No description available.

This thesis focuses on the faunal remains from a sequence of 11 Epipalaeolithic and ten Neolithic sites in the eastern Jordanian steppe, with the aim of investigating the subsistence practices of hunters and herders between 20,000bp and 7,500bp, and their temporal and geographic variability within the study region. The first section outlines the archaeological and palaeoenvironmental background of the southern Levant; reviews subsistence evidence and models for the periods concerned; and describes the study area and sites. The second section concerns methodological approaches. A model of gazelle ethology for prehistoric eastern Jordan is presented, since this taxon is dominant in many of the study assemblages. Eleven modern case studies are used to predict population structure, demography and mobility, drawing on the principles of behavioural ecology. The archaeozoological methodologies used in the thesis are explained. The third section presents the results of the analyses. Taxonomic identification, quantification and faunal diversity are described and discussed for each assemblage, and broad temporal and geographical trends highlighted. Whether the assemblage compositions reflect the environmental changes discussed earlier is considered. It is demonstrated that the size diminution observed in both gazelle and hare between the late Pleistocene and early Holocene is probably attributable to climatic change. The question of selectivity in the taxa killed by prehistoric hunters is investigated. This is approached through ecological modelling and it is concluded that no strong selective biasses are observed. The nature of gazelle hunting is then further explored; the age profiles and sex ratios of the animal culls are compared to the model of gazelle social composition, and seasonal hunting times are proposed. The results suggest that none of the Epipalaeolithic assemblages shows signs of selective culling. Two Neolithic assemblages contain high proportions of juveniles, and interpretations relating to herd management practices, intensive hunting, and the targetting of vulnerable animals are discussed. The treatment of carcasses of the hunted animals is investigated. Body part representation, butchery and processing evidence, and taphonomic factors are considered, in order to present a picture of the activities undertaken at each site. The appearance of domestic caprines in eastern Jordan is considered. An assessment is made of their wild/domestic status, the management of herds and of carcass treatment. The results of the faunal remains analysed are integrated with other forms of archaeological evidence to discuss issues of mobility, contact and exchange, and to consider the changing and varied use of this area in prehistory.

This thesis provides a detailed account and analysis of Anglo-French relations in the Levant and their impact on the more general relationship between the British and the Free French during the important year of 1943. It aims to examine and explain how the Levant, traditionally an area of mutual suspicion and rivalry, created and accentuated discord and dissension between wartime Allies and , on occasion , even came perilously close to rupturing their relations. The introduction provides a survey of Anglo-French relations in the region as a backdrop against which the period covered by the thesis must be viewed. Chapters I-IV examine two policies pursued by Britain in the interests of the war effort, the persuasion of the Free French to honour their independence pledge to Syria and Lebanon and the encouragement of the formation of a unified French movement in North Africa. Arising from these policies, the mounting tensions between the Foreign Office and its principal representative in the Levant and between Churchill and de Gaulle are explored. The influence of deteriorating AngloFrench relations in the Levant on the Churchill-de Gaulle relationship is considered as are the high-level AngloFrench discussions in the summer of 1943 which acknowledged the need for better co-operation in the Levant. Chapters V and VI investigate the increasing Bri tish involvement in Levant politics, which resulted in the establishment of strongly nationalist and anti-French governments in both Syria and Lebanon. Chapters VII-XII are concerned exclusively with events in the Lebanon during late October and November 1943 which provoked a major crisis in Anglo-French relations. Attention is focused on the efforts of the Foreign Office and their French counterparts to defuse the crisis and to lessen its overall impact, and is contrasted with the intransigence displayed by Churchill and de Gaulle and with the belligerence of both French and British authorities on the spot. The final chapters deal with the efforts made to heal the breach in the Anglo-French relationship by both sides and the attempt by both to re-evaluate and reform their policies in the Levant. The troubled course of the AngloFrench alliance in the Levant throughout the remainder of the war, including the crisis in Syria in May and June 1945, is examined in a brief epilogue.

No description available.

Trade between two regions often necessitates that the respective parties are political entities. This was indeed the case for trade between Egypt and the Levant during the Middle Bronze Age (ca. 2000-1550 BC, MBA) and Late Bronze Age (ca. 1550-1200 BC, LBA). Scientific analyses of Canaanite jars, transport vessels, from the site of Memphis, Egypt provided an ideal proxy for examining the relationship between trade and politics. During the MBA, Levantine peoples were present at the site of Tell el-Dabca in the eastern Nile Delta. However, archaeologically there is little evidence for contact between these peoples and the Egyptians at Memphis. Results of comparison of MBA Canaanite jars from both sites suggest the political situation fostered trade with the Levant and limited interaction with the Egyptians. During the LBA, Egyptian kings controlled territory in the Levant. A comparison of MBA and LBA Canaanite jars from Memphis revealed that the political changes in some cases affected the trade partners but not in others. Further, the production of the jars appeared to have altered in some regions. These results suggest that the affect of political situations on trade can vary, from only minor changes, to the complete exclusion of trade partners and the introduction of new trade contacts. However, the influence of lucrative trade networks on political developments was also illustrated. The utility of provenance studies of ceramics for understanding the complex relationship between trade and politics was confirmed.

