Xudong Wang1,2
Danling Fan1Steffen Kiel3
Shanggui Gong1
Qiangyong Liang4Jun Tao4
Duofu Chen1,2
Dong Feng1,2*- 1Shanghai Engineering Research Center of Hadal Science and Technology, College of Marine Sciences, Shanghai Ocean University, Shanghai, China
- 2Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
- 3Swedish Museum of Natural History, Department of Palaeobiology, Stockholm, Sweden
- 4Ministry of Land and Resources of the People's Republic of China Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou, China
The natural dynamics of fluid flow at methane seeps and increasingly human activities influence the biogeochemistry of the microenvironment and further determine the activity of the chemosynthetic communities within these ecosystems. However, ways to reconstruct short-term fluid flow dynamics and to decipher the influence of scientific exploration at seeps are limited. In this study, we present high-resolution trace elements/Ca ratios (Li/Ca, Mg/Ca, Ti/Ca, Mn/Ca, Co/Ca, Cu/Ca, Zn/Ca, Sr/Ca, Zr/Ca, Mo/Ca, Ba/Ca, Th/Ca and U/Ca ratios) from the shells of two species of chemosymbiotic bivalves (the thiotrophic vesicomyid clam Archivesica marissinica and the methanotrophic mussel Gigantidas haimaensis) from the Haima cold seeps of the South China Sea. We found that the complex distribution patterns of some trace elements (Mg/Ca, Sr/Ca, Mo/Ca and U/Ca ratios) in G. haimaensis are largely controlled by mineral composition or age. The observation of Co/Ca and Ba/Ca ratios in both species indicate strong physiological and environmental control on the incorporation of trace elements during the biomineralization process. Besides, the distribution patterns of other trace elements provide information that can be used to discuss open issues such as the loss of trace elements after death of the bivalves, and the possible influence of human activities such as sediment disturbance. Overall, this study emphasizes the potential for using high-resolution element geochemistry of seep bivalve shells to reveal the physiological and environmental factors that control the growth of bivalves, and to elucidate the potential history of fluid discharge at cold seeps.
Introduction
The cold seep system is dynamic in both time and space (Suess, 2020). At present, there is a basic understanding of the activity rhythm of cold seep system on a long-time scale (millennia and above, Chen et al., 2019). Yet, increasing evidence points to short-term events such as tides or monsoons also having an influence on methane flux (Himmler et al., 2016; Wang, S. et al., 2020), but the overall frequency of such microenvironmental changes in cold seep systems remains unclear (Leifer et al., 2004; Johansen et al., 2017).
The bivalve shell is an excellent archive to reveal the evolution of their living environment on a relatively short timescale because the lifespan of bivalves can range from several to hundreds of years (Barry et al., 2007; Schöne et al., 2013). As opposed to the soft tissue of bivalves, the corresponding shell is likely to integrate and preserve elements from their environment during their whole life (Immenhauser et al., 2015). Indeed, shell carbonate layers of bivalves can provide insights into various environmental conditions during their lifetime, while soft tissue can only give us instantaneous snapshots at a certain time (Vander Putten et al., 2000; Gillikin et al., 2006; Schöne et al., 2013; Feng et al., 2018; Wang, X. et al., 2020).
