The effect of Mg2+on boron incorporation into carbonate and the infl uence of B/Ca proxies for the deep ocean carbonate system

HE Maoyong, XIAO Yingkai

(1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China; 2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China; 3. Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi'an 710061, China)

The effect of Mg2+on boron incorporation into carbonate and the infl uence of B/Ca proxies for the deep ocean carbonate system

HE Maoyong1,3, XIAO Yingkai2

(1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China; 2. Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China; 3. Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi'an 710061, China)

Background, aim, and scopeB/Ca proxies for the deep ocean carbonate system is an important proxy to evaluate carbon sink in sea. Mg2+is common element in sea which can effect B/Ca values of marine carbonate.Materials and methodsThe infl uence of Mg2+in a parent solution on boron incorporation in an inorganic carbonate precipitate is studied using a different solubility method technique. The calcium carbonate precipitate is characterized by scanning electron microscopy and X-ray diffraction. The boron concentration of the samplers is analyzed by ICP-AES.ResultsThe calcium carbonate precipitate is confi rmed to be low-Mg calcite. The boron concentrations in the precipitated calcite increased from 63.91 μg·g-1to 582.41 μg·g-1when the artifi cial solution pH values increased from 7.40 ± 0.03 to 8.80 ± 0.03.DiscussionThe results show that boron uptake by low-Mg calcite is greater than boron uptake by free-Mg calcite grown under nearly identical conditions, and the boron concentration in low-Mg calcite is higher than in free-Mg calcite by 2.57 average time (from 1.83 to 3.56). This result suggests that the mechanism for borate-boron co-precipitation with Mg2+present is different than without Mg2+present, and the Mg2+clearly modifies calcite crystal morphology, as identified in SEM images.ConclusionspH has a signifi cant effect on the incorporation of boron into synthetic carbonate, and the Mg2+also infl uence on boron incorporation into calcite precipitate.Recommendations and perspectivesThe data provide a signifi cant scientifi c basis for B/Ca proxies for the deep ocean carbonate system. It is recommended that the Mg2+would be consider when using B/Ca proxies.

effect; magnesium ions; boron; precipitated inorganic carbonate

1 Introduction

Based on the research by Hemming and Hanson (1992), the foraminifera B/Ca ratios have increasingly been used as a paleo-carbonate ion or paleo-pH proxy because borate ions are preferentially incorporated into the calcite lattice relative to boric acid (Foster, 2008; Yu et al, 2010). In recent years, foraminiferal B/Ca ratio analysis, which is a paleoceanographic method with significant potential, has generated significant concern (H?nisch and Allen, 2013). Marine carbonates (e.g., corals and foraminifera) from sediment core or culture experiments reveal that the ratios of boron to calcium (B/Ca) varied with pH, temperature, light, salinity, and seawater boron concentration (Rae et al, 2011; Kender et al, 2014). To apply boron trace element abundance as a geochemical tracer, the factors that influence boron uptake by calcium carbonate must be discerned (Liu et al, 2010; Deng et al, 2012; Xiao et al, 2012). Over the past few decades, several inorganic calcite precipitation experiments have been performed to evaluate the factors that infl uence boron incorporation into marine biocarbonates by comparing such incorporation with that of boron into inorganic calcite, yielding signifi cant achievements. For example, the level of boron coprecipitated into calcite increased by increasing the parent solution pH; the level of boron that coprecipitates with CaCO3is proportional to the concentration of boron in the parent solution; boron is coprecipitated more readily with aragonite than calcite; and the content in aragonite is higher than calcite by 1.5 to 2 (Hemming et al, 1995; Sanyal et al, 2000; Xiao et al, 2006, 2008; Astilleros et al, 2010; Ruiz-Agudo et al, 2010; Dissard et al, 2012).

In recent years, the role of magnesium in the growth of calcite was considered. For inorganic calcite precipitation, boron incorporation into Mg(OH)2and boron isotope fractionation during brucite deposition experiments by Xiao et al (2006, 2008) and Xiao et al (2009, 2011) showed that the adsorption capacity for boron with Mg2+was comparatively strong in the presence of Mg2+. Astilleros et al (2002, 2010) systematically studied the role of Mg2+in the growth of calcite by the AFM. They provided an explanation for the development of “dead zones”, which was based on the restrictions that the underlying substrate imposes on the lateral spread of overgrowing layers (the “template effect”).

The main objective of this study was to further assess the influence of magnesium ions on boron incorporation in an inorganic carbonate precipitate. These experiments were conducted (1) to evaluate the systematics of boron coprecipitation in carbonates with Mg2+at different pH, (2) to determine the effect of Mg2+on boron incorporation into precipitated inorganic carbonate, and (3) to improve the understanding of the mechanisms driving the boron and magnesium incorporation into calcium carbonate.

