Japan Geoscience Union Meeting 2018

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-OS Ocean Sciences & Ocean Environment

[A-OS09] Marine ecosystems and biogeochemical cycles: theory, observation and modeling

Wed. May 23, 2018 10:45 AM - 12:15 PM 105 (1F International Conference Hall, Makuhari Messe)

convener:Shin-ichi Ito(Atmosphere and Ocean Research Institute, The University of Tokyo), Takafumi Hirata(Faculty of Environmental Earth Science, Hokkaido University), Eileen E Hofmann (共同), Enrique N Curchitser (Rutgers University New Brunswick), Chairperson:Hirata Taka(Hokkaido University)

11:00 AM - 11:15 AM

[AOS09-07] Nitrate isotope distributions in the subarctic and subtropical North Pacific

*Chisato Yoshikawa1, Akiko Makabe1, Yohei Matsui1, Takuro Nunoura1, Naohiko Ohkouchi1 (1.Japan Agency for Marine-Earth Science and Technology)

Keywords:Marine nitrogen cycle, Nitrogen isotopes, North Pacific

Nitrogen isotopic composition of nitrate (δ15NNitrate) is widely used as a tracer of ocean-internal nitrogen cycling (consumption and regeneration) and ocean-external nitrogen inputs and losses (N2-fixation; fixation of N2 gas into bioavailable nitrogen such as ammonia by diazotrophs, and denitrification; microbial respiration using nitrate as an electron acceptor). When the phytoplankton assimilates nitrate, nitrogen isotopes are fractionated. A δ15NNitrate value increases, in conjunction with nitrate depletion, due to an isotopic effect during nitrate assimilation by phytoplankton. When denitrification occurs in the water column, a δ15NNitrate value extremely increases due to a strong isotopic effect. N2-fixation produces fixed nitrogen with a δ15N value of ~0‰, as nitrogen fixers take up N2 gas with little isotopic effect. This fixed nitrogen with low δ15N value is eventually converted into low-δ15NNitrate through degradation of nitrogenous organic compounds called remineralization and subsequent nitrification. Those signatures of δ15NNitrate in the euphotic zone are conserved in nitrogenous organic compounds and transfers to the sinking particles and deep-sea sediments. Here we determined δ15NNitrate and δ18ONitrate along 47°N in the subarctic North Pacific and 149°E in the western North Pacific. In the western subarctic gyre, known as High Nutrient, Low Chlorophyll (HNLC) region, the δ15NNitrate and the differences between δ15NNitrate and δ18ONitrate, or Δ(15-18), in the intermediate and deep waters were significantly lower than the surrounding area. Between the western subarctic gyre and the Alaskan gyre, there was an observed 0.4‰ increase in δ15NNitrate and a 0.6‰ increase in Δ(15-18) associated with a 7.2 μM decrease in the nitrate concentration at the surface. These results suggest that the 15N-depleted nitrate is generated by nitrified nitrate from remineralization of organic matter synthesized by partial consumption of surface nitrate pool, and the 15N enrichment toward the east is affected by the increase in utilization of surface nitrate pool. Assuming Rayleigh distillation kinetics, the increase in utilization between the western subarctic gyre and the Alaskan gyre, going from 29% to 85% utilization, corresponded to a change in δ15N of organic matter from 2.6‰ to 4.9‰. This study also revealed that the 15N-depleted nitrate in the surface water of the western subtropical gyre is generated by N2-fixation, whereas the 15N-enriched nitrate in the intermediate water at the western margin of North America is generated by water-column denitrification. The δ15N sediment record in the western subarctic North Pacific is expected to reflect the past changes in the HNLC region, but may also be controlled by water-column denitrification and N2-fixation.