H. Achyuthan et al., MINERAL REPLACEMENT OF PLANT-ROOTS IN FLUVIAL SEDIMENTS OF THE LINK CHANNEL OF KRISHNA RIVER, NEAR YEDURWADI, BELGAUM DISTRICT, KARNATAKA, Journal of the Geological Society of India, 50(6), 1997, pp. 765-768
Micromorphology, XRD analyses and SEM studies of rhizoliths from Late
Middle Pleistocene yellowish brown silty fluvial sediments of Yedurwad
i reveal that calcium carbonate has a localized source. Silica and cal
cium carbonate are formed by the plant roots through their metabolic a
ctivity creating a favourable microenvironment for the processes of Si
O2 and CaCO3 precipitation and replacement.