Hyperaccumulation of metals and metalloids is a rare phenomenon, currently known in only about 720 plant species; yet, it has a broad geographic and phylogenetic distribution (Reeves et al., 2017). Hyperaccumulators are defined on the basis of exceptionally high concentrations of a given metallic element in their foliar tissue, exceeding specified criteria that are typically 2-3 orders of magnitude higher than is generally found in most plants and at least one order of magnitude higher than in other plants growing on metalliferous soils (Reeves, 2003;van der Ent et al., 2013). These high concentrations are toxic to normal plants, but hyperaccumulators have sufficient metal tolerance to survive and to reproduce on metalliferous soils, and the majority of such species are restricted to these habitats (Pollard et al., 2014). Hypotheses that have been proposed to explain the evolution of hyperaccumulation (Boyd and Martens, 1992;Boyd, 2014) include tolerance or disposal of substrate metals, drought resistance, allelopathy, "inadvertent" accumulation of the metal via mechanisms for uptake of another element, and defense against herbivores and pathogens.Regulation of elemental uptake, including processes of exclusion, accumulation, and hyperaccumulation, has broad implications for plant biochemistry, physiology, ecology, and evolution. The extreme elemental concentrations found in hyperaccumulators have made them useful systems for study of nutrient acquisition, transport, and homeostasis (van der Ent et al., 2013), plant-herbivore interactions PREMISE: Hyperaccumulation of heavy metals in plants has never been documented from Central America or Mexico. Psychotria grandis, P. costivenia, and P. glomerata (Rubiaceae) have been reported to hyperaccumulate nickel in the Greater Antilles, but they also occur widely across the neotropics. The goals of this research were to investigate the geographic distribution of hyperaccumulation in these species and explore the phylogenetic distribution of hyperaccumulation in this clade by testing related species.METHODS: Portable x-ray fluorescence (XRF) spectroscopy was used to analyze 565 specimens representing eight species of Psychotria from the Missouri Botanical Garden herbarium. RESULTS:Nickel hyperaccumulation was found in specimens of Psychotria costivenia ranging from Mexico to Costa Rica and in specimens of P. grandis from Guatemala to Ecuador and Venezuela. Among related species, nickel hyperaccumulation is reported for the first time in P. lorenciana and P. papantlensis, but no evidence of hyperaccumulation was found in P. clivorum, P. flava, or P. pleuropoda. Previous reports of hyperaccumulation in P. glomerata appear to be erroneous, resulting from taxonomic synonymy and specimen misidentification.CONCLUSIONS: Hyperaccumulation of nickel by Psychotria is now known to occur widely from southern Mexico through Central America to northwestern South America, including some areas not known to have ultramafic soils. Novel aspects of this research include the successful predi...

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.

Odontarrhena serpyllifolia (Desf.) Jord. & Fourr. (=Alyssum serpyllifolium Desf.) occurs in the Iberian Peninsula and adjacent areas on a variety of soils including both limestone and serpentine (ultramafic) substrates. Populations endemic to serpentine are known to hyperaccumulate nickel, and on account of this remarkable phenotype have, at times, been proposed for recognition as taxonomically distinct subspecies or even species. It remains unclear, however, to what extent variation in nickel hyperaccumulation within this taxon merely reflects differences in the substrate, or whether the different populations show local adaptation to their particular habitats. To help clarify the physiological basis of variation in nickel hyperaccumulation among these populations, 3 serpentine accessions and 3 limestone accessions were cultivated hydroponically under common-garden conditions incorporating a range of Ni concentrations, along with 2 closely related non-accumulator species, Clypeola jonthlaspi L. and Alyssum montanum L. As a group, serpentine accessions of O. serpyllifolia were able to tolerate Ni concentrations approximately 10-fold higher than limestone accessions, but a continuous spectrum of Ni tolerance was observed among populations, with the least tolerant serpentine accession not being significantly different from the most tolerant limestone accession. Serpentine accessions maintained relatively constant tissue concentrations of Ca, Mg, K, and Fe across the whole range of Ni exposures, whereas in the limestone accessions, these elements fluctuated widely in response to Ni toxicity. Hyperaccumulation of Ni, defined here as foliar Ni concentrations exceeding 1g kg−1 of dry biomass in plants not showing significant growth reduction, occurred in all accessions of O. serpyllifolia, but the higher Ni tolerance of serpentine accessions allowed them to hyperaccumulate more strongly. Of the reference species, C. jonthlaspi responded similarly to the limestone accessions of O. serpyllifolia, whereas A. montanum displayed by far the lowest degree of Ni tolerance and exhibited low foliar Ni concentrations, which only exceeded 1 g kg−1 in plants showing severe Ni toxicity. The continuous spectrum of physiological responses among these accessions does not lend support to segregation of the serpentine populations of O. serpyllifolia as distinct species. However, the pronounced differences in degrees of Ni tolerance, hyperaccumulation, and elemental homeostasis observed among these accessions under common-garden conditions argues for the existence of population-level adaptation to their local substrates.