Isotope Paleohydrology of Lakes Albert, Edward and Victoria, East Africa

9706522 东非的大型湖泊是大陆尺度热带水文学的敏感监测器，提供长期连续的十年尺度水平衡和温度档案，以测试热带海洋水分输送的演变模型。 我们的问题是阅读和量化这些特征。 该地区以前的研究缺乏明确区分温度和降水影响所需的工具。 与此相反，本研究提出应用新技术的氧和氢同位素分析的水生纤维素和脂质，这将使我们能够区分降水信号。 其目标是量化阿尔伯特湖、爱德华湖和维多利亚湖在过去15,000年中水平衡变化的幅度和时间，并确定其对当地和区域生物圈的影响。 这些湖泊的水动态的时间序列也将与尼罗河沿着的植被和文明史进行比较。 该工作计划包括汇编一个现代陆地和水生纤维素/18 O数据库，以确认水生纤维素的不依赖于温度和物种的氧同位素生化分馏系数。 该数据库将用于约束古水文解释。 对所有三个湖泊的现有岩心样本进行分析，以不到300年的增量，将提供水生纤维素，从而提供过去15 000年来的湖水氧同位素时间序列剖面。 这些主要的氧同位素信号的湖泊沃茨将来自P：E比和停留时间的变化，可以忽略地下水和高山水的影响。 预计对水生脂质的其他分析将反映湖水的D值。 仔细考虑流域和湖泊水水文之间的相互作用，以及过去的海洋同位素值可能允许测试这些盆地的水分来源（大西洋与印度洋）的历史。 该研究为热带地区古水文学研究提供了新的思路和方法，并有助于约束古气候模型的预测。

9706522 The large lakes of East Africa are sensitive monitors of continental-scale tropical hydrology that provide long continuous decadal-scale archives of water balance and temperature to test evolving models of tropical ocean moisture transport. Our problems is to read and quantify such signatures. Prior studies in the region have lacked the tools necessary to unequivocally separate temperature and precipitation effects. In contrast, this study proposes to apply new techniques of oxygen and hydrogen isotopic analyses of aquatic cellulose and lipids that will allow us to differentiate the precipitation signal. The objectives are to quantify the magnitude and timing of shifts in the water balances of Lakes Albert, Edward, and Victoria over the last 15,000 years and determine their implications for the local and regional biosphere. The time-series of water dynamics in these lakes will also be compared with the history of vegetation and civilization along the Nile. The workplan includes compilation of a modern terrestrial and aquatic cellulose/ 18O database to confirm the temperature-independent and species-independent oxygen isotopic biochemical fractionation factor of aquatic cellulose. This database will be used to constrain paleohydrologic interpretations. Analyses of available core samples from all three lakes at less than 300 year increments will provide aquatic cellulose and hence lake water oxygen isotopic time-series profiles over the last 15,000 years. These primary oxygen isotopic signals of the lake waters will derive from shifts in P:E ratios and residence times with negligible groundwater and high mountain water effects. Additional analyses in aquatic lipids are expected to reflect D values of the lake water. Careful consideration of interactions between the watershed and lake water hydrologies as well as of past ocean isotopic values may allow testing for the history of moisture sources (Atlantic vs. Indian Ocean) to these basin. This study should provide sensi tive new approaches to the study of paleohydrology in tropical regions and help constrain paleoclimate model predictions.