Crop plants transport irregularly shaped mineral particles from root to shoot: Tracking and quantifying

Most microplastics are emitted, either directly or via the degradation of plastics, to the terrestrial environment and accumulate in large amounts in soils, representing a potential threat to terrestrial ecosystems. It is very important to evaluate the uptake of microplastics by crop plants because of the ubiquity of microplastics in wastewaters often used for agricultural irrigation worldwide. Here, we analyse the uptake of different microplastics by crop plants (wheat (Triticum aestivum) and lettuce (Lactuca sativa)) from treated wastewater in hydroponic cultures and in sand matrices or a sandy soil. Our results provide evidence in support of submicrometre- and micrometre-sized polystyrene and polymethylmethacrylate particles penetrating the stele of both species using the crack-entry mode at sites of lateral root emergence. This crack-entry pathway and features of the polymeric particles lead to the efficient uptake of submicrometre plastic. The plastic particles were subsequently transported from the roots to the shoots. Higher transpiration rates enhanced the uptake of plastic particles, showing that the transpirational pull was the main driving force of their movement. Our findings shed light on the modes of plastic particle interaction with plants and have implications for crops grown in fields contaminated with wastewater treatment discharges or sewage sludges. The presence of microplastics in wastewaters used for irrigation highlights the urgency of analysing the possible uptake of microplastics by crop plants. This study shows that submicrometre and micrometre plastic particles from treated wastewater enter the steles of crop plants via a crack entry at sites of lateral root emergence.

To investigate the uptake and transport patterns of variously sized particles in Peyer's patches (PPs) of calves, intestinal loops were created in four newborn and two 2-month-old calves, and the loops were inoculated with various particles, including carbon black, fluorescein isothiocyanate (FITC)-labeled latex, FITC-labeled dextran, bovine serum, and recombinant mouse prion protein (rMPrP). The intestinal loops were recovered at 3, 6, 9, and 24 h in newborn calves and at 24 h in 2-month-old calves after inoculation, and the transport of the particles was examined by histological and immunohistochemical means. The uptake of the particles was quantified by estimation of signal intensities. A greater intensity was found in newborn calves compared with the 2-month-old calves. The peak uptake of carbon black, FITC-labeled latex, and rMPrP in the PPs of the distal ileum occurred at 6 h after inoculation in newborn calves and then progressively decreased with time. Uptake was also dependent on the site within the small intestine and the size of the particle studied. The transport of carbon black, FITC-labeled latex, and FITC-labeled dextran occurred via the bloodstream, the mesenteric lymph nodes, and the liver of newborn calves. rMPrP was found primarily in the interfollicular regions of the submucosa of the distal ileum of newborn calves. Thus, distal ileal PPs are probably more effective at particle absorption than the jejunal PPs, and the peak uptake of the PPs within the newborn calf occurs at 6 h after inoculation.

The factors that determine whether an exogenous mineral particle will be taken up by tracheobronchial epithelial cells are unclear. We have previously proposed that active oxygen species play a role in this process, most likely through iron-catalyzed formation of hydroxyl radical and subsequent lipid peroxidation of cell membranes. To further examine this hypothesis, we prepared rat tracheal explant cultures and exposed them for 1 h to suspensions of amosite asbestos or titanium dioxide (rutile) that had been preincubated with varying concentrations of a mixture of ferrous and ferric chloride. Explants were then maintained in organ culture in air/CO2 for 1 wk to allow particle or fiber uptake to occur. Particles or fibers in the tracheal epithelium were determined by light microscopic morphometry. Similarly treated explants were assayed for malondialdehyde as a measure of lipid peroxidation in the epithelial cells. Asbestos fibers without added iron caused lipid peroxidation, but this was not true of titanium dioxide particles. For both types of dust, increasing adsorbed iron concentrations were associated with increasing particle uptake and increasing lipid peroxidation. These observations suggest that cationic iron may play a major role in particle uptake by tracheobronchial epithelia, and that particle uptake is also related to iron-mediated lipid peroxidation.

