Ca Shuttling in Vesicles During Tip Growth in Neurospora crassa

Tip-growing organisms maintain an apparently essential tip-high gradient of cytoplasmic Ca²⁺. In the oomycete Saprolegnia ferax, in pollen tubes and root hairs, the gradient is produced by a tip-localized Ca²⁺ influx from the external medium. Such a gradient is normally dispensable for Neurospora crassa hyphae, which may maintain their Ca²⁺ gradient by some form of internal recycling. We localized Ca²⁺ in N. crassa hyphae at the ultrastructural level using two techniques (a) electron spectroscopic imaging of freeze-dried hyphae and (b) pyroantimoniate precipitation. The results of both methods support the presence of Ca²⁺ in the wall vesicles and Golgi body equivalents, providing a plausible mechanism for the generation and maintenance of the gradient by Ca²⁺ shuttling in vesicles to the apex, without exogenous Ca²⁺ influx. Ca²⁺ sequestration into the vesicles seems to be dependent on Ca²⁺–ATPases since cyclopiazonic acid, a specific inhibitor of Ca²⁺ pumps, eliminated all Ca²⁺ deposits from the vesicles of N. crassa.