1. Introduction
Soils are more than inert substrates for plants — they are living systems with intricate biological networks that are essential for sustaining ecosystems, agriculture, and atmospheric balance. Within this labyrinth of particles and pores exists a staggering diversity of microorganisms, particularly bacterial communities that drive carbon cycling, nutrient transformations, and soil structure maintenance (Ponge, 2015; Fierer, 2017). These microbes are foundational to ecosystem services, and the richness and evenness of their communities are often interpreted as indices of soil health and resilience to stress (Shu et al., 2021).
Despite this central role, soil environments increasingly face contamination from human activities. Heavy metals, notably lead (Pb), have accumulated in soils near industrial areas, mines, agricultural systems, and urban landscapes due to smelting, waste deposition, and agrochemical overuse (Wang et al., 2018; Cui et al., 2018). Unlike micronutrients that play biological roles at low concentrations, lead is non-essential and toxic even at low exposure levels. Once in soils, Pb binds strongly to particles and organic matter, resisting degradation and often remaining bioavailable for decades or centuries (Violante et al., 2010; Alengebawy et al., 2021). Because of this persistence, a single contamination event can exert long-term pressure on microbial communities, potentially compromising soil function and ecological stability.
Lead’s toxicity is not uniform. Its effects hinge on bioavailability, which is shaped by soil pH, moisture, organic matter, and redox conditions (Olaniran et al., 2013; Zhao et al., 2020). Lower pH, for instance, can increase the mobility of Pb ions, intensifying their interaction with microbial cells. Conversely, high organic content may chelate metals, buffering their toxicity. Such interactions make it clear that community responses to Pb cannot be simply predicted from concentration alone — rather, they emerge from dynamic interactions among soil chemistry, contaminant speciation, and microbial physiology.
To systematically understand the impacts of Pb on microbial communities, researchers have increasingly turned to molecular tools like PCR-DGGE and high-throughput sequencing of 16S rRNA and functional genes (e.g., nirK) (Bhakta et al., 2018; Pérez-Cobas et al., 2020). These approaches provide both taxonomic depth and functional inference, enabling comparisons across gradients of contamination. In meta-analytical frameworks, such data can be aggregated to reveal overarching patterns, thresholds of ecological change, and predictors of sensitivity or resilience.
One of the central observations in contaminated soils is that microbial diversity and richness often diminish with increasing heavy metal load (Luo et al., 2018; Zhao et al., 2020). Diversity metrics like the Shannon index — which accounts for both abundance and evenness — tend to decline in soils with elevated Pb. Richness estimators such as Chao1, which emphasize rare taxa, also often decrease, indicating a loss of less abundant species under pollutant stress (Tseng et al., 2021; Zhao et al., 2020). These decreases reflect selective pressures that favor metal-tolerant taxa while sensitive species decline or disappear.
Yet this pattern is not strictly linear. Across multiple studies, microbial communities often exhibit threshold-dependent responses, in which little change occurs up to a certain Pb concentration, beyond which diversity collapses rapidly (Lin et al., 2019; Wang et al., 2019). These thresholds may represent ecological tipping points where community structure reorganizes and functional capacity is altered. Identifying such thresholds is vital for risk assessment and environmental policy, as they provide more meaningful guidance than simple dose–response relationships.
The functional consequences of Pb contamination are particularly salient in processes like denitrification, the microbial conversion of nitrate to nitrogen gases. Denitrification is essential for nitrogen balance in soils and is highly sensitive to environmental stressors (Liu et al., 2018). Because many enzymes involved in denitrification (e.g., nitrite and nitric oxide reductases) are periplasmic or associated with cell surfaces, they are more exposed to external toxins like Pb and thus particularly vulnerable (Hu et al., 2019). Suppressed denitrification can lead to nitrogen leaching into waterways and elevated emissions of nitrous oxide (N₂O), a potent greenhouse gas.
Understanding how communities retain or lose function under Pb stress also invokes concepts of resistance, resilience, and redundancy (Allison & Martiny, 2008; Griffiths & Philippot, 2012). Resistance refers to the ability of a community to withstand disturbance without changing; resilience describes the capacity to return to a pre-disturbance state; and redundancy suggests that multiple taxa can perform the same function, buffering the system against biodiversity loss. Although some taxa may decline under Pb pressures, functional redundancy may permit core processes to persist, albeit often in altered form.