1. Submerged macrophytes have important physical and structural effects on lowland streams. This study investigated the ability of submerged macrophytes to modify the near‐bed flow and to retain mineral and organic particles in patches of four common macrophytes in shallow Danish streams during mid‐summer.2. In dense patches of Callitriche cophocarpa and Elodea canadensis, where near‐bed velocity was reduced, the sediment surface was markedly raised and enriched with fine particles. In dense patches of Ranunculus peltatus, fine sediments were deposited among rooted shoots in the upstream part of the patches, while erosion and coarse sediments prevailed in the downstream part of the patches because of the strong vortices that formed at the rear and moved up under the trailing canopy. The open canopy of Sparganium emersum, with its streamlined leaves, had little effect on flow and sediment.3. Patterns of sediment deposition and composition were closely related to the morphology and canopy structure of plant species and the presence of low velocity above the sediment among the rooted shoots. The mineral particles retained probably originate from bed‐load, and the enrichment with finer particles within the patches probably results mainly from size‐selective processes during erosion and transport of particles rather than during deposition. The mixed sediment composition within patches suggests that the flow‐resistant shoots generate an environment conducive to deposition of all transported particles.4. Fine sediments within macrophyte beds contained high concentrations of organic matter, carbon, nitrogen and phosphorus. The wide scatter in the relationships between mineral grain size and the content of organic matter and nutrients reflects the spatial and temporal complexity of erosion, transport and sedimentation of mineral and organic particles.5. Enrichment of sediment within macrophyte beds relative to the surrounding substratum ranged from 780 g organic matter m–2, 30 g N m–2 and 25 g P m–2 for the flow‐resistant dense canopies af Callitriche cophocarpa to 150 g organic matter m–2, 6.6 g N m–2 and 3.4 g P m–2 for the open canopies of Sparganium emersum. Retention of nutrient‐rich particles within the macrophyte beds is probably of limited importance for plant growth in most lowland European streams, because macrophyte growth is rarely nutrient limited.

Among the various missions assigned to the SHOM and responding to the French Navy and public administration requests (involved in environmental affairs), one of the recent objectives is to ensure better knowledge of the continental maritime area. Among coastal projects, the one we deal in this study consists in evaluating the optical properties of shelf waters. This project called "Turbidity" focuses more particularly on turbidity processes having an impact on submarine visibility. This project is structured around three topics: (1) spatial and in-situ observations of the turbidity, (2) acoustic measurements for detection of particles loads and (3) a modelling approach. The modelling theme, presented here, involves development of simulation tools coupling hydrodynamics (the physical frame is provided by the MARS3D model developed by Ifremer), biological and sedimentary dynamics (provided by the model SiAM3D developed by Ifremer). An optical model completes this tool, in order to convert the turbidity parameters in terms of submarine visibility. The actual configuration of the model simulates the turbid waters above the French Atlantic continental shelf. The project includes also an adaptation of this framework to the Persian gulf area. The model takes into account the mineral and organic (living and non-living) particles which influence the optical properties of water. The biological production follows specific conditions of light, nutrients inputs and ocean dynamics. And the mineral particles are coming from river discharges and exchanges fluxes with the sediment (erosion and deposit). The complexity of the processes requires a modelling approach. At this complexity of particles origin, adds the complexity of the circulation of waters masses and particulate transport in coastal area (dynamic of freshwater plumes, gradients of water's density, influence of mixing by winds, tides and waves, and interactions of these processes with coastline and bathymetry). Consistent with the observations, the model reproduces reasonably well the main algal and mineral seasonal structures. The two mains axes planned to improve quantitative assessment are (1) the modelling of particulate structures and (2) the optical model: (1) modelling presents encouraging results but is actually limited by a coarse spatial resolution of the model, by simplified forcing fluxes (wave, wind and sunshine) and by simplified hydro-sedimentary and biological schemes; (2) the optical module is based on empirical laws coming from literature and is limited to a monochromatic approach; however, in-situ measurements cruises are planned in order to be suited to the specific characteristics of the study areas. The difficulty of this feasibility study is based on the fact that neither in-situ measurements, nor model estimations are directly linked to the visibility parameters. In-situ, visibility is assessed with the measurement of inherent optical properties. With the model, it is deduced from the particles concentrations. Moreover, the biological and sedimentary transport models are not able to reproduce the whole nature and multitude of particles and molecules influencing the optical properties. All this makes the visibility distances difficult to assess.

Suspensions of insoluble particles are available on the market for foliar fertilizers. The question whether uptake of particles into the leaf interior is possible is under debate. The present study examines stomatal uptake of mineral particles into leaves of Avena sativa after spraying an aqueous suspension of calcium carbonate particles. By choosing a plant species with large stomata, confirming wide open stomata at the time of spraying and using a “super spreading” organosilicone surfactant, conditions were optimized for stomatal uptake. Scanning electron microscopical (SEM) examination confirmed particles in the intercellular spaces mostly in the vicinity of stomata. The number and size of particles was larger if leaves were treated with wide open than with closed stomata. The chemical identity of the particles was examined with electron‐dispersive x‐ray spectrography (EDX), confirming the presence of calcium carbonate particles among other particles of unknown origin. In conclusion, this study provides evidence for surfactant‐assisted stomatal uptake of mineral particles from sprayed suspensions in species with large stomata under specific conditions favoring stomatal uptake.

