La Pisidie, région montagneuse du sud-ouest de l’Asie Mineure, est un véritable conservatoire toponymique de la culture et des langues anatoliennes. Notre thèse porte sur la toponymie et l’ethnonymie de la Pisidie et sur la persistance des langues anatoliennes dans la toponymie de la région. La toponymie et l’ethnonymie nous révèlent l’emprise sur le territoire de chaque peuplement, qu’il s’agisse du peuplement anatolien ou des peuplements exogènes (principalement grecs et romains). En effet, par le choix de la langue utilisée pour créer le nom du lieu ou du peuple, nous en apprenons davantage sur la région. Après avoir réalisé un catalogue des toponymes et des ethnonymes de la Pisidie classés par types et discuté leur origine à l’aide d’arguments linguistiques pour chacun d’entre eux, nous étudions la présence grecque et les colonies romaines en envisageant les dominations successives du point de vue de la toponymie. Plusieurs thèmes sont abordés : la question du contrôle de la région à l’époque hellénistique, les fondations séleucides, ainsi que les colonies romaines fondées par Auguste. Puis, nous nous concentrons sur l’identité des Pisidiens, en étudiant la question de leur origine et des topoi qui leurs sont associés. Les continuités et les ruptures territoriales de la Pisidie sont abordées avant un panorama toponymique présentant un classement linguistique et un classement sémantique des toponymes en fonction du référentiel sémantique (eau, relief, végétation, etc.). L’essentiel des toponymes est descriptif et renvoie à des éléments du paysage. / Pisidia, a mountainous region in southwestern Asia Minor, is a real toponymic conservatory of Anatolian culture and languages. Our thesis deals with the toponymy and ethnonymy of Pisidia and the persistence of Anatolian languages in the toponymy of the region. Toponymy and ethnonymy reveal the territorial control of each settlement, whether it be Anatolian population or exogenous settlements (mainly Greek and Roman). Indeed, by choosing the language used to create the name of the place or the people, we learn more about the region. After having produced a catalog of toponyms and ethnonyms of the Pisidia classified by types and after having discussed their origin using linguistic arguments for each one, we study the Greek presence and the Roman colonies by considering the successive domination in regard to toponymy. Several themes were discussed : the question of the control of the region during the Hellenistic period, the Seleucid foundations, as well as the Roman colonies founded by Augustus. Then we focus on the identity of the Pisidians, studying the question of their origin and the topoi associated with them. The continuities and territorial cleavage of Pisidia are discussed before a toponymic panorama showing a linguistic classification and a semantic classification of toponyms based on the semantic repository (water, relief, vegetation, etc.). Most of the place names are descriptive and refer to elements of the landscape.

The complete consumption of the oceanic domain of a tectonic plate by subduction into the upper mantle results in continent subduction, although continental crust is typically of lower density than the upper mantle. Thus, the sites of former oceanic domains (named suture zones) are generally decorated with stratigraphic sequences deposited along continental passive margins that were metamorphosed under low-grade, high-pressure conditions, i.e., low temperature/depth ratios (< 15°C/km) with respect to geothermal gradients in tectonically stable regions. Throughout the Mesozoic and Cenozoic (i.e., since ca. 250 Ma), the Mediterranean realm was shaped by the closure of the Tethyan Ocean, which likely consisted in numerous oceanic domains and microcontinents. However, the exact number and position of Tethyan oceans and continents (i.e., the Tethyan