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Organic Metabolite Uptake by Diazotrophs in the North Pacific Ocean

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modified on 2024-08-07, 19:27

Dinitrogen (N2) fixation by diazotrophs sustains biological productivity in the ocean. Diazotroph groups include photoautotrophic cyanobacteria, non-cyanobacterial diazotrophs (NCDs) and the recently discovered N2-fixing haptophyte. NCDs' ecology and metabolism are poorly understood despite being ubiquitous in the ocean and often the dominant group in nifH gene surveys. NCDs are primarily heterotrophic, acquiring carbon and energy from external sources of dissolved organic matter (DOM). Their interactions with DOM still need to be clarified. Strikingly, photoautotrophic diazotrophic cyanobacteria have been shown to use DOM, often allowing them to cope with nutritional and energetic stress. Conventional DOM amendment incubations do not allow discerning how different diazotroph groups use DOM molecules. Here, we amended surface microbial communities from the North Pacific Ocean with 13C-labelled DOM derived from phytoplankton cultures and used DNA stable isotope probing and nifH gene amplicon sequencing to identify diazotrophs capable of taking up DOM. We further used a metabolomics approach to characterise the 13C-labelled DOM composition. The addition of 13C-DOM induced a shift from Crocosphaera and other less abundant cyanobacterial diazotrophs, such as Trichodesmium, to a predominance of NCDs in stations when the N2-fixing haptophyte show low relative abundance. Our results reveal overlooked osmotrophic behaviour by diverse diazotroph lineages with substantial spatial variability driven by the background biogeochemical environment.

Funding

This research was supported by the BNP Paribas Foundation for Climate and Biodiversity project NOTION (MB) and the NSF grant OCE-2023498 (KTK), and also benefited from the ASIA platform (Université de Lorraine-INRAE; https://a2f.univ-lorraine.fr/en/asia-2/). We would like to thank the captain, crew of R/V Kilo Moana and T. Rohrer for field logistical support, and the Ocean Technology Group from the University of Hawai'i for their technical assistance before and during cruise. We thank M. Mills for the help setting up the onboard incubators and pump system during the cruise. The platform of cytometry for microbiology (precym.mio.osupytheas.fr) and S. Nunige are acknowledged for flow cytometry and nutrient analyses, respectively. The MIMS equipment used in this study was obtained with European FEDER Funds. We would like to thank F. M. Cornejo-Castillo for valuable insights and discussion on the preliminary results of this manuscript. M. Vallet acknowledges the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation), Friedrich Schiller Universität Jena, and is supported by the consortium SFB1127 ChemBioSys, Project number 239748522.