2 Experiment

2.1 Instrumentation

ICP-AES (Perkin Elmer Optima 4300DV) was used to analyze boron concentrations.

The morphologies of the dry precipitates were characterized by Powder X-ray Diffraction (PXRD), and the shapes, particle size distributions, and aspect ratios of the particles were observed by Scanning Electron Microscope (SEM).

2.2 Reagents and materials

All chemical reagents used in this study were purchased from the Tianjin Kermel Reagent Co. Ltd. High-purity NH3and CO2gases (≥99.99%) were usedtoo. MgCO3· 3H2O was synthesized from MgCl2and (NH4)2CO3(Wang et al, 2008).

2.3 Experimental methods

2.3.1 CaCO3precipitation

CaCO3was precipitated via a different solubility method technique. The experimental setup has been described in our previous work (He et al, 2013). Synthesized MgCO3· 3H2O (0.138 g) was added slowly to the artificial magnesium-free seawater instead of Li2CO3. And approximately 100 mg of calcium carbonate was generated. The samples were treated following the method of He et al (2013) too.

2.3.2 Powder X-ray Diffraction (PXRD) and Scanning Electron Microscope (SEM)

X-ray diffraction (XRD) measurements were conducted using an X'Pert PRO MPD with Cu-Kαradiation (40 kV, 200 mA), and 0.02 step and 2θrange of 20° to 60° were selected to analyze the crystal structure and crystal orientation.

The sizes and morphologies of the CaCO3precipitates were characterized using a JEOS JSM-6700F scanning electron microscope at 20 kV after sputter-coating with Au.

3 Results and Discussion

3.1 Characterization of precipitated CaCO3

The solids recovered from the coprecipitation experiments were characterized with XRD to distinguish calcite from the other polymorphs of CaCO3(Fig.1).

Fig.1 shows the representative XRD patterns of the CaCO3obtained in the presence of Mg2+at 15 h with variable pH. All of the relatively sharp peaks are characteristic of low-Mg calcite (LMC) of (Mg0.03Ca0.97) (CO3) (JCPDS file: 01-089-1304). Vousdoukas et al (2007) documented that LMC (a polymorph of CaCO3, containing less than 4% MgCO3with a formula (Mg0.03Ca0.97)(CO3)) is the dominant precipitated carbonate phase as a result of water mixing. This has been confi rmed in the present study.

The crystal structures of carbonate can be further identified by evaluating their SEM. Fig.2 shows representative SEM images of low-Mg-calcite (LMC).

Fig.1 XRD patterns of CaCO3prepared in different pH conditions: (a) pH = 7.8, (b) pH = 8.2, and (c) pH = 8.6

3.2 The effect of pH on boron incorporation into calcite precipitate with/without Mg2+

Fig.3 shows plots of the boron concentrations measured experimentally in low-Mg calcites. The results indicate that pH has a significant effect on the incorporation of boron into low-Mg calcites. The amount of co-precipitated boron increased with the parent solution pH, from 63.91 μg·g-1at pH = 7.4 to 582.41 μg·g-1at pH = 8.8. The fi ndings of the current study are consistent with previous results of boron incorporation into CaCO3by Sanyal et al (2000), Xiao et al (2008), and He et al (2013). As shown in Fig.3, the primary factor controlling boron incorporation into precipitated synthetic arbonate was the parent solution pH. The level of boron that coprecipitated with carbonate increased with the parent solution pH, with or without Mg2+in the solution. The Mg2+modifies calcite crystal morphology to influence on boron incorporation into calcite precipitate.

At low boron concentrations (B≤0.025 M), boron primarily forms two molecular species in solution: B(OH)3(boric acid; planar, trigonally coordinated) and(borate ion, tetrahedrally coordinated). The following equilibrium is found:

Fig.2 SEM images of CaCO3crystals (a) This study at pH = 8.2 and (b) He et al (2013) at pH = 8.2.

Fig.3 Measured boron content of precipitated carbonates relative to pH

Based on the research by Hemming and Hanson (1992). the incorporation ofinto marine carbonate follows the equilibrium reaction:

CaCO3+? Ca(HBO3) ++ H2O (2)

3.3 The effect of Mg2+on boron incorporation into calcite precipitate

Fig.2a is SEM images of LMC in the presence of Mg2+, and Fig.2b is SEM images of calcite precipitated at same condition without Mg2+. Fig.2 indicates that the presence of Mg2+has clearly been shown to modify calcite crystal morphology. It also supports previous research that Mg2+can alter the crystal structure (Paquette and Reede, 1995; Park et al, 2008). Mg2+has a higher affinity for certain sites, and it is likely adsorption or dehydration during incorporation that preferentially reduces growth in specific directions, such as toward the edges and corners. This nonuniform Mg2+adsorption on the calcite surface produces new crystal surfaces, which have a higher Mg2+density and lower growth rate than the original calcite seed surfaces. Under these conditions, boron is coprecipitated more easily with low-Mg calcite than with calcite.

