Le Tchad Des Lacs Les Zones Humides Sahéliennes Au Défi Du Changement Global Christine Raimond, Florence Sylvestre, Dangbet Zakinet Et Abderamane Moussa (Éd.)

Total Page:16

File Type:pdf, Size:1020Kb

Le Tchad Des Lacs Les Zones Humides Sahéliennes Au Défi Du Changement Global Christine Raimond, Florence Sylvestre, Dangbet Zakinet Et Abderamane Moussa (Éd.) Le Tchad des lacs Les zones humides sahéliennes au défi du changement global Christine Raimond, Florence Sylvestre, Dangbet Zakinet et Abderamane Moussa (éd.) DOI : 10.4000/books.irdeditions.30450 Éditeur : IRD Éditions Lieu d'édition : Marseille Année d'édition : 2019 Date de mise en ligne : 29 août 2019 Collection : Synthèses ISBN électronique : 9782709927161 http://books.openedition.org Édition imprimée Date de publication : 1 juin 2019 ISBN : 9782709927154 Nombre de pages : 368 Référence électronique RAIMOND, Christine (dir.) ; et al. Le Tchad des lacs : Les zones humides sahéliennes au défi du changement global. Nouvelle édition [en ligne]. Marseille : IRD Éditions, 2019 (généré le 21 décembre 2020). Disponible sur Internet : <http://books.openedition.org/irdeditions/30450>. ISBN : 9782709927161. DOI : https://doi.org/10.4000/books.irdeditions.30450. © IRD Éditions, 2019 Conditions d’utilisation : http://www.openedition.org/6540 Le Tchad des lacs Les zones humides sahéliennes au défi du changement global Christine Raimond, Florence Sylvestre, Dangbet Zakinet et Abderamane Moussa (éd.) Éditeur : IRD Éditions Lieu d'édition : Marseille Année d'édition : 2019 Date de mise en ligne : 29 août 2019 Collection : Synthèses http://books.openedition.org Édition imprimée Date de publication : 1 juin 2019 Nombre de pages : 368 Ce document vous est offert par OpenEdition Center USR 2004 Référence électronique RAIMOND, Christine (dir.) ; et al. Le Tchad des lacs : Les zones humides sahéliennes au défi du changement global. Nouvelle édition [en ligne]. Marseille : IRD Éditions, 2019 (généré le 29 août 2019). Disponible sur Internet : <http://books.openedition.org/irdeditions/30450>. © IRD Éditions, 2019 Conditions d’utilisation : http://www.openedition.org/6540 Le Tchad des lacs Les zones humides sahéliennes au défi du changement global Le Tchad des lacs Les zones humides sahéliennes au défi du changement global Éditeurs scientifiques Christine RAIMOND, Florence SYLVESTRE, Dangbet ZAKINET, Abderamane MOUSSA Ce volume a bénéficié du soutien financier de l’Ambassade de France au Tchad. IRD Éditions INSTITUT DE RECHERCHE POUR LE DÉVELOPPEMENT Collection Synthèses Marseille, 2019 Coordination éditoriale Sylvie Hart Préparation éditoriale Stéphanie Quillon (34) Mise en page Desk (53) Maquette de couverture Michelle S aint-Léger Maquette intérieure Pierre Lopez Photo de couverture Livraison de fourrage à Yao. L’augmentation des populations sédentaires et transhumantes et de leur bétail accroît fortement la pression sur les ressources (Yao, février 2016). © CNRS/M. Schuster p. 4 de couverture Multifonctionnalité de l’espace en bordure du lac Fitri (Gamsa, janvier 2016). Les jardins maraîchers et la pêche entravent le passage saisonnier des troupeaux vers les bourgoutières sur les îles. © CNRS/C. Raimond La loi du 1er juillet 1992 (code de la propriété intellectuelle, première partie) n’autorisant, aux termes des alinéas 2 et 3 de l’article L. 122-5, d’une part, que les « copies ou reproductions strictement réser- vées à l’usage du copiste et non destinées à une utilisation collective » et, d’autre part, que les analyses et les courtes citations dans le but d’exemple ou d’illustration, « toute représentation ou reproduction intégrale ou partielle faite sans le consentement de l’auteur ou de ses ayants droit ou ayants cause, est illicite » (alinéa 1er de l’article L. 122-4). Cette représentation ou reproduction, par quelque procédé que ce soit, constituerait donc une contre- façon passible des peines