Search Results (579)

Atmospheric deposition in industrial basins of Central Asia is strongly influenced by local emissions and wintertime dispersion conditions. This study characterized snowpack at 63 sampling stations across Ust-Kamenogorsk, Kazakhstan, including operational background station 1, on 24–26 February 2025 after a 116-day accumulation period. Major ions were determined in a spatially distributed exploratory subset of 16 samples, and trace elements were measured in samples from all 63 stations by means of inductively coupled plasma mass spectrometry and optical emission spectrometry. Mean meltwater pH and total dissolved solids were 6.55 ± 0.34 and 37.3 ± 18.0 mg L⁻¹, respectively. Charge-balance errors for the 16 hydrochemical samples ranged from −0.3% to +0.7%. Using the contamination index based on exceedances of the current Kazakhstan water-quality thresholds, 48 stations had CI < 1, seven had CI = 1–3, and eight had CI > 3; the highest value (60.21) occurred at station 26. Principal component analysis showed that the first three components explained 53.6% of the variance and separated a broad mineral/industrial aerosol association from a Pb–Cd–Zn association consistent with non-ferrous metallurgy and mixed urban sources. Cadmium was therefore interpreted as the principal contributor to the MPC-normalized index at the most affected stations, rather than as the dominant component by absolute concentration. The dissolved fraction can be mobilized during spring melt, indicating a potential pathway to soils and receiving waters, although direct ecological or human-health risk was not quantified. Station-level point mapping and projection along the NW–SE axis showed localized multi-element maxima rather than a monotonic citywide gradient. Full article

Background/Objectives: Manganese (Mn) is a neurotoxic trace element whose excessive accumulation in the brain can induce hippocampal damage via oxidative stress, mitochondrial dysfunction, neuroinflammation, and apoptosis. This study investigated whether honokiol (HNK) and its liposomal nanoformulation (HNK-LNPs) can ameliorate Mn-induced hippocampal neurotoxicity by modulating key antioxidant and mitochondrial regulatory pathways. Methods: Male Wistar rats were subjected to Mn exposure to induce hippocampal neurotoxicity and were treated with HNK or HNK-LNPs. We assessed oxidative status via NRF2/HO-1 signaling, antioxidant defenses (glutathione, GPx, SOD, CAT), and oxidative indices (ROS, MDA). Neuroinflammatory markers (NF-κB, TNF-α, IL-1β, IL-6, Iba-1), mitochondrial respiratory chain function and ATP levels, SIRT1/PGC-1α signaling, and neurotransmitter homeostasis were evaluated. We analyzed apoptosis using Bax, Bcl-2, caspase-3, and cytochrome c, along with histopathological and ultrastructural examination of the hippocampus. Results: Mn exposure was associated with NRF2/HO-1 downregulation, depleted endogenous antioxidants, increased ROS and MDA levels, and increased NF-κB–driven neuroinflammation and microglial Iba-1 expression. Mn was further associated with reduced ATP synthesis, dysregulation of SIRT1/PGC-1α signaling, and disrupted neurotransmitter balance, with a pro-apoptotic shift (elevated Bax, caspase-3, cytochrome c; reduced Bcl-2) and neuronal degeneration. Co-treatment with HNK, and more prominently with HNK-LNPs, was associated with reversing these alterations, restoring antioxidant and mitochondrial pathways, dampening inflammatory cascades, normalizing neurotransmitters, and favoring neuronal survival, with many indices approaching control values and consistently surpassing free HNK. Conclusions: Liposomal encapsulation significantly enhances honokiol’s neuroprotection against Mn-induced hippocampal neurotoxicity, likely via improved CNS bioavailability and coordinated modulation of NRF2/HO-1 and SIRT1/PGC-1α pathways. These findings support HNK-LNPs as a promising multi-mechanistic therapeutic strategy for metal-induced and related neurotoxic brain disorders. Full article

