Introduction

Arsenic (As), cited as the most hazardous chemical substance, is immensely concerned due to its ubiquitous contamination with an exceedingly varying concentration in environments caused by anthropogenic and natural sources (Yan et al. 2015). Arsenic usually changes its forms biochemically in the surroundings with four stable oxidation states, i.e. elemental As (As0), arsenate (As(V)), arsenite (As(III)) and arsine (As(-III)) (Miyashita et al. 2016). Inorganic As, especially As(V), is more abundantly found in aerobic and aquatic environment as a major contaminant at global scale (Hasegawa et al. 2010). Inorganic As undergoes methylation process and changes into organoarsenicals such as monomethylarsonic acid (MMA), dimethylarsinic acid (DMA), arsenobetaine (AsB), and arsenocholine (AsC) owing to microbial-mediated biotransformation (Li et al. 2019; Roy et al. 2015).

Cyanobacteria can play critical roles in As biotransformation and biogeochemical processes in diverse environment including oceans, freshwater, soil and groundwater. (Duncan et al. 2015; Maeda et al. 1990, 1993; Roy et al. 2015; Wang et al. 2015; Zhang et al. 2014). They are able to adsorb and uptake As vastly using their large specific surface area and functional groups in cell membrane, alter its valence change, and convert it into methylation As species (Thomas et al. 2004; Yan et al. 2016). Microcystis aeruginosa (M. aeruginosa), the main contributor to serious cyanobacterial bloom, found abundantly in eutrophic freshwater systems, is highly tolerant of As in both field and laboratory settings (Che et al. 2018; Wang et al. 2013a, b; Zeng et al. 2019). Nowadays, cyanobacteria blooms, especially Microcystis, accompanied by As pollution are observed in many eutrophic freshwater lakes. M. aeruginosa rapidly increase their biomass in short periods combined with its high As toleration, making it possible to be used in As removal (Jia et al. 2018; Sulaymon et al. 2013; Wang et al. 2020).

Except for heavy metals, recent researches have shown the wide presence of various nanoparticles (NPs) in aquatic ecosystems. Iron oxide nanoparticles (nano-Fe2O3) are one of the most widely explored and utilized metal nanomaterials in catalysts, medical diagnostics, magnetic materials, cosmetics, coatings/paints/pigments and electronics due to their novel properties such as excellent finite-size effect, optical performance, super paramagnetism and inherent biocompatibility (Hu et al. 2017; Keller et al. 2013). The extensive application of nano-Fe2O3 has led to their inevitably release into the aquatic environment during production, usage and disposal. Generally, nano-Fe2O3 are considered environmentally friendly, biocompatible, low toxicity, biodegradable and the most stable iron oxide (Bashiri Rezaie and Montazer 2020). Similarly, nano-Fe2O3 is recognized to be one of primary components in natural clay minerals in the environment (Braunschweig et al. 2013). Furthermore, many researches have reported that nano-Fe2O3 could enhance seed germination, chlorophyll content, root growth in some plants such as Vigna radiata L., Citrullus lanatus and Citrus maxima (Alidoust and Isoda 2013; Hu et al. 2017; Li et al. 2013; Ren et al. 2011). However, nano-Fe2O3 was also considered toxic and obviously decreased the sizes of Nannochloropsis sp. and Isochrysis sp. due to their agglomerates on the surface of algal cells (Demir et al. 2015).

The widespread occurrence of nano-Fe2O3 in diverse water systems may thus alter or affect the fate of coexisting pollutants such as As(V) prevailing in aerobic aquatic environment and its biotransformation caused by microalgae, even their microcystins release. To date, few researches have investigated the impacts of nano-Fe2O3 on As bioaccumulation and biotransformation caused by algae in aquatic systems as well as microcystins release. Therefore, the objectives of this study were to explore the effects of nano-Fe2O3 on the growth of M. aeruginosa, to investigate As(V) toxicity combined with nano-Fe2O3, and to analyze As uptake, species, and its subcellular distribution as well as toxins release in M. aeruginosa impacted by nano-Fe2O3. The obtained findings on how nano-Fe2O3 influence As(V) metabolisms in freshwater algae can contribute to better understandings in biogeochemical behavior, aquatic ecosystem health involved As toxic effects, and remediation of As-contaminated waters, which potentially impacted by nano-Fe2O3.

