HR: 0800h
AN: GC51C-1063    [Abstracts]
TI: Late Holocene Lacustrine Records of Climate and Vegetation Change From Southern Patagonia, Chile
AU: * Moy, C M
EM: moyc@stanford.edu
AF: Dept. of Geological and Environmental Sciences, Stanford University, Braun Hall (Bldg. 320), Stanford, CA 94305 United States
AU: Francois, J
EM: tepu4@hotmail.com
AF: Departamento de Ciencias Ecol\'{o}gicas, Universidad de Chile, Las Palmeras 3425, \~{N}u\~{n}oa, Santiago, 653 Chile
AU: Moreno, P
EM: pimoreno@abello.dic.uchile.cl
AF: Departamento de Ciencias Ecol\'{o}gicas, Universidad de Chile, Las Palmeras 3425, \~{N}u\~{n}oa, Santiago, 653 Chile
AU: Villa Martinez, R
EM: rodrigo.villa@umag.cl
AF: Centro de Estudios del Cuaternario, Universidad de Magallanes, Avenida Bulnes 01855, Punta Arenas, 6200000 Chile
AU: Dunbar, R B
EM: dunbar@stanford.edu
AF: Dept. of Geological and Environmental Sciences, Stanford University, Braun Hall (Bldg. 320), Stanford, CA 94305 United States
AB: The westerly wind field is one of the most prominent atmospheric circulation features in the Southern Hemisphere, having a major impact on the climate of Chile and hydrographic conditions in the Southern Ocean. The latitudinal position and strength of the westerlies directly influences the amount and isotopic composition of precipitation that falls in southern Chile. Although instrumental records provide information on how the westerlies have varied over the recent past there is still an incomplete understanding of how the strength and latitudinal position of the southern westerlies have changed during the Holocene and how the wind field has varied at millennial to sub-decadal timescales. In this study we relate changes in the westerly winds to changes in water balance as recorded in closed-basin lakes. Sediment cores were obtained from Laguna Guanacos in Parque Nacional Torres del Paine (51$\deg$S, 72$\deg$W) during the austral summer of 2004 and sampled at 1-2cm intervals for pollen, charcoal, and stable isotope analysis. Laguna Guanacos is a small closed-basin lake situated in the core of westerly wind belt and is therefore sensitive to fluctuations in the strength and position of the westerlies. The sediment cores obtained from the lake reveal high concentrations of organic mater ($\sim$20%) and biogenic carbonate, which is rare in Chilean Patagonia. AMS radiocarbon dates on the organic and carbonate fractions indicate that the record spans the last $\sim$14,000 calendar years and modern dates from core tops suggest little influence by old or dead carbon sources. Pollen analysis on the late Holocene portion of the record reveals a significant expansion of the {\it Nothofagus} forest since $\sim$3500 cal yr BP, suggesting an overall increase in precipitation during this interval. Millennial- and centennial-scale fluctuations in bulk carbonate content and forest and steppe pollen are superimposed upon this pattern, providing a view of a highly dynamic westerly wind regime and forest-steppe ecotone response in southern Patagonia. These results will be discussed in conjunction with carbon and oxygen isotopic data derived from the biogenic carbonate phases exposed in the late Holocene portion of the record.
DE: 9360 South America
DE: 3344 Paleoclimatology
DE: 1845 Limnology
DE: 1040 Isotopic composition/chemistry
DE: 1620 Climate dynamics (3309)
SC: Global Climate Change [GC]
MN: 2004 AGU Fall Meeting