Caves and climate history: Stalagmites as valuable indicators of environmental evolution
 

n° 389 - January 2001

 

CNRS scientists have developed a system for simultaneous continuous measurement of laser fluorescence parameters in order to probe a stalagmite's secrets and provide insights into environmental and climatic evolution and rhythms in the Vercors massive. The researchers working on this project come from various CNRS units: the "Enregistrement à haute résolution de l'environnement dans les dépôts laminés karstiques" (High Resolution Environmental Analysis of Stratified Karst Deposits") group; the "Laboratoire de physique des lasers, atomes et molécules" (Laboratory for the Physics of Lasers, Atoms and Molecules); and the "Laboratoire de géographie de l'Université de Savoie" (University of Savoy Geography Laboratory)

A stalagmite's growth is linked to its external environment. CO2-charged water percolates into the ground and dissolves limestone. When the water enters an underground void, a drop in CO2 pressure disturbs the equilibrium and precipitates carbonates, producing calcite stalagmites and stalactites drop by drop, and trapping particles from the external environment inside them. Growth is seasonal, dependent on water volume and the number and type of particles, and as a result the stalagmites develop a stratified structure that reflects their environment rather like tree rings.

Non-destructive laser-induced fluorescence is being used to interpret these strata. Three parameters are studied: reflectance, which provides information regarding the macroscopic optical properties of the calcite, showing up particles due, for example, to land clearance; fluorescence, which characterizes the organic matter trapped in the calcite and, being seasonal, produces a high resolution geochronometer enabling the stalagmites to be dated; and the maximum fluorescence wavelength, which characterizes the size of the trapped organic matter, enabling local soil formation to be studied. The team has developed a new fluorescence index, the Laser Induced Fluorescence Index (LIFI), for deducing the maximum wavelength at any point in a sample without measuring the whole emission spectrum.

This new tool paves the way for powerful mathematical tools to interpret the records contained in stalagmites.



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