Materials and Methods

Algal culture and nano-Fe2O3 characterization

M. aeruginosa was obtained from the Freshwater Algae Culture Collection at the Institute of Hydrobiology (FACHB-905), Chinese Academy of Sciences. And the obtained algae were maintained axenically in Erlenmeyer flasks containing BG11 medium under intermittent illumination (40 W, 16 h light/8 h dark) at 25 ± 1 °C on an orbital incubation (125 rpm). In addition, commercially available nano-Fe2O3 (99.5%, 30 nm) were purchased from Macklin Inc. (Shanghai, China). A stock solution of 100.0 g/L nano-Fe2O3 was prepared by dispersing nanoparticles in BG11 medium (Millipore, Billerica, MA, USA) and applying sonication for 30 min (50 W/L at 40 kHz) to promote stable suspension. An extra 30-min application of sonication was conducted immediately before dosing. The average hydrodynamic diameter and the zeta potential of nano-Fe2O3 were 164.5 ± 11.3 nm and -11.7 ± 0.1 mV, respectively, determined by a Zetasizer Nano ZS90 dynamic light scattering spectrometer (DLS, Malvern Instruments Ltd., UK). Furthermore, As(V) stock solution with concentration of 1.0 g/L was prepared using Na3AsO4·12H2O and stocked in dark at 4 °C until usage.

Tolerance of nano-Fe2O3 to M. aeruginosa

The tested algae of M. aeruginosa with an initial cell density approx. 1.0 × 107 cells/mL were transferred to modified BG11 culture (Fe3+ free) with one of eight concentrations of nano-Fe2O3 (0, 0.1, 0.5, 1, 5, 10, 100 and 1000 mg/L) after centrifugation and twice sterile water washing. All treatments were cultured in the modified BG11 media for 96 h. The algal optical density (OD) at a wavelength of 680 nm, chlorophyll a (Chla) and the maximum photosynthetic quantum yield of PSII (Yield) were measured every 24 h. The algal specific growth rate calculated by OD, Chla and Yield were used to determine the stress effects impacted by nano-Fe2O3.

As(V) adsorption onto nano-Fe2O3 in algal culture medium

It is vital to understand As(V) adsorption on nano-Fe2O3 during the biokinetics process. To investigate As(V) adsorption on nano-Fe2O3, identical As(V) concentration of 100 µg/L in 100 mL of BG11 with final concentrations of nano-Fe2O3 at 0.1, 1 and 5 mg/L suspensions in Erlenmeyer flasks was prepared, respectively. At the period of 3, 5, 7, 9, 11 and 24 h, 5 mL nano-Fe2O3 suspensions were collected and filtered with 0.45 µm syringe filter after centrifugation at 12 000 g for 5 min. Both the supernatant and the original Fe2O3 suspension were collected to measure As concentrations, and the adsorption rate (%) of As(V) onto nano-Fe2O3 were calculated. Three parallels were set for each treatment.

As(V) toxicity, uptake kinetics and biotransformation

As(V) toxicity response to nano-Fe2O3 as iron sources

Taking into account the tolerated data obtained from the above-mentioned experiments of nano-Fe2O3 and a similar iron concentration in BG11, appropriate nano-Fe2O3 level (5 mg/L) was chosen to conduct As(V) toxicity experiments. A series of As(V) concentrations (from 0 to 100 mg/L) were prepared in the sterile modified media with 5mg/L nano-Fe2O3. After 30-min bath ultrasonication, algal cells were then inoculated with initial cell density approx. 1.0 × 107 cells/mL and cultured for 96 h in 250-mL Erlenmeyer flasks. The toxicity of As(V) was expressed as 96 h EC50 (effective concentration for 50% of test algae) which were estimated by a sigmoidal dose–response curve equation based on OD, Chla, and Yield (Karadjova et al. 2008). At the end of these experiments, all the amounts of intracellular total As (TAs) and Fe were measured separately from the survival groups that treated with As(V), together with microcystins release in media.

