Biogeosciences, 17, 3203–3222, 2020 https://doi.org/10.5194/bg-17-3203-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. The contribution of microbial communities in polymetallic nodules to the diversity of the deep-sea microbiome of the Peru Basin (4130–4198 m depth) Massimiliano Molari1, Felix Janssen1,2, Tobias R. Vonnahme1,a, Frank Wenzhöfer1,2, and Antje Boetius1,2 1Max Planck Institute for Marine Microbiology, Bremen, Germany 2HGF MPG Joint Research Group for Deep-Sea Ecology and Technology, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany apresent address: UiT the Arctic University of Tromsø, Tromsø, Norway Correspondence: Massimiliano Molari (
[email protected]) Received: 16 January 2020 – Discussion started: 3 February 2020 Revised: 27 April 2020 – Accepted: 15 May 2020 – Published: 25 June 2020 Abstract. Industrial-scale mining of deep-sea polymetal- tween the Clarion–Clipperton Fracture Zone (CCZ) and the lic nodules will remove nodules in large areas of the sea Peru Basin suggest that changes in environmental setting floor. The regrowth of the nodules by metal precipita- (e.g. sedimentation rates) also play a significant role in struc- tion is estimated to take millions of years. Thus, for fu- turing the nodule microbiome. ture mining impact studies, it is crucial to understand the role of nodules in shaping microbial diversity and function in deep-sea environments. Here we investigated microbial- community composition based on 16S rRNA gene sequences 1 Introduction retrieved from sediments and nodules of the Peru Basin (4130–4198 m water depth). The nodule field of the Peru Polymetallic nodules (or manganese nodules) occur in Basin showed a typical deep-sea microbiome, with domi- abyssal plains (4000–6000 m water depth) and consist pri- nance of the classes Gammaproteobacteria, Alphaproteobac- marily of manganese and iron as well as many other metals teria, Deltaproteobacteria, and Acidimicrobiia.