palaeogeography) remains debated. This is particularly the case of Western and Central Anatolia, where a continental fragment was accreted to the southern composite margin of the Eurasia sometime between the Late Cretaceous and the early Cenozoic. The most frontal part of this microcontinent experienced subduction-related metamorphism around 85-80 Ma, and collision-related metamorphism affected more external parts around 35 Ma. This unsually-long period between subduction- and collision-related metamorphisms (ca. 50 Ma) in units ascribed to the same continental edge constitutes a crucial issue to address in order to unravel how Anatolia was assembled. The Afyon Zone is a tectono-sedimentary unit exposed south and structurally below the front high-pressure belt. It is composed of a Mesozoic sedimentary sequence deposited on top of a Precambrian to Palaeozoic continental substratum, which can be traced from Northwestern to southern Central Anatolia, along a possible Tethyan suture. Whereas the Afyon Zone was defined as a low-pressure metamorphic unit, high-pressure minerals (mainly Fe-Mg-carpholite in metasediments) were recently reported from its central part. These findings shattered previous conceptions on the tectono-metamorphic evolution of the Afyon Zone in particular, and of the entire region in general, and shed light on the necessity to revise the regional extent of subduction-related metamorphism by re-inspecting the petrology of poorly-studied metasediments. In this purpose, I re-evaluated the metamorphic evolution of the entire Afyon Zone starting from field observations. Low-grade, high-pressure mineral assemblages (Fe-Mg-carpholite and glaucophane) are reported throughout the unit. Well-preserved carpholite-chloritoid assemblages are useful to improve our understanding of mineral relations and transitions in the FeO-MgO-Al2O3-SiO2-H2O system during rocks’ travel down to depth (prograde metamorphism). Inspection of petrographic textures, minute variations in mineral composition and Mg-Fe distribution among carpholite-chloritoid assemblages documents multistage mineral growth, accompanied by a progressive enrichment in Mg, and strong element partitioning. Using an updated database of mineral thermodynamic properties, I modelled the pressure and temperature conditions that are consistent with textural and chemical observations. Carpholite-bearing assemblages in the Afyon Zone account for a temperature increase from 280 to 380°C between 0.9 and 1.1 GPa (equivalent to a depth of 30-35 km). In order to further constrain regional geodynamics, first radiometric ages were determined in close association with pressure-temperature estimates for the Afyon Zone, as well as two other tectono-sedimentary units from the same continental passive margin (the Ören and Kurudere-Nebiler Units from SW Anatolia). For age determination, I employed 40Ar-39Ar geochronology on white mica in carpholite-bearing rocks. For thermobarometry, a multi-equilibrium approach was used based on quartz-chlorite-mica and quartz-chlorite-chloritoid associations formed at the expense of carpholite-bearing assemblages, i.e., during the exhumation from the subduction zone. This combination allows deciphering the significance of the calculated radiometric ages in terms of metamorphic conditions. Results show that the Afyon Zone and the Ören Unit represent a latest Cretaceous high-pressure metamorphic belt, and the Kurudere-Nebiler Unit was affected by subduction-related metamorphism around 45 Ma and cooled down after collision-related metamorphism around 26 Ma. The results provided in the present thesis and from the literature allow better understanding continental amalgamation in Western Anatolia. It is shown that at least two distinct oceanic branches, whereas only one was previously considered, have closed during continuous north-dipping subduction