As(V) uptake kinetics and biotransformation affected by nano-Fe2O3

M. aeruginosa with initial cell density approx. 1.0 × 107 cells/mL were inoculated and cultured for 5 days, in which As(V) level was fixed at 100 μg/L, and nano-Fe2O3 concentration was set as 0, 0.1, 1 and 5 mg/L in modified BG11 media (iron free). After 2, 4, 8, 12, 18, 48, 72, 96 and 120 h of exposure, algal solutions (approx. 20 mL) were sampled to measure intracellular TAs concentration by referring our previous pretreatment methods (Wang et al. 2018a, b). At the end of the experiments (120 h), As species in algal cells and media were all pretreated and detected separately, together with As distribution at subcellular levels for 0 and 5 mg/L nano-Fe2O3 treatments, in order to identify As(V) biotransformation and As subcellular distribution affected by nano-Fe2O3.

Regarding the simultaneous As uptake and release, a nonlinear one-compartment model was selected to describe the measured intracellular TAs for each treatment over time according to the following first-order kinetics:

$${[As}_{\mathrm{int}}]={k}_{u}/{k}_{e}\times \left[{As}_{\text{ext}}\right]\times \left(1-{e}^{{k}_{e}t}\right)$$

Herein, \({As}_{\text{int}}\) (μg/g dry weight) refers to the intracellular TAs; \({As}_{\text{ext}}\) (μg/L) refers to the extracellular As concentration and is assumed as a constant, and t (h) refers to the exposure time; ku (L/g/h and ke (/h) are the rate constants of As uptake and release, respectively (Wang et al. 2014).

According to the kinetic equilibrium of As uptake and release by M. aeruginosa, the selected model was applied if ke > 0. The modeling was operated with the program GraphPad Prism 8.0. The bioconcentration factor (BCF) of As was calculated as BCF (L/g) = ku/ke (Bradac et al. 2009).

Analytical methods

The As subcellular distribution experiments of M. aeruginosa exposed at 100 μg/L As(V) under free and 5 mg/L nano-Fe2O3 were conducted according to the differential centrifugation procedure (Siebers et al., 2013). Four fractions were acquired, namely cell walls, chloroplasts, cell organelles and cytoplasmic supernatant. Besides,TAs, As species including As(III), As(V), DMA and MMA in the media and algal cell as well as OD were all detected according to our previous methods used for sample preparation and analysis (Wang et al. 2018a, b, 2014). In brief, the samples we obtained as per the above procedures were further diluted to measure As using inductively coupled plasma mass spectrometry (ICP-MS) and As speciation using high-performance liquid chromatography coupled to inductively coupled plasma-mass spectrometry (HPLC-ICP-MS) (i.e., Agilent LC1100 series coupled with the Agilent ICP-MS 7800a; Instrumental Analysis Center of Huaqiao University). In addition, algal Chla and yield were observed using an advanced phytoplankton fluorometer (Phyto-PAM, Walz, Germany) after 10 min of dark conditioning of the fresh algae solution (Chalifour and Juneau 2011). The concentrations of microcystins in media were measured using enzyme-linked immunosorbent assay kit (ELISA, purchased from Institute of Hydrobiology, Wuhan, China) according to manufacturer's instructions after membrane filtration. Furthermore, two As genes (arsC and arsM) are critically involved in As bioreduction and methylation processes in algae. Herein, the relative gene expression levels of arsC and arsM genes were also quantified in the tested algae at the first day by Real-Time PCR under different nano-Fe2O3 treatments (Wang et al. 2019). The detailed quantifications were described in the Supplementary data.

Statistical analysis

All experiments were performed in triplicate, and the results were expressed as their means with corresponding standard deviations (SD). The one-way analysis of variance (ANOVA), t test and Pearson correlation analysis were conducted using IBM SPSS Statistics 23. Significant differences were considered acceptable when P < 0.05. Graphics were generated using Origin Pro 2017 and GraphPad Prism 8.0.