No description available.

This project documents the multi-scalar formation processes of two northern Levantine coastal Paleolithic cave sites using field geology, archaeological micromorphology and sediment geochemistry. Located in within several hundred meters of each other, the sequences from Üçağızlı I and II present an opportunity to compare late Middle and early Upper Paleolithic hominin adaptations to a similar coastal environment. The morphologies of the sites and the suite of coastal geomorphic features available to the area's Paleolithic occupants were impacted by fluctuations in sea level as well as tectonic events. The sites share similar formation histories that include active karstic processes, marine inundation, occupation by hominins, partial collapse of the cave vaults, and erosion of the uppermost archaeological deposits. Mousterian occupation of Üçağızlı II began after the formation of a series of stable sea level features that date to Marine Isotope Stage (MIS) 5a. Hominin utilization of the highly eroded portions of the cave continued at least through the middle of MIS 3, although the cultural attribution of the youngest materials is presently unknown. Üçağızlı I contains a sequence of Initial Upper Paleolithic, Ahmarian and Epipaleolithic materials dating to MIS 3 and 2. Micromorphology of the archaeological sediments reveals strong anthropogenic contributions to the infilling of both caves, in particular the deposition of abundant, well-preserved wood ashes. In both sequences, post-depositional insect bioturbation has negatively impacted the combustion features, resulting in alteration of the original sedimentary fabrics and loss of information regarding hominin activities such as sweeping, rake-out and dumping of ashes. In Üçağızlı II, the dominant mode of sedimentation is anthropogenic; a series of intact and cemented combustion features located beneath the highest point of the cave ceiling is surrounded by sediment exhibiting evidence of both rodent and insect bioturbation. In Üçağızlı I, phases of human activity alternated with periods of natural sedimentation. Combustion features in the site include isolated hearths, stacks of hearths, rake-out or sweeping deposits, ash dumps, and mixed burned materials that have been impacted by colluvial reworking and bioturbation. In sum, the two sites contain similar types of anthropogenic sediments despite differing cultural affiliation.

No description available.

No description available.