between 92 and 45 Ma. Between 85-80 and 70-65 Ma, a narrow continental domain (including the Afyon Zone) was buried into a subduction zone within the northern oceanic strand. Parts of the subducted continent crust were exhumed while the upper oceanic plate was transported southwards. Subduction of underlying lithosphere persisted, leading to the closure of the southern oceanic branch and to subduct the front of a second continental domain (including the Kurudere-Nebiler Unit). This followed by a continental collisional stage characterized by the cease of subduction, crustal thicknening and the detachment of the subducting oceanic slab from the accreted continent lithosphere. The present study supports that in the late Mesozoic the East Mediterranean realm had a complex tectonic configuration similar to present Southeast Asia or the Caribbean, with multiple, coexisting oceanic basins, microcontinents and subduction zones. / Kontinentale Subduktion resultiert aus dem Abtauchen des ozenanischen Gebiets einer tektonischen Platte in den Oberen Erdmantel. Dies geschieht obwohl die kontinentale Erdkruste normalerweise eine geringere Dichte besitzt als der Obere Erdmantel. Die Lage ehemaliger ozeanischer Gebiete (auch als Suturzonen bezeichnet) ist dementsprechend durch stratigraphische, sedimentäre Gesteinsabfolgen gekennzeichnet, die entlang des passiven Kontinentalrandes abgelagert wurden. Anschließend wurden diese Gesteine unter niedrigen Temperaturen und hohem Druck umgewandelt, auch niedrig-gradige Hochdruckmetamorphose genannt. Während der gesamten Zeitspanne des Mesozoikums und Känozoikums (seit etwa 250 Millionen Jahren bis heute) wurde der mediterrane Raum durch die kontinuierliche Schließung des Tethyschen Ozeans (dem heutigen Mittelmeer) geprägt, der vermutlich in zahlreichen kleineren Ozeanen und Mikrokontinenten aufgeteilt war. Dennoch bleiben die genaue Anzahl und Lage der tethyschen Ozeane und Kontinente (die Paläogeographie der Tethys) bis heute umstritten. Das ist insbesondere der Fall in West- und Zentral-Anatolien, wo im Zeitraum zwischen der Oberen Kreide (vor 98 bis 65 Mio. J.) und dem unteren Känozoikum (vor 65 bis 40 Mio. J.) ein kontinentales Fragment am südlichen Kontinentalrand der Eurasischen Platte angelagert wurde (auch als Akkretion bezeichnet). Der vorderste Bereich von diesem Fragment erfuhr vor etwa 85-80 Millionen Jahren eine metamorphe Umwandlung, die mit den Prozessen der fortschreitenden Subduktion assoziiert werden können. Hingegen wurden die hinteren Bereiche erst später vor ca. 40-30 Mio. J. durch die Kollison der zwei Platten metamorph überprägt. Die ungewöhnlich lange Zeitspanne von etwa 40-50 Mio. J. zwischen den metamorphen Prozessen der Subduktion und der Kollision, stellt eine entscheidende Frage zum Verständnis der Entstehung von Anatolien dar. Die Afyon Zone repräsentiert hierbei eine tektonisch-beanspruchte sedimentäre Gesteinseinheit, die in einer strukturell tieferen Position bezüglich des frontalen metamorphen Hochdruckgürtels liegt und südlich von ihm anzutreffen ist. Die Afyon Zone besteht aus mesozoischen sedimentären Einheiten (250 bis 65 Mio. J. alt), die auf präkambrischem (älter als 545 Mio. J.) bis paläozoischem Untergrund (bis vor 250 Mio J.) abgelagert wurden, und vom nordwestlichen bis zentralen Anatolien, entlang der vermutlichen Tethys-Suturzone, verfolgt werden können. Obwohl die Afyon-Zone als eine niedrig-temperierte metamorphe Gesteinseinheit bezeichnet wird, wurde in letzter Zeit von Vorkommen von Hochdruckmineralen (v.a. Eisen(Fe)-Magnesium(Mg)-Karpholith in metamorphen Sedimenten) im zentralen Bereich berichtet. Diese neuen Erkenntnisse stellen die bisherigen Interpretationen zur tektonisch-metamorphen Entstehung der gesamten Region in Frage, insbesondere der der Afyon-Zone. Deshalb war eine erneute gründliche Überarbeitung und Untersuchung der wenig