Results and Discussion

Algal growth under various nano-Fe2O3 levels

The specific growth rate (µ) calculated by OD (µOD) ranged from 0.00 to 0.37 /d (Fig. 1). Except for the nano-Fe2O3 concentrations of 100 and 1000 mg/L, there were insignificant differences for µOD with an overall mean of 0.35 ± 0.01 /d and a coefficient of variation (CV) of 0.03 under the other given nano-Fe2O3 levels, while for µChla calculated by Chla, it ranged from 0.22 to 0.32 /d. Similar to µOD, no obvious differences of µChla were observed from 0 to 10 mg/L nano-Fe2O3 treatments, with an overall mean of 0.30 ± 0.02 /d and CV of 0.05. The inhibition of Chla was found at 1000 mg/L nano-Fe2O3 concentrations. Nano-Fe2O3 concentration was found to be significantly correlated with µOD and µChla with the correlation coefficient of -0.801 and -0.723 (P < 0.01), respectively. Impliedly, µOD and µChla could greatly respond the effects of M. aeruginosa to nano-Fe2O3, and the induced potential algal toxicity was exhibited at more than 100 mg/L concentrations. It was similar to the results that FerMEG12 (pristine flake-like milled Fe(0) nanoparticles (nZVI)) was toxic to Chlamydomonas sp. at concentration higher than 50 mg/L (Nguyen et al. 2018). The high algal specific growth rate with paired little CV for µOD and µChla at the concentrations less than 10 mg/L indicated that toxicity and variation in M. aeruginosa growth were relatively low affected by nano-Fe2O3 with less than 10 mg/L.

Fig. 1
figure 1

Specific growth rate of M. aeruginosa based on OD and Chla under different nano-Fe2O3 conditions (The different lowercase and uppercase represent significant differences of OD and Chla at 0.05, respectively)

Arsenate toxicity

The As(V) 96 h EC50 for M. aeruginosa under 5 mg/L nano-Fe2O3 conditions obtained by OD, Chla and Yield correlated with As concentrations in media and algal cells was found to be well fitted by the sigmoidal dose–response curve with an R2 range from 0.831 to 0.979 (Fig. S1). M. aeruginosa was more sensitive to As(V) coexisting with nano-Fe2O3 as iron sources. The As(V) 96 h EC50 calculated from OD and Chla correlated with As concentrations in media and algal cells was less than four to five orders of magnitude compared with nano-Fe2O3 free, but it was unobvious for Yield (Table 1). Yield as the sensitive indicator of M. aeruginosa to As(V) toxicity was changed slightly when iron ion substituted by nano-Fe2O3 in aquatic systems compared with OD and Chla. Nano-Fe2O3 as iron sources of M. aeruginosa was considered to remarkably inhibit the algal OD and Chla under As(V) treatments. This is partly caused by iron deficiency decreasing photosynthetic efficiency due to the participation of iron in Chla synthesis (Osório et al. 2014). Similar tendency was found for As(V) 96 h EC50 with the order of Yield > OD > Chla under nano-Fe2O3 conditions obtained from As concentrations whether in media or in algal cells. In addition, the intracellular As concentration could reflect As(V) toxicity notably, which reduced the toxicity differences between OD, Chla and Yield when growth inhibition was plotted against it. Similar observation was reported for Chlamydomonas reinhardtii and Scenedesmus obliquus (Wang et al. 2013a, b). All 96 h EC50 of As(V) obtained from media or intracellular concentrations were more than that of Chlamydomonas reinhardtii and Scenedesmus obliquus for 48 h EC50, which indicated the higher As tolerance of M. aeruginosa even impacted by nano-Fe2O3 (Wang et al. 2013a, b).

Table 1 D96 h EC50 obtained from OD, Chla and Yield of M. aeruginosa under different nano-Fe2O3 conditions

As(V) concentration was found to be significant negatively correlated with OD, Chla and Yield, showing the correlation coefficient of -0.937, -0.880 and -0.852 (P < 0.01), respectively. Yield was positively correlated with OD and Chla, showing the correlation coefficient of 0.821 and 0.831(P < 0.01). As the indicator of the ability to transform light energy into chemical energy, Yield could reflect As(V) toxicity well for M. aeruginosa, and it was obviously different from the result that Yield could not be a robust indicator of algal growth rate and nutrient status (Kruskopf and Flynn 2006). Meanwhile, Yield become less sensitive indicator compared with OD and Chla to reflect As(V) toxicity under nano-Fe2O3 as the iron sources conditions (Table 1), partly caused by its photosynthesis inhibition (Chen et al. 2005).

