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Late Quaternary Spatio-temporal Limnological Variations in the Altiplano of Bolivia and Peru1

Published online by Cambridge University Press:  20 January 2017

Denis Wirrmann  and
Philippe Mourguiart
Denis Wirrmann
Affiliation:
ORSTOM, BP 1857, Yaoundé, Cameroon
Philippe Mourguiart
Affiliation:
ORSTOM, CP 9214, La Paz, Bolivia
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Abstract

Between the western and eastern Andean cordilleras in Peru and Bolivia, there are three main lacustrine basins: Lake Titicaca, Lake Poopó, and the group of Coipasa-Uyuni. For the past few millennia, highly variable environmental conditions have been recorded in their sediments. Today a latitudinal meteorological gradient influences the lakes' status, leading to specific deposits and ostracod communities. Lake Titicaca in the north is oligohaline, whereas Lake Poopó further south is polyhaline. In the south, the Coipasa-Uyuni depression is characterized by a 12,000-km2 surficial salt crust. During the Late Pleistocene (ca. 40,000 to 25,000 yr B.P.), the water depth and salinity in paleolake Poopó fluctuated widely and paleolake Titicaca was slightly larger than at present. Sedimentation was mostly biocarbonate in the shallower areas and it was detrital-organic in the deepest zones. During the Holocene, a dry period transformed Lake Poopó into a "salar" with evaporite precipitation. Lake Titicaca registered a large decline in water level (8100-3600 yr B.P.) initially inducing gypsum precipitation followed by short influxes of water, with an ostracod faunal composition similar to that of the modern brines of Lake Poopó. Lake Titicacas' present condition only appeared between 2200 and 1500 yr B.P.

Type
Research Article
Information
Quaternary Research , Volume 43 , Issue 3 , May 1995 , pp. 344 - 354
Copyright
University of Washington

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Footnotes

This study was performed through an agreement between ORSTOM (Institut Français de Recherche Scientifique pour le Developement en Coopération) and UMSA (Universidad Mayor de san Anddrés, La Paz, Bolivia).

