As photosynthesis rates rise, leaves ultimately become net nutrient sources, supplying carbohydrates to the remainder of the plant. This sink-to-source transition is likely to have profound effects on mineral distribution, sequestration, and compartmentalization of essential elements in plants. But determining these effects is challenging due to the difficulty in measuring such distributions over large areas, such as a whole leaf or plant.
In a new article in the Journal of Experimental Biology (doi:10.1093/jxb/erw111), Cornell University graduate student Monica R. Carvalho demonstrates the use of large-area x-ray fluorescence mapping with the 384-element Maia detector (described further here and here) to explore just this question. The paper, entitled, “Spatiotemporal distribution of essential elements through Pupulus leaf ontogeny,” describes calcium, potassium, and zinc concentration maps obtained from XRF scans of a series of seven poplar leaves varying in age and size and spanning the transition from sink to source. The calcium distribution in particular exhibits a striking change as a function of leaf age, and in a manner consistent with other physiological changes known to be associated with this transition.
Plan-view XRF maps such as those in Figure 1 were obtained primarily at F3 station, from oven-dried leaves with a 0.02 mm focused beam. Critical information about the localization of elements within leaf tissues was obtained from additional XRF maps, obtained from hydrated leaf cross-sections with 0.01 mm spatial resolution.
Inquiries about XRF mapping at CHESS should be directed to Arthur Woll (arthurwoll@cornell.edu) or Rong Huang (rh66@cornell.edu).