Late-Glacial to Late-holocene Shifts in Global Precipitation Delta(sup 18)O

Reconstructions of Quaternary climate are often based on the isotopic content of paleo-precipitation preserved in proxy records. While many paleo-precipitation isotope records are available, few studies have synthesized these dispersed records to explore spatial patterns of late-glacial precipitation delta(sup 18)O. Here we present a synthesis of 86 globally distributed groundwater (n 59), cave calcite (n 15) and ice core (n 12) isotope records spanning the late-glacial (defined as 50,000 to 20,000 years ago) to the late-Holocene (within the past 5000 years). We show that precipitation delta(sup 18)O changes from the late-glacial to the late-Holocene range from -7.1% (delta(sup 18)O(late-Holocene) > delta(sup 18)O(late-glacial) to +1.7% (delta(sup 18)O(late-glacial) > delta(sup 18)O(late-Holocene), with the majority (77) of records having lower late-glacial delta(sup 18)O than late-Holocene delta(sup 18)O values. High-magnitude, negative precipitation delta(sup 18)O shifts are common at high latitudes, high altitudes and continental interiors

Effects of heavy metal pollution in the Pilcomayo river system, Bolivia, on resident human populations

The Pilcomayo river in Bolivia drains the Potosi mining district and flows downstream, exposing indigenous populations, who rely on the river for drinking water, irrigation and fish, to elevated levels of toxic metals. A preliminary analysis of agricultural soil and crops from four riverside Pilcomayo communities has shown that many agricultural fields are contaminated with heavy metals (Ag, Cd, Cu, Pb, Sb, Zn) and arsenic (As) However, concentrations of these elements in most crops are within guideline values. Concentrations of metals and As in samples of drinking water are, for the most part, lower than concentrations in Pilcomayo river water taken at the respective communities, and the drinking water concentrations are within guideline values. Exceptions are Sb and As concentrations in two of the communities. In irrigation waters, Zn and Pb exceed recommended guideline values in two of the communities, and may lead to high Zn and Pb values in some crops and soils. The work carried out to date suggests that the strategies used by these communities appear to considerably reduce their risks to exposure. Work is ongoing to develop more complex and effective strategies based on further geochemical analyses and social science surveys.