Numerous studies have shown that elemental compositions in shell carbonates can provide valuable insights into past environments. Previous studies have successfully established the relationship between Sr/Ca (or Mg/Ca) and temperature, although these relationships may vary greatly among or within species (Branson et al., 2018). An alternative temperature proxy (Sr/Li ratio) was developed (Juárez-Aguilar et al., 2019), and the vital effects of Sr and Li incorporation into aragonite shells can be reduced by normalizing Sr/Ca to Li/Ca. In addition, the shell Mn/Ca ratio (Marali et al., 2017), Ba/Ca ratio (Gillikin et al., 2006; Schöne et al., 2013) and U/Ca (Kim et al., 2015; Poitevin et al., 2020) ratio were also thoroughly investigated as potential indicators of diagenetic trends, weathering intensity, salinity, paleoproductivity, pH and so on. However, the calcifying fluid chemistry and the corresponding mechanistic of shell formation appear to involve complex physiological responses and geochemical controls (e.g., Vander Putten et al., 2000; Schöne et al., 2013; Marali et al., 2017; Markulin et al., 2020). To date, only a few studies explored the high-resolution element geochemistry of deep-sea bivalve shells (Schöne and Giere, 2005; Shirai et al., 2008; Wisshak et al., 2009), and only one of them focused on cold seep areas (Torres et al., 2001). Torres et al. (2001) investigated shells of the vesicomyid clam Calyptogena kilmeri from seep sites in Monterey canyon (California, USA) and confirmed that clamshells can be used as paleotracers of fluid seepage events. However, they only investigated the Ba/Ca ratio of this chemoautotrophic bivalve. Lietard and Pierre (2008) performed a high-resolution stable isotope (δ18O and δ13C) and cathodoluminescence study of lucinid bivalve shells (Myrtea aff. amorpha) from methane seeps in the Eastern Mediterranean Sea and demonstrated the potential of these methods to reconstruct methane release event, although the influence of metabolic effect could not be completely ruled out.
In the present study, we investigated two species of chemosymbiotic bivalves from the South China Sea. Using microstructure and high-resolution element geochemistry of their shells, the purpose of this study was to reconstruct short-term fluid flow dynamics and to shed light on the short-term microenvironmental changes of cold seep ecosystems.
Materials and methods
Sample collection and preservation
Specimens of two species of seep-restricted, chemosymbiotic bivalves (Archivesica marissinica: thiotrophic, infaunal; and Gigantidas haimaensis: methanotrophic, epifaunal or semi-infaunal) were collected at the active Haima cold-seep area (water depth: ~1400 m) in the northwestern South China Sea (Figure 1; Liang et al., 2017). Once onboard the ship, the soft tissue and corresponding shell of bivalves were dissected and washed with deionized water to remove salt. The shells were air-dried and placed in a sealed sample bag for analysis.
Figure 1 Map showing the location of the samples.
Shell preparation
It impossible to create a shell chronology for the specimens since the absolute growth rate of seep bivalves is currently unknown. In an attempt to record a longer life history, 4 relatively large individuals with the length between 12.5 and 16.8 cm (A. marissinica: C2015 + C2020; G. haimaensis: M2020 + M2021) were chosen for this study. The relationships between length, width and height among the two species are almost the same, illustrating that they grew freely and were not limited by additional factors (Table 1). To obtain cross section of bivalves, we used a diamond saw to slice the shells along the axis of maximal growth, following the prevailing practice (Vander Putten et al., 2000; Torres et al., 2001; Markulin et al., 2020). To determine the shell microstructure and facilitate the laser ablation analysis, the cross section of the shells was polished with silicon carbide sandpaper (2000Cw, Ying Qiu Brand).
Table 1 Seep bivalve information including: (1) species; (2) chemoautotrophic type; (3) length, (4) width, (5) height and (6) thickness of shells; (7) sampling time; (8) status when sampling; (9) total laser spots.
Analytical procedure
Scanning electron microscopy
A Coxem EM30 PLUS SEM system (South Korea) with an accelerating voltage of 15 kV was used to observe the microstructures of A. marissinica and G. haimaensis at Shanghai Ocean University. Shell fragments from several sections along the cross sections of each species were sputter-coated with a gold layer prior to observation, and the magnification varied from 969 to 2600 times (Figure 3).
X-ray diffraction
A LabX XRD-6100 X-ray diffractometer system (Shimadzu, Japan) at Shanghai Ocean University was used to analyze the mineral composition of bulk shells (individual microstructures could not be separated since the extremely thin thickness of shell). Approximately 40 mg shell powder was prepared for each sample. The X-ray source was a Cu anode operated at 40 kV and 30 mA using CuKα radiation equipped with a diffracted beam graphite monochromator. The samples were scanned in step scan mode at an interval of 10-80° (2θ), with a step size of 0.02° and a count time of 0.6 s per step (2°/min). The diverging, scattering, and receiving slits were 1.0 mm, 1.0 mm and 0.15 mm, respectively. The carbonate type of shells was identified by using XRD processing software JADE 6.0.