Intracellular TAs contents after 96 h As(V) exposure were increased with increasing As(V) levels in media, and the maximum iron contents was found at 0.5 mg/L As(V) concentrations and then showed a decline tendency (Fig. 2). The above-mentioned phenomenon confirmed As toxicity on M. aeruginosa. Kinetic constants for As uptake under 5 mg/L nano-Fe2O3 were calculated by fitting hyperbolic models to the data of As accumulation using the nonlinear regression module (Kahle and Zauke 2002). Arsenic influx can be well described by the Michaelis–Menten equation with R2 value of 0.995 (Fig. S2). The maximum uptake rate Vmax (mg/g/d) and the half saturation concentrations (Km (mg/L)) were 26.12 and 746.10, respectively, which was greater than that of nano-Fe2O3 free after 15 days exposure (Wang et al. 2013a, b), but less than Vmax of Chlamydomonas reinhardtii (51.1 mg/g/d) and Scenedesmus obliquus (39.5 mg/g/d) from short-term (4 h) experiments under phosphate deficiency conditions and more than that of Km not exceeding of 0.5 mg/L As(V), respectively (Wang et al. 2013a, b). This indicated that there was high As(V) tolerance of M. aeruginosa even under 5 mg/L nano-Fe2O3 conditions. Although there was iron free in media, the residual iron in algal cells was still able to maintain its normal growth. Moderate iron supply derived from nano-Fe2O3 was found in our study. Furthermore, the depressed iron accumulation in algal cells could reflect As(V) toxicity indirectly (Fig. 2).

Fig. 2
figure 2

Intracellular TAs and iron contents in M. aeruginosa under different As concentrations affected by 5 mg/L nano-Fe2O3. (The vertical coordinate axis for As accumulation is presented by logarithmic)

Microcystins in media

Microcystin in media under different As(V) concentrations was investigated at the end of the As(V) toxicity experiments (Fig. 3). The average concentration of microcystin in media was 7.26 ± 0.67 mg/L after 96 h algal culture under different As(V) treatments. It was more than 150 times compared with previous results of 0.04 mg/L under 1.0 × 107 cells/mL without As(V) stress (Pei et al. 2014), and less than the peak concentration of 29 mg/L found in Lake Oubeira, Algeria (Nasri et al. 2008). These were different from the generally assumption that microcystin did not exceed 0.01 mg/L in cyanobacteria-contaminated water (Cao et al. 2018). In our experiments, microcystin in media was found positively correlated with As concentrations but negatively correlated with intracellular Fe content with the Pearson's correlation coefficient of 0.630 (P < 0.01) and -0.554 (P < 0.05), respectively. The results were consistent with previous studies that the production of microcystin in M. aeruginosa could be accelerated by As(V) in media (Gong et al. 2011). However, it was different from the founding that the intracellular and extracellular quantity of microcystin could be promoted under iron-replete conditions (Wang et al. 2018a, b). Previous studies suggested that iron uptake in M. aeruginosa was not congruent with the upregulation of microcystin synthesis (Takaara et al. 2019). Specifically, it can partly be elucidated by the inhibition of As accumulation in algal cells due to iron uptake and thus decreased the abiotic stresses for M. aeruginosa. Microcystin concentrations in media decreased first and then increased with increasing As(V) concentrations. The lowest microcystin concentration in media was observed at 1 mg/L As(V) treatments with significantly differences from other As(V) treatments. Gong et al. (Gong et al. 2011) had reported that As(V) at higher than 7.5 mg/L could promote microcystin content in M. aeruginosa by inhibiting algal growth, and the lowest microcystin production was found at 0.75 mg/L As(V) treatment. The consistent results illustrated that nano-Fe2O3 did not significantly alter microcystin release trends with different As(V) concentrations even though the toxicity of M. aeruginosa regulated by nano-Fe2O3.

Fig. 3
figure 3

Microcystins in media of M. aeruginosa under different As concentrations affected by nano-Fe2O3 of 5 mg/L (The different letters represent significant differences at 0.05)

