Scientists at Sainsbury Laboratory Cambridge University have found that the mineral vaterite, a polymorph of calcium carbonate, is a dominant component of the protective silvery-white crust that forms on the leaves of a number of alpine plants, which are part of the Garden’s national collection of European Saxifraga species.
Naturally occurring vaterite is rarely found on Earth. Small amounts of vaterite crystals have been found in some sea and freshwater crustaceans, bird eggs, the inner ears of salmon, meteorites and rocks. This is the first time that the rare and unstable mineral has been found in such a large quantity and the first time it has been found to be associated with plants.
The discovery of vaterite was made through a collaboration between SLCU and Cambridge University Botanic Garden as part of an ongoing research project that is probing the inner workings of plants in the Garden using new microscopy techniques, including Raman spectroscopy. Dr Raymond Wightman, the Microscopy Core Facility Manager at SLCU’s microscopy facility, has a Renishaw inVia™ Raman microscope which is used for studying aspects of plant development and plant cell biology. This is integrated with a confocal laser scanning microscope (CLSM), allowing correlated Raman and fluorescence measurements. Dr Wightman is also investigating correlative FLIM-confocal-Raman microscopy for observing protein–protein interactions, 3D cellular organisation and distribution of molecular species.
Vaterite was found to be a dominant component of the protective silvery-white crust of the plants. Dr Wightman said: “In this case, the inVia microscope not only identified signatures corresponding to calcium carbonate as forming the crust, but was also able to differentiate between the calcite and vaterite forms when it was present as a mixture while still attached to the leaf surface.”
The research findings have been published in Flora.