shorelines of the Holocene Megalake Chad (Africa, Sahara) investigated with very high resolution satellite imagery (Pléiades) : example of the Goz Kerki paleo-spit
DOI :
https://doi.org/10.52638/rfpt.2014.114Mots-clés :
african humid period, beach ridges, paleo-lake, littoralRésumé
Megalake Chad (350,000 km2), the largest paleo-lake of the Sahara-Sahel area, is one of the most emblematic marker of the hydroclimatic changes that occurred during the African Humid Period (AHP; ca. 11,500 — 5,000 years BP) in subtropical Africa. From field surveys, the existence of Megalake Chad is well demonstrated by widespread typical lake deposits. However, considering the very large size of this paleo-lake, it is best evidenced and understood from space. Conspicuous paleo-littoral features distributed along hundreds of kilometers are clearly visible on second generation satellite images. These features represent major archives of the Megalake Chad and of the climate during the AHP. This paper is the first attempt to investigate the paleo-littoral of Megalake Chad with very high resolution satellite imagery. A Pléiades scene (images and DEM) is used to characterize the fossil sand spit of the Goz Kerki, which is one of the most representative and best preserved littoral features of Megalake Chad. Thanks to Pléiades stereoscopic images the geomorphology and the lithology of this paleo-spit can now be detailed and the evolution of the paleo-bathymetry of Megalake Chad can be reconstructed. This brings new insights into the paleo-environments and paleo-climates of the Sahara-Sahel region.
Téléchargements
Références
Bouchette F., Schuster M., Ghienne J.-F., Denamiel C., Roquin C., Moussa A., Duringer Ph., 2010. Hydrodynamics in the Holocene Lake Mega-Chad. Quaternary Research 73, 226—236.
Callot Y., Fontugne M., 2008. Les sites lacustres d'âge holocène dans l'est du Grand Erg occidental (nord-ouest du Sahara algérien). Géomorphologie 3,187—200.
Cohen A.S., 2003. Paleolimnology: The History and Evolution of Lake Systems. Oxford University Press, New York, 528p.
Contoux C., Jost A., Sepulchre P., Ramstein G., Krinner G., Schuster M., 2013. Impact of the Megalake Chad on climate and vegetation during the late Pliocene and the mid-Holocene. Climate of the Past 9, 1417—1430.
Damnati B., 2000. Holocene lake record in the Northern Hemisphere of Africa. Journal of African Earth Sciences 31, 253—262.
deMenocal, P.B., Tierney J.E., 2012. Green Sahara: African Humid Periods Paced by Earth's Orbital Changes. Nature Education Knowledge 3(10):12
Drake N., Bristow C., 2006. Shorelines in the Sahara: geomorphological evidence for an enhanced monsoon from palaeolake Megachad. Holocene 16, 901—911.
Durand A., 1995. Geomorphological records of neotectonics in the Lake Chad Basin: the changes in drainage pattern and the pseudo shoreline of Lake Megachad in Kadzell. C. R. Acad. Sci. 321, 223—229.
Evans O.F., 1942. The origin of spits, bars and related structures. Journal of Geology 50, 846—863.
Fabre J., Petit-Maire N., 1988. Holocene climatic evolution at 22-23° N from two palaeolakes in the Taoudenni area (northern Mali). Palaeogeogr., Palaeoclimatol., Palaeoecol. 65, 133—148.
Gasse F., 2000. Hydrological changes in the African tropics since the Last Glacial Maximum. Quaternary Science Reviews 19, 189—211.
Ghienne J.-F., Schuster M., Bernard A., Duringer Ph., Brunet M., 2002. The Holocene giant Lake Chad revealed by Digital Elevation Models. Quaternary International 87, 81—85.
Kröpelin S., Verschuren D., Lezine A.-M., Eggermont H., Cocquyt C., Francus P., Cazet J.P., Fagot M., Rumes B., Russell J.M., Darius F., Conley D.J., Schuster M., Suchodoletz H., Engstrom D.R., 2008. Climate-Driven Ecosystem Succession in the Sahara: The Last 6000 Years. Science 320, 765—769.
Kuper R., 2006. After 5000 BC: The Libyan desert in transition. C. R. Palevol 5, 409—419
Leblanc M., Favreau G., Maley J., Nazoumou Y., Leduc C., Stagnitti F., van Oevelen P.J., Delclaux F., Lemoalle J., 2006. Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data. Paleogeogr. Paleoclimatol. Paleoecol. 239, 16—27.
Le Quellec J.-L., 1999. Répartition de la grande faune sauvage dans le nord de l' Afrique durant l'Holocène. L'Anthropologie 103, 161—176.
Lezine, A.-M. 2009. Climatic history of the African and Arabian deserts. C. R. Geosciences 341, 569—574.