studierten metamorph-überprägten Sedimentgesteine in diesem Gebiet notwendig. Deshalb, überarbeitete ich die metamorphe Entwicklung der gesamten Afyon Zone, beginnend mit intensiver Geländearbeit und -beobachtungen. Mineralvergesellschaftungen aus Karpholith und Glaukophan, die unter niedrigen Temperaturen und hohem Druck entstanden sind, wurden in der gesamten Gesteinseinheit gefunden. Guterhaltene Mineralvergesellschaftungen aus Karpholith und Chloritoid sind nützlich für das Verständnis unter welchen Temperatur- und Druck-Bedingungen die Gesteine in die Tiefe gelangen (prograde Metamorphose). Durch die Untersuchungen von Gesteinsgefügen und der Eisen-Magnesium-Verteilung zwischen den Mineralien Karpholith und Chloritoid lassen sich Aussagen zu der Bildungstemperatur und dem Druck dieser Minerale machen. Dafür benutzte ich eine verbesserte Datenbank mit Mineraleigenschaften, die mir die Modellierung von Temperatur und Druck erlaubte und im Einklang mit den chemischen und mikroskopischen Beobachtungen steht. Es ergab sich, dass die Karpholith-haltigen Gesteine in der Afyon-Zone einen Temperaturanstieg von 280 zu 380°C (bei einer Tiefe von 30-35 km) erfahren haben. Um noch bessere Aussagen über die Entstehung zu treffen, wurden auch radiometrische Datierungen an Proben aus der Afyon-Zone, sowie an zwei weiteren Sedimentgesteinseinheiten (Ören- und Kurudere-Nebiler-Einheit aus SW Anatolien) gemacht. Für die Altersbestimmung benutzte ich die weitverbreitete 40Ar-39Ar Datierungsmethode an Hellglimmer-Mineralien in den Karpholith-haltigen Gesteinen. Temperatur und Druck können auch bestimmt werden, wenn man den Übergang von einer Mineralvergesellschaftung zu einer anderen Vergesellschaftung beobachtet. Dies gilt zum Beispiel für den Übergang von einer Karpholith-haltigen Zusammensetzung zu einer Quartz-Chlorit-Glimmer und Quartz-Chlorit-Chloritoid Mineralvergesellschaftung wenn tief subduzierte Gesteine wieder nach oben gelangen (Exhumation). Damit lassen sich die radiometrischen Alter den metamorphen Prozessen zu bestimmten Temperaturen und Drücken zuordnen. Mit diesen Erkenntnissen lassen sich die Afyon-Zone und die Ören-Einheit einem Hochdruck-Gebirgsgürtel in der späten Kreidezeit zuordnen, während die Kurudere-Nebiler Einheit durch die mit der Subduktion in Verbindung stehende Metamorphose vor ca. 45 Mio. J. beeinflusst wurde. Später wurde diese Einheit durch die Metamorphose, resultierend aus der Kollision vor 26 Mio. J., abgekühlt. Die Ergebnisse dieser und anderer Arbeiten erlauben es die Anlagerung von Kontinenten in West-Anatolien besser zu verstehen. Es wird gezeigt, dass mindestens zwei (im Gegensatz zu vorher einem) voneinander unabhängige Ozeanarme während der Subduktion von 92 bis 45 Millionen Jahren geschlossen wurden. Zwischen 85-80 und 70-65 Millionen Jahren, wurde ein schmales kontinentales Gebiet (welches die Afyon-Zone beinhaltet) in die Subduktionszone hineingzogen. Teile der subduzierten kontientalen Kruste kamen wieder an die Oberfläche (Exhumation), während die obere ozeanische Platte südwärts transportiert wurde. Die anhaltende Subduktion im oberen Bereich des Erdmantels (Lithosphäre) führte zu der Schließung des südlichen Ozeanarms und zu der Subduktion des zweiten kontinentalen Gebietes (welches die Kurudere-Nebiler-Einheit beinhaltete). Darauf folgte die kontinentale Kollisionsphase unter dem Ausklingen der Prozesse der Subduktion, der Krustenverdickung und der Abtrennung der subduzierten ozeanischen Platte von der akkretionierten kontientalen Lithosphäre (auch als Delamination bezeichnet). Die hier präsentierte Arbeit unterstüzt die Annahme das während der Oberen Kreidezeit das Ost-Mediterrane Gebiet tektonsich komplex angeordnet war, vergleichbar mit dem heutigen Südost-Asien oder der Karibik, mit ihren vielen gleichzeitig existierenden ozeanischen Becken, Mikrokontinenten und Subduktionszonen.