LA-ICP-MS
The concentrations of Li, Mg, Ca, Ti, Mn, Co, Cu, Zn, Sr, Zr, Mo, Ba, Th, and U were determined by means of laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) in spot analysis mode along the growth axis of the shells near their outside layer (Figures 2C, D). The distance between the two laser spots is about 1mm (Figure 2), although the time span represented by two laser spots between shells or even in same shell, is different (bivalve grow faster when they were young). According to the sample size, the number of laser spots is 153 (C2015),111 (C2020),116 (M2020) and144 (M2021), respectively (Table 1). Analyses were performed at Shanghai Chemlabprop Technology Co., Ltd. using an ESI NWR193 ArF excimer laser ablation system equipped with a TwoVol2 ablation cell operating at 193 nm wavelength connected to an Agilent 7900 quadrupole ICP-MS. High-energy laser pulses hit the sample surface, and high-purity helium (99.999%) was used as the carrier gas at 700 ml/min flow to transfer the ablated material to the ICP for ionization before analysis. Satisfactory sensitivity and sufficiently low levels of oxide formation (ThO/Th < 0.2%) and fractionation effect (232Th/238U≈100%) were accomplished by daily optimization, consisting of adjusting the gas flow, sampling depth, and lens setting while ablating the glass standard reference material NIST SRM 612. The ablation was operated using a spot size of 100 μm, an energy density of ~3 J/cm2 and a pulse repetition rate of 15 Hz. The background signal was measured for 10 s prior to each ablation. Ablation time was 50 s, followed by 15 s wash out. The operational conditions of LA-ICP-MS are summarized in Table S1.
Figure 2 Images of typical seep bivalve shells and their cross sections. Clam identified as Archivesica marissinica (C2020; A) and mussel identified as Gigantidas haimaensis (M2020; B). The distance between two laser points is about 1 mm.
To ensure the data quality, NIST SRM 612 glass reference material was used as the quality monitoring standard. The data were exported after being processed with the Iolite 4 software (Paton et al., 2011), and the measured values are shown in Table S2.
Results
Shell microstructure of the seep bivalves
The thickness of the methanotrophic mussel shell (M2020: 0.57mm; M2021: 0.71mm) was less than one-third that of the thiotrophic clam shell (C2015: 2.35mm; C2020: 1.92mm. Table 1, Figures 2C, D). The microstructure of A. marissinica is rather simple since the whole shell is composed of a uniform laminated structure, the orientation of the laminae is consistent with the direction of growth (Figures 3A, C). The shell of G. haimaensis can be roughly divided into 5 parts from outside to inside layers (Figure 3): outer (fibrous) prismatic layer → outer nacre layer → myostracum → inner nacre layer → simple prismatic layer (Génio et al., 2012). Specifically, the fibers of the outer prismatic layer are oriented at an oblique angle to the outer nacreous layer. Between the outer and inner nacre layers, there is myostracum - a thin extra layer secreted by virtually all bivalves where they attach the mantle or the muscles to the shell. The inner edge of shell is a simple prismatic layer, a universal microstructure among mussels (family Mytilidae), with the prisms oriented vertically to the inner nacreous layer (Génio et al., 2012).
Figure 3 Schematic drawing of A. marissinica (A) and G. haimaensis (B). The numbers represent laminated structures (1), outer prismatic layer (2), outer nacre layer (3), myostracum (4), inner nacre layer (5) and simple prismatic layer (6). The blue line with arrow represents the path of the laser spot, the blue point represents the transition position of mineral phase (aragonite to calcite). (C) SEM image of A. marissinica (C2020); (D, E) SEM image of G. haimaensis (M2020). dog: direction of growth.