Maley J., 2004. Le bassin du Tchad au quaternaire récent : formations sédimentaires, paléoenvironnements et préhistoire : la question des paléotchads. In: Sémah A.-M. & Renault-Miskovsky J. (Eds), L'évolution de la végétation depuis deux millions d'années. Artcom et Errance, Paris, 179-217pp.
Olivry J.C., Chouret A., Lemoalle J., Bricquet J.P., 1996. Hydrologie du lac Tchad. ORSTOM Paris, 266p.
Pachur H.J., Kröpelin S. 1987. Wadi Howar: paleoclimatic evidence from an extinct river system in the southeastern Sahara. Science 237, 298—300.
Pachur H.J., Rottinger F., 1997. Evidence for large extended palaeolake in the eastern Sahara as revealed by spaceborne radar lab images. Remote Sensing of Environment 61, 437—440.
Paillou Ph., Schuster M., Farr T., Tooth S., Rosenqvist A., Lopez S., 2009. Mapping of a Major Paleodrainage System in Eastern Libya using Orbital Imaging Radar: The Kufrah River. Earth and Planet. Science Letters 277, 327—333.
Pias J., Guichard E., 1957. Origine et conséquences de l'existence d'un cordon sableux dans la partie sud-ouest de la cuvette tchadienne. C. R. Acad. Sci. 244, 791—793.
Pierrot-Deseilligny M., Paparoditis N., 2006. A multiresolution and optimization-based image matching approach: an application to surface reconstruction from SPOT5-HRS stereo imagery. IAPRS vol XXXVI-1/W41, ISPRS Workshop on Topographic Mapping from Space, Ankara, Turkey.
Pierrot-Deseilligny M., 2007. MicMac, un logiciel pour la mise en correspondance automatique d'images dans le contexte géographique. Bulletin d'Information Scientifique et Technique de l'IGN 77.
Pilkey O.H., Neal W.J., Kelley J.T., Cooper J.A.G., 2011. The world's beaches: a global guide to the science of the shoreline. University of California Press, Berkeley and Los Angeles, 283p.
Schneider J.-L., 1967.Évolution du dernier lacustre et peuplement préhistorique aux Pays Bas du Tchad. Bull. ASEQUA 14/15, 203—215.
Schuster M., Duringer Ph., Ghienne J.-F., Roquin C., Sepulchre P., Moussa A., Lebatard A.-E., Mackaye H.T., Likius A., Vignaud P., Brunet M., 2009. Chad Basin: paleoenvironments of the Sahara since the late Miocene. C. R. Geosciences 341, 612—620.
Schuster M., Duringer Ph., Ghienne J.-F., Vignaud P., Mackaye H.T., Likius A., Brunet M., 2006. The age of the Sahara Desert. Science 311, 821.
Schuster M., Roquin C., Duringer Ph., Brunet M., Fontugne M., Mackaye H.T., Vignaud P., Ghienne J.-F., 2005. Highlighting Holocene Lake Mega-Chad paleoshorelines from space. Quaternary Science Reviews 24, 1821—1827.
Schuster M., Duringer Ph., Ghienne J.-F., Vignaud P., Beauvilain A., Mackaye H.T., Brunet M., 2003. Coastal conglomerate around the Hadjer el Khamis inselbergs (western Chad, central Africa): new evidence for Lake Mega-Chad episodes. Earth Surface Processes and Landforms 28, 1059—1069.
Sereno P.C., Garcea E.A.A., Jousse H., Stojanowski C.M., Saliège J.-F., et al., 2008. Lakeside Cemeteries in the Sahara: 5000 Years of Holocene Population and Environmental Change. PLoS ONE 3(8): e2995. doi: 10.1371/journal.pone.0002995
Sepulchre P., Ramstein G., Schuster M., 2009. Modelling the impact of tectonics, surface conditions and Sea Surface Temperatures on Saharan and sub-Saharan climate evolution. C. R. Geosciences 341, 603—611.
Sepulchre P., Schuster M., Ramstein G., Krinner G., Girard J.-F., Fluteau F., Vignaud P., Brunet M., 2008. Evolution of Lake Chad Basin during the mid-Holocene: a preliminary approach from lake to climate modeling. Global and Planetary Change 61, 41—48.
Tilho J., 1925. Sur l'aire probable d'extension maxima de la mer paléotchadienne. C. R. Acad. Sci. 181, 643—646.
Téléchargements
Publié-e
Comment citer
Numéro
Rubrique
Licence
(c) Tous droits réservés Mathieu Schuster, Claude Roquin, Abderamane Moussa, Jean-François Ghienne, Philippe Duringer, Frédéric Bouchette, Arnaud Durand, Bernard Allenbach 2022
Cette œuvre est sous licence Creative Commons Attribution 4.0 International.
Les auteurs conservent les droits d'auteur et accordent à la revue le droit de première publication de l'œuvre sous une licence Creative Commons Attribution (CC-BY) 4.0 qui permet à d'autres de partager l'œuvre avec une reconnaissance de la paternité de l'œuvre et de sa publication initiale dans cette revue.