Seasonal and interannual variations in nitrogen availability and particle export in the northwestern North Pacific subtropical gyre

Mino, Y., Sukigara, C., Honda, M. C., Kawakami, H., Wakita, M., Sasaoka, K., Yoshikawa, C., Abe, O., Kaiser, J. ORCID: https://orcid.org/0000-0002-1553-4043, Kimoto, K., Kitamura, M., Fujiki, T., Matsumoto, K. and Saino, T. (2020) Seasonal and interannual variations in nitrogen availability and particle export in the northwestern North Pacific subtropical gyre. Journal of Geophysical Research: Oceans, 125 (5). ISSN 2169-9275

[thumbnail of Accepted_Manuscript]
Preview
PDF (Accepted_Manuscript) - Accepted Version
Download (2MB) | Preview

Abstract

Time series of particulate nitrogen isotope delta (PN-δ 15N) and flux of trapped particles at 200 m were determined in the northwestern North Pacific subtropical gyre between 2010 and 2014 in order to examine temporal variations in mixed layer nitrate availability and downward particle export. Lower PN-δ 15N (<4‰) seen every winter corresponded to convective nitrate supply triggering phytoplankton blooms. Greater particle fluxes were associated with higher CaCO 3 concentrations (mass fraction >50%), implying that new nitrogen supply stimulated predominantly coccolithophore growth and downward transport of coccoliths. Even in the stratified summer of 2011, a δ 15N drop associated with a spike in particulate flux was found and was attributed to the uplift of nitrate-rich deep waters due to a mesoscale cyclonic eddy passing the mooring station. Total nitrate input sustains 86–93% of annual new production in this region while nitrogen fixation accounts for the rest. Trapped particles also showed that the winter δ 15N decrease appeared earlier in the 2011–2012 blooms than those in 2013–2014, coinciding with 8% higher CaCO 3 concentrations and a 40% lower particulate organic carbon to inorganic carbon export ratio, R(POC:PIC). This reflected stronger convective mixing and hence larger nutrient supply in 2011–2012, caused by larger ocean heat loss related to winter monsoon intensity. Such interannual change of winter R(POC:PIC) can affect CO 2 uptake rate in the northwestern North Pacific subtropical gyre where anthropogenic CO 2 accumulates in subtropical mode waters.

Item Type: Article
Uncontrolled Keywords: poc:pic export ratio,coccolithophore,delta n-15 of particles,nitrate supply,the western north pacific subtropical gyre,time-series sediment trap,geophysics,forestry,oceanography,aquatic science,ecology,water science and technology,soil science,geochemistry and petrology,earth-surface processes,atmospheric science,earth and planetary sciences (miscellaneous),space and planetary science,palaeontology ,/dk/atira/pure/subjectarea/asjc/1900/1908
Faculty \ School: Faculty of Science > School of Environmental Sciences
University of East Anglia Research Groups/Centres > Theme - ClimateUEA
UEA Research Groups: Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Related URLs:
Depositing User: LivePure Connector
Date Deposited: 22 Apr 2020 08:48
Last Modified: 20 Mar 2023 10:48
URI: https://ueaeprints.uea.ac.uk/id/eprint/74811
DOI: 10.1029/2019JC015600

Downloads

Downloads per month over past year

Actions (login required)

View Item View Item