Biological N₂O Fixation in the Eastern South Pacific Ocean and Marine Cyanobacterial Cultures

<div><p>Despite the importance of nitrous oxide (N₂O) in the global radiative balance and atmospheric ozone chemistry, its sources and sinks within the Earth’s system are still poorly understood. In the ocean, N₂O is produced by microbiological processes such as nitrification and partial denitrification, which account for about a third of global emissions. Conversely, complete denitrification (the dissimilative reduction of N₂O to N₂) under suboxic/anoxic conditions is the only known pathway accountable for N₂O consumption in the ocean. In this work, it is demonstrated that the biological assimilation of N₂O could be a significant pathway capable of directly transforming this gas into particulate organic nitrogen (PON). N₂O is shown to be biologically fixed within the subtropical and tropical waters of the eastern South Pacific Ocean, under a wide range of oceanographic conditions and at rates ranging from 2 pmol N L⁻¹ d⁻ to 14.8 nmol N L⁻¹ d⁻¹ (mean ± SE of 0.522±1.06 nmol N L⁻¹ d⁻¹, n = 93). Additional assays revealed that cultured cyanobacterial strains of <i>Trichodesmium</i> (H-9 and IMS 101), and <i>Crocosphaera</i> (W-8501) have the capacity to directly fix N₂O under laboratory conditions; suggesting that marine photoautotrophic diazotrophs could be using N₂O as a substrate. This metabolic capacity however was absent in <i>Synechococcus</i> (RCC 1029). The findings presented here indicate that assimilative N₂O fixation takes place under extreme environmental conditions (i.e., light, nutrient, oxygen) where both autotrophic (including cyanobacteria) and heterotrophic microbes appear to be involved. This process could provide a globally significant sink for atmospheric N₂O which in turn affects the oceanic N₂O inventory and may also represent a yet unexplored global oceanic source of fixed N.</p>