Abstract
We investigated trophic transfer of cadmium (Cd) through an Arctic marine food web in Hudson Bay and compared it with mercury (Hg), a metal known to strongly biomagnify. We evaluated blue mussel, sea urchin, common eider, sculpin, Arctic cod, and ringed seal for the influence of dietary and biological variables on variation in Cd and Hg concentrations. Age and size influenced metal concentrations among individuals within a vertebrate species. Consumer carbon and sulfur isotope values were correlated with their Cd and Hg concentrations, indicating habitat-specific feeding influenced metal bioaccumulation. Trophic transfer patterns for Cd depended on the vertebrate tissue, with food web biodilution observed for the muscle but not the liver. Liver Cd concentrations were higher in ringed seal and some common eider relative to prey. In contrast, we observed mercury biomagnification for both tissues. Tissue- and species-specific physiology can explain discrepancies of Cd trophic transfer in this Arctic marine food web.
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Introduction
Cadmium (Cd) is a non-essential element present in marine food webs. Exposure to elevated levels of Cd can result in health consequences for fish and wildlife. For example, dietary Cd exposure has been linked to kidney, bone, and reproductive damage in mammals (summarized in Marettová et al. 2015; Thévenod and Lee 2013) and has immunotoxic effects (Desforges et al. 2016). Additionally, exposure to higher concentrations of Cd can reduce fish growth (Ng and Wood 2008), reduce nutrition uptake, and cause kidney and reproductive organ damage in birds (Marettová et al. 2015; Wayland and Scheuhammer 2011). Researchers have detected elevated concentrations of Cd in tissues of marine mammals and seabirds in Arctic environments (Brown et al. 2016; Mallory et al. 2014; Wayland et al. 2001). Ocean food web studies have typically concluded that Cd does not biomagnify (Campbell et al. 2005; Cardwell et al. 2013; Gao et al. 2021; Gray 2002). However, uncertainties remain regarding Cd transfer in marine food webs since Cd biomagnification has been observed in benthic food webs with macroinvertebrates (Cheung and Wang 2008; Croteau et al. 2005) and since Cd concentrations were found to increase with trophic position in Arctic seabirds (Øverjordet et al. 2015).
Both natural and anthropogenic sources of Cd contribute to exposure levels in the Arctic. Cadmium enters the Arctic Ocean via long-range atmospheric transport and via deposition of volcanic and industrial emissions (De Vera et al. 2021), though the fluxes are relatively low compared to background transport via oceanic currents (Macdonald et al. 2000). Natural and anthropogenic sources of Cd also contribute to coastal environments via river transport of Cd-containing materials (Lambelet et al. 2013), including from mining (Søndergaard and Mosbech 2022). In addition, climate change-induced alterations to the Arctic environment, including thawing of permafrost, loss of costal sea ice, and atmospheric changes are leading to changes in transport and deposition of metals in Arctic aquatic ecosystems (AMAP 2021).
Carbon, nitrogen, and sulfur isotopes (δ13C, δ15N, and δ34S) are widely used to evaluate the role of trophic position and habitat-specific feeding on metal bioaccumulation. Dietary δ13C values undergo minimal change as carbon is transferred through the food web; therefore, δ13C values can provide information on relative carbon sources (Post 2002). In aquatic ecosystems, higher δ13C values indicate that individuals are feeding on benthic carbon sources, and lower (more negative) δ13C values indicate that individuals are feeding on pelagic carbon sources (Post 2002). Similarly, sulfur stable isotopes can provide information on habitat-specific feeding of biota. The δ34S values of pelagic-feeding Arctic marine mammals are higher than benthic-feeding Arctic marine mammals (Szpak and Buckley 2020). Sulfur stable isotopes can also indicate feeding in coastal estuarine habitats due to lower values in biota influenced by freshwater inputs of sulfate (Fry 2013). Finally, variation in δ34S values can reflect differences in the degree of sulfate reduction in foraging habitats (Habicht and Canfield 1997). The δ15N values of biota provide information on the trophic position of individuals as δ15N values increase significantly between a consumer and their food source (Post 2002).
