Academic literature on the topic 'Holocène – Mali'

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Journal articles on the topic "Holocène – Mali"

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Dumesnil, J., F. Valentin, and A. Vialet. "Le squelette de l'homme fossile d'Asselar (Mali, Holocène ancien) : observations archéothanatologiques." Bulletins et Mémoires de la Société d'Anthropologie de Paris 30, no. 1-2 (2018): 102–6. http://dx.doi.org/10.3166/s13219-017-0199-4.

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L'homme fossile d'Asselar, découvert en 1927 dans l'actuel Mali, n'a été que peu exploité depuis l'étude de Boule et Vallois (1932). Daté de l'Holocène ancien, il est, avec la série d'Hassi-el-Abiod, un témoin des populations vivant dans un Sahara alors « vert », bien différent de celui que nous connaissons aujourd'hui. L'hypothèse d'un dépôt funéraire, écartée dès la première étude au profit de celle d'une noyade et d'un enfouissement accidentel, est considérée pour la première fois selon les principes de l'anthropologie de terrain et grâce à l'imagerie médicale qui permet un accès complet et
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Huysecom, E., S. Ozainne, F. Raeli, A. Ballouche, M. Rasse, and S. Stokes. "Ounjougou (Mali): A history of holocene settlement at the southern edge of the Sahara." Antiquity 78, no. 301 (2004): 579–93. http://dx.doi.org/10.1017/s0003598x00113237.

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The area of Ounjougou consists of a series of gullies cut through Upper Pleistocene and Holocene formations on the Dogon Plateau in the Sahel at the south edge of the Sahara Desert. Here the authors have chronicled a stratified sequence of human occupation from the tenth to the second millennium BC, recording natural and anthropogenic strata containing artefacts and micro- and macro- palaeoecological remains, mostly in an excellent state of preservation. They present a first synthesis of the archaeological and environmental sequence for the Holocene period, define five main occupation phases f
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Ozainne, Sylvain, Laurent Lespez, Yann Le Drezen, Barbara Eichhorn, Katharina Neumann, and Eric Huysecom. "Developing a Chronology Integrating Archaeological and Environmental Data from Different Contexts: The Late Holocene Sequence of Ounjougou (Mali)." Radiocarbon 51, no. 2 (2009): 457–70. http://dx.doi.org/10.1017/s0033822200055855.

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At Ounjougou, a site complex situated in the Yamé River valley on the Bandiagara Plateau (Dogon country, Mali), multidisciplinary research has revealed a rich archaeological and paleoenvironmental sequence used to reconstruct the history of human-environment interactions, especially during the Late Holocene (3500–300 cal BC). Geomorphological, archaeological, and archaeobotanical data coming from different sites and contexts were combined in order to elaborate a chronocultural and environmental model for this period. Bayesian analysis of 54 14C dates included within the general Late Holocene s
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Linseele, Veerle. "SIZE AND SIZE CHANGE OF THE AFRICAN AUROCHS DURING THE PLEISTOCENE AND HOLOCENE." Journal of African Archaeology 2, no. 2 (2004): 165–85. http://dx.doi.org/10.3213/1612-1651-10026.

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Several assumptions on the size of the African aurochs have been tested primarily using measurements assembled from the literature. During the Holocene, the African aurochs was indeed smaller than its European and Near Eastern cousins and it appears also to have been more gracile. The available African aurochs measurements of this period probably derive mostly from male animals, since many females may have been misidentified as domestic cattle. Therefore, the degree of sexual dimorphism remains unknown, although iconographic evidence suggests that it may have been marked. Male Holocene aurochs
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Kusumgar, Sheela, Rachna Raj, L. S. Chamyal, and M. G. Yadav. "Holocene Paleoenvironmental Changes in the Lower Mahi Basin, Western India." Radiocarbon 40, no. 2 (1997): 819–23. http://dx.doi.org/10.1017/s0033822200018774.

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Evidence of paleoenvironmental changes during the Holocene from the Lower Mahi basin of Western India have been documented. The unpaired S2 surface all along the estuarine zone of the Mahi basin has been identified as an uplifted marine terrace. The terraces have preserved in their lithosections fairly distinct horizons of grayish brown clays rich in marine microfauna. The intervening silty-sand horizons are indicative of freshwater origin. The sedimentary structure and faunal assemblage indicate that these units have been deposited in a marginal marine environment. The 14C ages obtained on th
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Neumann, Katharina, Ahmed Fahmy, Laurent Lespez, Aziz Ballouche, and Eric Huysecom. "The Early Holocene palaeoenvironment of Ounjougou (Mali): Phytoliths in a multiproxy context." Palaeogeography, Palaeoclimatology, Palaeoecology 276, no. 1-4 (2009): 87–106. http://dx.doi.org/10.1016/j.palaeo.2009.03.001.