The meta-analytical perspective reveals that soil properties modulate Pb impacts. For example, studies have shown that soils with higher organic content or buffering capacity often show milder declines in microbial metrics compared to acidic, low-organic soils (Pan et al., 2020; Zhao et al., 2020). Co-contaminants like Cu and Zn can interact synergistically or antagonistically with Pb, further complicating predictions of community responses (Tseng et al., 2021). These multifactor effects underscore the need for integrative analyses that go beyond single-site reports.
Taxonomically, certain microbial phyla appear more tolerant to Pb stress. Proteobacteria, Actinobacteria, and Acidobacteria often remain prevalent or even dominate in heavily contaminated soils, suggesting inherent or acquired mechanisms of metal tolerance (Zhao et al., 2020). In contrast, other groups decline sharply under Pb pressure, reinforcing the idea of selective filtering. Such shifts not only alter taxonomic composition but can reshape microbial networks and ecosystem functions.
Temporal factors also matter. Long-term contaminated sites may harbor communities that have adapted over time, displaying both structural resilience and functional shifts that differ from those in recently contaminated soils (Beattie et al., 2018; Wang et al., 2019). This legacy effect complicates remediation because adapted communities may not revert readily to baseline states even after metal reductions.
Despite the ecological importance of these findings, many studies remain context-specific. By synthesizing data across landscapes — from smelting sites and mining fields to agricultural soils — meta-analyses help distill general patterns and highlight common predictors of microbial response (Luo et al., 2018; Lin et al., 2019). Such synthesis also aids in identifying knowledge gaps, such as how mixed pollutants and soil management practices interact to shape long-term microbial trajectories.
In addition to taxonomic shifts, Pb contamination influences microbial biomass and metabolic activity (Song et al., 2018). Lower biomass carbon and suppressed enzyme activities are common in high-Pb soils, further indicating that heavy metals exert pressure not only on “who is there” but on “what they can do.” These functional metrics are especially relevant for soil processes that govern nutrient cycling and soil productivity.Taken together, a systematic review and meta-analysis approach reveals that lead contamination affects soil microbial communities in complex, threshold-dependent ways that are mediated by soil chemistry, legacy effects, co-contaminants, and functional capacities. These insights provide a foundation for risk assessment, remediation prioritization, and sustainable land management strategies aimed at sustaining soil health in the face of persistent pollutants.
Soils are more than inert substrates for plants — they are living systems with intricate biological networks that are essential for sustaining ecosystems, agriculture, and atmospheric balance. Within this labyrinth of particles and pores exists a staggering diversity of microorganisms, particularly bacterial communities that drive carbon cycling, nutrient transformations, and soil structure maintenance (Ponge, 2015; Fierer, 2017). These microbes are foundational to ecosystem services, and the richness and evenness of their communities are often interpreted as indices of soil health and resilience to stress (Shu et al., 2021).
Despite this central role, soil environments increasingly face contamination from human activities. Heavy metals, notably lead (Pb), have accumulated in soils near industrial areas, mines, agricultural systems, and urban landscapes due to smelting, waste deposition, and agrochemical overuse (Wang et al., 2018; Cui et al., 2018). Unlike micronutrients that play biological roles at low concentrations, lead is non-essential and toxic even at low exposure levels. Once in soils, Pb binds strongly to particles and organic matter, resisting degradation and often remaining bioavailable for decades or centuries (Violante et al., 2010; Alengebawy et al., 2021). Because of this persistence, a single contamination event can exert long-term pressure on microbial communities, potentially compromising soil function and ecological stability.
Lead’s toxicity is not uniform. Its effects hinge on bioavailability, which is shaped by soil pH, moisture, organic matter, and redox conditions (Olaniran et al., 2013; Zhao et al., 2020). Lower pH, for instance, can increase the mobility of Pb ions, intensifying their interaction with microbial cells. Conversely, high organic content may chelate metals, buffering their toxicity. Such interactions make it clear that community responses to Pb cannot be simply predicted from concentration alone — rather, they emerge from dynamic interactions among soil chemistry, contaminant speciation, and microbial physiology.
To systematically understand the impacts of Pb on microbial communities, researchers have increasingly turned to molecular tools like PCR-DGGE and high-throughput sequencing of 16S rRNA and functional genes (e.g., nirK) (Bhakta et al., 2018; Pérez-Cobas et al., 2020). These approaches provide both taxonomic depth and functional inference, enabling comparisons across gradients of contamination. In meta-analytical frameworks, such data can be aggregated to reveal overarching patterns, thresholds of ecological change, and predictors of sensitivity or resilience.
