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Journal articles on the topic 'Littoraux – Mauritanie'

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Author: Grafiati
Published: 7 July 2024

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1

Thibaud, Jean-Marc. "Étude des Collemboles (Hexapoda) Interstitiels des Sables Littoraux de Mauritanie." Annales de la Société entomologique de France (N.S.) 32, no. 4 (December 31, 1996): 475–79. http://dx.doi.org/10.1080/21686351.1996.12279171.

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2

Caussanel, Claude, A. t. Dia, André Nel, Issac Ould Bouraya, and Jean-marc Thibaud. "Prospection préliminaire de la biodiversité des Insectes des sables littoraux de Mauritanie." Bulletin de la Société entomologique de France 102, no. 1 (1997): 67–72. http://dx.doi.org/10.3406/bsef.1997.17308.

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3

Gushchin, A. V., and Khallagi Ould Mokhamad Fall. "Ichthyofauna of littoral of the gulf Arguin, Mauritania." Journal of Ichthyology 52, no. 2 (March 2012): 160–71. http://dx.doi.org/10.1134/s0032945212010055.

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4

Thiam, Aboubakry. "Le Littoral Sud de la Mauritanie entre Conservation et Aménagement." مجلة الدراسات التاريخية و الاجتماعية, no. 3 (2014): 21–32. http://dx.doi.org/10.12816/0012813.

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5

Mareï, Nora, and Jérôme Lombard. "Tous les chemins mènent à Nouakchott. Routes, usages et territoires dans la Mauritanie contemporaine." Flux 135-136, no. 1 (June 30, 2024): 59–88. http://dx.doi.org/10.3917/flux1.135.0059.

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Abstract:
Alors que les infrastructures ont servi de support au développement territorial de la Mauritanie, depuis la route de Rosso jusqu’à celle de Nouadhibou, sans compter les plus récentes qui longent le fleuve Sénégal au sud ou qui, au centre, relient Atar et Tidjikja, il convient de regarder autrement leurs effets sur les circulations de personnes et de marchandises qui se déploient à l’intérieur comme à l’extérieur du pays. Nouakchott, capitale créée ex-nihilo au moment de l’indépendance, devient au rythme des transformations du pays un carrefour singulier. Les grandes routes du pays rayonnent, depuis ce pôle urbain, selon trois orientations principales : un axe littoral Nord-Sud, maillon des relations entre Maroc, Mauritanie et Sénégal ; la route vers Tindouf en Algérie, qui nous projette, dans le jeu diplomatique régional ; la route de l’Espoir enfin ou Transmauritanienne qui traverse le sud du pays d’ouest en est, jusqu’aux portes du Mali. En tentant de dépasser l’image que se donne la Mauritanie en Afrique de l’Ouest, celle d’un pays reliant ses voisins les uns aux autres, notre objectif est de saisir la manière dont, dans l’histoire récente du pays, les pouvoirs politiques successifs ont construit le réseau d’infrastructures, et surtout l’usage qu’en font les différentes catégories de la population mauritanienne.
6

Gushchin, A. V. "Feeding offish young on the littoral of the Gulf Arguin (Mauritania)." Вопросы ихтиологии 53, no. 6 (2013): 718–25. http://dx.doi.org/10.7868/s0042875213050068.

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7

Gushchin, A. V. "Feeding of fish young from littoral of the gulf Arguin (Mauritania)." Journal of Ichthyology 53, no. 9 (November 2013): 731–38. http://dx.doi.org/10.1134/s0032945213050068.

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8

Boulay, Sebastien. "Le savoir-faire des femmes Imrâgen du littoral mauritanien à l'épreuve de la mondialisation." Revue d'anthropologie des connaissances 5, 3, no. 3 (2011): 492. http://dx.doi.org/10.3917/rac.014.0492.

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9

Toure, A., C. Diop, M. Cabral, M. Diop, E. Ould Ahmed, F. Sagna, M. Ould Mahmoud, A. Kane, M. Fall, and A. Diouf. "Détermination de la teneur en métaux lourds de différents produits halieutiques du littoral sénégalo-mauritanien." Toxicologie Analytique et Clinique 28, no. 2 (June 2016): S46. http://dx.doi.org/10.1016/j.toxac.2016.03.079.