Carbonate mineral compositions
The mineral compositions of the two seep bivalves correspond to the properties of their microstructure. XRD results of A. marissinica show that the shell consists solely of aragonite, while the shell of G. haimaensis is composed of calcite and aragonite (Table S3). According to microstructure of the shell and previous research experience (Kennish et al., 1996; Kennish et al., 1998a; Kennish et al., 1998b), it is inferred that the fibrous prismatic layer of G. haimaensis is composed of calcite while the other layers are aragonitic (Génio et al., 2012; Immenhauser et al., 2015). The transition from aragonite phase to calcite phase of M2020 and M2021 occurred at laser point 40 and 46, respectively.
Element concentrations
Element results were reported in the form of trace element/calcium (TE/Ca) ratios in Table S4. The Mg/Ca ratio of G. haimaensis (~200-14000 μmol/mol, seawater at Sanya Bay: ~4900-5400 μmol/mol, Wu et al., 2014) is significantly higher than that of A. marissinica (~100-1200 μmol/mol, pore water at Haima active cold seep area: ~5300-17700 μmol/mol, Wang et al., 2018), which is quite different from the Mg/Ca ratio of their living environments. In addition, the ranges of other element concentrations of the two species were very similar (Figures 4–6).
Figure 4 Elements/Ca ratios of the bivalve shells. (A1, A2) Mg/Ca ratios; (B1, B2) Sr/Ca ratios; (C1, C2) Mo/Ca ratios; (D1, D2) U/Ca ratios; (E1, E2) Co/Ca ratios; (F1, F2) Ba/Ca ratios. C2015 and C2020 are A. marissinica; M2020 and M2021 are G. haimaensis. The blue dotted lines indicate the change from aragonite to calcite in G. haimaensis.
Figure 5 Elements/Ca ratios of the bivalve shells. (A1, A2) Li/Ca ratios; (B1, B2) Mn/Ca ratios; (C1, C2) Cu/Ca ratios; (D1, D2) Zn/Ca ratios. C2015 and C2020 are A. marissinica while M2020 and M2021 are G. haimaensis. The blue dotted lines indicate the change from aragonite to calcite in G. haimaensis, the green dotted line represents the boundary where elements may be lost for C2015.
Figure 6 Elements/Ca ratios of the bivalve shells. (A1, A2) Ti/Ca ratios; (B1, B2) Zr/Ca ratios; (C1, C2) Th/Ca ratios. C2015 and C2020 are A. marissinica while M2020 and M2021 are G. haimaensis. The blue dotted lines indicate the change from aragonite to calcite in G. haimaensis.
Discussion
Factors controlling TE/Ca ratios of seep bivalve shells
The factors driving the incorporation of trace elements into bivalve shells are complex and mainly include environmental factors (e.g., temperature, salinity, organic matter, microstructure, nutrition, pollution, etc.) and physiological regulation (e.g., mineral composition, growth rate, etc., Vander Putten et al., 2000; Gillikin et al., 2006; Shirai et al., 2014). Bivalves from shallow and deep-sea are facing different survival pressures. Compared to the shallow bivalves, the living environment for deep sea bivalves is relatively stable and the survival challenge mainly comes from food supply (Wisshak et al., 2009). Although a continuous line of sampling points intuitively suggests a time series with an equal amount of time between each point, the time interval between two sample points in the late stage of growth was much longer than at the beginning of growth, because bivalves grow much faster in their early stage and considerably slower when they get older (Barry et al., 2007). In addition, the faster the growth rate of the bivalve, the less physiological control it has over how much trace elements are incorporated into the shell. Our discussion is based on the relative age framework of the shell and draws on the achievements of previous studies (Vander Putten et al., 2000; Gillikin et al., 2006).
