Mechanistic study of arsenic uptake, transformation and tolerance in arsenic hyperaccumulator Pteris vittata

Pteris vittata, the first reported arsenic hyperaccumulating plant, is potentially used in phytoremediation of arsenic, as it can accumulate up to 2.3% of arsenic in its fronds. In this study, the mechanisms of arsenic tolerance, uptake and transformation were studied in the plant. Arsenic species were analyzed by HPLC-AFS. Results showed that arsenic was mainly accumulated in leaflets, and inorganic arsenate and arsenite were only species in P. vittata. Arsenite was the predominant species in leaflets, whereas arsenate was the predominant species in roots. Arsenic induced the synthesis of thiol containing compounds in P. vittata. As-induced thiol was purified by a novel method: covalent chromatography following preparative HPLC. The purified thiol was characterized as a phytochelatin with two units (PC2). ^ In P. vittata, enhanced tolerance likely results from unusual intracellular detoxification mechanisms. Although PC-dependent sequestration of arsenic into vacuoles is essential for nonhyperaccumulators, this sequestration is not the major arsenic tolerance mechanisms in this arsenic hyperaccumulator. PC-independent sequestration of arsenic is likely the major arsenic tolerance mechanism. PC-dependent arsenic detoxification is probably a supplement to this major mechanism. ^ Interactions between arsenic and phosphate were studied. Under hydroponic condition, arsenic supply decreased the concentrations of phosphate in roots. In soil, arsenic increased the concentrations of phosphate in roots. Arsenic concentrations in rachises and leaflets were not affected by arsenic supply in either hydroponic or soil system. Phosphate decreased arsenic accumulation in roots, rachises and leaflets in the hydroponic system. ^ The uptake kinetics of arsenate, arsenite, monomethyl arsinic acid (MMA), dimethyl arsonic acid, and phosphate were studied in P. vittata. Phosphate uptake systems in Pteris vittata cannot distinguish phosphate and As(V), resulting in As hyperaccumulation. Arsenic hyperaccumulation in this plant is an inevitable consequence during phosphate acquisition. Arsenate, arsenite and MMA are transported via the phosphate uptake systems. The co-transport of arsenite/phosphate and MMA/phosphate is reported for the first time in plants. These unique phenomena are useful for understanding arsenic hyperaccumulation and the evolution of this capacity in P. vittata. ^

Seasonal plant water uptake patterns in the saline southeast Everglades ecotone

The purpose of this study was to determine the seasonal water use patterns of dominant macrophytes coexisting in the coastal Everglades ecotone. We measured the stable isotope signatures in plant xylem water of Rhizophora mangle, Cladium jamaicense, and Sesuvium portulacastrum during the dry (DS) and wet (WS) seasons in the estuarine ecotone along Taylor River in Everglades National Park, FL, USA. Shallow soilwater and deeper groundwater salinity was also measured to extrapolate the salinity encountered by plants at their rooting zone. Average soil water oxygen isotope ratios (δ 18O) was enriched (4.8 ± 0.2‰) in the DS relative to the WS (0.0 ± 0.1‰), but groundwater δ 18O remained constant between seasons (DS: 2.2 ± 0.4‰; WS: 2.1 ± 0.1‰). There was an inversion in interstitial salinity patterns across the soil profile between seasons. In the DS, shallow water was euhaline [i.e., 43 practical salinity units (PSU)] while groundwater was less saline (18 PSU). In the WS, however, shallow water was fresh (i.e., 0 PSU) but groundwater remained brackish (14 PSU). All plants utilized 100% (shallow) freshwater during the WS, but in the DS R. mangle switched to a soil–groundwater mix (δ 55% groundwater) while C. jamaicense and S. portulacastrum continued to use euhaline shallow water. In the DS, based on δ 18O data, the roots of R. mangle roots were exposed to salinities of 25.4 ± 1.4 PSU, less saline than either C. jamaicense(39.1 ± 2.2 PSU) or S. portulacastrum (38.6 ± 2.5 PSU). Although the salinity tolerance of C. jamaicense is not known, it is unlikely that long-term exposure to high salinity is conducive to the persistence of this freshwater marsh sedge. This study increases our ecological understanding of how water uptake patterns of individual plants can contribute to ecosystem levels changes, not only in the southeast saline Everglades, but also in estuaries in general in response to global sea level rise and human-induced changes in freshwater flows.

Water Uptake Patterns of an Invasive Exotic Plant in Coastal Saline Habitats

Schinus terebinthifolius Raddi (Schinus) is one of the most widely found woody exotic species in South Florida. This exotic is distributed across environments with different hydrologic regimes, from upland pine forests to the edges of sawgrass marshes and into saline mangrove forests. To determine if this invasive exotic had different physiological attributes compared to native species in a coastal habitat, we measured predawn xylem water potentials (Ψ), oxygen stable isotope signatures (δ18O), and sodium (Na+) and potassium (K+) contents of sap water from plants within: (1) a transition zone (between a mangrove forest and upland pineland) and (2) an upland pineland in Southwest Florida. Under dynamic salinity and hydrologic conditions, Ψ of Schinus appeared less subject to fluctuations caused by seasonality when compared with native species. Although stem water δ18O values could not be used to distinguish the depth of Schinus and native species' water uptake in the transition zone, Ψ and sap Na+/K+ patterns showed that Schinus was less of a salt excluder relative to the native upland species during the dry season. This exotic also exhibited Na+/K+ ratios similar to the mangrove species, indicating some salinity tolerance. In the upland pineland, Schinus water uptake patterns were not significantly different from those of native species. Differences between Schinus and native upland species, however, may provide this exotic an advantage over native species within mangrove transition zones.