Le bassin de Levant, localisé à l’extrémité la plus orientale de la Méditerranée, se situe à jonction de trois plaques tectoniques majeures (Afrique, Arabie, Eurasie ainsi que la microplaque Anatolienne). Il est bordé à l’Est par la faille du Levant (frontière Arabie/Afrique), qui représente un système transformant de 1000 km de long, reliant le rift dans la Mer Rouge au sud avec la zone de convergence le long du Taurus au nord (frontière Arabie/Eurasie). Son extrémité nord est marquée par la frontière convergente Afrique/Anatolie soulignée par l’arc de Chypre. Le bassin Levantin a enregistré l’interaction entre ces différentes plaques au cours du Cénozoïque et sa bordure Est a été en particulier déformée par la mise en place de la faille du Levant. Cette limite de plaque majeure est marquée au Liban par un relais compressif qui a été actif depuis la fin du Miocène. Jusque récemment, l’absence de données sismiques dans la partie centrale du bassin levantin (offshore Liban) a constitué un handicap important dans la caractérisation de ce basin. Dans ce secteur, la géométrie, cinématique, l’âge des structures tectoniques ne sont pas connus. Plusieurs questions en découlent. Quel est impact de la frontière transformante du Levant sur la structure du bassin? Le bassin a-t-il enregistré d’autres déformations au cours du Cénozoïque ? Quel est l’effet de la structuration ancienne et profonde de la marge sur la déformation actuelle ? Ce travail s’est appuyé sur l’interprétation des données sismiques 2D et 3D de haute qualité dont deux cubes 3D de 4290 m3 et sept lignes 2D de 830 km de long. Cette étude a permis d’identifier les structures tectoniques affectant le secteur offshore Libanais et de caractériser leurs origines. Plusieurs familles de failles tout au long de la marge Est du bassin ont été identifiées et témoigne d’une histoire tectonique méso-cénozoïque longue et complexe. Les structures reconnues sont tout d’abord (1) des failles chevauchantes NNE-SSW actives depuis le début du Tertiaire jusqu’à la fin Miocène, (2) des anticlinaux NNE-SSW formés durant le Miocène supérieur et se localisant sur des structures préexistantes et (3) des failles décrochantes dextres, héritées des structures mésozoïques et réactivées durant le Miocène supérieur. Seules les failles décrochantes dextres montrent des preuves d’une activité actuelle, liée à la transpression au long de la faille du Levant. Ces structures constituent le prolongement vers l’ouest de la frontière de plaque du Levant sous un régime transpressif et une compression NW-SE. Nous mettons en évidence que cette frontière de plaque montre une évolution au cours du Néogène avec une forte décroissance de la composante de raccourcissement à partir du Pliocène. La mise en évidence de jeux plus anciens témoigne d’une structuration profonde E-W de la marge, vraisemblablement héritée des tectoniques mésozoïques. L’impact de cette structuration a été évalué à travers une modélisation analogique. Les résultats démontrent le rôle considérable de cet héritage sur l’évolution du relais compressif de la faille du Levant au Liban, entre autre en localisant la déformation le long de couloirs E-W et en segmentant les structures transpressives NNE-SSW. Ces résultats nous conduisent à interpréter les structures E-W comme majeures et traduisant la prolongation vers l’ouest du bassin mésozoïque des Palmyrides. Nous mettons ici en évidence le rôle majeure d’une marge sur la structure d’une frontière de plaques transformante. Le développement de failles antithétiques (failles dextres dans une frontière transformante senestre), connus dans d’autres frontières de ce type, est ici clairement associé à une anisotropie profonde forçant la localisation de la déformation. / The Levant Basin is located at the easternmost Mediterranean at the intersection of three major tectonic plates (Africa, Arabia, Eurasia and the smaller Anatolian microplate). The Levant Fracture System (Arabia-Africa plate boundary) borders the basin to its east and represents a 1000 km long left-lateral transform system linking rifting in the Red Sea with plate convergence along the Taurus Mountains (Arabia-Eurasia plate boundary). The Levant Basin is bordered to the north by the Cyprus Arc (Africa-Eurasia plate boundary). The interaction between these tectonic plates had important consequences on the evolution of the Levant Basin whereby its eastern boundary has been affected by deformation along the Levant Fracture System. This major plate boundary is associated with a restraining bend in Lebanon and has been active since the Late Miocene. Until recent days, the absence of seismic data in the central Levant Basin was an obstacle against characterizing the tectonic setting of the basin. In this area, the geometry, kinematics and the age of the tectonic structures are poorly understood. A focal question thus remains on how the Levant Basin was affected by this adjacent plate boundary. Therefore, what is the impact of the deformation along the Levant Fracture System since the Late Miocene on this basin and how can we assess it? Has the latter been affected by other tectonic regimes prior to the onset of transpression? If so, how would the existing structures influence the style of modern deformation? In this study, high quality 2D and 3D seismic reflection data (with two 4290 m3 3D seismic cubes and seven 830 km long 2D seismic lines) were interpreted allowing identification and timing of the structures in the Levant Basin offshore Lebanon. Several fault families, mapped along the margin, are remnants of a lasting and complex tectonic history since Mesozoic times. These include NNE-SSW striking thrust faults active during the early Tertiary and inactive since the Pliocene; NNE-SSW striking anticlines folded during the Late Miocene and overlying pre-existing structuresd; and ENE-WSW striking dextral strike-slip faults inherited from Mesozoic times and reactivated during the Late Miocene. Only the dextral strike-slip faults show evidence of current activity and are interpreted to be linked to transpression along the Levant Fracture System. They constitute the westward extension of the plate boundary, formed under a transpressif regime and a NW-SE compression. We have showed how this plate boundary has evolved through the Neogene with a decrease in the shortening component during the Pliocene.The identification of pre-existing structures along the eastern Levant margin shed the light on the deep structuration affecting this area, inherited from Mesozoic tectonic events. The impact of these structures was tested through analogue modeling. Results indicated a considerable impact of pre-existing structures on the development of the restraining bend, localizing deformation at the onset of transpression and responsible of segmenting the restraining bend along an ENE direction. These ENE-WSW faults are thus major and are most likely associated with the deformation affecting the Palmyra basin since the Mesozoic, which is thus extending westward to Lebanon. This study has shown the important role of a margin on a strike-slip plate boundary. Namely, the development of antithetic faults (local dextral strike-slip faults in a regional sinistral strike-slip plate boundary) known in other similar plate boundaries is associated with a deep crustal anisotropy localizing the subsequent deformation.