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协同生物矿化策略固定泡孔海链藻钙化过程中的锶。

A synergetic biomineralization strategy for immobilizing strontium during calcification of the coccolithophore Emiliania huxleyi.

机构信息

Institute of Non-metallic Minerals, Key Laboratory of Solid Waste Treatment and Resource Recycle, Southwest University of Science and Technology, Mianyang, 621010, China.

Low-cost Wastewater Treatment Technology International Sci-Tech Cooperation Base of Sichuan Province, Mianyang, 621010, China.

出版信息

Environ Sci Pollut Res Int. 2018 Aug;25(23):22446-22454. doi: 10.1007/s11356-018-1271-4. Epub 2018 Jan 24.

Abstract

The coccolithophore species Emiliania huxleyi has one of the most global distributions in the modern oceans. They are characteristically covered with calcite scales called coccoliths. In this study, stable strontium immobilization during the calcification process was investigated to indirectly assess a proposed bioremediation approach for removing Sr contamination from marine environments. Results indicate that E. huxleyi has high Sr tolerance and removal efficiency in response to Sr stress ranging from 5.6 to 105.6 ppm. Sr immobilization during E. huxleyi calcification indicates a concentration-dependent synergistic mechanism. At lower concentrations of Sr (25.6 ppm), Sr is incorporated into coccoliths through competitive supply between Sr and Ca. In addition, calcite productivity decreases with increased Sr removal efficiency due to crystallographic transformation of coccoliths from hydrated calcite into aragonite at 55.6 ppm Sr. Further formation of strontianite at 105.6 ppm Sr is due to precipitation of Sr on the edge of the rims and radial arrays of the coccoliths. Our study implies that coccolithophores are capable of significant removal of Sr from the marine environment.

摘要

颗石藻物种 Emiliania huxleyi 在现代海洋中具有最广泛的分布之一。它们的特征是覆盖着碳酸钙鳞片,称为颗石。在这项研究中,研究了钙化过程中稳定的锶固定化,以间接评估一种从海洋环境中去除 Sr 污染的生物修复方法。结果表明,E. huxleyi 对 Sr 胁迫具有很高的耐受性和去除效率,范围从 5.6 到 105.6 ppm。E. huxleyi 钙化过程中的 Sr 固定化表明存在浓度依赖的协同机制。在较低浓度的 Sr(25.6 ppm)下,Sr 通过 Sr 和 Ca 的竞争供应掺入颗石中。此外,由于 55.6 ppm Sr 时颗石的水合碳酸钙向霰石的晶型转变,碳酸钙生产力随着 Sr 去除效率的增加而降低。在 105.6 ppm Sr 下进一步形成天青石是由于 Sr 在颗石边缘和放射状排列的边缘上的沉淀。我们的研究表明,颗石藻能够从海洋环境中大量去除 Sr。

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