prévues au titre III de la loi précitée. © IRD, 2019 ISBN : 978-2-7099-2715-4 Composition du comité scientifique Likius ANDOSSA Abderamane MOUSSA paléontologue, université de N’Djamena, géologue, université de N’Djamena, Tchad Tchad Sougnabé PABAME Ali Brahim BECHIR socioéconomiste, Institut de recherche pastoraliste, Institut national d’élevage en élevage pour le développement, Tchad de Moussoro, Tchad Christine RAIMOND Tchago BOUIMON géographe, Centre national archéologue, université de N’Djamena, de la recherche scientifique, France Tchad Frédéric REOUNODJI Mirjam de BRUIJN géographe, ministère de l’Enseignement anthropologue, université de Leyde, supérieur et de l’Innovation, Tchad Pays-Bas Mathieu SCHUSTER Guillaume FAVREAU géologue, Centre national de la recherche hydrogéochimiste, Institut de recherche scientifique, France pour le développement, Niger Florence SYLVESTRE Abderamane HAMIT paléoclimatologue, Institut de recherche hydrogéochimiste, université pour le développement, France de N’Djamena, Tchad Christine VALLET-COULOMB Olivier LANGLOIS hydrogéochimiste, Aix-Marseille Université, archéologue, Centre national France de la recherche scientifique, France Nicolas WALDMANN Jacques LEMOALLE paléoclimatologue, université Haifa, Israel hydroécologue, Institut de recherche pour le développement, France Dangbet ZAKINET chef de mission, lac Fitri, historien, Robert MADJIGOTO université de N’Djamena, Tchad géographe, université de N’Djamena, Tchad Géraud MAGRIN géographe, université Paris 1 Panthéon-Sorbonne, France Sommaire Préface ................................................................. 11 Remerciements ......................................................... 13 Introduction ........................................................... 15 Christine Raimond, Florence Sylvestre, Dangbet Zakinet, Abderamane Moussa Partie 1 Les lacs tchadiens du Pléistocène à l’Anthropocène........... 33 Introduction ........................................................... 35 Christine Raimond, Florence Sylvestre Chapitre 1 Changements environnementaux et climatiques à la période humide africaine Holocène dans le bassin du lac Fitri (Tchad) ................................................... 39 Mathieu Schuster, Florence Sylvestre, Christine Raimond, Abderamane Moussa, Yassine Abakar, Tashi Yalikun Chapitre 2 Paléoenvironnements et variations paléohydrologiques du lac Tchad au cours des 12 000 dernières années ................ 53 Florence Sylvestre, Pierre Deschamps, Adoum Bari Sinine, Remadji Rirongarti, Jean-Charles Mazur, Nicolas Waldmann, Paula do Amaral, Camille Bouchez, Jean-Claude Doumnang Chapitre 3 Des hommes et des lacs. Peuplement des zones lacustres du Borkou (Tchad) à l’Holocène ........................................................... 65 Yves Gauthier, Christine Gauthier Le Tchad des lacs Chapitre 4 Mission archéologique franco-tchadienne aux lacs d’Ounianga (Tchad). Principaux résultats des deux premières missions de terrain .............................................................. 85 Vincent Mourre, Guemona Djimet, Tchago Bouimon, Marie-Pierre Coustures, Barbara Eichhorn, Jean Mbairo, Caroline Robion-Brunner, Margareta Tengberg Chapitre 5 Variabilité des crues et des paysages du lac Fitri depuis les grandes sécheresses des années 1970-1980 ............. 99 Tashi Yalikun, Christine Raimond, Angeline Kemsol Nagorngar, Dangbet Zakinet, Mathieu Schuster, Florence Sylvestre Partie 2 Dynamique des socioécosystèmes lacustres ................... 121 Introduction ........................................................... 123 Christine Raimond, Florence Sylvestre Chapitre 6 Les lacs d’Ounianga. Mieux comprendre leur dynamique hydrologique et écologique par une approche interdisciplinaire .................. 