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DOI | 10.1016/j.epsl.2020.116287 |
Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization | |
Stamm F.M.; Méheut M.; Zambardi T.; Chmeleff J.; Schott J.; Oelkers E.H. | |
发表日期 | 2020 |
ISSN | 0012821X |
卷号 | 541 |
英文摘要 | A combination of theoretical predictions and isotopic equilibration experiments using the three-isotope method have been performed to assess Si isotope fractionation among minerals, and aqueous species in the presence of dissolved catechol. Aqueous Si in abiotic ambient temperature aqueous solutions is dominated by the IV-coordinated H4SiO4 0 species, but the presence of aqueous catechol provokes the formation of a VI-fold Si-catechol complex. Results show an equilibrium Si fractionation factor of ∼19‰ between the VI-fold coordinated Si-catechol complex and the IV-fold coordinated aqueous silicic acid, an amplitude never previously observed for silicon. The fractionation between V-fold Si-organo complexes (with diolate, glyconate or methyllactate groups) and silicic acid has also been estimated through theoretical predictions to be about −10‰. These extreme fractionations can be used to improve our ability to interpret the Si isotope compositions of natural solids, and in particular those associated with marine silica biomineralization processes (e.g. sponge spicules). © 2020 Elsevier B.V. |
关键词 | equilibrium isotope fractionationfirst principle calculationorgano-silicon complexesSi coordination changesiliconthree-isotope method |
英文关键词 | Biomineralization; Coordination reactions; Phenols; Silica; Aqueous species; Fractionation factors; Isotopic equilibration; Organic complexation; Si isotopes; Silica biomineralization; Silicic acids; Silicon isotopes; Isotopes; aqueous solution; benzene; biomineralization; complexation; experimental study; isotopic composition; isotopic fractionation; silicon; theoretical study |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/202902 |
作者单位 | Géosciences Environnement Toulouse, CNRS-UPS-OMP, 14 av. Édouard Belin, Toulouse, 31400, France; LEGOS, Laboratoire d'Etudes en Géophysique et Océanographie Spatiales (CNRS/UPS/CNES/IRD), Observatoire Midi-Pyrénées, 14 Avenue Edouard Belin, Toulouse, 31400, France; Department of Earth Sciences, UCL, Gower Street, London, WC1E 6BT, United Kingdom |
推荐引用方式 GB/T 7714 | Stamm F.M.,Méheut M.,Zambardi T.,et al. Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization[J],2020,541. |
APA | Stamm F.M.,Méheut M.,Zambardi T.,Chmeleff J.,Schott J.,&Oelkers E.H..(2020).Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization.Earth and Planetary Science Letters,541. |
MLA | Stamm F.M.,et al."Extreme silicon isotope fractionation due to Si organic complexation: Implications for silica biomineralization".Earth and Planetary Science Letters 541(2020). |
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