Polarized and persistent Ca2+ plumes define loci for formation of wall ingrowth papillae in transfer cells

Transfer cell morphology is characterized by a polarized ingrowth wall comprising a uniform wall upon which wall ingrowth papillae develop at right angles into the cytoplasm. The hypothesis that positional information directing construction of wall ingrowth papillae is mediated by Ca2+ signals generated by spatiotemporal alterations in cytosolic Ca2+ ([Ca2+](cyt)) of cells trans-differentiating to a transfer cell morphology was tested. This hypothesis was examined using Vicia faba cotyledons. On transferring cotyledons to culture, their adaxial epidermal cells synchronously trans-differentiate to epidermal transfer cells. A polarized and persistent Ca2+ signal, generated during epidermal cell trans-differentiation, was found to co-localize with the site of ingrowth wall formation. Dampening Ca2+ signal intensity, by withdrawing extracellular Ca2+ or blocking Ca2+ channel activity, inhibited formation of wall ingrowth papillae. Maintenance of Ca2+ signal polarity and persistence depended upon a rapid turnover (minutes) of cytosolic Ca2+ by co-operative functioning of plasma membrane Ca2+-permeable channels and Ca2+-ATPases. Viewed paradermally, and proximal to the cytosol-plasma membrane interface, the Ca2+ signal was organized into discrete patches that aligned spatially with clusters of Ca2+-permeable channels. Mathematical modelling demonstrated that these patches of cytosolic Ca2+ were consistent with inward-directed plumes of elevated [Ca2+](cyt). Plume formation depended upon an alternating distribution of Ca2+-permeable channels and Ca2+-ATPase clusters. On further inward diffusion, the Ca2+ plumes coalesced into a uniform Ca2+ signal. Blocking or dispersing the Ca2+ plumes inhibited deposition of wall ingrowth papillae, while uniform wall formation remained unaltered. A working model envisages that cytosolic Ca2+ plumes define the loci at which wall ingrowth papillae are deposited.