The mineral composition of shell carbonate is controlled by physiological regulation. The Mg/Ca and Sr/Ca ratios show an inverse pattern in G. haimaensis and remain constant in A. marissinica (Figures 4A2, B2). This is consistent with the fact that most of the derived heterodont bivalves shell (to which the vesicomyids belong) is aragonite and mussel shell (Family mytilids) is the mixture of calcite and aragonite. In G. haimaensis, the outer, calcitic layer near the umbones is so thin that it could not be targeted by our sampling method. Thus at a specific position (blue dot in Figure 3B, point 40 for M2020 and point 46 for M2021), our LA-ICP-MS sampling points moved from the aragonitic nacre layer into the calcitic outer layer, resulting in obvious changes in the Mg/Ca and Sr/Ca ratios (Figures 4A2, B2). Aragonite is generally richer in Sr than calcite. However, interestingly, the Sr/Ca ratios of A. marissinica is similar to the calcitic part of G. haimaensis but much lower than its aragonitic part, highlights the strong physiological control on the incorporation of Sr into seep bivalve shells.
Molybdenum (Mo) enrichment in cold seep systems is a very common and useful trace element proxy (Wang et al., 2019). The behavior of Mo in pore water changes when the H2S concentration exceeds 11 μM, and Mo in pore water will be scavenged and enter the sediment and then be captured by pyrite, resulting in a sharp decrease in Mo in pore water (Helz et al., 1996). In this study, except for C2020, the Mo/Ca ratios of the bivalve shells were higher in their early stage of life and then gradually decreased with occasional peaks. Visually, the Mo/Ca ratio of G. haimaensis is probably related to their Mg/Ca and Sr/Ca ratios (i.e. mineral composition). However, the trend of Mo/Ca ratio is inconsistent with the theoretical calculation based on density functional theory (incorporation stability of molybdate anions: calcite > aragonite. Midgley et al., 2020), and there is also no difference of Mo concentration in aragonite versus calcite (Wang et al., 2019). For bivalves, it was found that the incorporation of Mo into the shell is influenced by the growth rate (Tabouret et al., 2012). Therefore, a simple explanation for the Mo pattern observed here is that the bivalves get more control over Mo incorporation with age. However, this is not the case for C2020; possibly, Mo concentration were lower during its early life. Interestingly, there is virtually no difference in Mo concentration between the infaunal (=living within the sediment) A. marissinica and the epifaunal G. haimaensis (Figures 4C1, C2).
The U/Ca ratios of seep bivalves seem to be closely related to their corresponding Sr/Ca ratios, implying that the incorporation of U into shells could be related to mineral composition (Figure 4, Cravo et al., 2002). It is also found that the U/Ca ratio of marine bivalve shells is higher in the early stage of life but drops below the detection limit in the later stage due to vital effects (Gillikin and Dehairs, 2013). Therefore, as far as the seep-inhabiting species investigated here are concerned, the U/Ca ratios could be regulated by physiological factors, especially among G. haimaensis.
Cobalt (Co) is a biologically essential element (Saito et al., 2004). Co2+ competes with Ca2+ ions during biomineralization (Bellotto and Miekeley, 2007; Honig et al., 2020). Co is a vital component of vitamin B12 (cyanocobalamin), which is a coenzyme in many cellular processes, including the synthesis of DNA and the oxidation of fatty acids (Blust, 2011; Pouil et al., 2017). There are few exhaustive studies of Co on the physiological effect of bivalves thus far. Previous research indicates that the changes in lipid and sterol metabolism increased with increasing Co2+ concentrations, and it is possible that Co2+ provokes oxidation damage in mussels (Nechev et al., 2006). Another study showed that the concentration of Co in the clam Ruditapes philippinarum increases with increasing CO2 (acidified seawater, Sezer et al., 2018). In a recent study, Honig et al. (2020) found that several TE/Ca ratios differed significantly between age classes, and Co/Ca ratios were usually greater in larvae than in juveniles. It can be determined that the incorporation of Co into shell carbonate is physiologically regulated. With increasing age, the Co/Ca ratios of the shells exponentially decline in both bivalves (Figures 4E1, E2). As far as we know, there is no unambiguous knowledge of this trend. The most likely scenario is that the cobalt-assimilation rate of bivalves slows down with age. Based on this observation, we suppose that the Co/Ca ratios of seep bivalve shells have the potential to be a tool to calculate the age of bivalves at seeps, as long as we obtain the age-confirmed sample and ascertain the function between the age and Co/Ca ratios of seep bivalves. However, the potential of this approach needs to be validated in other seep areas.