127 Thijs Van der Meeren, Pierre Deschamps, Florence Sylvestre, Baouyé Kemkong, Abderamane Moussa, Mathieu Schuster, Dirk Verschuren Chapitre 7 Étude de la dynamique hydrologique des lacs Iro et Fitri par une approche isotopique ......................................... 139 Chloé Poulin, Bruno Hamelin, Christine Vallet-Coulomb, Guinbé Amngar, Bichara Loukman, Jean-François Crétaux, Jean-Claude Doumnang, Abdallah Mahamat Nour, Guillemette Menot, Florence Sylvestre, Pierre Deschamps Chapitre 8 Caractérisation des paramètres physicochimiques des eaux souterraines de la région du lac Iro ....................... 155 Guinbé Amngar, Abderamane Hamit Chapitre 9 Fluctuation des récoltes de sorgho repiqué et potentialités de culture. Une analyse par télédétection dans la région du lac Fitri ......... 173 Angeline Kemsol Nagorngar, Christine Raimond, Robert Madjigoto, Valère Jofack Sokeng, Datoloum Djimassal, Joseph Libar, Fernand Kouamé Koffi 8 Sommaire Chapitre 10 La végétation pastorale du lac Fitri. État des lieux et dynamique. 189 Ali Brahim Béchir, Koussou Mian-Oudanang, Alhassine Mahamat, Tchoudiba Bourdjolbo Partie 3 Gouvernance des territoires, logiques sociales et hétérogénéité des acteurs .................................... 203 Introduction ........................................................... 205 Christine Raimond, Florence Sylvestre, Dangbet Zakinet Chapitre 11 Évolution technologique et gestion d’un espace halieutique dans la cuvette nord du lac Tchad ................................... 209 Hadiza Kiari Fougou, Jacques Lemoalle Chapitre 12 De l’insécurité de Boko Haram au conflit intercommunautaire dans le lac Tchad. Le conflit Peul/Boudouma au Niger ................................. 225 Mahamadou Abdourahamani, Maman Waziri Mato Chapitre 13 Pratiques et enjeux de la sécurisation foncière autour du lac Fitri ..................................................... 239 Audrey Mbagogo Koumbraït Chapitre 14 Économie des échanges au lac Fitri. Un déficit récurrent en produits alimentaires ...................... 253 Blaise Bémadji, Ngaressem Goltob Mbaye Chapitre 15 Les territoires d’eau ou comment gérer les ressources halieutiques dans les espaces lacustres ? Les lacs Fitri et Iro ...................................................
Recommended publications
  • Marbled Teal Marmaronetta Angustirostris on the Ounianga Lakes in Chad 35-42 Ornithol
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Ornithologische Jahresberichte des Museum Heineanum Jahr/Year: 2009 Band/Volume: 27 Autor(en)/Author(s): Schönbrodt Robert Artikel/Article: Marbled Teal Marmaronetta angustirostris on the Ounianga lakes in Chad 35-42 Ornithol. Jber. Mm. Heineanum 27 (2009): 35-42 Marbled Teal Marmaronetta angustirostris on the Ounianga lakes in Chad Marmelenten Marmaronetta angustirostris auf den Ounianga-Seen im Tschad (Sahara) Robert Schönbrodt At the turn of the year 2008/2009 I took part in a three week expedition to northern Chad. The itinerary included oases and lakes north west of the Mourdi Depression: a.m. 4 Jan 2009 the Demi Oasis, and in the afternoon and evening the uninhabited Teguedei Oasis and Saline followed by Lake Boko. Lake Boko was again visited early on 6 Jan followed by the south shore of Lake Ounianga Serir Osaia, at midday Lake Katam and in the afternoon the Ounianga Kebir Oasis and the east shore of Lake Ou­ nianga Kebir (Lake Yoa). Early on 6 Jan the expedition visited a small lake east of the Ounianga Kebir Oasis and later a stretch of shore on the southern edge of Lake Yoa. On 5 and 6 Jan 2009 some 525 Marbled Teal were observed on three of the lakes - a surprisingly high number but nonetheless a minimum figure. Due to the short and random observation stops, and as not all lakes in the complex were visited, a number of Marbled Teal probably remained undetected. Nonetheless, the numbers quoted qua­ lifies the Ounianga Lake complex (from N 19°037E 20°29’ to N 18°547E 20°54’) as an important Marbled Teal settlement sites, probably not described to date.