The purpose of this study was to determine the role of food web processes in controlling high Cd concentrations detected in Arctic marine biota. We sampled animals from multiple trophic levels (primary, secondary, and tertiary consumers) and from both benthic and pelagic habitats near four communities in east Hudson Bay (EHB), Canada. We also explored the role of biological variables such as age and size in explaining variation in Cd concentrations within and between sampled species from EHB. Further, we compared the dynamics of Cd in the EHB food web to those of mercury (Hg). In aquatic systems, microbial and photochemical processes can transform inorganic Hg into an organic form called methylmercury (MeHg) (Lehnherr 2014). Methylmercury is well studied in aquatic food webs and is known to strongly biomagnify in Arctic marine food webs (Braune et al. 2015). Therefore, if Cd does biomagnify in the Hudson Bay food web, we would expect to see similar trends to those of Hg in the same food web. This research addresses uncertainties regarding processes that elevate Cd concentrations in Arctic marine vertebrates feeding on benthic and pelagic prey.
Methods
Study area
Hudson Bay is a Canadian subarctic marine ecoregion and the most southerly extension of inland sea with Arctic oceanic conditions (Gupta et al. 2022; Stewart and Barber 2010). The ice cover period for Hudson Bay extends from approximately December to June in the southern reaches (Gupta et al. 2022). This ecosystem supports a typical Arctic marine food web that includes keystone species such as Arctic cod (Boreogadus saida), ringed seal (Pusa hispida), and polar bear (Ursus maritimus) (Stewart and Barber 2010). The study area in EHB encompassed three communities along the coast (Kuujjuaraapik, Umiujaq, and Inukjuak) and a fourth community (Sanikiluaq) on the Belcher Islands, within a latitudinal range of 55° 17′ N to 58° 27′ N (Fig. 1). Little anthropogenic development has occurred along the shores in the study area, but Hudson Bay receives large inputs of fresh water from its watershed, including from major hydroelectric developments in northern Quebec and Manitoba (Stewart and Barber 2010).
Several bioindicator taxa were selected to design a study that incorporated both benthic and pelagic trophic transfer in the marine food web. Ringed seal in Hudson Bay feed on forage fish such as species of sand lance (Ammodytes spp.) and capelin (Mallotus villosus), benthic sculpin (Cottidae), and to a lesser extent Arctic cod, and crustacean invertebrates such as amphipods and mysids (Chambellant et al. 2013). Common eiders (Somateria mollissima) are diving seaducks that consume benthic invertebrates such as molluscs, crustaceans, and polychaetes in coastal areas (Galaktionov et al. 2021). Arctic cod and sculpin occupy pelagic and benthic habitats, respectively; however, both fishes consume a mix of pelagic and benthic fauna (Buckley and Whitehouse 2017; Landry et al. 2018). Finally, blue mussel (Mytilus edulis) and sea urchin (Echinoidea) were selected as pelagic and benthic bioindicators, respectively, due to filter feeding of mussels on particulate organic matter in the water column and feeding on benthic algae and on plants by sea urchins.
Sample collection
Wildlife and marine invertebrate samples were collected through community-based projects during the summer, fall, and winter between the years of 2014 and 2017 by Inuit hunters from the four communities. We provided sampling kits and field sheets to record collection information by local hunters who harvested common eiders and ringed seals. In most cases, the liver and muscle were removed in the field and placed in the sampling bags from the kits for storage and transport, although a few whole eiders were shipped frozen to the National Wildlife Research Centre (NWRC), a facility of Environment and Climate Change Canada in Ottawa, Canada, for dissection. Ringed seal length and girth were recorded in field sheets. Arctic cod and sculpin were line caught and shipped in plastic bags frozen whole. Blue mussel and sea urchin were collected by hand or by using a bottom-dredge net, usually in groups of ten animals per site (range 4–11), and frozen for storage and transport. Zooplankton were collected only at Sanikiluaq using a 1 m diameter, 1000-µm mesh net, towed by boat, and frozen in 500-mL HDPE containers for shipment.
In the laboratory at NWRC, blue mussel soft tissues and sea urchin gonads were removed from shells and processed as pools. Fish were weighed, measured for total length, and dissected to retrieve the liver and dorsal muscle. Otoliths were collected and aged using the crack and burn method by AAE Tech (La Salle, Manitoba, Canada). The fish stomachs were examined, and if present, undigested prey was collected for analysis. Muscle samples, fish livers, and small prey samples were freeze-dried for 48 h and manually homogenized within their containers. Seal and eider livers, mussel soft tissues, urchin gonads, and the larger prey samples were mechanically homogenized and freeze-dried for 48 h.
