used to test the model. Two types of palimpsests, differing in the rate of accumulation and thus in their effects on the anthropogenic remains, were discerned. Based on these results we review some other Lower Paleolithic instances. A sliding scale of formation processes provides a much needed middle ground between the scales of coarse, time-averaged formation processes and short, “near real-life” behavioral episodes and is an appropriate archaeological frame of reference.     

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).