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一次海底火山喷发形成了一个全新的微生物栖息地。

A submarine volcanic eruption leads to a novel microbial habitat.

作者信息

Danovaro Roberto, Canals Miquel, Tangherlini Michael, Dell'Anno Antonio, Gambi Cristina, Lastras Galderic, Amblas David, Sanchez-Vidal Anna, Frigola Jaime, Calafat Antoni M, Pedrosa-Pàmies Rut, Rivera Jesus, Rayo Xavier, Corinaldesi Cinzia

机构信息

Department of Life and Environmental Sciences, Polytechnic University of Marche, Ancona 60131, Italy.

Stazione Zoologica Anton Dohrn, Naples, Naples 80121, Italy.

出版信息

Nat Ecol Evol. 2017 Apr 24;1(6):144. doi: 10.1038/s41559-017-0144.

DOI:10.1038/s41559-017-0144
PMID:28812643
Abstract

Submarine volcanic eruptions are major catastrophic events that allow investigation of the colonization mechanisms of newly formed seabed. We explored the seafloor after the eruption of the Tagoro submarine volcano off El Hierro Island, Canary Archipelago. Near the summit of the volcanic cone, at about 130 m depth, we found massive mats of long, white filaments that we named Venus's hair. Microscopic and molecular analyses revealed that these filaments are made of bacterial trichomes enveloped within a sheath and colonized by epibiotic bacteria. Metagenomic analyses of the filaments identified a new genus and species of the order Thiotrichales, Thiolava veneris. Venus's hair shows an unprecedented array of metabolic pathways, spanning from the exploitation of organic and inorganic carbon released by volcanic degassing to the uptake of sulfur and nitrogen compounds. This unique metabolic plasticity provides key competitive advantages for the colonization of the new habitat created by the submarine eruption. A specialized and highly diverse food web thrives on the complex three-dimensional habitat formed by these microorganisms, providing evidence that Venus's hair can drive the restart of biological systems after submarine volcanic eruptions.

摘要

海底火山爆发是重大灾难性事件,可用于研究新形成海床的定殖机制。我们对加那利群岛耶罗岛附近的塔戈罗海底火山喷发后的海底进行了探索。在火山锥顶部附近,深度约130米处,我们发现了大片由白色长细丝组成的垫子,我们将其命名为“金星之发”。显微镜和分子分析表明,这些细丝由包裹在鞘内的细菌丝状体构成,并被体表共生细菌定殖。对这些细丝的宏基因组分析确定了硫丝菌目一个新的属和种,即维纳斯硫熔岩菌。“金星之发”展现出一系列前所未有的代谢途径,从利用火山排气释放的有机和无机碳,到摄取硫和氮化合物。这种独特的代谢可塑性为定殖于海底火山喷发形成的新栖息地提供了关键的竞争优势。一个专门且高度多样的食物网在由这些微生物形成的复杂三维栖息地中蓬勃发展,这证明“金星之发”能够推动海底火山喷发后生物系统的重启。

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