Laboratory analyses
All chemical analyses were performed on freeze-dried and homogenized material, and concentrations are reported on a dry weight basis. Total mercury (THg) concentrations were measured in tissues (n = 436) using a Direct Mercury Analyzer 80 (Milestone Inc., Shelton, Connecticut, USA) at NWRC. One replicate was analyzed for every ten samples and had a mean relative standard deviation of 2.5% (n = 52). Six types of reference materials were analyzed with a mean recovery of 95% (range 84–108%, n = 108) (Table S1). The method detection limit was 0.007 µg/g dry weight or lower, and samples were always above detection.
Methylmercury (MeHg) is the chemical form of Hg that biomagnifies through food webs, and invertebrate tissues and liver can have variable proportions of THg as MeHg, while the muscle contains predominately MeHg (Chételat et al. 2020). A subset of zooplankton, prey items, blue mussel, sea urchin, fish liver, and seal liver samples (n = 96) was analyzed for MeHg at NWRC, Flett Research Ltd. (Winnipeg, Canada), or the University of Montreal (Montreal, Canada), depending on the year. Duplicate samples were analyzed and had a mean relative standard deviation of 2.9% (n = 13). The mean recovery of certified reference materials was 92% (range 84–104%, n = 15) (Table S2). The method detection limit was 0.004 µg/g dry weight or lower.
Cadmium concentrations were analyzed for the full sample set (n = 345) by acid digestion and detection on an inductively coupled plasma mass spectrometer (ICP-MS) at NWRC or RPC laboratories (Fredericton, Canada). Duplicate samples were analyzed and had a mean relative standard deviation of 2.1% (n = 14). The mean recovery of certified reference materials was 98% (range 93–124%, n = 18) (Table S3). The method detection limit was 0.01 µg/g dry weight or lower.
Stable isotope ratios of carbon, nitrogen, and sulfur in biota were measured in invertebrates and vertebrate muscle (n = 271) on a DeltaPlus XP Isotope Ratio Mass Spectrometer interface by a ConFlo II to a Vario EL III elemental analyzer at the Ján Veizer Stable Isotope Laboratory at the University of Ottawa (Ottawa, Canada). Lipid content was measured in the livers of cod and sculpin and a subset of ringed seal liver, eider liver, blue mussel, and sea urchin (n = 124). Acid hydrolysis method AOAC 948.15 was employed to quantify tissue lipid content at RPC laboratories.
Statistical analyses
All statistical analyses were completed using R version 4.0.2 (R Core Team 2021). Information regarding testing of assumptions for statistical tests can be found in Appendix A—Supplementary Information. The complete dataset for this study is publicly available on the Open Data Portal of the Government of Canada (GOC 2022).
Sculpin and Arctic cod had variable and in some cases high lipid content in their livers, which dilute protein-bound metal concentrations (Amlund et al. 2007; López-García et al. 2014). For Arctic cod, for example, there was a negative correlation between lipid content and metal concentrations in the liver (Table S4). Therefore, we used lipid-normalized concentrations for the liver of fish, eider, and seal and whole-body measurements of blue mussel and gonads of sea urchin in the statistical models using the liver. Lipid normalization was calculated as follows: lipid normalized [metal] = [metal]/(1 − lipid portion), where lipid portion has values between 0 and 1 and is assumed to contain negligible metal concentrations (Amlund et al. 2007; López-García et al. 2014). Normalization was applied using individual % lipid values for Arctic cod and sculpin liver, which were highly variable, and average % lipid values for eider liver, seal liver, mussel, and urchin, which had low and consistent lipid content. Vertebrate muscle is typically low in lipid (≤ 10%) (Braune et al. 1999; Pedro et al. 2019; Schantz et al. 1993) and similar to lipid content of blue mussel and sea urchin (8% and 21%, respectively); therefore, statistical models that included the muscle for higher trophic levels did not include lipid-normalized data.
We used THg concentrations for the liver and for the muscle and MeHg concentrations for invertebrates. The % MeHg of the muscle exceeds 80% for included species (Dietz et al. 1996; Houserová et al. 2007; Wagemann et al. 1998). However, the % MeHg of invertebrate tissues is more variable, and we wanted to account for the greater variation. Therefore, we only included the subset of invertebrates that had MeHg concentrations measured in our analyses. The % MeHg in the liver of vertebrates is more variable (50–90%) than in the muscle. Therefore, we conducted an additional general linear mixed model (GLMM) analysis where we used MeHg-corrected values for liver data. For the analysis, we used measured values for MeHg concentrations for a subset of ringed seal liver (n = 13). We calculated MeHg concentrations in the liver of Arctic cod, sculpin, and common eider by multiplying the THg concentration in the liver by the average proportion of MeHg in the liver for each species (0.75, 0.50, and 0.81, respectively) reported in literature (Harley et al. 2015; Wayland et al. 2001). When we refer to models that include both THg and MeHg data, we simply use “Hg” when describing the results.