    [Show full text]
  • Climatic Changes and Cultural Responses During the African
    Climatic Changes and Cultural Responses During the African Humid Period Recorded in Multi-Proxy Data David McGee, Massachusetts Institute of Technology, Cambridge MA USA Peter deMenocal, Columbia University, New York, NY USA Oxford Research Encyclopedia of Climate Science, 2017, doi: 10.1093/acrefore/9780190228620.013.529 Summary The expansion and intensification of summer monsoon precipitation in North and East Africa during the African Humid Period (AHP; c. 15,000–5,000 years before present) is recorded by a wide range of natural archives, including lake and marine sediments, animal and plant remains, and human archaeological remnants. Collectively this diverse proxy evidence provides a detailed portrait of environmental changes during the AHP, illuminating the mechanisms, temporal and spatial evolution, and cultural impacts of this remarkable period of monsoon expansion across the vast expanse of North and East Africa. The AHP corresponds to a period of high local summer insolation due to orbital precession that peaked at ~11–10 ka, and it is the most recent of many such precessionally paced pluvial periods over the last several million years. Low-latitude sites in the North African tropics and Sahel record an intensification of summer monsoon precipitation at ~15 ka, associated with both rising summer insolation and an abrupt warming of the high northern latitudes at this time. Following a weakening of monsoon strength during the Younger Dryas cold period (12.9–11.7 ka), proxy data point to peak intensification of the West African monsoon between 10–8 ka. These data document lake and wetland expansions throughout almost all of North Africa, expansion of grasslands, shrubs and even some tropical trees throughout much of the Sahara, increases in Nile and Niger River runoff, and proliferation of human settlements across the modern Sahara.
    [Show full text]
  • Palynological Evidence for Gradual Vegetation and Climate Changes During the African Humid Period Termination at 13◦ N from a Mega-Lake Chad Sedimentary Sequence
    Clim. Past, 9, 223–241, 2013 www.clim-past.net/9/223/2013/ Climate doi:10.5194/cp-9-223-2013 of the Past © Author(s) 2013. CC Attribution 3.0 License. Palynological evidence for gradual vegetation and climate changes during the African Humid Period termination at 13◦ N from a Mega-Lake Chad sedimentary sequence P. G. C. Amaral1, A. Vincens1, J. Guiot1, G. Buchet1, P. Deschamps1, J.-C. Doumnang2, and F. Sylvestre1 1CEREGE, Aix-Marseille Universite,´ CNRS, IRD, College` de France, Europoleˆ Mediterran´ een´ de l’Arbois, BP 80, 13545 Aix-en-Provence cedex 4, France 2Departement´ des Sciences de la Terre, Universite´ de N’Djamena (UNDT) BP 1027 N’Djamena, Chad Correspondence to: P. G. C. Amaral ([email protected]) Received: 16 May 2012 – Published in Clim. Past Discuss.: 18 June 2012 Revised: 18 December 2012 – Accepted: 19 December 2012 – Published: 29 January 2013 Abstract. Located at the transition between the Saharan and period. However, we cannot rule out that an increase of Sahelian zones, at the center of one of the largest endorheic the Chari–Logone inputs into the Mega-Lake Chad might basins, Lake Chad is ideally located to record regional envi- have also contributed to control the abundance of these taxa. ronmental changes that occurred in the past. However, until Changes in the structure and floristic composition of the veg- now, no Holocene archive was directly cored in this lake. etation towards more open and drier formations occurred In this paper, we present pollen data from the first sed- after ca. 6050 cal yr BP, following a decrease in mean Pann imentary sequence collected in Lake Chad (13◦ N; 14◦ E; estimates to approximately 600 (−230/+600) mm.
