Rhizobia-diatom symbiosis fixes missing nitrogen in the ocean.
Nitrogen (N2) fixation in oligotrophic surface waters is the main source of new nitrogen (N) to the ocean1 and plays a key role in fueling the biological carbon pump2. Oceanic N2 fixation is almost exclusively attributed to cyanobacteria, even though genes encoding nitrogenase, the enzyme fixing N2...
Published in: | Nature |
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Main Authors: | , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Publishing Group
2024
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Subjects: | |
Online Access: | https://doi.org/10.1038/s41586-024-07495-w https://pubmed.ncbi.nlm.nih.gov/38723661 |
Summary: | Nitrogen (N2) fixation in oligotrophic surface waters is the main source of new nitrogen (N) to the ocean1 and plays a key role in fueling the biological carbon pump2. Oceanic N2 fixation is almost exclusively attributed to cyanobacteria, even though genes encoding nitrogenase, the enzyme fixing N2 into ammonia, are widespread among marine bacteria and archaea3-5. Little is known about these non-cyanobacterial N2-fixers and direct proof that they can fix N in the ocean is missing. Here we report the discovery of a non-cyanobacterial N2-fixing symbiont, Candidatus Tectiglobus diatomicola, which provides its diatom host with fixed-N in return for photosynthetic carbon. The N2-fixing symbiont belongs to the order Rhizobiales and its association with a unicellular diatom expands the known hosts for this order beyond the well-known N2-fixing rhizobia-legume symbioses on land6. Our results show that the rhizobia-diatom symbiosis can contribute as much fixed-N as cyanobacterial N2-fixers in the tropical North Atlantic, and that they may be responsible for N2 fixation in the vast regions of the ocean where cyanobacteria are too rare to account for the measured rates. |
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