Nitrogen availability and mineral particles contributed fungal necromass to the newly formed stable carbon pool in the alpine areas of Southwest China

Tacrolimus (FK) and cyclosporine (Cs) are potent immunosuppressants that effectively prevent the rejection of transplanted organs including liver and small intestine. Our study examined the effects of these immunosuppressants on Peyer's patches, which play an important role in mucosal immune response through uptake and transport of enteric microorganisms and macromolecules in the gut-associated lymphoid tissues. After administration of FK and Cs, we assessed changes in lymphoid follicle structure and quantified the uptake and transport of particles in the follicle associated epithelium (FAE) including M cells, using fluorescent latex microspheres in rabbit Peyer's patches. Rabbits, five in each group, received oral administration of FK (3.2 mg/kg), Cs (10 mg/kg), or phosphate-buffered saline daily for 7 days. After 2 days of withdrawal, rabbits were anesthetized, and received injections with 2 ml of the suspension of 0.5-microm fluorescent microspheres (1010/ml) into ligated intestinal segments containing Peyer's patches. After 2 hr of gentle agitation, segments were removed, rinsed, fixed with periodate-lysine-2% paraformaldehyde, frozen, and sections were stained with fluorescent phalloidin to label brush border actin filaments. The size of the lymphoid follicles in each group was measured under a light microscope. The number of microspheres in follicles was assessed in graphically defined areas of follicles from each group. In addition, immunohistochemical analysis of CD43 and MHC-II positive cells in FAE of lymphoid follicles of each group was performed. FK and Cs significantly reduced the height of lymphoid domes and the height and width of follicles, as compared to those of controls. In both FK and Cs groups, the numbers of microspheres that adhered, were taken up and were transported into lymphoid follicles were smaller than in controls, indicating that their movement rates into deep layers were markedly reduced. Furthermore, FK and Cs reduced the mean numbers of CD43 and MHC-II positive cells in FAE per unit area (mm2) as compared with controls. These findings suggest that FK and Cs may produce immunosuppressive effects, at least in part, through reduction of the uptake and transport of particles into Peyer's patches, and by reduction of the number of immunoreactive cells in FAE of Peyer's patches.

The role of reactive surface sites and complexation by humic acids in the interaction of clay mineral and iron oxide particles

Complex intestinal and hepatic in vitro barrier models reveal information on uptake and impact of micro-, submicro- and nanoplastics

We examined a range of responses of root cortical cells to Rhizobium sp. inoculation to investigate why rhizobia preferentially nodulate legume roots in the zone of emerging root hairs, but generally fail to nodulate the mature root. We tested whether the inability to form nodules in the mature root is due to a lack of plant flavonoids to induce the bacterial genes required for nodulation or a failure of mature cortical cells to respond to Rhizobium spp. When rhizobia were inoculated in the zone of emerging root hairs, changes in beta-glucuronidase (GUS) expression from an auxin-responsive promoter (GH3), expression from three chalcone synthase promoters, and the accumulation of specific flavonoid compounds occurred in cortical cells prior to nodule formation. Rhizobia failed to induce these responses when inoculated in the mature root, even when co-inoculated with nod gene-inducing flavonoids. However, mature root hairs remained responsive to rhizobia and could support infection thread formation. This suggests that a deficiency in signal transduction is the reason for nodulation failure in the mature root. However, nodules could be initiated in the mature root at sites of lateral root emergence. A comparison between lateral root and nodule formation showed that similar patterns of GH3:gusA expression, chalcone synthase gene expression, and accumulation of a particular flavonoid compound occurred in the cortical cells involved in both processes. The results suggest that rhizobia can "hijack" cortical cells next to lateral root emergence sites because some of the early responses required for nodule formation have already been activated by the plant in those cells.

Polycyclic aromatic hydrocarbons (PAHs) are widespread chemicals that are potentially carcinogenic and toxic to human due to dietary intake of food crops contaminated by PAHs. To date, the mechanisms underlying root uptake and acropetal translocation of PAHs in crops are poorly understood. Here we describe uptake and translocation of phenanthrene (a model PAH) in relation to nitrogen form and concentration in wheat and lettuce seedlings. At concentrations of 0-15 mM, phenanthrene uptake by roots is enhanced with an increase in ammonium and inhibited with an increment of nitrate. Phenanthrene concentration in shoots is much lower than in roots, suggesting that the direction of phenanthrene transport is acropetal. Ammonium reduces both phenanthrene accumulation and bioconcentration factor in shoots, as well as translocation factor, but nitrate elevates them. Phenanthrene uptake increases nutrient solution pH in the treatments with either nitrate or ammonium. Thus, it is concluded that the root uptake and acropetal translocation of phenanthrene in crops are associated with nitrogen form. Our results provide both a novel insight into the mechanism on PAH transport in higher plants and a promising agronomic strategy to minimize PAH contamination in crops or to improve phytoremediation of PAH-contaminated soils or water via nitrogen management.