Agricultural biomass fly ash (BFA) has attracted increasing interest as a liming material and nutrient source for acidic soils, although its effects on trace element availability and plant accumulation remain insufficiently understood. This study characterized agricultural BFA and evaluated its short-term effects on soil chemical properties, nutrient and trace element availability, and trace element concentrations in maize biomass. Unlike previous studies focusing primarily on biomass ash characterization or crop performance, this study integrates biomass fly ash characterization with post-harvest soil properties, nutrient and trace element availability, and trace element accumulation in maize biomass. A 60-day greenhouse pot experiment was conducted in an acidic loamy sand using BFA and commercial agricultural lime (CAL) applied at rates corresponding to 0.5×, 1.0×, and 1.5× soil hydrolytic acidity. Both amendments increased soil pH, reduced hydrolytic acidity, and increased base saturation, although CAL produced a stronger liming effect. BFA supplied substantially more K and Mg and increased soil total carbon and electrical conductivity, while CAL was more effective in increasing Ca availability. Changes in soil trace element availability were generally limited, although Zn and Cr increased after BFA application. Trace element responses in maize biomass were element-specific: concentrations of Fe, Cu, Co, and Cd increased, Mn decreased, and Zn and Ni showed no consistent dose-dependent pattern. Nevertheless, the concentrations measured in maize remained within ranges commonly reported for plants grown on uncontaminated soils. PCA supported the contrasting effects of the amendments, associating BFA more strongly with nutrient availability, total carbon, and electrical conductivity and CAL with soil deacidification and Ca enrichment. Under the conditions of this short-term pot experiment, agricultural BFA improved selected chemical properties of acidic soil without causing pronounced increases in trace element accumulation in maize biomass. Field-scale and long-term studies, including chromium speciation, are required before broader agricultural application can be recommended. Full article

This study investigates the spatiotemporal distribution of heavy metals in urban soils of Thessaloniki, Greece, over a four-year monitoring period (2021–2024). A total of 664 soil samples were collected across diverse land-use types during both wet (winter) and dry (summer) seasons. Soil physicochemical properties were analyzed alongside cadmium (Cd), copper (Cu), lead (Pb), and zinc (Zn) concentrations. The results reveal distinct, element-specific accumulation dynamics driven by continuous anthropogenic inputs. Statistical and geospatial analyses confirm that Cd exhibits a highly significant, progressive accumulation and spatial expansion toward residential areas. In contrast, Cu and Pb demonstrate a gradual, chronic enrichment, eventually reaching a saturation point where winter precipitation is insufficient to offset summer deposition. Zn presents as a severe but temporally stable contamination burden, anchored to the northwestern industrial–port sector. Furthermore, the alkaline properties of the local urban soils were found to act as an effective sink, immobilizing contaminants and preventing downward leaching. The Geo-accumulation Index (I_geo) confirms a progressive decline in soil quality driven primarily by cadmium, while the other trace elements exhibit persistent, stable profiles. Overall, this study establishes a vital geochemical baseline of total heavy metal loading in Mediterranean urban soils, emphasizing the need for targeted emission controls and future mobile-fraction assessments to guide sustainable urban management. Full article

Municipal solid waste landfill leachate represents one of the most environmentally challenging liquid effluents in modern waste management; however, its high nitrogen and phosphorus content renders it a potentially valuable nutrient source for microalgal phycoremediation. Here, Chlorella sp. and Scenedesmus sp. were cultivated for 15 days in CHU-10 standard medium and 50% (v/v) municipal landfill leachate from Nauta, Peru, and characterized across 33 biochemical variables, 14 physicochemical parameters, and 32 metal ions and trace elements. A sequential competitive multivariate pipeline comprising principal component analysis (PCA), hierarchical cluster analysis (HCA), permutational multivariate analysis of variance (PERMANOVA), and linear discriminant analysis (LDA) was applied to both the biochemical and bioremediation datasets. Leachate supplementation increased peak biomass density by 26.6–28.3% and elevated total protein by 56.9% in Chlorella sp. and 73.4% in Scenedesmus sp., while reducing total lipids by 37–46% and suppressing polyunsaturated fatty acid production. Both species achieved net biological removal efficiencies (NBRE) exceeding 86% for ammonium and ammonia; toxic elements, including Cd (~96%), Al (~92%), As (~90%), and Pb (~90%), were removed at higher NBRE than macro- and micronutrient categories. LDA achieved 100% leave-one-out cross-validation accuracy for species classification from both physicochemical and 32-element NBRE profiles. These findings indicate two complementary valorization directions, contingent on further biomass safety verification: leachate-grown Scenedesmus sp. shows a favorable combination of protein enrichment and nutrient removal for single-cell protein production integrated with bioremediation, while Chlorella sp. in standard medium shows a more favorable fatty acid profile for nutraceutical applications. Because leachate-grown biomass also accumulates inorganic and trace-element constituents from the medium, its suitability for protein or nutraceutical use requires direct heavy-metal characterization of the harvested biomass, independent of the demonstrated removal efficiency from the liquid phase. Full article

