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大型硫细菌与磷矿的形成

Large sulfur bacteria and the formation of phosphorite.

作者信息

Schulz Heide N, Schulz Horst D

机构信息

Institute for Microbiology, University of Hannover, Schneiderberg 50, D-30167 Hannover, Germany.

出版信息

Science. 2005 Jan 21;307(5708):416-8. doi: 10.1126/science.1103096.

Abstract

Phosphorite deposits in marine sediments are a long-term sink for an essential nutrient, phosphorus. Here we show that apatite abundance in sediments on the Namibian shelf correlates with the abundance and activity of the giant sulfur bacterium Thiomargarita namibiensis, which suggests that sulfur bacteria drive phosphogenesis. Sediments populated by Thiomargarita showed sharp peaks of pore water phosphate (</=300 micromolar) and massive phosphorite accumulations (>/=50 grams of phosphorus per kilogram). Laboratory experiments revealed that under anoxic conditions, Thiomargarita released enough phosphate to account for the precipitation of hydroxyapatite observed in the environment.

摘要

海洋沉积物中的磷矿是必需营养元素磷的一个长期汇。我们在此表明,纳米比亚陆架沉积物中磷灰石的丰度与巨大硫细菌——纳米比亚嗜硫珠菌的丰度和活性相关,这表明硫细菌驱动了磷的形成。有纳米比亚嗜硫珠菌存在的沉积物显示出孔隙水磷酸盐的尖锐峰值(≤300微摩尔)和大量磷矿堆积(≥每千克50克磷)。实验室实验表明,在缺氧条件下,纳米比亚嗜硫珠菌释放出的磷酸盐足以解释在该环境中观察到的羟基磷灰石沉淀。

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