201. Sea Level Modulation of Atlantic Nitrogen Fixation Over Glacial Cycles.
- Author
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Auderset, Alexandra, Fripiat, François, Creel, Roger C., Oesch, Lukas, Studer, Anja S., Repschläger, Janne, Hathorne, Ed, Vonhof, Hubert, Schiebel, Ralf, Gordon, Laura, Lawrence, Kira, Ren, Haojia Abby, Haug, Gerald H., Sigman, Daniel M., and Martínez‐García, Alfredo
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DENITRIFICATION ,SEA level ,NITROGEN fixation ,GLACIAL Epoch ,ATMOSPHERIC carbon dioxide ,SEA ice ,NITROGEN isotopes - Abstract
N2 fixation in low‐latitude surface waters dominates the input of fixed nitrogen (N) to the global ocean, sustaining ocean fertility. In the Caribbean Sea, higher foraminifera‐bound (FB‐)δ15N indicates a decline in N2 fixation during ice ages, but its cause and broader implications are unclear. Here, we report three additional Atlantic FB‐δ15N records, from the subtropical North and South Atlantic gyres (MSM58‐50 and DSDP Site 516) and the equatorial Atlantic (ODP Site 662). Similar glacial and interglacial δ15N in the equatorial Atlantic suggests a stable δ15N for the nitrate below the gyre thermoclines. The North Atlantic record shows a FB‐δ15N rise during the ice ages, resembling a previously published FB‐δ15N record from the South China Sea. The commonality among the FB‐δ15N records is that they resemble sea level‐driven variation in regional shelf area, with high FB‐δ15N (inferred reduction in N2 fixation) during periods of low shelf area. The South China Sea shows the largest δ15N signal, the subtropical North Atlantic shows less, and the South Atlantic shows the least, the same ordering as the ice age reductions in continental shelf area in the different regions. Reduced shelf sedimentary denitrification would have increased the nitrogen‐to‐phosphorus ratio of the nutrient supply to open ocean surface waters, leading to decreased N2 fixation and thus higher gyre thermocline nitrate δ15N, explaining the higher FB‐δ15N of peak ice ages. These observations identify shelf sediment denitrification as an important regional driver of modern N2 fixation and imply strong basin‐scale coupling of fixed nitrogen losses and inputs. Plain Language Summary: Nitrogen fixation plays the crucial role in the ocean of supplying bioavailable nitrogen (N), a major nutrient for phytoplankton growth. Variations in nitrogen fixation over time can, therefore, significantly impact ocean productivity and, consequently, carbon sequestration in the ocean interior. To infer past changes in nitrogen fixation during ice ages, we measured the nitrogen isotope (15N‐to‐14N) ratio of organic matter preserved within the carbonate skeleton of planktic foraminifera. Our study reveals a substantial reduction in nitrogen fixation during ice ages in the low‐nutrient regions of the North Atlantic, with only minor variations in the South Atlantic. The basin‐dependent changes are attributed to sea level‐driven reductions in regional continental shelf area during ice ages, resulting in diminished sedimentary denitrification and subsequently lower phosphorus excess in the surface waters downstream of the continental shelves. Overall, our study highlights the importance of regional factors, like shelf sediment denitrification, in influencing oceanic nitrogen fixation within a given ocean basin. Furthermore, it suggests that changes in nitrogen fixation cannot explain the decline in atmospheric carbon dioxide concentration during ice ages. Key Points: Reduction of nitrogen fixation in the Atlantic Ocean during ice ages, proportional to sea‐level variations in regional shelf areaRegional coupling between nitrogen fixation and shelf sedimentary denitrification in the subtropical gyresChange in nitrogen fixation cannot explain the lowering of atmospheric CO2 during ice ages [ABSTRACT FROM AUTHOR]
- Published
- 2024
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