This dissertation aims at analyzing the debates among intellectuals concerning humanism, and concurrently designed &ldquo / Turkish Humanism Project&rdquo / during the nation/identity-building process in the early decades of Turkey&rsquo / s Republican Era. During in&ouml / n&uuml / Era (1938-1950), the nationalism and westernization of Atat&uuml / rk&rsquo / s reforms turned into an uncompromising secularism, and consequently humanist culture and &ldquo / humanism&rdquo / became the quasi-formal ideology of the state. In order to spread the newly designed cultural policy, then unnamed &ldquo / Turkish Humanism Project&rdquo / was developed. The present dissertation starts with debates on humanism among those intellectuals who were influential over the decision of the state to support humanist culture. Following that, it analyzes the three pillars of the project, namely, Greek and Latin lessons in high school curriculum, establishment of the Translation Office, and opening of the Village Institutes, respectively. In the dissertation, the emergence of humanism in the country is discussed in an historical perspective. Moreover, the general understanding of both the intellectuals and the state of humanism as a solution to the problems faced in cultural and national identity-building process and in westernization movement is demonstrated. As that perception evolved into another perception that humanism was now the cure to all kinds of problems in the society, humanism was charged with tasks too burdensome for such a project to accomplish. This evolution is also demonstrated in the dissertation. The failure of all three pillars of Turkish Humanism Project is attributed not only to the political turmoil during the period but also to the inability of country&rsquo / s intellectuals to conceptualize any phenomena in question as well as their turning the project into a &ldquo / utopian romanticism&rdquo / in the course of time. Nevertheless, the most important factor behind the failure is defined as the rejection by then existing social structure of a concept to alien Turkish national-being, imposed on the society. While the dissertation aims at revealing the intellectual map of the early Republican intellectuals, it also attempts at making an inventory of the debates about &ldquo / humanism&rdquo / , and hence modestly contributes to the existing relevant literature which is insufficient and at times inaccurate.

The aim of this study is to delineate the Campanian-Maastrichtian boundary by using planktonic foraminifers. In this manner, Kokaksu Section (Bartin, NW Anatolia) was selected and the Akveren Formation, characterized by a calciturbiditic-clayey limestone and marl intercalation of Campanian-Maastrichtian age, was examined. 59 samples were emphasized for position of boundary. Late Campanian-Maastrichtian planktonic foraminifers were studied in thin section and by washed samples. Two different biostratigraphical frameworks have been established. Globotruncanid zonation consists of Campanian Globotruncana aegyptiaca Zone, Upper Campanian-Middle Maastrichtian Gansserina gansseri Zone and Upper Maastrichtian Abathomphalus mayaroensis Zone, whereas heterohelicids biozonation includes Campanian Pseudotextularia elegans Zone, Lower Maastrichtian Planoglobulina acervuloinides Zone, Middle Maastrichtian Racemiguembelina fructicosa Zone and Upper Maastrichtian Pseudoguembelina hariensis Zone. Campanian-Maastrichtian boundary was determined as the boundary between Pseudotextularia elegans and Planoglobulina acervuloinides zones and Cretaceous-Tertiary boundary was designated by total disappearance of Late Cretaceous forms. Heterohelicid biozonation has been established in this study for the first time in Turkey. Collecting 300 individuals from each sample, diversity and abundance of assemblages were analyzed in terms of genus and species. ir evaluation of are important in observation of evolutionary trends and ecological changes. Moreover, evolution of different morphotypes is important in this evaluation. Such a study is new in Turkey in terms of examination of responses of planktonic foraminifers to environmental changes. Taxonomic framework has been constructed to define each species and differences of comparable forms have been discussed. Both scanning electron microscope (SEM) photographs and thin section photographs were used in order to show se distinctions.