    [Show full text]
  • Modern and Early Holocene Mollusc Fauna of the Ounianga Lakes (Northern Chad): Implications for the Palaeohydrology of the Central Sahara
    JOURNAL OF QUATERNARY SCIENCE (2011) 26(4) 433–447 ISSN 0267-8179. DOI: 10.1002/jqs.1469 Modern and early Holocene mollusc fauna of the Ounianga lakes (northern Chad): implications for the palaeohydrology of the central Sahara BERT VAN BOCXLAER,1,2* DIRK VERSCHUREN,2 GEORG SCHETTLER3 and STEFAN KRO¨ PELIN4 1Research Unit Palaeontology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281-S8, B-9000 Ghent, Belgium 2Limnology Unit, Department of Biology, Ghent University, Ghent, Belgium 3GeoForschungsZentrum Potsdam, Potsdam, Germany 4African Archaeology Unit, Institute of Prehistoric Archaeology, University of Cologne, Ko¨ln, Germany Received 28 April 2010; Revised 20 October 2010; Accepted 22 October 2010 ABSTRACT: The fresh and saline lakes of Ounianga Kebir and Serir in northeastern Chad are among the very few permanent aquatic ecosystems currently existing in the hyper-arid core of the Sahara desert. The confirmed modern fauna of aquatic molluscs at Ounianga comprises three widespread species (Melanoides tuberculata, Biomphalaria pfeifferi and Lymnaea natalensis), of which only the first appears to maintain a thriving population. We recovered seven more species of gastropods, among which one is new to science (Gabbiella ouniangaensis), and one bivalve species from early Holocene outcrops of diatomaceous limestone at Ounianga Serir. All species except one are known to be commonly spread between lake and river systems by birds, and in its entirety this species-rich fossil mollusc fauna of Ounianga Serir resembles that of other Saharan lake sites known to have been hydrologically isolated during the early Holocene. The impoverished modern mollusc fauna, which lacks even the widespread and opportunistic species Bulinus truncatus, may have become established relatively recently through new colonisation events, following eradication of the early Holocene mollusc fauna during a later episode of high salinity or desiccation.
    [Show full text]
  • Climat De L'afrique Du Nord Pendant L'holocène Vendredi 16 Mai 2014 8H50-18H45 Holocene North African Climate
    t Colloque de séminaires organisé par Colloque de séminaires organisé par CHAIRE ÉVOLUTION DU CLIMAT ET CHAIREDE L’OCÉ ÉVOLUTIONAN DU CLIMAT ET DE L’OCÉAN M. Édouard BARD, Professeur M. Édouard BARD, Professeur Année académique 2013-2014 Année académique 2011-2012 Climat de l’Afrique du Nord L’océan et le changement climatique : pendant l’Holocène Michel Dukhan / variations de la circulation océanique © IRD OceanHolocene and North climate African change: Climate variations in the ocean circulation © É. Bard Vendredi 16 mai 2014 Vendredi8h50-18h45 30 mars 2012 08h50 Édouard BARD et Peter 9h00-18h30 de MENOCAL Introduction 09h00 Édouard BARD (Collège de France & CEREGE d’Aix-en-Provence) An Introduction on North African Climate Viewed from Geological Archives 9h00 Édouard BARD (Collège de France & CEREGE, Aix-en-Provence) 09h45 Stefan KROEPELIN (Université de Cologne) IntroductionGeoarchaeological and paleoceanographic and Lake Yoa Data Sets perspective from the Eastern Sahara vs. Abrupt Onset 10h00 Gillesand REVERDINTermination of (CNRS, the So-Called Laboratoire “African d’OcéanographieHumid Period” et du Climat, IPSL, 4, 10h30 PlaceFlorence Jussieu, SYLV ESParis)TRE (IRD & CEREGE d’Aix-en-Provence) AtlanticNorthern surface Tropics currents Monsoonal Changes during the African Humid Period Revealed by Lake Chad Sedimentary Archives 11h00 Harry BRYDEN (School of Ocean and Earth Science, Université de Southampton) 11h15 Jessica TIERNEY (Woods-Hole Oceanographic Institution, USA) VariabilityBiomarker in Evidence the deep for circulationAbrupt
