期刊
HOLOCENE
卷 14, 期 4, 页码 525-535出版社
ARNOLD, HODDER HEADLINE PLC
DOI: 10.1191/0959683604hl729rp
关键词
stable isotopes; saline lake; palaeohydrology; 'Little Ice Age'; twentieth century; central Argentina
Laguna Mar Chiquita, a highly variable closed saline lake located in the Pampean plains of central Argentina, is presently the largest saline lake in South America (similar to 6000 km(2)). The availability of historical, instrumental lake-level and salinity data for the past 100 years allows for the calibration of the isotopic archive recorded in the lake sediments. Prolonged intervals with either negative or positive hydrological balances have severely modified lakewater levels, salinity and primary productivity, and have also controlled the isotopic composition of both the authigenic carbonate (delta(18)O(carb) and delta(13)C(carb)) and sedimentary organic matter (delta(13)C(carb)). Extensive evaporation during lowstand stages results in an enrichment of O-18 and C-13 in the lake waters, and is recorded in the sediments as the most positive delta(18)O(carb) and delta(13)C(carb) compositions (0.0parts per thousand and -1.9parts per thousand, respectively). Conversely, more negative delta(18)O(carb) and delta(13)C(carb) values (-1.8parts per thousand and -3.8parts per thousand, respectively) are the result of increasing freshwater input into the lake system. The delta(13)C(om) values are related to the isotopic composition of the dissolved inorganic carbon pool and the carbonate equilibrium of the lake water. Relatively low delta(13)C(om) values correspond with high lake levels, low salinity, low alkalinity and high lake productivity. High salinity during lowstands diminishes the amount of primary production and the delta(13)C(om), value is correspondingly high. The calibrated isotopic model was extrapolated to reconstruct precipitation-evaporation variability from the end of the 'Little Ice Age' (c. AD 1770) to the present. Low water levels predominated until the last quarter of the twentieth century, when a positive hydrological balance without equivalent in the previous history of Laguna Mar Chiquita became dominant.
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