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10

Barusseau, J. P., R. Certain, R. Vernet, and J. F. Saliège. "Late Holocene morphodynamics in the littoral zone of the Iwik Peninsula area (Banc d'Arguin — Mauritania)." Geomorphology 121, no. 3-4 (September 2010): 358–69. http://dx.doi.org/10.1016/j.geomorph.2010.05.006.

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11

Gushchin, A. V., and P. C. Goudswaard. "Distribution of the Common Cockle Cerastoderma edule (Linnaeus 1758) (Molluska: Bivalvia) in the Littoral Zone of Levrier Bay, Mauritania." Biology Bulletin 48, no. 7 (December 2021): 959–66. http://dx.doi.org/10.1134/s106235902107013x.

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12

Barusseau, Jean-Paul, Raphaël Certain, Robert Vernet, and Jean-François Saliège. "Morphosedimentological record and human settlements as indicators of West-African Late Holocene climate variations in the littoral zone of the Iwik peninsula (Banc d’Arguin – Mauritania)." Bulletin de la Société Géologique de France 180, no. 5 (September 1, 2009): 449–56. http://dx.doi.org/10.2113/gssgfbull.180.5.449.

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Abstract:
Abstract The geomorphological, sedimentological and archaeological studies of coastal features in the Iwik-Aouatil area show two categories of coastal sedimentary units: very extensive sand flats and linear relief features covered by a thin veneer of anthropogenic Anadara senilis shell-middens. These units provide an opportunity to discuss the return to arid conditions in western Sahara during the Late Holocene, when climate changes induced the alternating occurrence of more or less dry episodes, from around 5 ka until today. These constructions reflect the global climate change within the general framework known for the region. Two different processes occurred: (1) constant deposition of wide sand-flats and (2) construction of sedimentary ridges at specific moments. These processes demonstrate the existence of (1) constant sand discharge during the whole period as sand availability is not a limiting factor and (2) a substantially increased sand influx during the 4.2-3.2 ka episode. Because of sea-level stability in the Banc d’Arguin area during the Late Holocene, the variability of morphogenetic agents is considered to be the likely cause of fluctuations, influencing sand input rate and implying that either sand was delivered in greater abundance (aridity crisis and stronger winds) or littoral drift was more powerful (stronger waves and more frequent storms in the northern part of the Atlantic ocean), or both simultaneously. The action of these two driving forces in the depositional processes observed in the Iwik-Aouatil coastal plain is evaluated with respect to the occurrence of episodes of rapid climate changes (RCCs) and North Atlantic Oscillation (NAO) changes. A climate pattern combining episodes of RCC and NAO positive (NAO+) index during the 4.5-3.2 ka period is convenient for both sand supply, which accelerates the southwestward migration of barchan’s lines, and sand transportation, which improves the efficiency of the littoral drift.
13

Foster, Noel. "Sébastien Boulay and Bruno Lecoquierre,Le Littoral mauritanien à l'aube du XXIe siècle : Peuplement, gouvernance de la nature, dynamiques sociales et culturelles." Journal of North African Studies 17, no. 4 (September 2012): 728–30. http://dx.doi.org/10.1080/13629387.2012.686300.

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14

Sidoumou, Z., M. Roméo, M. Gnassia-Barelli, Ph Nguyen, and R. Caruba. "Détermination de la qualité des eaux du littoral mauritanien par la mesure des métaux traces chez les mollusques Donax rugosus et Venus verrucosa." Hydroécologie Appliquée 4 (1992): 33–41. http://dx.doi.org/10.1051/hydro:1992204.

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15

Sterrenburg, F. A. S., and F. J. G. Sterrenburg. "An Outline of the Marine Littoral Diatom Biocoenosis of the Banc d’Arguin, Mauritania, West Africa." Botanica Marina 33, no. 5 (1990). http://dx.doi.org/10.1515/botm.1990.33.5.459.

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