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Mees, Florias, and Eddy Keppens. "Stable isotope geochemistry of magnesite from Holocene salt lake deposits, Taoudenni, Mali." Geological Journal 48, no. 6 (2012): 620–27. http://dx.doi.org/10.1002/gj.2476.

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Dupuy, Christian, Jean Riser, and Famori Sissoko. "L'abandon du site protohistorique de Dialaka (Mali) à l'Holocène supérieur [ Early Holocene abandonment of the protohistorical site of Diakala (Mali).]." Quaternaire 6, no. 2 (1995): 57–61. http://dx.doi.org/10.3406/quate.1995.2038.

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Fabra, Mariana, and Claudina V. González. "Oral Health and Diet in Populations of Central Argentina during the Late Holocene: Bioarchaeological and Isotopic Evidence." Latin American Antiquity 30, no. 4 (2019): 818–35. http://dx.doi.org/10.1017/laq.2019.69.

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We studied the temporal and spatial variation of diet and oral health of human populations that inhabited the central region of Argentina during the Late Holocene (4000–300 BP) by evaluating isotopic data (δ13Ccol, δ15N), physiological stress indicators (tooth wear), and infectious dental diseases (caries). The sample of 49 individuals was recovered from archaeological sites located in the province of Córdoba, dated by AMS on collagen to a range of 4058 ± 89 years BP to 370 ± 15 14C years BP. After calculating the prevalence of caries and the average dental wear, we compared these values based
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Jousse, H., H. Obermaier, M. Raimbault, and J. Peters. "Late Holocene economic specialisation through aquatic resource exploitation at Kobadi in the Méma, Mali." International Journal of Osteoarchaeology 18, no. 6 (2008): 549–72. http://dx.doi.org/10.1002/oa.956.

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Dissertations / Theses on the topic "Holocène – Mali"

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Mazhoud, Farida. "Apport de l'imagerie médicale et tridimensionnelle à l'étude de restes humains datant de l'Holocène ancien (Sahara malien et mauritanien) : Analyse craniologique comparative." Thesis, Aix-Marseille, 2013. http://www.theses.fr/2013AIXM3124/document.

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L’objet de cette étude est une analyse de 32 individus néolithiques représentés par des crânes et/ou des mandibules mis au jour au Mali et en Mauritanie. Les individus composant l’échantillon ostéoarchéologique sont issus de cinq sites présentant des différences géographiques et chronologiques. En dépit de ces différences, nous nous sommes interrogés sur les liens qui pouvaient exister entre eux. Cette analyse, qui a consisté à reconsidérer les caractères morphologiques des crânes et/ou mandibules, leur variabilité, s’est appuyée sur une technologie nouvelle : l’imagerie médicale et tridimensi
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Garnier, Aline. "La dynamique d’un système fluvial et des zones humides associées en Afrique soudano-sahélienne au cours de l'Holocène : Approches géomorphologique et biogéographique. L'exemple du Yamé au Mali." Caen, 2013. https://tel.archives-ouvertes.fr/tel-01084539.

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Le système fluvial est façonné par des flux hydrologiques et de matières dont la dynamique dépend essentiellement des conditions environnementales au sein du bassin versant. Les enregistrements sédimentaires du fond de vallée représentent alors un indicateur clé de l’évolution des relations Nature/Société. Pourtant, en Afrique de l’Ouest, la recherche s’est souvent concentrée sur d’autres milieux, en particulier lacustres. Dans ce contexte, nous proposons un modèle d’évolution sur le temps long d'un système fluvial afin de s’interroger sur les variables de contrôle (naturelles et/ou anthropiqu
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Aucour, Anne-Marie. "Sedimentologie des depots lacustres holocenes de la region de taoudenni (mali) : implications paleoclimatiques." Aix-Marseille 2, 1988. http://www.theses.fr/1988AIX22043.

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L'etude des sediments lacustres holocenes de la region de taoudenni a ete realisee a partir d'etudes de terrain. Ces depots constituent un enregistrement quasi-continu des evenements climatiques holocenes. L'analyse sedimentologique (evaporites, carbonates, mineraux argileux, granulometrie et morphoscopie de la fraction detritique, fraction organique, diatomees) permet de preciser le role des facteurs climatiques dans l'alimentation et le fonctionnement des differents bassins lacustres etudies. Elle conduit a schematiser les fluctuations sedimentaires et lacustres aux echelles de temps 10**(4)
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Books on the topic "Holocène – Mali"

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Paleoenvironnements du Sahara: Lacs holocenes a Taoudenni (Mali). Diffusion, Presses du CNRS, 1991.

