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Abstract
Based on the data obtained from the multipurpose regional geochemical survey (1:250000) in the Beijing, Tianjin and Heibei Province, and the basic conception of geochemical baseline and environmental background values, the study area (Northern Haihe plain) was divided into three statistical units in light of the different depositional conditions. By using the method of standardization, that is, after repeatedly crossing out the surface soil anomalous data, geochemical baselines of various indicators were obtained through the correlation between other elements and inert element Ti, and after repeatedly crossing out the deep soil anomalous data, mean values, standard deviations and variation coefficients of 34 indicators were obtained, and thus characterized the background values. The above study may be cited as major scientific basis for regional soil environmental quality evaluation and monitoring.
Fungi possess prominent tolerance and detoxification capacities in highly metal(loid)-polluted systems, yet little is known about their responding behaviors under different contamination conditions. Here, we systematically investigated the structure and function profiles of fungal communities in an abandoned reservoir mainly contaminated by multiple metal(loid)s such as Al, Be, Cd, Co, Cr, and Cu. This abandoned reservoir consisted of three distinct zones, i.e., Zone I with the shortest deprecation time and the highest metal(loid) contamination; Zone II with the medium deprecation time and medium metal(loid) contamination; and Zone III with the longest abandonment time and the lowest metal(loid)contamination. The lowest pH and the highest contents of OM, TN, and TP were also observed for the high-contamination Zone I, followed by the moderate-contamination Zone II and the low-contamination Zone III. Fungal biodiversity was found to be robust and dominated by many endurable genera in Zone I, and notable cooperative relationships among fungal species facilitated their viability and prosperity under severe metal(loid) contaminations. Differently, the lowest biodiversity and fragile co-occurrence network were identified in Zone II. As metal(loid) contaminations reduced from Zone I to Zone III, dominant fungal functions gradually changed from undefined saprotroph guild to parasites or pathogens of plant-animal (i.e. animal pathogen, endophyte, and plant pathogen). Moreover, metal(loid)s combined with physicochemical properties jointly mediated the fungal taxonomic and functional responses to different metal(loid) contamination levels. Overall, this study not only broadens the understanding of taxonomic and functional repertoires of fungal communities under different metal(loid) contaminated conditions, but also highlights the crucial contributions of specific fungi to bioremediation and management in varying metal(loid)-polluted environments.
Assessing the impacts of parent material on distributions of potentially toxic elements (PTEs) in soils has significant consequences in the apportionment of their sources. In this study, geochemical distributions and sources of PTEs in the soils developed in quaternary sediments and granite plutons of Pearl River Delta (PRD), South China, were investigated. The results indicate that there are systematic differences between the concentrations of oxides and PTEs in the soils developed in these two parent materials. The parent material predominantly determines the element distributions in the soils. The PTEs of the deep soils developed in quaternary sediments originated mainly from mafic, felsic, and carbonate sources materials as well as polymetallic deposits. For the deep soils developed in granite plutons, the element associations are governed mainly by their geochemical affinities and behaviors and the mineral compositions of granite plutons. Anthropogenic activities impact the features of the PTEs in the surface soils of PRD. However, superimposed regional-scale pollution was found to not hide the effect of the parent material on the distribution of PTEs in the surface soils.
Heavy metal contamination poses considerable threats to various ecosystems, yet little is known about the assembly and adaptation of microbial communities at sites with combined heavy metal(loid) pollution. Here, we examined metal(loid) pollutants and bacterial communities in three zones (Zones Ⅰ, Ⅱ, and Ⅲ) of an abandoned sewage reservoir with different usage years. The contamination level of multiple metal(loid)s was higher in Zone Ⅰ than in the other zones, and arsenic (As), zinc (Zn), selenium (Se), copper (Cu), tin (Sn), molybdenum (Mo), antimony (Sb), cadmium (Cd), lead (Pb), thallium (Tl), and nickel (Ni) were the major contaminants (pollution load index > 1). Bioavailable forms of titanium (Ti), chromium (Cr), Sn, and cobalt (Co) played essential roles in shaping the microbial structure, and physicochemical properties, especially organic matter (OM) and pH, also mediated the microbial diversity and composition in the metal(loid) contaminated zones. Metal–microbe interactions and heatmap analysis revealed that the bioavailability of metal(loid)s promoted the niche partitioning of microbial species. Metal-resistant species were abundant in Zone Ⅰ that had the highest metal-contaminated level, whereas metal-sensitive species prevailed in Zone Ⅲ that had the lowest pollution level. The bioavailable metal(loid)s rather than physicochemical and spatial variables explained a larger portion of the variance in the microbial community, and the homogeneous selection was the dominant ecological process driving the assembly of the microbial community. Overall, our study highlighted the importance of metal(loid) bioavailability in shaping microbial structure, future bioremediation, and environmental management of metal(loid) contaminated sites.
Geoc hemical parameters of top and deep soils as well as geochemical baseline and background were calculated based on multi-purpose regional geochemical survey covering Yangtze River-Huaihe River basin of Anhui Province. The concentrations of most elements in top soils are mainly controlled by their concentrations in deep soils. The concentrations of some elements in different soil layen are apparendy different. Soil formation processes and anthropogenic activities have had remarkable impact on the distribution of elemental concentrations in soils. It is demonstrated that soil parent material usually has significant influence on geochemical baseline. Geochemical baselines of soils derived from the same parent materials have the tendency to vary in different geographical units. Therefore calculation of soil geochemical baseline should consider spatial variation. These results can be widely used in eco-geochemistry and related multi-discipline research.
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