One of the central observations in contaminated soils is that microbial diversity and richness often diminish with increasing heavy metal load (Luo et al., 2018; Zhao et al., 2020). Diversity metrics like the Shannon index — which accounts for both abundance and evenness — tend to decline in soils with elevated Pb. Richness estimators such as Chao1, which emphasize rare taxa, also often decrease, indicating a loss of less abundant species under pollutant stress (Tseng et al., 2021; Zhao et al., 2020). These decreases reflect selective pressures that favor metal-tolerant taxa while sensitive species decline or disappear.
Yet this pattern is not strictly linear. Across multiple studies, microbial communities often exhibit threshold-dependent responses, in which little change occurs up to a certain Pb concentration, beyond which diversity collapses rapidly (Lin et al., 2019; Wang et al., 2019). These thresholds may represent ecological tipping points where community structure reorganizes and functional capacity is altered. Identifying such thresholds is vital for risk assessment and environmental policy, as they provide more meaningful guidance than simple dose–response relationships.
The functional consequences of Pb contamination are particularly salient in processes like denitrification, the microbial conversion of nitrate to nitrogen gases. Denitrification is essential for nitrogen balance in soils and is highly sensitive to environmental stressors (Liu et al., 2018). Because many enzymes involved in denitrification (e.g., nitrite and nitric oxide reductases) are periplasmic or associated with cell surfaces, they are more exposed to external toxins like Pb and thus particularly vulnerable (Hu et al., 2019). Suppressed denitrification can lead to nitrogen leaching into waterways and elevated emissions of nitrous oxide (N₂O), a potent greenhouse gas.
Understanding how communities retain or lose function under Pb stress also invokes concepts of resistance, resilience, and redundancy (Allison & Martiny, 2008; Griffiths & Philippot, 2012). Resistance refers to the ability of a community to withstand disturbance without changing; resilience describes the capacity to return to a pre-disturbance state; and redundancy suggests that multiple taxa can perform the same function, buffering the system against biodiversity loss. Although some taxa may decline under Pb pressures, functional redundancy may permit core processes to persist, albeit often in altered form.
The meta-analytical perspective reveals that soil properties modulate Pb impacts. For example, studies have shown that soils with higher organic content or buffering capacity often show milder declines in microbial metrics compared to acidic, low-organic soils (Pan et al., 2020; Zhao et al., 2020). Co-contaminants like Cu and Zn can interact synergistically or antagonistically with Pb, further complicating predictions of community responses (Tseng et al., 2021). These multifactor effects underscore the need for integrative analyses that go beyond single-site reports.
Taxonomically, certain microbial phyla appear more tolerant to Pb stress. Proteobacteria, Actinobacteria, and Acidobacteria often remain prevalent or even dominate in heavily contaminated soils, suggesting inherent or acquired mechanisms of metal tolerance (Zhao et al., 2020). In contrast, other groups decline sharply under Pb pressure, reinforcing the idea of selective filtering. Such shifts not only alter taxonomic composition but can reshape microbial networks and ecosystem functions.
Temporal factors also matter. Long-term contaminated sites may harbor communities that have adapted over time, displaying both structural resilience and functional shifts that differ from those in recently contaminated soils (Beattie et al., 2018; Wang et al., 2019). This legacy effect complicates remediation because adapted communities may not revert readily to baseline states even after metal reductions.
Despite the ecological importance of these findings, many studies remain context-specific. By synthesizing data across landscapes — from smelting sites and mining fields to agricultural soils — meta-analyses help distill general patterns and highlight common predictors of microbial response (Luo et al., 2018; Lin et al., 2019). Such synthesis also aids in identifying knowledge gaps, such as how mixed pollutants and soil management practices interact to shape long-term microbial trajectories.
In addition to taxonomic shifts, Pb contamination influences microbial biomass and metabolic activity (Song et al., 2018). Lower biomass carbon and suppressed enzyme activities are common in high-Pb soils, further indicating that heavy metals exert pressure not only on “who is there” but on “what they can do.” These functional metrics are especially relevant for soil processes that govern nutrient cycling and soil productivity.Taken together, a systematic review and meta-analysis approach reveals that lead contamination affects soil microbial communities in complex, threshold-dependent ways that are mediated by soil chemistry, legacy effects, co-contaminants, and functional capacities. These insights provide a foundation for risk assessment, remediation prioritization, and sustainable land management strategies aimed at sustaining soil health in the face of persistent pollutants.