The aim of this study is to establish the planktonic foraminiferal biozonation, to construct the sequence stratigraphical framework and to determine the foraminiferal response to sedimentary cyclicity in the sedimentary sequence spanning Upper Cretaceous-Paleocene in the Haymana basin (Central Anatolia, Turkey). In order to achieve this study, the stratigraphic section was measured from sedimentary sequence of the Haymana, Beyobasi and YeSilyurt formations. The sedimentary sequence is mainly characterized by flyschoidal sequence that is composed of alternating of siliciclastic and carbonate units. On the account of the detailed taxonomic study of planktonic foraminifers, the biostratigraphic framework was established for the Maastrichtian-Paleocene interval. The biozonation includes 7 zones / Pseudoguembelina hariaensis, P&amp / #945 / , P1, P2, P3, P4 and P5 zones. The Cretaceous-Paleogene (K/P) boundary was delinated between the samples HEA-105 and 106. In order to construct the sequence-stratigraphical framework, the A, B, C and D-type meter-scale cycles were identified. Based on the stacking patterns of them, six depositional sequences, six third and two second order cycles were determined. Third order cycles coincide with the Global Sea Level Change Curve. On the account of the conducted petrographic analysis sandstone, mudstone, marl, limestone and muddy-limestone lithofacies were recorded in the studied samples. In order to demostrate the response of foraminifers to cyclicity, quantitative analysis has been carried out by counting the individuals of planktonic, benthonic foraminifers and ostracods. The best response to sedimentary cyclicity was revealed from planktonic foraminifers. The average abundance of planktonic foraminifers increases in the transgressive systems tract and decreases in the highstand systems tract.

This study aims to find out the patterns of economic, social and political participation of the youth in urban South-eastern Anatolia Region of Turkey. Analyses of the data reveal that youth in the South Eastern Anatolia Region does not and cannot participate in various dimensions of the society. Youth in South-eastern Anatolia cannot participate into the labour market. There are too limited job opportunities in the region. On the other hand, working young people are prone to low quality working conditions. Young people also cannot participate into the social life in the public sphere. Social and economic pressures and lack of opportunities are limiting young people in a social life mainly in the private sphere within a closed community. Finally, youth in South-eastern Anatolia Region are keeping themselves away from political mechanisms. Political structure is not attracting young people because of the negative experiences that the people participated in politics having for years. One of the most important findings of the study is that different dimensions of participation namely participation in the labour market, participation in social life and political participation are dependent on each other. Another result is that both the level and experiences of youth participation are highly determined by the social characteristics such as gender, family background, education level and age.

In this study, morphology, anatomy and systematics of the Genus Lathyrus L. (Leguminosae) in Central Anatolia is presented. Comparative morphological characters and their variation in the Genus / Calyx, leaf, corolla and pollen grains micro-morphology of the species / Anatomy of the species / Ecology, endemism, phytogeography and IUCN threat categories of the species / Numerical analysis and Revision of the genus in Central Anatolia were conducted. For the first time the calyx, corolla and leaf micromorphology, and the anatomical characteristics of Lathyrus were examined. Infrageneric delimitation of the species is performed by using multivariate analysis. As a result of morphological and anatomical data, it is suggested that L. haussknechtii should be classified as different species not variety of L. brachypterus. v The collected specimens was crosschecked with neighboring floras and the existing type specimens known from Turkey ANK, GAZI, HUB, KNYA, CUFH, Erciyes, and Royal Botanic Garden Edinburgh (RBGE) herbaria. Morphological and micromorphological characters of pollen grains were revealed. It was determined that the pollen grains size and sculpturing were important diagnostic characters for the species. The statistical analysis was applied to compare P/E ratios of the pollen grains of studied taxa. According to this analysis, the P/E ratio is important diagnostic feature for most of the sections and the species. Sectional key and species key were prepared and updated. Expanded descriptions, GPS data, some photographs and some notes on the taxonomy of the species were given.