The Ba/Ca ratios of shallow-water bivalve shells have been used to reconstruct the primary productivity of their living environment, which is often related to phytoplankton blooms (Vander Putten et al., 2000; Kelemen et al., 2019; Fröhlich et al., 2022), the amplitude of the chlorophyll peaks is often used to explain the peak value of the Ba/Ca ratio of bivalve shells (Goodwin et al., 2013; Doré et al., 2020). Therefore, as long as the Ba/Ca ratio of bivalve shells is not strongly physiologically controlled, the change in Ba in the environment can be reflected in shells because the Ba/Ca ratio of bivalve shells is usually related to the Ba/Ca ratio of environmental water (Gillikin et al., 2006; Goodwin et al., 2013). There are many factors that lead to an increase in Ba in the environment. In addition to autochthonic effects, such as the formation of barite (BaSO4) crystals caused by flocs after phytoplankton decay (Doré et al., 2020), autochthonic effects also include the addition of Ba-rich external fluids to the environment (such as freshwater, groundwater, hydrothermal fluids, upwelling caused by typhoons and storms, etc. Shirai et al., 2008; Goodwin et al., 2013; Markulin et al., 2020), which may lead to changes in salinity in the environment. As mentioned by some previous studies, Ba/Ca ratios in bivalve shells can be used to track salinity (Gillikin et al., 2006; Poulain et al., 2015). The Ba/Ca ratios of C2020 (A. marissinica) have a relatively flat distribution pattern with lower values (Ba/Ca ratios of C2015 is below detection limit) while the Ba/Ca ratios of G. haimaensis exhibit notable fluctuations with uncertain cycles and large relative amplitudes. The Ba/Ca ratio pattern of G. haimaensis appears to be typical for bivalves, as it has been recognized in almost all Ba/Ca ratio profiles of bivalve shells — relatively stable for most of their lifetime interrupted by occasional sharp peaks (Gillikin et al., 2008; Schöne et al., 2013; Poulain et al., 2015; Marali et al., 2017; Markulin et al., 2020). The study site is an area of active seepage with an obvious Ba front in the sediment (the highest concentration of Ba is ~1200 ppm, Liu, S et al., 2020), indicating a considerable Ba supply. Therefore, in our opinion, the peak Ba/Ca ratios of seep bivalves are affected by the discharge of Ba-rich fluids. The same conclusion was reached by Torres et al. (2001), although the peak Ba/Ca ratio in our study (10 μmol/mol) is much lower than theirs (up to 80 μmol/mol). It is necessary to analyze more shells collected from the same cold seep area in the future. If there is strong interindividual reproducibility of the Ba/Ca ratio, then environmental driving factors that control the incorporation of Ba in shells exist.
In summary, due to its monomineralic composition, the distribution of trace elements in A. marissinica has its unique advantages in constraining physiological mechanism and reconstructing the changes of microenvironment in the study area. The distribution of trace elements in the bimineralic G. haimaensis and other mussel shells is easily affected by mineral composition, as reflected in the Mg/Ca and Sr/Ca ratios, and potentially the U/Ca ratios, too. To solve the issues with bimineralic shells encountered in this study, the application of chemical staining could be used to distinguish aragonite from calcite in future research (Kato et al., 2003). In addition, we propose that the Mo/Ca ratios in the studies bivalves were controlled by age (i.e. growth rate), and probably affected by environmental factors (for C2020). The Co/Ca ratios of seep bivalve shells intuitively indicates that the rate of Co incorporated into the shell carbonate slows down with age, opening the potential to utilize this trend to constrain the age of seep bivalves.
Loss of trace elements in shells after death of the bivalves?