Some Cd concentrations in the muscle of fish and ringed seal were below analytical detection limits. For ringed seal muscle data, we followed the 2006 US EPA Guideline and substituted non-detected samples with 1/2 the detection limit because < 15% of the samples were below the analytical detection limit (Shoari and Dubé 2018; USEPA 2006). Over 50% of the Arctic cod and sculpin muscle samples were below the analytical detection limits (n = 14 of 16 and n = 11 of 15, respectively), and standard data estimation/adjustment techniques could not be performed on the left-censored data (Shoari and Dubé 2018; USEPA 2006); therefore, we removed the muscle Cd data of Arctic cod and sculpin from analyses but did use liver Cd data for these species in relevant analyses.
We conducted correlation and regression analyses, respectively, to examine co-variance of metal concentrations between tissues of the same individual and to examine the influence of age or size on metal concentrations (Table S5). We conducted GLMMs to investigate food web patterns of metal concentrations. We included dietary tracers, specifically, δ15N, δ13C, and δ34S ratios as fixed effects, and we included location of sample collection as a random effect. We conducted two GLMMs (one for Cd and one for Hg) using muscle concentrations for vertebrates, whole-body concentrations for blue mussel, and gonad concentrations for sea urchin. We then conducted two more GLMMs using lipid-normalized concentrations in the liver for vertebrates, whole-body concentrations for blue mussel, and gonad concentrations for sea urchin.
Finally, we calculated the trophic magnification slopes (TMS) for both metals in the EHB food web. We ran simple linear regressions of log metal concentrations versus δ15N ratios. We used metal concentrations in the muscle for vertebrate species. Additional analyses completed using zooplankton and prey item samples are presented in Appendix A—Supplementary Information.
Results
Metal concentrations in marine biota
Metal concentrations varied widely among biota and between tissue types from the same species (Table 1). Average Cd concentrations in biota ranged more than three orders of magnitude from 0.006 to 24.0 µg/g dw. Average Cd concentrations were highest in ringed seal and in common eider liver and were lowest in fish muscle. Average THg concentrations in biota ranged from 0.067 to 20.3 µg/g dw, with the highest levels observed in ringed seal and common eider liver and the lowest levels in sea urchin gonads. Interestingly, both metals were more concentrated in the liver than in the muscle of vertebrate animals, with the exception of THg in fish. For both fish species, THg concentrations were higher in the muscle than in the liver.
Biological and geographic drivers of metal concentrations within species
We observed geographic variation in metal concentrations for common eider and blue mussel, which were the only biota collected at all four communities (Table 1). We observed larger location differences for Cd than for THg. Muscle Cd concentrations of common eiders from Kuujjuaraapik (0.433 ± 1.03 µg/g dw) and from Sanikiluaq (0.463 ± 0.343 µg/g dw) were almost half the average concentrations found at Inukjuak (0.849 ± 0.714 µg/g dw) and at Umiujaq (0.774 ± 0.671 µg/g dw). Common eider liver from Kuujjuaraapik had a lower average Cd concentration (7.01 ± 8.55 µg/g dw) than the other three sampling locations. Blue mussels from Kuujjuaraapik also had a lower average Cd concentration (2.98 ± 0.756 µg/g dw) than the other three sampling locations. In contrast, THg concentrations in the muscle and in the liver of common eider were comparable among locations, and we observed minor variation in THg of blue mussel.
Biological variables explained some within-species variation of metal concentrations, though the influences were not consistent among biota or metals. We were unable to conduct these analyses for Cd concentrations in fish muscle because a high number (> 50%) of samples were below the level of detection. Metal concentrations in the muscle were positively correlated with those in the liver from the same animals for both common eider and ringed seal (Table S6). Age was not an important explanatory variable of metal concentrations in fish liver, and a significant positive effect was only observed for Cd in Arctic cod liver (Table 2). Similarly, length was generally not a strong explanatory variable, and positive effects were only found for THg in the liver and muscle of Arctic cod and in the muscle of ringed seal. In contrast, length was negatively correlated with Cd in Arctic cod liver though the association was weak. Axial girth was not an important variable for explaining variation of Cd concentrations in ringed seal liver but was positively related to liver THg concentration. Overall, biological variables more strongly explained THg concentrations in fish and ringed seal (R2 from 0.15 to 0.76) than Cd concentrations in biota (R2 ≤ 0.11).