Selenium (Se) is an essential trace element for humans and animals, with nutritional functions and abiotic stress regulation capacity, and has been confirmed to alleviate heavy metal toxicity and inhibit its accumulation in crops. Soil lead contamination has become a prominent environmental safety problem in agricultural production, particularly in South China, and lead over-standard in edible crops poses irreversible threats to the human nervous system and blood circulation through food chain transmission. As an efficient exogenous antagonist, Se can comprehensively regulate the absorption, translocation, and compartmentalization of lead in soil–plant systems. This review systematically summarizes the interactive effects of soil physicochemical properties, crop genotypes, and Se speciation on plant lead uptake, and focuses on phytochelatin synthase (PCS), the core rate-limiting enzyme for intracellular heavy metal chelation, to elucidate the molecular cascade of Se-mediated PCS-dependent lead detoxification. We further outline multi-pathway agronomic Se applications for lead reduction; analyze key limiting factors, including Se concentration, application method, and rhizosphere microbial community; and discuss contradictory results and unresolved questions in existing studies. Current evidence confirms that appropriate Se treatment increases glutathione (GSH) content via antioxidant system regulation, upregulates PCS gene transcription and activity, promotes phytochelatins (PCs) polymerization, and forms stable PC-Pb complexes sequestered in vacuoles to reduce cytoplasmic lead mobility. Additionally, Se reshapes rhizosphere microbial community composition to lower soil Pb²⁺ bioavailability and enhances lignin and pectin biosynthesis in root cell walls to physically block root Pb²⁺ influx. Nevertheless, critical knowledge gaps remain unaddressed: (1) upstream signal transduction cascades triggering Se-induced differential PCS expression; (2) precise Pb²⁺ binding sites and affinity of PC oligomers; (3) valence-dependent disparities in selenate, selenite, and nano-Se (SeNPs) modulating PCS activity; and (4) standardized field Se fertilization protocols tailored to staple and tropical tuber crops such as cassava. This review provides systematic theoretical reference and technical foundations for dissecting Se-Pb antagonistic molecular networks, developing Se-enriched low Pb²⁺ functional fertilizers, and mitigating Pb²⁺ contamination risk in agricultural commodities. Full article

Low-TOC saline lacustrine shales are widespread in Cenozoic basins of northwestern China and Central Asia, yet their organic matter accumulation (OMA) mechanisms under arid, saline conditions remain poorly understood. We analyzed TOC, major and trace elements, and C–O isotopes in 64 core samples from eight wells in the western Qaidam Basin, and reconstructed terrigenous input, weathering intensity, paleoproductivity, redox conditions, and salinity. TOC ranges from 0.04% to 1.10% (mean 0.32%), with a statistically significant upward trend from the Shangganchaigou (mean 0.25%) to the Shangyoushashan Formation (mean 0.43%) (Kruskal–Wallis, p = 0.010). The climate was dry–cold with progressive aridification (increasing δ¹⁸O and Sr/Ba). The water body evolved from closed, strongly reducing, and unstable to more open, weakly reducing, and increasingly saline. We propose that limited nutrient supply set a low baseline for organic enrichment. Weakened terrigenous dilution and enhanced water-column stability then drove the gradual TOC increase. This reveals that OMA can occur without concurrent productivity rise, sustained solely by long-term preservation improvement, offering new constraints for source rock evaluation in arid lacustrine basins. Full article