As(V) uptake kinetics affected by nano-Fe2O3

The TAs concentration in algal cells increased with increasing exposure time for different nano-Fe2O3 treatments (Fig. S3), which were well fitted to the nonlinear one-compartment model with the R2 (between 0.894 and 0.963) (Fig. S3; Table S1). The calculated ku for uptake rate constant for As(V) in M. aeruginosa under different nano-Fe2O3 treatments ranged from 0.170 ~ 0.627 L/g/h. The values of ku were observed to slightly decreased under lower nano-Fe2O3 (0.1 and 1 mg/L), but prominently increased under 5 mg/L nano-Fe2O3. They were lower than that of M. aeruginosa exposed at 10 µM As(V) with ku from 6.58 to 136.90 L/g/h (Wang et al. 2014). Moreover, it was similar to green algae Chlamydomonas reinhardtii (0.40 L/g/h) but more than Scenedesmus obliquus (0.09 L/g/h) at 75 µg/L As(V) exposures for 144 h (Wang et al. 2013a, b). In addition, the BCF decreased from 38.46 to 11.40 L/g (Fig. 4), indicating that As accumulated in M. aeruginosa was reduced with increasing nano-Fe2O3 in media. However, it was more than Chlamydomonas reinhardtii (6.15 L/g) at 75 µg/L As(V) exposures (Wang et al. 2013a, b). Furthermore, the small ke value for the efflux rate constants (0.005 ~ 0.055 /h) suggested a sluggish As release from M. aeruginosa, but it increased with nano-Fe2O3 increasing especially for 5 mg/L nano-Fe2O3 which was quintuple of the free nano-Fe2O3 and caused the decrease of BCF. Specifically, ke values in this study were lower than Chlamydomonas reinhardtii (0.065 /h), but similar to our previous study of M. aeruginosa (0.017 ~ 0.055 /h) when they all exposed at 75 µg/L As(V) conditions (Wang et al. 2013a, b; Wang et al. 2018a, b). Therefore, nano-Fe2O3 as iron sources of M. aeruginosa accelerated intracellular As release and decreased intracellular As accumulation. It can be explained by the dilute As(V) concentration in media by As(V) sequestration through high adsorption of nano-Fe2O3 (Fig. S4) (Lin et al. 2019). Furthermore, the rapid As absorption equilibrium in algal cells with nano-Fe2O3 thus decreased As intracellular BCF. Specifically, the BCF of As in M. aeruginosa was reduced by 38% under 0.1 mg/L nano-Fe2O3 compared with nano-Fe2O3 free in media. It was different from the result that As BCF in Daphnia magna was increased with nano-TiO2 as a positive carrier (Li et al. 2016).

Fig. 4
figure 4

Estimated As uptake rate constants ku (L/g/h), intracellular As efflux rate constants Ke (/h) and BCF (L/g) of M. aeruginosa under different nano-Fe2O3 level treatments

As(V) biotransformation affected by nano-Fe2O3

Except for only As(V) and trace amount of DMA were detected in media under nano-Fe2O3 free treatments, As(III) in media was also determined with less than 1 μg/L concentration under nano-Fe2O3 treatments (Fig. 5). Our previous study shows that M. aeruginosa at As(V) exposures was observed with higher organic As (OAs) release rate than that of As(III) (Wang et al. 2013a, b). In this study, relatively high As(III) release in media was decreased with increasing nano-Fe2O3, but OAs concentrations showed opposite tendency (Fig. 5). This indicated that As biotransformation in media was improved to a certain extent by nano-Fe2O3 as iron sources for M. aeruginosa. It might be caused by the high conductivity of nano-Fe2O3 and could enhance electron transfer in living organisms to accelerate As(V) biological reduction as well as the subsequent methylation in algal cells and their rapid release to media (Lin et al. 2019). Meanwhile the reported adsorption capacity of nano-Fe2O3 on As(III) was twice than that of As(V) (Tang et al. 2011), which could partly enhance As(III) biotransformation of M. aeruginosa. The detailed mechanisms need further investigation.

Fig. 5
figure 5

Arsenic species in media and algal cells under different nano-Fe2O3 level treatments (The different letters represent significant differences at 0.05)

Although three As species including As(V), As(III) and DMA were all found in algal cells, As(V) remained dominant species with more than 75.0% of intracellular TAs, followed by As(III) with 15.3–24.4% under different nano-Fe2O3 treatments. The intracellular As accumulation decreased with increasing nano-Fe2O3, and significant differences were observed for intracellular As(V) accumulation especially under more than 1 mg/L nano-Fe2O3 treatments (Fig. 5b). This result was consistent with As BCF observed in M. aeruginosa under different nano-Fe2O3 treatments, and was different from nano-TiO2 to accelerate As accumulation in M. aeruginosa (Luo et al. 2018). Whether in media or in algal cells, As(V) biotransformation (the amount of As(III) and methylated As species) were all improved under 1 mg/L nano-Fe2O3 treatments, which indicated that a suitable nano-Fe2O3 level in aquatic environment could increase As biotransformation. This is supported by the higher relative gene expression levels (2−∆CT) of arsC and arsM in elevated nano-Fe2O3 treatments (Fig. S5). Previous studies reported that 5 mg/L nano-Fe2O3 stimulated green algae growth and elevated algal lipid and polyunsaturated fatty acids contents by the dissolved trace ions of nano-Fe2O3 as a trace element for algal growth (He et al. 2017).