Trophic influences on metal concentrations
Mean δ15N values ranged from 6.0 ± 0.2‰ to 15.7 ± 1.1‰ (Fig. 2, Table S7). Blue mussel and sea urchin had the lowest mean δ15N values of sampled species. Arctic cod, ringed seal, and sculpin shared similar trophic positions in this food web as indicated by their similar mean δ15N values. Mean δ13C values ranged from − 23.4 ± 0.5‰ to − 15.7 ± 3.1‰ in sampled biota (Fig. 2, Table S7). The observed δ13C values indicate variation in habitat-specific feeding among sampled species. Mean δ34S values ranged from 13.0 ± 0.6‰ to 20.7 ± 1.5‰ (Fig. 2, Table S7). We observed variation in δ34S values among species, which indicates differences in foraging behavior. We observed contrasting food web patterns between Cd and Hg when using the muscle for vertebrate species in the GLMM models (Table 3). Cadmium concentrations of biota were negatively correlated with δ15N values (an indicator of trophic position), while an expected positive correlation was found for Hg concentrations (Table 3, Fig. 3). These results indicated food web biodilution of Cd in contrast with biomagnification of Hg in the same food web. The TMS for Cd in the EHB food web was − 0.192 ± 0.018 (Table 4, Fig. 3). The TMS for Hg in the EHB food web was 0.150 ± 0.007 (Table 4, Fig. 3). While we did not include Arctic cod and sculpin samples in the analyses using Cd concentrations in vertebrate muscle, Cd concentrations in fish muscle tissue are lower than concentrations of Cd in invertebrates (Table 1), which also indicates biodilution of Cd, even if we were unable to quantify the exact rate of biodilution. Habitat-specific feeding, indicated by a correlation with δ13C values, also explained Cd but not Hg concentrations in the food web (Table 3). A negative correlation suggested a greater reliance on pelagic carbon was associated with higher Cd concentrations. Sulfur isotope values explained Hg but not Cd concentrations in the food web. Mercury concentrations were negatively correlated with δ34S values.
We found a different food web pattern for Cd when the GLMM models were run using the liver for vertebrate species (Table 5). Note that this Cd GLMM model included fish liver data (which, unlike fish muscle, had Cd concentrations consistently above analytical detection limits). We observed both Hg and Cd concentrations were positively correlated with δ15N (Table 5, Fig. 4). However, the correlation between log Cd concentrations and δ15N was weak (ß coef = 0.027 ± 0.010, P = 0.006), compared to the correlation between log Hg concentrations and δ15N (ß coef = 0.171 ± 0.013, P < 0.001), and the former correlation was only significant after accounting for other factors in the model. Liver Cd concentrations ranged more than two orders of magnitude among vertebrate species with a similar trophic position, and there was no simple correlation between liver Cd concentration and δ15N (Fig. 4). Additionally, δ13C and δ34S values were significant explanatory variables for Cd and for Hg concentrations, indicating influences of habitat-specific feeding on metal concentrations in biota (Table 5). Similar to the other models using the muscle (Table 3), liver Cd and liver Hg concentrations were negatively correlated with δ13C values, reflecting enhanced bioaccumulation associated with feeding on pelagic carbon sources. Cadmium and Hg concentrations of biota were negatively correlated with δ34S values (Table 5), indicating an effect of habitat-specific feeding on metal exposure. The GLMM we ran using MeHg-corrected values for liver data showed the same patterns as the GLMM run using THg concentrations in the liver (Table S8).
Discussion
Trophic transfer patterns for Cd depended on the vertebrate tissue examined. We observed food web biodilution for muscle Cd concentrations of marine vertebrates. This finding was consistent with Cd biodilution reported in other aquatic food webs (Campbell et al. 2005; Cardwell et al. 2013; Pantoja-Echevarría et al. 2023; Sun et al. 2020) and contrasts with Cd biomagnification reported for Arctic seabirds (Øverjordet et al. 2015) and for a benthic coastal food web (Croteau et al. 2005). Liver Cd concentrations of marine vertebrates showed a weak positive correlation with trophic position, though only for some species. In contrast, we observed strong Hg biomagnification in the food web for both the muscle and liver. The contrasting trends observed for Cd and Hg transfer in the EHB food web suggest that biomagnification is not a likely explanation for elevated Cd concentrations in the liver of some Arctic marine vertebrates (e.g., Dietz et al. 1998; Mallory et al. 2004, 2014, 2017). Rather, our findings suggest that tissue- and species-specific physiology may more accurately explain Cd concentration patterns. Our study indicates that tissue type and the inclusion of lower trophic level biota are important for investigating food web processes, and caution is warranted when interpreting Cd biomagnification in marine biota over a narrow range in trophic position (Chevrollier et al. 2022; Øverjordet et al. 2015; Tian et al. 2022).