Accurately identifying organic-rich shale intervals remains a major challenge in lacustrine shale oil exploration, particularly in continental rift basins characterized by rapid environmental change and pronounced vertical heterogeneity. This study investigates the upper Jiufotang Formation in the Ludong Sag, Kailu Basin, NE China, using total organic carbon (TOC), vitrinite reflectance, multi-stage programmed rock pyrolysis, and major and trace element geochemistry to constrain the processes governing organic matter enrichment and hydrocarbon occurrence. The studied shales contain abundant organic matter, with TOC values ranging from 1.91% to 7.55% and averaging 4.22%. Type II₂ kerogen and vitrinite reflectance values of 0.60–0.94% indicate oil-prone organic matter at low-mature to mature stages within the oil generation window. Multi-stage pyrolysis shows that the hydrocarbon assemblage is dominated by bound oil and residual kerogen-derived fractions, whereas the low-temperature movable oil fraction is limited. TOC is more strongly associated with the high-temperature pyrolysis fractions than with the light free-oil fraction, indicating that organic matter abundance primarily controls residual hydrocarbon generation potential but does not directly determine present-day movable oil content. Multiple elemental proxies are collectively consistent with deposition in a hydrologically restricted, variably brackish–saline lacustrine system with water-mass differentiation. Redox-sensitive indicators, including V/(V + Ni) and Mo, suggest persistent weakly reducing to reducing bottom-water conditions. After correction for carbonate- and phosphate-associated Ca, CIA values fall within a narrow range of approximately 67–70, indicating moderate and relatively stable source area chemical weathering. Organic matter enrichment was governed by the coupled effects of organic matter supply, preservation under stratified oxygen-deficient waters, and sedimentary dilution. We therefore propose a two-stage process framework in which depositional productivity–preservation coupling first promoted organic matter accumulation, whereas subsequent thermal maturation, hydrocarbon expulsion, retention, and adsorption reshaped the present hydrocarbon occurrence state. The results demonstrate that high organic matter abundance and residual generation potential do not necessarily translate into high movable oil content and provide a well-scale geochemical basis for source rock evaluation and future multi-well assessment in continental rift lake systems. Full article

Kanamycin (KANA), a widely used aminoglycoside antibiotic in animal husbandry, is associated with residue accumulation in foods due to improper use, threatening food safety. Detecting trace KANA in complex food systems such as dairy, meat, and apicutural products remains challenging because of matrix interferences (e.g., proteins, lipids, and co-existing ions) and limitations of conventional methods, which require labor-intensive pretreatment and sophisticated instrumentation. Aptamer-based fluorescent biosensors have emerged as promising tools for rapid, sensitive KANA detection with high specificity and on-site analysis potential. DNA aptamers act as selective recognition elements that bind KANA and undergo conformational changes for efficient signal transduction. This review summarizes recent advances in fluorescent aptasensors for KANA detection, with an emphasis on food system applications. Aptamer selection strategies are outlined, highlighting split aptamers’ advantages in binding precision and structural stability. Labeled and label-free sensing modes are compared in terms of design principles, analytical performance, and suitability for complex food matrices. Attention is paid to strategies for mitigating matrix interference and improving detection reliability in real samples. Despite progress, challenges remain in sensor stability, reproducibility, and on-site deployment. Overall, aptamer-based fluorescent biosensors provide a powerful platform for rapid antibiotic residue monitoring and advance food safety-oriented sensing technologies. Full article

The concentrations of 18 metal(loid)s were measured in five marine invertebrate species (Oxystele tigrine and sinensis, Marthasterias glacialis, Cymbula oculus and granatina, Parechinus angulosus, and Mytilus galloprovincialis) and five macroalgae/seaweed species (Aeodes orbitosa, Gelidium pristoides, Caulerpa filiformis, Ulva sp., and Bifurcaria brassicac formis) collected from eight sites within the marine environment of False Bay, Cape Town, South Africa. To assess the potential human health hazards associated with consumption, samples were acid digestion and analysed using inductively coupled plasma optical emission spectrometry (ICP-OES). The analysed elements included trace metals (Fe, Mn, Zn) toxic metals (Pb, Cd, As), transition metals (Ta, Ti), alkali metals (Li), and metalloid (Se, As). Metal concentration varied widely among species and locations, with values ranging from Zn: not detected (nd)—3836.04 mg/kg dry weight (dw); As: nd—77.98 mg/kg dw; Pb: nd—301.15 mg/kg dw; Li: nd—97.28 mg/kg dw, indicating diverse metal accumulation patterns. Human health risk was evaluated using the target hazard quotient (THQ) and hazard index (HI). Arsenic consistently exceeded the THQ threshold of one across all sites, and all the HI values were greater than one for all edible species, suggesting potential non-carcinogenic health risks associated with the consumption, except for M. glacialis, which is not commonly consumed. The HI metrics demonstrate the adverse impacts of metal concentration in marine biota. The observed spatial and biological variability in metal accumulation highlights the limitations of relying solely on metal concentrations for assessing health risks, food safety or anthropogenic contamination, and therefore more frequent and comprehensive monitoring is recommended. Full article