Based on the observation of some TE/Ca ratios of C2015, there is the potential of element loss (decline in concentration) after the bivalve dies. At the time of collection, C2015 was the only dead individual of all four samples. Compared to the other three bivalve shells, the TE/Ca ratios of C2015 often show a flatter distribution pattern (Figure 5). As mentioned earlier, the Mg/Ca and Sr/Ca ratios of seep bivalve shells are mainly controlled by physiological factors. The mineral composition of C2015 is aragonite, and the ratios of Mg/Ca and Sr/Ca should be relatively stable if there are no other factors involved. This is true for the Sr/Ca ratio but not for the Mg/Ca ratio. After laser point 93, the Mg/Ca ratio of C2015 was significantly increased, implying that Mg may lost before laser point 93 (Figure 4). The same patterns are also observed for the Li/Ca, Mn/Ca, Cu/Ca and Zn/Ca ratios, which all exhibit lower ratios before laser point 93 (green dot line in Figure 5). Furthermore, the decreasing trend of the Co/Ca ratio of C2015 stopped at point 3 (Figure 4E1), which is obviously different from the logarithmic decreasing trend of the other three samples. The Ba/Ca ratios of C2015 were not reported because the content of Ba is lower than the detection limit. Therefore, Co and Ba may also be lost. A possibility is that these trace elements are actually contained in the organic matter within the shell. The presence of organic matter occupies the position of lattice in bivalve shells, thus affect the contents of lattice-bound trace elements. At the same time, trace elements can be adsorbed on organic matter of the shell (Roditi et al., 2000; Vander Putten et al., 2000). It has been observed that organic matter degradation effects the contents of Mn, Mg, Sr and Pb in shells (Takesue et al., 2008). The collected fresh shells obviously contained more organic matter, whereas in C2015, the organic matter had already decayed. It is of course also possible that this phenomenon is caused by individual differences (for example, the M2021 overall has a flatter distribution of Mn/Ca than M2020, whereas M2020 has a much flatter distribution of Cu/Ca compared to M2021), follow-up research is needed on this issue.
The potential influence of human activity on cold seep systems
With the further expansion of human activities to deep-sea cold seep areas, such as fishing, onshore and offshore mining, pollution, and also scientific investigation, these ecosystems are increasingly threatened. For example, epifaunal seep communities on the Hikurangi Margin were disturbed by bottom trawling (Bowden et al., 2013), seep faunas off of northern Papua New Guinea are affected by tailings from onshore mining (Samadi et al., 2015), mining of gas hydrates is explored along continental margins (Song et al., 2014), and trash and other leftovers of human activities are found at increasingly great depth (Schlining et al., 2013). Unfortunately, the deep sea is a slow world, which is not only manifested in the slow growth of various microorganisms, but also in the slow recovery of the environment after being changed (Neves et al., 2015). Now, this tendency has drawn the attention of some countries and international organizations (Van Dover et al., 2012; Danovaro et al., 2020). For example, the Croker Carbonate Slabs in the Irish Sea, as “submarine structures formed by leaking gases”, have been designated as a marine protected area (MPA) under the European Commission’s Habitats Directive (Judd et al., 2020).
At an active cold seep site in the South China Sea, called ‘site F’, Wang et al. (2017) found that the concentrations of K, Mg, Sr, Cu, Mo and V increased toward the outer edge of bivalve shells, indicating more abundant concentrations of trace metals in ambient seawater in recent years, which suggests that human activities may interfere with the cold seep area. The studies of tubeworms in cold seep area also found that the top and root of the tubeworms were strongly affected by the environment, causing the anomaly of some redox sensitive elements and rare earth elements (Duperron et al., 2014; Bayon et al., 2020).