Tissue- and species-specific physiology can explain the patterns of Cd concentrations in this Arctic marine food web. The discrepancy in trends observed between the liver and muscle is likely due to Cd detoxification in the vertebrate study species (Gao et al. 2021). The muscle consistently has lower Cd concentrations than the liver and kidney in fish and in wildlife (Dietz et al. 1996; Wayland and Scheuhammer 2011). This difference may be due to higher Cd depuration rates in the muscle relative to the liver, at least for fishes (de Conto Cinier et al. 1999; Pavlaki et al. 2021; Soegianto et al. 2022). In vertebrate animals, Cd is detoxified through binding to metallothionein proteins and storage in the liver and in the kidney (Wayland and Scheuhammer 2011). Subcellular measurements of Cd indicate that this metal is largely bound as stable metallothionein complexes in the liver (Desjardins et al. 2022; Monteiro et al. 2019). These findings explain why we observed such low Cd concentrations in fish muscle but detected Cd in fish liver and why we found the highest Cd concentrations in the liver of ringed seal and common eider. Elevated liver Cd concentrations likely reflect greater detoxification and storage of this metal, instead of greater dietary exposure to top predators due to biomagnification. The differences in Cd concentrations that we observed between Arctic marine vertebrates may also be due to species-specific physiology, such as differences in metallothionein production and the rate of detoxification in the liver (Le Croizier et al. 2019; Lucia et al. 2012). In contrast, we found higher concentrations of Hg in both the liver and muscle of vertebrate species, which in this case is attributed to biomagnification because of the strong positive correlations with trophic position.
We observed variation in feeding habitats: benthic versus pelagic, indicated by variation in δ13C values, and sulfate-reducing versus oxidizing environments, indicated by variation in δ34S values. Foraging behavior influenced metal concentrations in sampled biota. Pelagic feeding was associated with higher Cd concentrations in the Hudson Bay food web. This finding is consistent with studies of another Arctic marine food web (Campbell et al. 2005) and of pinnipeds on the Uruguayan coast (De María et al. 2021). Polar crustaceans can have elevated Cd concentrations and may be an important dietary source of Cd to marine vertebrates (Lischka et al. 2020; Macdonald et al. 2000; Macdonald and Sprague 1988). However, our findings differ from a study that measured Cd in ringed seal across the Canadian Arctic, where liver concentrations increased with relative carbon source, indicating benthic feeding enhanced Cd bioaccumulation (Brown et al. 2016). Nevertheless, the same study found that seals which fed primarily on pelagic amphipods near one of the communities in our study area (Inukjuak) had the highest measured Cd concentrations (Brown et al. 2016). Thus, it could be the case that some fish and some ringed seal in our study were feeding more on pelagic invertebrates leading to overall higher concentrations of Cd in their tissues. We similarly observed that pelagic feeding was associated with greater Hg concentrations in vertebrate species, which has also been reported for other Arctic marine food webs (Campbell et al. 2005; Hilgendag et al. 2022). In the Arctic Ocean, Hg methylation occurs in the water column and the highest seawater methylmercury concentrations occur at subsurface depths where planktonic uptake may be important (Jonsson et al. 2022; Wang et al. 2018).
