Interactions of the manganese hyperaccumulator Phytolacca americana L. with soil pH and phosphate

Hyperaccumulators are plants that store exceptionally high concentrations of heavy metals or metalloids in their leaves. Phytolacca americana is one of the few species known to hyperaccumulate manganese (Mn); however, it is a common weedy species and has no specific association with high‐Mn soils. Neither the mechanism by which P . americana hyperaccumulates Mn nor the ecological significance of this trait are well understood. It has recently been suggested that P . americana secretes acids into the rhizosphere as a means of acquiring phosphate, which might coincidentally increase Mn uptake. To determine whether P . americana acidifies the surrounding soil, plants were grown in rhizoboxes providing access to living roots. A thin layer of agar containing bromocresol green pH indicator dye was placed on the roots to observe color changes indicating acidification. Comparative studies showed that P . americana acidifies the rhizosphere significantly more than the non‐accumulating plant Acalypha rhomboidea . A second experiment studied whether adjustment of soil pH and phosphate affect foliar Mn concentrations of P . americana . Concentrations of Mn in leaves were highest when plants were grown in acidified soils but were significantly lower in soils that were alkaline and/or enriched with phosphate. These results suggest that Mn hyperaccumulation may be a side effect of rhizosphere acidification as a phosphorus‐acquisition mechanism, rather than an adaptation in its own right. The findings provide fundamental information about hyperaccumulator physiology and evolution, and may be relevant to attempts to utilize P . americana for phytoremediation.