    [Show full text]
  • View on All the Lakes, of Which the Colours Contrast with the Sand Dunes Separated by Bare Rock Structures (World Heritage Committee, 2012)
    IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Lakes of Ounianga - 2020 Conservation Outlook Assessment Lakes of Ounianga 2020 Conservation Outlook Assessment SITE INFORMATION Country: Chad Inscribed in: 2012 Criteria: (vii) The site includes eighteen interconnected lakes in the hyper arid Ennedi region of the Sahara desert covering an area of 62,808 ha. It constitutes an exceptional natural landscape of great beauty with striking colours and shapes. The saline, hyper saline and freshwater lakes are supplied by groundwater and are found in two groups 40 km apart. Ounianga Kebir comprises four lakes, the largest of which, Yoan, covers an area of 358 ha and is 27 m deep. Its highly saline waters only sustain algae and some microorganisms. The second group, Ounianga Serir, comprises fourteen lakes separated by sand dunes. Floating reeds cover almost half the surface of these lakes reducing evaporation. At 436 ha, Lake Teli has the largest surface area but is less than 10 m deep. With their high quality freshwater, some of these lakes are home to aquatic fauna, particularly fish. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 02 Dec 2020 GOOD The values of the site are in good condition and there have been no signs of decline since inscription of the site in 2012. The level of threats remains low and there are no immediate threats to the Outstanding Universal Value of the site. Natural processes such as the siltation of the small two eastern lakes of Ounianga Kebir and dune encroachment into most of the other lakes persist, of course, in this hyperarid environment, but actions are being undertaken to address dunes encroachment.
    [Show full text]
  • Of 59 Accepted Version 1 Last Updated 25-Apr-2018 2 3 a Late Holocene
    Page 1 of 59 1 Accepted version 2 Last updated 25-Apr-2018 3 4 A late Holocene palaeoenvironmental ‘snapshot’ of the Angamma Delta, Lake 5 Megachad at the end of the African Humid Period. 6 7 Charlie S. Bristow1, Jonathan A. Holmes2, Dave Mattey3, Ulrich Salzmann4, Hilary J. 8 Sloane5 9 10 1. Department of Earth and Planetary Sciences, Birkbeck University of London, 11 Malet Street, London WC1E 7HX 12 2. Environmental Change Research Centre, Department of Geography, University 13 College London, Gower Street, London, WC1E 6BT, UK 14 3. Department of Earth Sciences, Royal Holloway, University of London, Egham, 15 Surrey, TW20 0EX, UK 16 4. Department of Geography and Environmental Sciences, Northumbria University, 17 Ellison Place, Newcastle upon Tyne, NE1 8ST, UK 18 5. NERC Isotope Geosciences Facilities, British Geological Survey, Keyworth, 19 Nottingham, NG12 5GG, UK 20 21 22 Keywords: Holocene; Palaeoecology; Sedimentology; Stable isotopes; Central 23 Africa; Lake Megachad 24 25 Page 2 of 59 26 Abstract 27 During the African Humid Period (AHP) there was a dramatic increase in the area of 28 lakes and wetlands. Lake Megachad, one of several huge lakes, underwent dramatic 29 fluctuations during the AHP prior to regression in the mid Holocene. However, the 30 timing and nature of AHP termination has been disputed. We present evidence from 31 sediments of the Angamma Delta, from the northern end of the palaeolake, for Lake 32 Megachad lake-level fluctuations at the end of the AHP. Delta slope deposits were 33 deposited over 7000 cal BP at the height of the AHP.