Mangrove microorganisms play a fundamental role in regulating sediment biogeochemical processes, particularly carbon storage and trace element cycling. Although numerous studies have examined microbial roles in individual processes, an integrated understanding of how microbial communities simultaneously regulate carbon storage and trace element dynamics in natural and restored mangrove ecosystems remains limited. This review synthesizes the global status of mangrove microbial research and the influence of microbes on carbon storage, trace element accumulation, and speciation in natural and restored mangrove ecosystems, while identifying emerging research trends and knowledge gaps. Our investigation revealed that research on the influence of microbes on carbon storage in mangrove sediments is increasing globally, with considerably increasing trends after 2017. However, less research has been reported on microbial trace metal interrelations than on carbon storage relationships, suggesting that there is limited focus from researchers on this topic. The available evidence indicates that sulfate reduction, microbial extracellular polymeric substances (EPS), microbial necromass formation, redox-driven biogeochemical coupling, and microbially mediated mineral transformations are the principal mechanisms promoting long-term carbon stabilization in mangrove sediments. Therefore, several studies have also suggested that microbial diversity regulates trace element accumulation and speciation through different pathways, such as redox transformation, bioadsorption, EPS-mediated binding or aggregation, biomineralization, and sulfide precipitation, in mangrove sediment. The principal conceptual contribution of this review is the development of an integrated framework demonstrating that microbial processes act as a central biogeochemical bridge connecting carbon storage and trace element cycling, rather than regulating these functions independently. Finally, we identify critical challenges and research priorities, including functional gene characterization, integrated metal–microbe–plant interactions, multi-omics approaches, long-term monitoring, and global meta-analyses, to improve mechanistic understanding and support evidence-based mangrove restoration and blue carbon management. Full article

The sustainable management of urban pruning residues is increasingly important for promoting circular bioeconomy practices and reducing green waste disposal. This study evaluated the composting potential of pruning biomass from 18 urban tree species (11 deciduous and 7 coniferous) and assessed the effects of biomass type and feedstock ratio on compost quality. Plant residues were composted with fresh cow manure using two compost ratios: V1 (700 g manure + 100 g plant biomass) and V2 (700 g manure + 700 g plant biomass). Compost quality was evaluated through pH, macroelement (N, P, K, Ca, Mg) and total microelement (Mn, Cu, and Zn) and heavy metal (Pb, Cd, and Ni) concentrations. The composting ratio was the primary factor controlling compost properties. V1 produced alkaline composts (pH 7.96–9.42) with higher nutrient concentrations, whereas V2 generated composts with pH values closer to neutrality (7.39–9.44). Increasing the proportion of plant biomass reduced macronutrient concentrations, with total N ranging from 2.23% in V1 to 0.72% in V2, and potassium decreasing by 50–80% relative to V1. In contrast, micronutrient concentrations increased in V2, reaching 1142.7 mg·kg⁻¹ Mn and 481.1 mg·kg⁻¹ Zn. Total heavy metal concentrations also increased with greater biomass incorporation, although values generally remained low; the highest Ni concentration (15.77 mg·kg⁻¹) was recorded in Paulownia tomentosa compost. Species-specific responses were observed for nutrient release and metal accumulation, highlighting differences between deciduous and coniferous feedstocks. The findings demonstrate that compost quality is primarily determined by the manure-to-biomass ratio, while tree species influence nutrient dynamics and trace element accumulation. Composts with higher manure proportions are suitable for nutrient enrichment and acidic soil amelioration, whereas biomass-rich composts provide enhanced micronutrient contents but require monitoring of heavy metal accumulation. Full article

As the primary component of harmful algal blooms, cyanobacteria exhibit unique adaptation strategies under environmental stress. The impact of erythromycin (ETM), a common macrolide antibiotic in aquatic environments, on colonial cyanobacteria remains unclear. This study examined the chronic toxic effects of different ETM concentrations (0.01, 0.1, 1, 10, 20 and 100 μg/L) on colonial Microcystis aeruginosa (M. aeruginosa) under varying nutrient conditions. Results showed that at 0.01–1 μg/L, ETM could promote the growth of M. aeruginosa, while high concentrations of ETM (≥10 μg/L) significantly inhibited growth (p < 0.05). Low-level ETM exposure accelerates M. aeruginosa growth by boosting PSII efficiency, extracellular polymeric substance (EPS) production, and the activities of superoxide dismutase (SOD) and catalase (CAT). Metatranscriptomic and metabolomic analyses further reveal that this stimulation is underpinned by enhanced trace-element uptake, reinforced carbon cycling, and increased biosynthesis of proteins, polysaccharides, and chlorophyll precursors. High-level ETM exposure inhibited the growth of M. aeruginosa, as evidenced by decreased photosynthesis, damaged membranes and suppressed metabolic activity. Metatranscriptomic and metabolomic analyses showed the upregulation of photosynthesis andpathways, metabolic pathways, and the accumulation of potent allelochemicals in P-limited cells exposed to 10 µg/L ETM relative to 10 µg/L ETM in nutrient-replete BG11 medium. Furthermore, phosphorus deficiency may enhance the potential of net methane formation. These findings underscore the complex interactions between antibiotic exposure and nutrient stress in cyanobacteria, with significant implications for environmental management of antibiotic contamination. Full article

