In “Interhemispheric climate linkages.” (V Markgraf, Ed.), pp. Glaciation during Marine Isotope Stage 2 in the American Cordillera. “Quaternary geology and geomorphology of South America.” Elsevier, Amsterdam.Ĭlapperton, C. Full- and late-glacial lake records along PEP-1 transect: Their role in developing inter-hemispheric paleoclimate interactions. P., Grosjean, M., Stine, S., and Sylvestre, F. Variations in atmospheric methane concentrations during the Holocene epoch.
Chapellaz, J., Schwander, J., Stauffer, B., and Raynaud, D. Palaeogeography, Palaeoclimatology, Palaeoecology 173, 21–42.īlunier, T. A 106 ka paleoclimate record from drill core of the Salar de Atacama, northern Chile. A 22,000-year record of monsoonal precipitation from northern Chile’s Atacama Desert. Tropical climate changes at millennial and orbital timescales in the Bolivian Altiplano. The flora of Llullaillaco National Park in the transitional winter-summer rainfall area of the northern Chilean Andes. K., Castor, C., Marticorena, C., Muñoz, M., Cavieres, L., Matthei, O., Squeo, F. Bulletin de l’ Institut Français d’Etudes Andines 24, 495–503.Īrroyo, M. Isotope hydrology and geochemistry of Northern Chile groundwaters.
Quaternary Research 47, 70–80.Īravena, R. Holocene paleohydrology of the tropical Andes from lake records. This region therefore provides an ideal natural laboratory for paleoclimatologists. Due to their sensitive location at the juncture between tropical and extratropical climate zones, paleoclimate records from this area may potentially provide important insights into the dynamics of the large-scale atmospheric circulation in the Central Andes in the past. The prominent mountain chain of the Andes stretches N-S, perpendicular to the zonal westerly airflow of the mid-latitudes, which creates distinct environmental gradients at meso-and micro-scales. It is located between the tropical and extratropical precipitation belts the vertical gradients of ecozones range from sea level at the Pacific Coast up to high mountains that reach into the mid-troposphere at 6000 m elevation. Indeed, this area is a key site in several respects. The Atacama Desert of the Central Andes (18°S to 28°S) has become a focal point of environmental research in recent years.
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