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Book chapters on the topic "Holocène – Mali"

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"Landmines, drugs and justice. The recent history of two Saharan mountains (Adrar des Iforas/Mali and Air Mts./Niger)." In Holocene Palaeoenvironmental History of the Central Sahara. CRC Press, 2009. http://dx.doi.org/10.1201/9780203874899-18.

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Ousseïni, Issa, Aboubacar Adamou, and Erhard Schulz. "Landmines, drugs and justice. The recent history of two Saharan mountains (Adrar des Iforas/Mali and Air Mts./Niger)." In Holocene Palaeoenvironmental History of the Central Sahara. CRC Press, 2009. http://dx.doi.org/10.1201/9780203874899.ch13.

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"Given the sample bias towards Sicilian sites, it is difficult to see any consistent regional differences expressed in burial practices. The start of burial and occupation at the three north Sicilian sites at around the beginning of the Holocene however, suggests that the appearance of these practices (in the archaeological record) may be related to particular circumstances of changed mobility within, and use of, the changing landscape in this area; earlier burials are known from peninsular Italy (Mussi 1986; 1987). Although the list is necessarily incomplete and the dating is uncertainly biassed, there is a suggestion in the figures as presented that burial in caves may have been confined to, or more common in, the final LUP and earlier Mesolithic; burial practice, at least in terms of place, may have been changing by the later Mesolithic. Interestingly, caves with Epipalaeolithic burials do not show continuity of use for the same practice into the Neolithic: different sites are chosen (see below). Arguments against marked regional differentiation are the generally similar burial position, and the occurrence of identical types of perforated deer teeth from Puglia and Sicilia. The perforated tooth from the Grotta del Cavallo in Puglia probably relates to the late Romanellian, perhaps at circa 10000-8000 cal.BC; those from the Grotta Romanelli to a similar date. Equivalence of practice, of course, does not necessarily correlate with equivalence of meaning, as is suggested by the different faunal contexts of these finds. The main hunted animals in Puglia were generally equids and bovines, but deer and pig in Sicilia. Discussion Italian Late Upper Palaeolithic and Mesolithic burials have been discussed by Mussi (1986; 1987), Mussi et al. (1989) and Zampetti & Mussi (1991). Although most of the burials are from outside the study area (mostly in Liguria), Mussi (1987) includes the Grotta di San Teodoro and Grotta delPUzzo (SIC), and the Grotta del Romito (CAL). She considers differences to reflect different emphases and conditions of social reproduction (1987: 45ff). In scheme A only certain sex-age individuals were buried, perhaps related to the circumstances of their death. She suggests that male hunters are represented at the Grotta di San Teodoro (although revision now suggests three tentatively identified females: Mussi 1987: 46; Fabbri 1993). In contrast, the burials at the Grotta del Romito represent scheme C, with both males and females, reflecting increased emphasis on social reproduction through exogamy (Mussi 1987: 47-8). She also notes the apparent contemporaneity of the first occupation and burials at the Grotta di San Teodoro, and argues that this represents the "colonisation" of Sicilia at a time when it was still "almost deserted" (Mussi 1987: 47-8). A similar argument is expanded by Zampetti & Mussi (1991), in which they also consider the evidence of 'art'. They argue that in the early Late Upper Palaeolithic there were burials of high-status individuals, perhaps related to control of information and partner exchange in a sparsely-populated landscape (Mussi 1987: 156). By the final Late Upper Palaeolithic they argue that there is more evidence of concern with descent, perhaps more stabilised (partner) exchange networks, and less evidence of pre-eminent individuals in the burials (Mussi 1987: 157). Stimulating though their interpretations are, in attempting to relate burial modes to changing social organisation and mapping of the social landscape, one might criticise some of the work in detail: for example, the burials from the Grotta del Romito are difficult to visualise as partners (see below). Any interpretation must be preceded by the realisation that the sample is extremely small and is already uncertainly biassed by accidents of excavation. Only certain people may have been buried; and the survival and excavation of burial (or other disposal sites) may be skewed. Thirdly, the representation of remains within those sites may be biassed, for example by the lower survival rates of infant and child remains. However, assuming that the sample is at least partly representative of the practices surrounding the dead, the following suggestions may be made." In Gender & Italian Archaeology. Routledge, 2016. http://dx.doi.org/10.4324/9781315428178-17.

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