We found a negative relationship between metal concentrations and δ34S values, which indicates an effect of foraging habitat on exposure. The pattern we observed is consistent with another Hg study conducted in northern Hudson Bay on Arctic seabird prey (Góngora et al. 2018). However, positive and non-significant correlations between metal concentrations and δ34S values in marine biota have also been reported (García Barcia et al. 2021; Lippold et al. 2020), which may be due to the influence of multiple processes on environmental δ34S gradients. The δ34S values of marine wildlife can be influenced by foraging in estuarine to saline transitions, benthic or pelagic habitats, and sulfate-reducing environments (Chételat et al. 2020). In our study, biota were collected from an entirely marine environment; therefore, we make the assumption that variation in δ34S values is more likely due to differences in degrees of sulfate reduction across foraging habitats rather than due to terrestrial or estuarine influences. Amiraux et al. (2023) observed high variability in δ34S values among benthic invertebrates sampled from Hudson Bay and noted lower δ34S values in species that fed within the sediment layer where sulfate reduction occurs. A similar trend was observed in species sampled from the Baltic Sea, where δ34S values helped further distinguish between epibenthic and infaunal food sources of the benthic-feeding velvet scoter (Melanitta fusca) (Morkūnė et al. 2018). We observed higher δ34S values in blue mussel and sea urchin which are both epibenthic species that feed above the sediment layer and lower δ34S values in eider and ringed seal which feed to some extent on infaunal taxa. Ringed seal may also feed on benthic fish such as sculpin that feed on infaunal taxa. Therefore, the negative relationship between metal concentrations and δ34S values we observed may suggest that feeding on fauna inhabiting sulfate-reducing environments may enhance metal exposure. Sulfate reduction is associated with greater MeHg production (Gilmour et al. 1992); therefore, biota feeding in areas where sulfate reduction occurs may be exposed to higher levels of MeHg. However, the relationship between foraging in habitats with higher degrees of sulfate reduction and increased cadmium bioaccumulation is unclear and warrants further investigation. Overall, sulfur isotope ratios provide complementary information to carbon isotope ratios because they help further distinguish benthic feeding by tracing consumption of infaunal versus epibenthic food sources.
We observed location effects in this study, specifically common eider livers and blue mussels sampled at Kuujjuaraapik had approximately half the average Cd concentrations of those biota sampled at the other three sites. The lower Cd concentrations observed in eider and in blue mussel suggest that there may be spatial differences in the bioavailability of Cd in east Hudson Bay. Uptake and depuration rates of Cd in marine invertebrates can be influenced by water quality variables including salinity, temperature, and pH (Pavlaki et al. 2017; Rainbow and Luoma 2011). Therefore, possible differences in water chemistry between sites may be contributing to the observed differences in blue mussel Cd concentrations, though further research is needed to evaluate the environmental drivers of spatial patterns in metal bioaccumulation.
Trophic magnification slopes have been widely measured to evaluate Hg biomagnification in food webs (Lavoie et al. 2013). Biomagnification rates of Hg, based on TMS values, can differ by latitude, environment (e.g., marine and fresh water), and even between habitats connected to the same food web (Hilgendag et al. 2022; Lavoie et al. 2013). The Hg TMS measured in this study (0.15 ± 0.01) is within the range of other studies of Arctic marine food webs (0.10–0.25) that included seabirds and marine mammals (as summarized in Hilgendag et al. (2022)). Few TMS values have been reported for Cd in Arctic marine food webs, and the value of − 0.19 ± 0.02 measured in this study is comparable, though steeper than the TMS (− 0.09) of Campbell et al. (2005). Signa et al. (2017, 2019) reported Cd TMS values of − 0.08 and − 0.07 for a Mediterranean food web and an Antarctic food web, respectively. The ecotoxicological significance of this variation in Cd biodilution rate is unclear.
Dietary exposure to Cd can be harmful to both humans and wildlife leading to kidney, bone, and/or reproductive damage (ATSDR 2012; Marettová et al. 2015; Thévenod and Lee 2013; Wayland and Scheuhammer 2011). In the Hudson Bay food web, average Cd concentrations in tissues were below adverse effect thresholds for sampled species (birds, 45–70 µg/g ww in the liver (Wayland and Scheuhammer 2011); marine mammals, 200 µg/g ww (AMAP 2005)). Exposure to the organic form of mercury (MeHg) is hazardous to human and to wildlife health. Methylmercury may pass the blood–brain barrier and cause neurological damage via oxidative stress, neuro-inflammation, cell death, neurogenesis impairment, calcium imbalance, DNA damage, changes to glutamate metabolism, and/or changes to neurotransmission (summarized in Novo et al. 2021). In the Hudson Bay marine food web, average Hg concentrations in tissues of sampled species were below wildlife adverse effect thresholds (fish, 0.5 µg/g ww in the muscle (Sandheinrich and Wiener 2011); birds, 20 µg/g ww in the liver (Shore et al. 2011); marine mammals, 61 µg/g ww in the liver (Rawson et al. 1993)). Overall, our data suggest that Arctic marine wildlife were at low risk of experiencing sublethal toxicological effects of Cd and Hg exposure, consistent with earlier assessment (Dietz et al. 1998; Fisk et al. 2005). However, our comparison with tissue burden thresholds provides only a preliminary scoping of toxicological risk, and more subtle subchronic effects, such as suppression of the immune system, may occur at lower tissue concentrations (Desforges et al. 2016).
