Causes of colour and fluorescence in speleothems

Speleothems fluoresce, when illuminated with UV light, between 410 and 460 nm. In this study, we attempted to determine the nature of the fluorophores . thought to be either trace elements or organic matter trapped in the calc ite. Fluorescence of solid speleothems and organic species extracted from t he calcite were measured to quantify their contribution to the observed flu orescence of the speleothems. All speleothems and extracts gave similar spe ctra with broad emission maxima centred around 410-430 nm, and two excitati on maxima at approximately 255 and 330 nm. The organic compounds were partl y characterized using fulvic acid (FA)-humic acid (HA) separation and molec ular size fractionation. Trace elements, determined by neutron activation a nalysis, do not appear to be responsible for the observed spectra, Organic matter. particularly FAs, were found to be the dominant fluorophore in the calcite. Of the FA, the dominant fractions were the hydrophilics. Darker sp eleothems, although having higher concentrations of FA and HA than light sp eleothems, had lower emission intensities, due to self-absorption. Average particulate organic matter (POM), FA, HA, and total organic matter (TOM) co ncentrations for the dark speleothems were twice that of their light counte rparts. (C) 2001 Elsevier Science B.V. All rights reserved.