References

Ahlfeld, F. (1972). “Geologi’a de Bolivia.” Editorial Los Amigos del Libro, La Paz-Cochabamba.Google Scholar
Benzecri, J.-P. (1973). “L’analyse des donnes,” Vol. 2. Dunod, Paris.Google Scholar
Boulange, B. Rodrigo, L. A., and Vargas, C. (1978). Morphologie, formation et aspects s6dimentologiques du lac Poop6 (Bolivie). Cahiers O.R.S.T.O.M., Serie Geologie 10, 69–78.Google Scholar
Boulange, B. Vargas, C., and Rodrigo, L. A. (1981). La sedimentation actuelle dans le lac Titicaca. Revue d’Hydrobiologie tropicale 14, 299–309.Google Scholar
Carbonel, P. Colin, J.-P. Danielopol, D. L. Loffler, H., and Neustrueva, I. (1988). Paleoecology of iimnic ostracodes: a review of some major topics. Palaeogeography, Palaeoclimatology, Palaeoecology 62, 413–461.CrossRefGoogle Scholar
Carmouze, J.-P., and Aquize, E. (1981). La regulation hydrique du lac Titicaca et I’hydrologie de ses tributaires. Revue d’Hydrobiologie tropicale 14, 311–328.Google Scholar
Carmouze, J.-P. Arze, C., and Quintanilla, J. (1978). Circulation de materia (agua-sales disueltas) atravls del sistema fluvio-lacustre del Altiplano: la regulation hidrica e hidroqufmica de los lagos Titicaca y Poop6. Cahiers O.R.S.T.O.M., Serie Gtologie 10, 49–68 Google Scholar
Carmouze, J.-P. Arce, C., and Quintanilla, J. (1981). Regulation hydrochimique du lac Titicaca et 1’hydroctumie de ses tributaires. Revue d’Hydrobiologie tropicale 14, 329–348.Google Scholar
Collot, D. Koriyama, F., and Garcia, E. (1983). Repartition, biomasses et production des macrophytes du lac Titicaca. Revue d’Hydrobiologie tropicale 16, 241–262.Google Scholar
Dejoux, C. (1992). The mollusca. In “Lake Titicaca. A Synthesis of Limnological Knowledge.” (Dejoux, C. and Iltis, A., Eds.), MOBI68. pp. 311–336. Kluwer, Dordrecht.Google Scholar
Francou, B., and Pizarro, L. (1985). El Nino y la sequia en los Altos Andes Centrales (Peru and Bolivia). Bulletin de I’Institut Franqais d’fctudes Andines 14, 1–18.CrossRefGoogle Scholar
Gouze, P. Argollo, J. Salidge, J.-F., and Servant, M. (1986). Interpretations paieoclimatiques des oscillations des glaciers au cours des 20 demiers milienaires dans les regions tropicales; exemple des Andes boliviennes. Comptes Rendus de I’Acadimie des Sciences Paris Srie 2 303, 219–224.Google Scholar
Greenacre, M. J. (1984). “Theory and Applications of Correspondance Analysis.” Academic Press, New York/London.Google Scholar
Hill, M. O. (1973). Reciprocal averaging: an eigenvector method of ordination. Journal of Ecology 61, 340–354.CrossRefGoogle Scholar
Iltis, A. Carmouze, J.-P., and Lemoalle, J. (1992). Physico-chemical properties of the waters. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 89–97. Kluwer, Dordrecht.Google Scholar
Iltis, A., and Mourguiart, P. (1992). Higher plants-, distribution and biomass. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 241–252. Kluwer, Dordrecht.Google Scholar
Kunzel, F., and Kessler, A. (1986). Investigation of level changes of Lake Titicaca by maximum entropy spectral analysis. Archiv fur Meteorologische Geographische Bioklimatologie 36, 219–227.Google Scholar
Lavenu, A. (1992). Formation and geological evolution, in “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and litis, A., Eds.), MOBI 68, pp. 3–15. Kluwer, Dordrecht.Google Scholar
Lavenu, A. Fornari, M., and Sebrier, M. (1984). Existence de deux nouveaux Episodes lacustres quatemaires dans 1’Altiplano Pdruvo-Bolivien. Cahiers O.R.S.T.O.M. Sirie Geologie 14, 103–114.Google Scholar
Lazzaro, X. (1981). Biomasses, peuplements phytoplanctoniques et production primaire du lac Titicaca. Revue d’Hydrobiologie tropicale 14, 349–380.Google Scholar
Lebart, L. Morineau, A., and Warwick, K. (1984). “Multivariate descriptive statistical analysis.” Wiley, New York.Google Scholar
Mariaca, C. J. (1985). “Balance hldrico de la cuenca del lago Poop6 y de los salares de Uyuni y Coipasa.” PHICAB Publicacion, La Paz.Google Scholar
Martin, L. Fournier, M. Mourguiart, P. Sifeddine, A. Turcq, B. Absy, M. L., and Flexor, M.-M. (1993). Southern oscillation signal in South American paleoclimatic data of the last 7000 years. Quaternary Research 39, 338–346.CrossRefGoogle Scholar
Mourguiart, P. (1992). The ostracoda. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Utis, A, Eds.), MOBI 68, pp. 337–345. Kluwer, Dordrecht.Google Scholar
