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Updated: Jan 31, 2026

Laboratory-determined Phosphorus Flux from Lake Sediments as a Measure of Internal Phosphorus Loading
Published on: March 6, 2014
Assessing the artificial radionuclide Cesium-137 spatial distribution in the Southern Hemisphere from lake sediment
Floriane Guillevic1, Pierre Sabatier2, Gerald Dicen3
1Environmental Geosciences, Department of Environmental Sciences, University of Basel, Basel, CH-4056, Switzerland.
Abstract:
When supported by a reliable geochronology, lake sediments provide important archives for environmental and climatic changes. Artificial radionuclides in general, and cesium-137 (137Cs) in particular, are frequently used to validate sediment chronologies over the past century. This review and meta-analysis assessed the spatial distribution and variability of 137Cs in lake records from the Southern Hemisphere, while also identifying geographical data gaps. The 137Cs profile shapes and inventories were compared and categorized, and their relationships with environmental variables were tested. The spatial distribution of available data reveals an imbalance in studies available across the Southern Hemisphere, with South America showing the greatest research coverage. While the sedimentation rate was identified as a key factor of 137Cs variability, two groups identified from the database presented high peak activities regardless of sedimentation rate, particularly in lakes located between 40°S and 50°S in Chile and Argentina. Lake geographic location (and their distance from nuclear test sites) appears to be the most influential factor explaining disparities in 137Cs deposition. Surprisingly, neither precipitation nor lake elevation showed a significant correlation with 137Cs peak activity.
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