Terrestrial carbonates provide important archives for reconstructing paleoenvironmental, paleoclimatic and hydrogeological conditions in semi-arid to arid continental basins. This study investigates the origin, mineralogical characteristics and geochemical properties of calcrete and dolocrete occurrences developed along the Konya Fault Zone within the Konya Closed Basin (Central Türkiye). Field observations, petrography, XRD, SEM–EDS, major and trace element geochemistry, REE analyses, stable isotopes (δ¹³C–δ¹⁸O), geostatistical methods and ESR dating were employed. The results reveal two distinct terrestrial carbonate systems. Dolocretes occur within Quaternary alluvial fan deposits developed on ultramafic–ophiolitic rocks, whereas calcretes developed pedogenically within Quaternary alluvial fan deposits overlying carbonate bedrock. Calcite, dolomite, quartz, palygorskite and smectitic clay minerals constitute the principal mineral phases. Rhizoliths, tubular structures, nodules, microbial filaments and laminated carbonate horizons indicate pedogenic carbonate accumulation. The association of palygorskite with dolomite and smectitic clay minerals suggests alkaline, Mg-rich pore waters under semi-arid conditions. Elevated Sr concentrations indicate prolonged groundwater–carbonate interaction, whereas high Ni and Co contents in the dolocretes reflect the influence of ultramafic source rocks. REE distributions are characterized by LREE enrichment, weak Eu anomalies and locally developed negative Ce anomalies, indicating pedogenic fractionation under oxidizing meteoric conditions. Stable isotope data indicate precipitation from meteoric waters influenced by soil-derived CO₂ under semi-arid climatic conditions dominated by C3 vegetation. ESR ages ranging from approximately 390–217 ka indicate carbonate formation during the Middle Pleistocene (MIS 11–MIS 7). Integrated mineralogical, geochemical, isotopic and chronological evidence indicates that the Konya terrestrial carbonates formed predominantly through pedogenic processes within meteoric vadose-zone conditions controlled by bedrock lithology (carbonate and ultramafic rocks), groundwater circulation and Quaternary climatic variability. These deposits represent important archives of Middle Pleistocene paleoenvironmental and paleohydrological evolution in Central Anatolia. Full article

Background: Copper is a trace element involved in key physiological and biochemical processes in humans, animals, and plants, and its homeostasis is tightly regulated. However, excessive exposure may cause adverse health and environmental effects. Copper-based plant protection products contribute to dietary exposure to copper and remain indispensable for the control of several crop diseases. Methods: This review summarizes the current state scientific and regulatory evidence on agricultural copper, identifies major knowledge gaps, and discusses strategies to support its sustainable use. A structured literature review was conducted using the PECO framework to define eligibility criteria, while key principles of the PRISMA 2020 statement were applied to improve the transparency of study identification and selection. Results: The available evidence confirms the dual role of copper as an essential micronutrient and a potentially toxic element, with adverse effects depending on exposure level, chemical form, bioavailability, and physiological status. Although copper remains an effective agricultural tool, long-term use may promote soil accumulation and environmental impacts. Current environmental risk assessment frameworks, originally developed for organic chemicals, do not fully account for the environmental behavior of inorganic metals. The review also examines copper occurrence, biological functions, agricultural uses, environmental fate, toxicity, and regulatory frameworks. Conclusions: Sustainable copper use requires balancing crop protection benefits with human health and environmental protection. Dietary exposure from authorized copper-based PPPs is generally considered negligible according to current EFSA PRIMo assessments, whereas occupational exposure and environmental accumulation remain important concerns. Future environmental risk assessment frameworks should better account for the environmental fate, natural background concentrations, bioavailability, and speciation of inorganic metals such as copper, thereby improving the scientific basis of regulatory decision-making. Full article