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Early-stage mineralization of hydrothermal tubeworms: New insights into the role of microorganisms in the process of mineralization

机译:热液虫的早期矿化作用:微生物在矿化过程中的作用的新见解

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摘要

As an important part of marine hydrothermal system, hydrothermal vent faunas live in hydrothermal inorganic environment and closely interact with hydrothermal inorganic environment. Sometimes, they can participate in the mineralization process of modern hydrothermal site. Hydrothermal vent faunas, particularly vestimentiferan and polychaete tubeworms, are occasionally preserved in the geological record. Study on the early mineralization process of hydrothermal vent fauna is significant for understanding the interaction between mineral and organism, and also the formation and preservation mechanism of geological fossil in hydrothermal environment. In this paper, the early stage of mineralization of Vestimentiferan Ridgeia piscesae tubes collected from Juan de Fuca Ridge is studied. The results showed that a lot of filamentous microorganisms were unevenly distributed on the surface of internal wall and in the interspace of the wall of tubeworm. In some cases, microorganisms aggregated as thin layers in or on the wall of tubeworm. The surfaces of microbial cells and the products of microbial degradation may play an important role in the early mineralization of tubeworm. Semitransparent thin layers of organic matter containing sulfur and sulfur granules were commonly found on the wall of tubeworm with lower degree of mineralization. The degradation production of these semitransparent thin layers may accelerate the mineralization of tube wall during the early stage. EDS results showed that on the tube walls some chemical elements such as Fe, P, Ca and Si are selectively enriched from ambient hydrothermal environment. Interestingly, P, Ca and Si covary with Fe content. Because element S originated from the bio-oxidation of H2S by symbiotic microorganism in the tissue of tubeworm, it can be considered as a biomarker when studying the mineralization process of tube wall. Based on the characteristics of tubeworms with different degrees of mineralization, we suggested that the early mineralization stage of tube wall was mainly controlled by microbial-induced mineralization and the degradation process of tube wall.
机译:作为海洋热液系统的重要组成部分,热液喷口动物群生活在热液无机环境中,并与热液无机环境紧密相互作用。有时,他们可以参加现代热液场的成矿过程。地热记录中偶尔保留了热液喷口动物区系,特别是前额叶虫和多毛cha虫。研究热液喷口动物区系的早期成矿过程,对于理解矿物与生物之间的相互作用,以及在热液环境下地质化石的形成与保存机制具有重要意义。本文研究了从胡安·德·富卡山脊采集的Vistimentiferan Ridgeia piscesae管的矿化早期。结果表明,许多丝状微生物均不均匀分布在结核虫的内壁表面和壁间。在某些情况下,微生物会在块虫壁内或壁上聚集成薄层。微生物细胞的表面和微生物降解的产物可能在块茎的早期矿化中起重要作用。含硫和硫颗粒的有机物半透明薄层通常发现在具有较低矿化度的块茎壁上。这些半透明薄层的降解产生可能在早期加速管壁的矿化。 EDS结果表明,管壁上的某些化学元素(如Fe,P,Ca和Si)从周围的热液环境中选择性富集。有趣的是,P,Ca和Si随Fe含量变化。由于元素S源自结核菌组织中共生微生物对H2S的生物氧化作用,因此在研究管壁矿化过程时可以将其视为生物标记。根据不同矿化程度的of虫的特征,我们认为管壁的早期矿化阶段主要受微生物诱导的矿化作用和管壁的降解过程控制。

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