Subcellular distribution of arsenic

From the subcellular distribution of As in algal cells (Fig. 6), we found that As primarily existed in cytoplasmic supernatant of the tested algae with more than 78.0% of TAs. There were insignificant differences of As in cytoplasmic supernatant and chloroplast fractions under both free and 5 mg/L nano-Fe2O3 treatments. More notably, As distributed in cell organelles was increased but decreased in cell walls by nano-Fe2O3 additive, which exhibited significant differences compared with nano-Fe2O3 free (Fig. 6). This indicated that nano-Fe2O3 as As carrier mainly affected As transportation from cell walls to organelles. It might be elucidated by the mild cell wall damage and strong affinity to cell membranes due to the uptake of nano-Fe2O3 for algal cells (Phenrat et al. 2009; Saxena et al. 2020). Meanwhile, chloroplasts were regarded as playing a central role in the cellular iron ion sink of plant cells (Jain and Connolly 2013). Iron deficiency in media might cause nano-Fe2O3 carried with As accumulated in algal organelles and increase As toxic effects (Fig. 2). From these aspects, As biotransformation in algae was then stimulated potentially by this increased toxic effects of As (Luo et al. 2018).

Fig. 6
figure 6

Subcellular distribution of As in algal cells under free and 5 mg/L nano-Fe2O3 treatments (* indicates significant differences at 0.05 level). CS, CW, CH and CO represent cytoplasmic supernatant, cell wall, chloroplasts, cell organelles, respectively

Environmental implication

In this study, we found nano-Fe2O3 reduce arsenate bioaccumulation in M. aeruginosa, but increase arsenic biotransformation (i.e., bioreduction and methylation). It suggests that As ecological risk in M. aeruginosa can be lowered by nano-Fe2O3 through its decreased accumulation of arsenic and its subsequent biotransformation into lower toxic species. Taking into account the wide distribution, elevated amount and high As adsorption of nano-Fe2O3 in the environment, the As risks in waters can be mitigated to some extent by nano-Fe2O3. Additionally, this mitigated role cannot lead to release excessive harmful microcystins from the tested algae, supported by the insignificant differences of microcystins release under different As treatments at 5 mg/L nano-Fe2O3 levels compared to other reported values. On the other hand, as the first report on how nano-Fe2O3 influence As metabolisms in freshwater algae, this study provided new insights into how nano-Fe2O3, as one of the components in natural nano-clay minerals, could be used to mitigate the As risks in aquatic environment. The findings would be helpful in the understanding and practical applications of natural clay minerals on algal bioremediation of As-contaminated water. However, various processes and uncertainties of As behaviors are needed to considered in-depth, involving the changes of crystal structures of nano-Fe2O3 and their adsorption of As, other more tested algal species and algal physiological dynamics, and other environmental influencing factors.

Conclusions

In summary, this study found that nano-Fe2O3 increased As(V) toxicity on M. aeruginosa. Meanwhile, nano-Fe2O3 did not significantly alter microcystin release even though the toxicity of M. aeruginosa regulated by nano-Fe2O3 under different As(V) concentrations. Due to the efflux rate constants of As increasing with the increase of nano-Fe2O3 and it was more exaggerated than the uptake rate constants increasing for 5 mg/L nano-Fe2O3 compared with nano-Fe2O3 free, the BCF of As was decreased by increasing nano-Fe2O3. The reduction of As(V) to As(III) and the subsequently methylation caused by M. aeruginosa were observed to be increased with nano-Fe2O3 addition, and the optimal As biotransformation was at 1 mg/L nano-Fe2O3 conditions. Nano-Fe2O3 as iron sources of M. aeruginosa regulated As subcellular distribution with declining in cell walls but increasing in cytoplasmic organelles. Accordingly, As accumulation of M. aeruginosa was decreased, but its biotransformation was increased due to nano-Fe2O3 addition in media. The obtained findings could benefit us to thoroughly understanding how nano-Fe2O3 as important natural clay minerals impacts on As biogeochemical behavior and its As removal application of microalgae.