FN Archimer Export Format PT J TI Sinking Trichodesmium fixes nitrogen in the dark ocean BT AF Benavides, Mar Bonnet, Sophie Le Moigne, Frédéric A. C. Armin, Gabrielle Inomura, Keisuke Hallstrøm, Søren Riemann, Lasse Berman-Frank, Ilana Poletti, Emilie Garel, Marc Grosso, Olivier Leblanc, Karine Guigue, Catherine Tedetti, Marc Dupouy, Cécile AS 1:1,2;2:1;3:1,3;4:4;5:4;6:5;7:5;8:6;9:1;10:1;11:1;12:1;13:1;14:1;15:; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:; C1 Aix Marseille Univ, Université de Toulon, CNRS, IRD, MIO UM 110, 13288, Marseille, France Turing Center for Living Systems, Aix-Marseille University, 13009, Marseille, France LEMAR, Laboratoire des Sciences de l’Environnement Marin, UMR6539, CNRS, UBO, IFREMER, IRD, 29280, Plouzané, Technopôle Brest-Iroise, France Graduate School of Oceanography, University of Rhode Island, South Kingstown, RI, USA Marine Biological Section, Department of Biology, University of Copenhagen, Helsingør, Denmark Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Mt, Carmel, Haifa, Israel C2 IRD, FRANCE UNIV AIX MARSEILLE, FRANCE IRD, FRANCE UNIV RHODE ISL, USA UNIV COPENHAGEN, DENMARK UNIV HAIFA, ISRAEL UM LEMAR IN WOS Cotutelle UMR copubli-france copubli-europe copubli-univ-france copubli-int-hors-europe IF 11 TC 15 UR https://archimer.ifremer.fr/doc/00788/89959/102613.pdf LA English DT Article CR TONGA 2019 BO L'Atalante AB The photosynthetic cyanobacterium Trichodesmium is widely distributed in the surface low latitude ocean where it contributes significantly to N2 fixation and primary productivity. Previous studies found nifH genes and intact Trichodesmium colonies in the sunlight-deprived meso- and bathypelagic layers of the ocean (200–4000 m depth). Yet, the ability of Trichodesmium to fix N2 in the dark ocean has not been explored. We performed 15N2 incubations in sediment traps at 170, 270 and 1000 m at two locations in the South Pacific. Sinking Trichodesmium colonies fixed N2 at similar rates than previously observed in the surface ocean (36–214 fmol N cell−1 d−1). This activity accounted for 40 ± 28% of the bulk N2 fixation rates measured in the traps, indicating that other diazotrophs were also active in the mesopelagic zone. Accordingly, cDNA nifH amplicon sequencing revealed that while Trichodesmium accounted for most of the expressed nifH genes in the traps, other diazotrophs such as Chlorobium and Deltaproteobacteria were also active. Laboratory experiments simulating mesopelagic conditions confirmed that increasing hydrostatic pressure and decreasing temperature reduced but did not completely inhibit N2 fixation in Trichodesmium. Finally, using a cell metabolism model we predict that Trichodesmium uses photosynthesis-derived stored carbon to sustain N2 fixation while sinking into the mesopelagic. We conclude that sinking Trichodesmium provides ammonium, dissolved organic matter and biomass to mesopelagic prokaryotes. PY 2022 PD OCT SO Isme Journal SN 1751-7362 PU Springer Science and Business Media LLC VL 16 IS 10 UT 000825172300001 BP 2398 EP 2405 DI 10.1038/s41396-022-01289-6 ID 89959 ER EF