    [Show full text]
  • Considerations of Wildlife Resources and Land Use in Chad
    Productive Sector Growth and Environment Division Office of Sustainable Development Bureau for Africa U.S. Agency for International Development Considerations of Wildlife Resources and Land Use in Chad James O. Keith Darrel C. H. Plowes Environmental Consultants SD Technical Paper No. 45 March 1997 Productive Sector Growth and Environment Division Office of Sustainable Development Bureau for Africa U.S. Agency for International Development Considerations of Wildlife Resources and Land Use in Chad James O. Keith Darrel C. H. Plowes Environmental Consultants March 1997 Publication services provided by AMEX International, Inc. Pursuant to the following USAID contract: Project Title: Policy, Analysis, Research, and Technical Support Project Project Number: 698-0478 Contract Number: AOT-0678-C-00-6066-00 Contents Foreword v Acknowledgments vii Executive Summary ix Glossary of Acronyms and Abbreviations xi Introduction 1 Animals and Plants of Chad 3 Birds of Chad 3 Mammals of Chad 3 Fishes of Chad 3 Reptiles and amphibians of Chad 3 Invertebrates of Chad 4 Plants of Chad 4 Biogeographic Regions of Chad 5 Northern Deserts and Mountains 5 Central Shrub Steppe 6 Southern Savanna Woodlands 6 Rivers and Flood Plains 7 Lakes 8 Wildlife Management in Chad 11 Organization and Activities 11 National Parks and Faunal Reserves 12 Human Agricultural Activities 15 Agricultural Impact on Wildlife 17 Habitat Alteration through Clearing for Agriculture 17 Shortening of Fallow Cycles 17 Intensification of Agricultural Management 17 Habitat Alteration due to Water Pollution 17 Toxicity Hazards of Iinsecticides 18 Use of Agrochemicals in Chad 18 Critical Wildlife Habitats 21 Lakes and Savanna Wetlands 21 The Tibesti and Ennedi Mountains of the North 22 National Parks and Faunal Reserves 22 iii Threatened Vertebrates of Chad 23 Mammals 23 Birds 23 Reptiles 24 References 25 FIGURES 1.
    [Show full text]
  • Humans As Agents in the Termination of the African Humid Period
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Frontiers - Publisher Connector REVIEW published: 26 January 2017 doi: 10.3389/feart.2017.00004 Humans as Agents in the Termination of the African Humid Period David K. Wright * Department of Archaeology and Art History, Seoul National University, Seoul, South Korea There is great uncertainty over the timing and magnitude of the termination of the African Humid Period (AHP). Spanning from the early to middle Holocene, the AHP was a period of enhanced moisture over most of northern and eastern Africa. However, beginning 8000 years ago the moisture balance shifted due to changing orbital precession and vegetation feedbacks. Some proxy records indicate a rapid transition from wet to dry conditions, while others indicate a more gradual changeover. Heretofore, humans have been viewed as passive agents in the termination of the AHP, responding to changing climatic conditions by adopting animal husbandry and spreading an agricultural lifestyle across the African continent. This paper explores scenarios whereby humans could be viewed as active agents in landscape denudation. During the period when agriculture was adopted in northern Africa, the regions where it was occurring were at the precipice of ecological regime shifts. Pastoralism, in particular, is argued to enhance Edited by: devegetation and regime shifts in unbalanced ecosystems. Threshold crossing events Valentí Rull, were documented in the historical records of New Zealand and western North
    [Show full text]
  • Holocene Dust Records from the West African Sahel and Their Implications
    PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Holocene dust records from the West African Sahel 10.1002/2013JD021283 and their implications for changes in climate Key Points: and land surface conditions • Holocene dust fluxes reconstructed from lake sediments at two sites in Helen E. Cockerton1, Jonathan A. Holmes2, F. Alayne Street-Perrott1, and Katherine J. Ficken1 West Africa • fl Low uxes in early Holocene followed 1Department of Geography, College of Science, Swansea University, Swansea, UK, 2Department of Geography, University by rise from around 2 kyr B.P. • Fluxes controlled by climate, sediment College London, London, UK availability, and latterly human activity Abstract We reconstructed aeolian dust accumulation during the Holocene from two radiocarbon-dated Supporting Information: lake-sediment sequences from the Manga Grasslands in northeastern Nigeria in order to investigate long-term • Readme • Text S1 changes in the Harmattan dust system over West Africa and evaluate their possible causes. Flux values • Table S1 were low in the early Holocene, decreasing further to a minimum at around 6.2 kyr B.P. after which time they increased, steadily until around 2 kyr B.P. and then more sharply after this time. The long-term Correspondence to: variations in dust flux agree broadly with changes in the exposed area of the Lake Chad Basin to the J. A. Holmes, [email protected] northeast of the study sites, which vary inversely with the volume of Paleolake Megachad. More proximal sources of dust, including the fine fraction of local dune sand and floodplains of nearby rivers, have also made a contribution to the total dust load during times of enhanced dune and fluvial activity.
