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...