A noteworthy phenomenon in this study is that there are abnormal Ti/Ca, Zr/Ca and Th/Ca ratio peaks in bivalve shells C2020, M2020 and M2021, but there are virtually no such peaks in C2015 (Figure 6). As far as we know, there is no report of the biological utilization of elements such as Ti, Zr and Th. Since these are typical elements of terrigenous sediments, one could propose that a drastic increase of these ratios in the bivalve shells was induced by their variability of the bivalves’ living environment. Since the discovery of “Haima” cold seeps in 2015, scientific research activities at this site have become an annual event. It is common for ROV cruise to Haima cold seep, and the frequency is increasing year by year (Liang et al., 2017; Wang et al., 2022). When the submersible is maneuvering or sampling, it induces large ‘dust clouds’, which will slowly settle on the seabed (Figure 7). We suspect that these activities affected the submarine cold seep ecosystem and have been written down into the trace element record of the bivalve shells to a certain extent.
Figure 7 Seafloor images showing the ‘dust clouds’ caused by the ROV during sampling. (A) Field of live and dead vesicomyid clams; (B–D) large bathymodiolin mussel beds.
Conclusion and implication
Analysis of high-resolution element geochemistry of shells of two species of seep bivalve from the Haima cold seeps in the South China Sea confirms that these shells are biogeochemical recorder of short-term environmental change and physiological parameters at cold seeps. The incorporation of trace elements such as Mg, Sr, Mo, U, Co, Ba in seep bivalve shells is mainly controlled by physiological and environmental factors; the distribution of Co could potentially be developed into an independent index to estimate the age of seep bivalves. Notwithstanding limitations, our results put forward some open questions concerning the element loss for dead shell (Li-Mn-Cu-Zn) and the influence of human activity on cold seep systems (Ti-Zr-Th). We propose the necessity to investigate seep bivalves on the basis of an absolute age framework and to understand their physiological characteristics in the future, which is a prerequisite for further determining the unique potential and effectiveness of this bioarchive in reconstructing environmental information on cold seep systems in a short time scale (years to decades). This study has examined only limited samples that span a relatively short time, our conclusions may thus reflect localized conditions only. Through more measurements over a larger area and longer timespan, the interactions between seep animals and the local environments may be further verified.
Data availability statement
The datasets presented in this study can be found in online repositories. The names of the repository/repositories and accession number(s) can be found in the article/Supplementary Material.
Author contributions
XW: conceptualization, methodology, data analysis, and writing-original manuscript. DaF: methodology. SK: writing-review & editing. SG: sample collection. QL: sample collection. JT: sample collection. DC: data analysis. DoF: conceptualization, supervision, funding acquisition, and writing-review & editing. All authors contributed to manuscript preparation. All authors contributed to the article and approved the submitted version.
Funding
This study was partially sponsored by the National Natural Science Foundation of China (Grants: 41730528, 42106059, 42225603), Shanghai Sailing Program (Grant: 21YF1416800), special funding for the development of science and technology of Shanghai Ocean University and startup foundation for young teachers of Shanghai Ocean University.
Acknowledgments
The crew and captain of the Haiyang-6 research vessel and Haima ROV are thanked for sample collection. We are grateful to Zice Jia (SHOU) for XRD measurement.
Conflict of interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Publisher’s note
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
Supplementary material
The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fmars.2022.960338/full#supplementary-material
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Keywords: methane seep, bivalve, bioarchive, trace elements, South China Sea
Citation: Wang X, Fan D, Kiel S, Gong S, Liang Q, Tao J, Chen D and Feng D (2022) Archives of short-term fluid flow dynamics and possible influence of human activities at methane seeps: Evidence from high-resolution element geochemistry of chemosynthetic bivalve shells. Front. Mar. Sci. 9:960338. doi: 10.3389/fmars.2022.960338
Received: 02 June 2022; Accepted: 25 July 2022;
Published: 12 August 2022.
Edited by:
Clara F. Rodrigues, University of Aveiro, PortugalReviewed by:
Niels De Winter, Vrije University Brussel, BelgiumJoachim Reitner, University of Göttingen, Germany
Copyright © 2022 Wang, Fan, Kiel, Gong, Liang, Tao, Chen and Feng. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Dong Feng, ZGZlbmdAc2hvdS5lZHUuY24=