    [Show full text]
  • Palaeoclimate Proxy Data from North Africa and Adjacent Areas of The
    Classification: Physical sciences: Earth, Atmospheric and Planetary Sciences Title: West African Monsoon dynamics inferred from abrupt fluctuations of Lake Mega-Chad. Short title: Lake Mega-Chad fluctuation since the Last Glacial Maximum Simon J. Armitagea, Charlie S. Bristowb, and Nick A. Drakec aCentre for Quaternary Research, Department of Geography, Royal Holloway University of London, Egham, Surrey, TW20 0EX, United Kingdom. bDepartment of Earth and Planetary Sciences, Birkbeck College, University of London, Malet Street, London, WC1E 7HX, United Kingdom. cDepartment of Geography, King’s College London, Strand, London, WC2R 2LS, United Kingdom. Corresponding author: Simon J. Armitage E-mail: [email protected] Tel +44 (0)1784 276124 Keywords African monsoon, Lake Chad, dust, African Humid Period 1 Abstract From the deglacial period to the mid-Holocene, North Africa was characterised by much wetter conditions than today. The broad timing of this period, termed the African Humid Period, is well known. However, the rapidity of the onset and termination of the African Humid Period are contested, with strong evidence for both abrupt and gradual change. We use optically stimulated luminescence dating of dunes, shorelines and fluvio-lacustrine deposits to reconstruct the fluctuations of Lake Mega-Chad, which was the largest pluvial lake in Africa. Humid conditions first occur at ~15 ka, and by 11.5 ka Lake Mega- Chad had reached a highstand, which persisted until 5.0 ka. Lake levels fell rapidly at ~5 ka, indicating abrupt aridification across the entire Lake Mega-Chad Basin. This record provides strong terrestrial evidence that the African Humid Period ended abruptly, supporting the hypothesis that the African monsoon responds to insolation forcing in a markedly non-linear manner.
    [Show full text]
  • View on All the Lakes, of Which the Colours Contrast with the Sand Dunes Separated by Bare Rock Structures (World Heritage Committee, 2012)
    IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org Lakes of Ounianga - 2020 Conservation Outlook Assessment Lakes of Ounianga 2020 Conservation Outlook Assessment SITE INFORMATION Country: Chad Inscribed in: 2012 Criteria: (vii) The site includes eighteen interconnected lakes in the hyper arid Ennedi region of the Sahara desert covering an area of 62,808 ha. It constitutes an exceptional natural landscape of great beauty with striking colours and shapes. The saline, hyper saline and freshwater lakes are supplied by groundwater and are found in two groups 40 km apart. Ounianga Kebir comprises four lakes, the largest of which, Yoan, covers an area of 358 ha and is 27 m deep. Its highly saline waters only sustain algae and some microorganisms. The second group, Ounianga Serir, comprises fourteen lakes separated by sand dunes. Floating reeds cover almost half the surface of these lakes reducing evaporation. At 436 ha, Lake Teli has the largest surface area but is less than 10 m deep. With their high quality freshwater, some of these lakes are home to aquatic fauna, particularly fish. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 02 Dec 2020 GOOD The values of the site are in good condition and there have been no signs of decline since inscription of the site in 2012. The level of threats remains low and there are no immediate threats to the Outstanding Universal Value of the site. Natural processes such as the siltation of the small two eastern lakes of Ounianga Kebir and dune encroachment into most of the other lakes persist, of course, in this hyperarid environment, but actions are being undertaken to address dunes encroachment.
    [Show full text]