“…Although these can provide good-quality images, microscopy (under both visible and fluorescent illumination) has been required to identify finer resolved features. Subsequent digital image processing has identified such things as grey-level changes throughout individual stalagmite lamina and within a group of laminae captured under polarised visible light (Xiaoguang et al, 1998), luminescence properties under UV-light (Baker et al, 1993;Ribes et al, 2000), and crystalline fabric and calcite porosity (Kendall and Broughton, 1978;Genty, 1993;Frisia et al, 2000). Such studies have aided the recognition of sub-annual lamina made up of white porous calcite lamina (WPL) and dark compact calcite lamina (DCL), which together make up an annual lamination (Genty, 1993); they also identified organic acid layers (humic and fulvic acids), which may be used to determine variations in the annual growth rate (Baker et al, 1993) as well as an indicator of paleoprecipitation (Proctor et al, 2002).…”