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  4. Dissolved Organic Nitrogen Cycling in the South China Sea From an Isotopic Perspective
 
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Dissolved Organic Nitrogen Cycling in the South China Sea From an Isotopic Perspective

Journal
Global Biogeochemical Cycles
Journal Volume
34
Journal Issue
12
Date Issued
2020
Author(s)
Zhang R
Wang X.T
HAO-JIA REN  
Huang J
Chen M
Sigman D.M.
DOI
10.1029/2020GB006551
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85097997206&doi=10.1029%2f2020GB006551&partnerID=40&md5=377d39b12bed8a73b2c10b43c10613ee
https://scholars.lib.ntu.edu.tw/handle/123456789/571631
Abstract
Dissolved organic nitrogen (DON) is the dominant form of fixed nitrogen in most low and middle latitude ocean surface waters. Here, we report measurements of DON isotopic composition (δ15N) from the west South China Sea (SCS), with the goal of providing new insight into DON cycling. The concentration of DON in the surface ocean is correlated (r?=?0.70, p?<?0.0001) with chlorophyll a concentration, indicating DON production in these surface waters. The concentration and δ15N of DON fall in a relatively narrow range in the surface ocean (4.6?±?0.1?μM and 4.3?±?0.2? vs. air, respectively; ±SD), similar to other ocean regions. The mean DON δ15N above 50?m (4.5?±?0.3?) is similar to the δ15N of nitrate in the “shallow subsurface” (i.e., immediately below the euphotic zone; 4.6?±?0.2?) but is higher than the δ15N of suspended particles in the surface ocean (~2.3?). This set of isotopic relationships has been observed previously (e.g., in the oligotrophic North Atlantic and North Pacific) and can be explained by the cycling of N between particulate organic nitrogen (PON), DON, and ammonium, in which an isotope effect associated with DON degradation preferentially concentrates 15N in DON. Consistent with this view, a negative correlation (r?=?0.70) between the concentration and the δ15N of DON is observed in the upper 75?m, suggesting an isotope effect of ~4.9?±?0.4? for DON degradation. Comparing the DON δ15N data from the SCS with other regions, we find that the δ15N difference between euphotic zone DON and shallow subsurface nitrate δ15N (Δδ15N(DON-NO3)) rises from ocean regions of inferred net DON production to regions of net DON consumption, with the SCS representing an intermediate case. ?2020. American Geophysical Union. All Rights Reserved.
Subjects
concentration (composition); dissolved organic nitrogen; euphotic zone; isotopic composition; nutrient cycling; organic nitrogen; particulate organic nitrogen; sea surface; seawater; Atlantic Ocean; Atlantic Ocean (North); Pacific Ocean; Pacific Ocean (North); South China Sea
SDGs

[SDGs]SDG13

[SDGs]SDG14

Type
journal article

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