Inhaled mineral particles that are not removed by macrophages or the mucociliary escalator tend to be taken up by pulmonary epithelial cells (Adamson and Bowden 1981; Bowden 1987). This process of is considerable pathologic importance. Depending on the exact mineral species, particle uptake may be associated with a variety of mutagenic events (Mossman et al 1990; Hei 1989; Hesterberg and Barrett 1985; Hei et al 1992). As well, some mineral particles are directly cytotoxic and their uptake leads to cell death and epithelial ulceration. Particles may also be transported through the cell cytoplasm to the underlying interstitial tissue (airway wall, alveolar interstitium), and in this location they can interact with interstitial macrophages to cause release of fibrogenic mediators, eventually leading to airway wall or interstitial fibrosis (Adamson et al 1989; Ferin et al 1992; Brody and Hill 1982).

Diabetic alterations of blood vessels have been well studied, but much less is known about the lymphatic system, which plays an important role in the transport of particles and defensive responses. Accordingly, we investigated lymphatic changes in diabetic rats. Ten, 30 or 60 days after alloxan-induced diabetes (40 mg/kg; i.v.), we studied thoracic duct lymph flow and lymphocyte output, thoracic duct lymph transport of radiotracer particles ((99m)Tc-dextran 500), lymph node uptake and scintigraphic visualization of subcutaneously injected radiotracer particles, as well as the effect of insulin administration and food deprivation. Diabetes significantly increased thoracic duct lymph flow and the transport of dextran from the footpad subcutaneous tissue. Abnormal lymphocyte output from the thoracic duct occurred in the first 10 days. Uptake of dextran into regional lymph nodes was decreased in diabetes. Insulin per se, although not normalizing blood sugar levels, appeared to recover thoracic duct lymphocyte output and lymph node uptake of (99m)Tc-dextran 500 without affecting the thoracic duct lymph flow or the amount of radiotracer recovered therein. Normalization of glycemia (by food deprivation) restored the lymph flow to control levels without modifying the lymphocyte output. On the other hand, under insulin-restored normoglycemic conditions, both the thoracic duct lymph flow and the lymphocyte output were normalized. These findings suggest that variables related to defensive mechanisms, such as lymphocyte recirculation and particles uptake into the lymph nodes can benefit from insulin treatment, whereas glycemic control can benefit transport mechanisms in the lymphatic system, such as lymph flow and lymphatic transport of particles.

The interactions between dissolved organic matter (DOM) and mineral particles are critical for the stabilization of soil organic matter (SOM) in terrestrial ecosystems. The processing of DOM by ectomycorrhizal fungi contributes to the formation of mineral-stabilized SOM by two contrasting pathways: the extracellular transformation of DOM (ex vivo pathway) and the secretion of mineral-surface-reactive metabolites (in vivo pathway). In this study, we examined how changes in nitrogen (N) availability affected the formation of mineral-associated carbon (C) from these two pathways. DOM was extracted from forest soils. The processing of this DOM by the ectomycorrhizal fungus Paxillus involutus was examined in laboratory-scale studies with different levels of ammonium. At low levels of ammonium (i.e., under N-limited conditions), the DOM components were slightly oxidized, and fungal C metabolites with iron-reducing activity were secreted. Ammonium amendments decreased the amount of C metabolites, and no additional oxidation of the organic matter was detected. In contrast, the hydrolytic activity and the secretion of N-containing compounds increased, particularly when high levels of ammonium were added. Under these conditions, C, but not N, limited fungal growth. Although the overall production of mineral-associated organic C was not affected by ammonium concentrations, the observed shifts in the activities of the ex vivo and in vivo pathways affected the composition of organic matter adsorbed onto the mineral particles. Such changes will affect the properties of organic matter-mineral associations and, thus, ultimately, the stabilization of SOM.IMPORTANCE Nitrogen (N) availability plays a critical role in the cycling and storage of soil organic matter (SOM). However, large uncertainties remain in predicting the net effect of N addition on soil organic carbon (C) storage due to the complex interactions between organic matter, microbial activity, and mineral particles that determine the formation of stable SOM. Here, we attempted to disentangle the effects of ammonium on these interactions in controlled microcosm experiments including the ectomycorrhizal fungus P.involutus and dissolved organic matter extracted from forest soils. Increased ammonium levels affected the fungal processing of the organic material as well as the secretion of extracellular metabolites. Although ammonium additions did not increase the net production of mineral-adsorbed C, changes in the decomposition and secretion pathways altered the composition of the adsorbed organic matter. These changes may influence the properties of the organic matter-mineral associations and, thus, the stabilization of SOM.