Fig.3 shows that the boron content inprecipitated carbonate was different in the presence of Mg2+andabsent of Mg2+in the solution. The results show that boron is coprecipitated more readily with Mg2+in the solution. The results of our experiments are similar to previous reports by Xiao et al (2008) with Mg2+for a similar pH, but are twice as large as the values reported by Sanyal et al (2000) and He et al (2013) without Mg2+in the solution.

3.4 The infl uence of Mg2+on B/Ca proxies for the deep ocean carbonate system

The surface water B/Ca ratio can be expressed asand was proposed to be a proxy for seawaterThe basic assumption behind this proxy is that the B/Ca ratio in foraminifera is a function of the ratio ofin seawater, with the later being pH dependent.

Compared with the conventional method of analyzing boron isotopes, the B/Ca ratio method is relatively easier and more stable. As a result, it is relatively suitable for high-resolution paleoceanographic studies. Yu et al (2010), Foster (2008), and Palmer et al (2010) used foraminiferal B/Ca ratios to reflect the deep water carbonate saturation state. They suggested that B/Ca ratios vary widely for different foraminifera species and thatKDis not a constant value for the same foraminifera species.

Although B/Ca proxies for the deep ocean carbonates system are widely used, the mechanisms of these proxies are not well accepted. Not only the method is constructed on the basis of an empirical function, but also the B/Ca is impacted of light and temperature (Dissard et al, 2012; Coadic et al, 2013). Mg is an element that is widely distributed in seawater. Mg is not only incorporated into foraminiferal and coral but also impacts the process of boron incorporation. A synthetic calcium carbonate experiment by Hemming et al (1995) showed that boron uptake by aragonite is greater than boron uptake by calcite grown under nearly identical conditions, whereas boron uptake by high-Mg calcite is intermediate. In our study, when all the other parameters are maintained constant, boron concentrations in calcite precipitate increase with increasing Mg2+(Fig.3). It is suggested thatKDperhaps was influenced by Mg2+. Additional work is clearly needed to understand the causes of this behavior, but this is unfortunately beyond the scope of this contribution. These observations complicate the application of B/Ca in planktic foraminifera to trace changes in the carbonate system.

4 Conclusions

Boron is coprecipitated more readily with low-Mg calcite than with calcite under the same pH and temperature conditions, and the levels of low-Mg calcite are higher than those of calcite by 1.83 to 3.56, with a 2.57 average value. The presence of Mg2+clearly modifies the calcite crystal morphology and may influence on B/Ca proxies for the deep ocean carbonate system.

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Mg2+離子對深海碳酸鹽中硼的摻入和B/Ca指標的影響

賀茂勇1,3，肖應(yīng)凱2

（1.中國科學(xué)院地球環(huán)境研究所 黃土與第四紀地質(zhì)國家重點實驗室，西安 710061；2.中國科學(xué)院青海鹽湖研究所，西寧 810008；3.陜西省加速器質(zhì)譜技術(shù)及應(yīng)用重點實驗室，西安 710061）

對母液中Mg2+離子對硼摻入無機碳酸鹽沉積的影響進行了研究。通過掃描電子顯微鏡和X射線衍射確定在Mg存在時生成的無機碳酸鹽是低鎂方解石。實驗發(fā)現(xiàn)：溶液的pH值是硼進入碳酸鹽的主要控制因素，低Mg2+方解石中硼的濃度從63.91 μg·g-1（pH = 7.40 ± 0.03）增加到582.41 μg·g-1（pH = 8.80 ± 0.03）。Mg2+離子嚴重影響硼進入碳酸鹽中的量，在相同實驗條件下，硼在低鎂方解石中的含量高于無Mg2+方解石中的含量，平均為2.57倍（1.83 — 3.56倍）。這一結(jié)果表明：有Mg2+離子時，硼摻入無機碳酸鹽的機制和無Mg2+離子的是不同的。Mg2+離子的存在改變了晶體的形貌。這對利用B/Ca指標恢復(fù)深海碳酸鹽系統(tǒng)研究有重要影響。

作用；鎂離子；硼；無機碳酸鹽沉積

10.7515/JEE201603009

Received Date:2015-11-30;Accepted Date:2016-01-08

Foundation Item:National Natural Science Foundation of China (41573013, U1407109); “Key Program” of the West Light Foundation of Chinese Academy of Sciences (42904101) ; Natural Science Fund of Shaanxi Province (2015JM4143)

HE Maoyong, E-mail: hemy@ieecas.cn