Conclusions
This study contributes to broader research on trophic transfer of Cd in marine food webs by presenting findings for the understudied Arctic Ocean. Large variation in Cd and Hg concentrations, which ranged three orders of magnitude in the Arctic marine food web of east Hudson Bay, was related to trophic position and foraging habitat. Mercury biomagnified predictably through the food web, whereas the trophic transfer patterns of Cd differed by vertebrate tissue type. Biodilution of Cd in the food web (based on vertebrate muscle) indicated that elevated Cd in the liver of ringed seal and common eider could not be explained by greater dietary exposure. Rather, elevated Cd concentrations in some Arctic marine mammals and seabirds are likely due to Cd detoxification and storage in the liver. Species-specific physiology may also play a role in controlling Cd tissue burdens, and future research could characterize detoxification processes for Arctic marine vertebrates, focusing on metallothionein production and subcellular partitioning of Cd.
Data availability
The data used in this study are available from the Open Data Portal of the Government of Canada at https://data-donnees.ec.gc.ca/data/substances/monitor/a-east-hudson-bay-network-research-initiative-on-regional-metal-accumulation-in-the-marine-food-web/?lang=en.
References
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Acknowledgements
We gratefully acknowledge the community coordinators and hunters from Kuujjuarapik, Inukjuak, Sanikiluaq, and Umiujaq who collected marine animals for the study. This research would not have been possible without your contributions. We thank Bobby Aculiak (Inukjuak), Allie Aculiak (Inukjuak), Billy Brian Kasudluak (Inukjuak), Davidee Mina (Inukjuak), Conilucy Naktialuk (Inukjuak), Peter Nulukie (Inukjuak), Charlie Angatookalook (Kuujjuaraapik), Jordan Kronenburg (Kuujjuaraapik), George Tooktoo (Kuujjuaraapik), Vincent Tooktoo (Kuujjuraapik), Samson Tooktoo (Kuujjuaraapik), Eddy Tooktoo (Kuujjuaraapik), Willie Novalinga (Kuujjaraapik), Johnny Kudluarok (Sanikiluaq), Stephan Kudluarok (Sanikiluaq), Simeonie Uppik (Sanikiluaq), Josie Amitook (Sanikiluaq), Salamonie Kowcharlie (Sanikiluaq), Johnny Kasudluak (Umiujaq), Peter Crow (Umiujaq), Charlie Kumarluk (Umiujaq), Suzanna Aragutak (Umiujaq), and Randy Aragutak (Umiujaq). We also thank Lucassie Arragutainaq (Hunters and Trappers Association, Sanikiluaq), Annie Kasudluak (Amiturvik Landholding Corp., Umiujaq), Pauloosie Kasudluak (Inukjuak), Raymond Mickpegak (Sakkuq Landholding Corp., Kuujjuaraapik), and Allie Nalukturuk (Niqautik Hunters Association of Inukjuak) for their leadership and support of the study. We thank Michelle Zanuttig, Jian Jun Yang, Emily Porter, and Yueting Shao at the National Wildlife Research Centre (ECCC) for their technical assistance with chemical analyses. We gratefully acknowledge the production of the study area map by Ines Peraza.
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Open Access funding provided by Environment & Climate Change Canada. This research was supported by funding from the Northern Contaminants Program (Crown-Indigenous Relations and Northern Affairs Canada, Project CB-06 and CB-08, 2013–2018) and Environment and Climate Change Canada (ECCC).
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Jillian Rohonczy: formal analysis, writing—original draft, writing—review and editing, and visualization. John Chételat: funding acquisition, conceptualization, investigation, writing—review and editing, and project administration. Stacey Robinson: funding acquisition, supervision, formal analysis, and writing—review and editing. Lucassie Arragutainaq: funding acquisition, conceptualization, investigation, and project administration. Joel P. Heath: funding acquisition, conceptualization, and project administration. Christine McClelland: investigation and data curation. Raymond Mickpegak: funding acquisition, conceptualization, investigation, and project administration. Mark Forbes: funding acquisition, supervision, formal analysis, and writing—review and editing.
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Rohonczy, J., Chételat, J., Robinson, S.A. et al. Contrasting trophic transfer patterns of cadmium and mercury in the Arctic marine food web of east Hudson Bay, Canada. Environ Sci Pollut Res 31, 20586–20600 (2024). https://doi.org/10.1007/s11356-024-32268-3
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DOI: https://doi.org/10.1007/s11356-024-32268-3