Mourguiart, P., and Carbonel, P. (1994). A quantitative method of paleolake level reconstruction using ostracod assemblages: an example from the Bolivian Altiplano. Hydrobiologia 288, 183–193.CrossRefGoogle Scholar
Mourguiart, P., and Roux, M. (1990). Une approche nouvelle du problfcme pos6 par les reconstructions des paloniveaux lacustres: utilisation d’une fonction de transfer! bas6e sur les faunes d’ostracodes. Giodynamique 5, 151–165.Google Scholar
Mourguiart, P. Wirrmann, D. Fournier, M., and Servant, M. (1992). Reconstruction quantitative des niveaux du Petit lac Titicaca au cours de l’Holocene. Comptes Rendus de VAcademie des Sciences, Paris, Strie 2 315, 875–880.Google Scholar
Northcote, T. G. (1992). Eutrophication and pollution problems. In“Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 551–561. Kluwer, Dordrecht.Google Scholar
Risacher, F., and Fritz, B. (1992). Mise en Evidence d’une phase climatique holocene extremement aride dans 1’Altiplano central, par la presence de la poly halite dans le salar de Uyuni (Bolivie). Comptes Rendus de I’Academie des Sciences, Paris, Serie 2 314, 1371–1377.Google Scholar
Roche, M.-A. Bourges, J. Cortes, J., and Mattos, R. (1992). Climatology and hydrology of the Lake Titicaca basin. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 63–88, Kluwer, Dordrecht.Google Scholar
Roche, M.-A., and Rocha, N. (1985). “Mapa pluviometrico de Bolivia y regiones vecinas.” PHICAB Publication, La Paz.Google Scholar
Rondeau, B. (1990). “G6ochimie isotopique et gdochronologie des stromatolites lacustres quatemaires de 1’Altiplano bolivien.” Unpublished M6moire de Maitrise en Sciences de la Terre, University du Quebec, Montreal.Google Scholar
Seltzer, G. O. (1991), “Glacial history and climate change in the Peruvian-Bolivian Andes.” Unpublished Ph.D. dissertation, University of Minnesota.Google Scholar
Servant, M., and Fontes, J.-C. (1978). Les lacs quatemaires des hauts plateaux des Andes boliviennes. Premieres interpretations pateoclimatiques. Cahiers O.R.S.T.O.M., Serie Geologie 10, 9–23.Google Scholar
Servant, M., and Fontes, J.-C. (1984). Les basses terrasses fluviatiles du Quaternaire recent des Andes boliviennes. Datations par le 14C. Interpretation paldoclimatique. Cahiers O.R.S.T.O.M., Serie Geologie 14, 15–28.Google Scholar
Servant, M. Fournier, M. Argollo, J. Servant-Vildary, S. Wirrmann, D., and Ybert, J.-P. (1994). The last glacial/interglacial transition in the Bolivian Andes (16-22° S. Lat.): Glacial and lake-level changes. “International Symposium on The termination of the Pleistocene in South America,” CADIC, Ushuaia, Argentina.Google Scholar
Servant-Vildary, S. (1978). Les diatom6es des depots lacustres quaternaires de FAltiplano bolivien. Cahiers O.R.S.T.O.M., Serie Geologie 10, 25–35,Google Scholar
Servant-Vildary, S., and Mello, E Sousa, S. H. (1993). Paleohydrology of the Quaternary saline Lake Ballivian (southern Bolivian Altiplano) based upon diatom studies. InternationaI Journal of Salt Lake Research 2, 69–85.CrossRefGoogle Scholar
Servant-Vildary, S., and Roux, M. (1990). Multivariate analysis of diatoms and water chemistry in Bolivian saline Lakes. Hydrobiologia 197, 267–290.CrossRefGoogle Scholar
Sheriff, F. (1979). Cartografia climetica de region andina boliviana. Revista Geograftca 89, 45–68. (2 maps included in text) Google Scholar
Wirrmann, D. (1992a). Morphology and bathymetry of Lake Titicaca. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 16–22. Kluwer, Dordrecht.Google Scholar
Wirrmann, D. (1992b). Lake Titicaca, Bolivia-Peru. In “Global Geological Record of Lake Basins” (Gierlowski-Kordesch, E. and Kelts, K., Eds.), Vol. 1. pp. 407–411, Cambridge, Univ. Press, Cambridge, UK.Google Scholar
Wirrmann, D., and De Oliveira Almeida, L. F. (1987). Low Holocene level (7,700 to 3,650 years ago) of Lake Titicaca (Bolivia). Palaeogeography, Palaeoclimatology, Palaeoecology 59, 315–323.CrossRefGoogle Scholar
Wirrmann, D. Mourguiart, P., and De Oliveira Almeida, L. F. (1988). Holocene sedimentology and Ostracods repartition in Lake Titicaca. Paleohydrological interpretations. In “Quaternary of South America and Antarctic Peninsula” (Rabassa, J., Ed.), Vol. VI, pp. 89–127. Balkema, Rotterdam.Google Scholar
Wirrmann, D. Ybert, J.-P., and Mourguiart, P. (1992). A 20,000 paleohydrological record from Lake Titicaca. In “Lake Titicaca. A Synthesis of Limnological Knowledge” (Dejoux, C. and Iltis, A., Eds.), MOBI 68, pp. 40–48. Kluwer, Dordrecht.Google Scholar