Fighting against the regional development disparities has been considered as one of the most important public policies recently. In this regard, Social Support Program, endorsed in 2008 under GAP Action Plan, is regarded as an important example of public intervention with increasing budget and geographical expansion. Objective of SODES is improving social inclusion of disadvantaged groups and enhancing regional social development. Accordingly, projects prepared by local actors to provide social inclusion, to increase employability and to support cultural, artistic and sports events are financed. &ldquo / Social inclusion&rdquo / is defined as policies and implementations targeting to increase access of disadvantaged groups to services like education, health, employment and social assistance. Debates on social inclusion literature include: lack of clear definition, dichotomy as &ldquo / them and us&rdquo / , focus on state rather than process and limited scope. Objective of this study is critically analyzing SODES, on the basis of social inclusion. In-depth interviews are conducted with beneficiaries, their families, project coordinators, local officials and policy makers to understand the impacts of the projects and SODES. It is observed that, there are important positive outcomes like the increase in schooling rate of girls. However, taking into consideration debates on social inclusion and evaluating SODES projects as a whole, it is argued that SODES has deficiencies regarding its project based structure, sustainability, accessibility of all target groups, evaluation, monitoring and institutionalization. The argument of the thesis is that such deficiencies of SODES are also arising from the concept of social inclusion which has its limitations in confronting structural inequalities in the society.

In this thesis, changing regional development policies and effects of these in Turkey is discussed. Regional inequalities have been one of the important concerns of the Republic of Turkey. However, the restructuring of state and capitalism during 1980&amp / #8217 / s led to a change in regional policies and Turkish regional polices have surely begun to be affected from new policies. Yet, these new policies do not seem to offer much about promoting development in underdeveloped regions. This study aims to analyze the effects of new regional policies with their successes and failures in order to find out whether they can offer a suitable policy framework for promoting development in underdeveloped regions of Turkey. With this aim, changing policies in Southern Eastern Anatolia Project (GAP) will be discussed. Transformation of GAP, from a project of irrigation and energy based on previous allocative regional policies to a sustainable human development project will be examined. According to findings of the study, some remarks will be made about policy framework that should be taken as a basis in GAP.

In the present study, for estimating the Central Asia contribution to the Anatolia, nine Alu insertion polymorphisms (ACE, PV92, FXIIIB, APO, A25, B65, TPA25, D1, HS4.32 ) in 100 individuals from Anatolia were examined. Alu insertion frequency for these loci were calculated as 0,410 / 0,220 / 0,579 / 0,963 / 0,067 / 0,667 / 0,390 / 0,427 / and 0,637 respectively and they were found to be in Hardy-Weinberg equilibrium (p&lt / 0,05). Observed insertion frequencies of each loci were compared with those of the previous observations (Din&ccedil / , 2003 / Comas et al., 2004) and it was found that the present study results were not different than those obtained by Comas et al. (2004). Thus, these two data were pooled (N = 143) and used to examine genetic relationships between populations from Eurasia and Africa. Pairwise Fst statistics indicated that there is higher genetic similarity between Anatolia and all of the Balkans and some of the Caucasian populations. Neighbor Joining (NJ) tree based on Reynold&rsquo / s genetic distances and Principal Component Analysis (PCA) both grouped the Anatolian populations with Balkans and some of the Caucasian populations and show clear differentiation of Asian populations from the Anatolian population. The relative genetic contribution of Central Asian genes to the current Anatolian gene pool was quantified using Admix analysis, considering for comparison populations of Balkans (Greek, Romania, Albania and Hungarian) and Central Asia (Uighur, Uzbeks, Tajicks, Kazaks, Kyrgyzes, Dungans). Estimates suggest roughly 28 % contribution from Asia to Anatolia in concordance with the previous estimation (Benedetto et al., 2001).