Isotope constraints on particulate nitrogen source and dynamics in the upper water column of the oligotrophic South China Sea

• Published in: Global biogeochemical cycles 2012-06, Vol.26 (2), p.n/a
• Main Authors: Kao, Shuh-Ji, Terence Yang, Jin-Yu, Liu, Kon-Kee, Dai, Minhan, Chou, Wen-Chen, Lin, Hui-Ling, Ren, Haojia
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biogeochemistry; Biological and medical sciences; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fractionation; Fundamental and applied biological sciences. Psychology; General aspects; Geobiology; Geochemistry; Isotopes; Nitrogen; nitrogen isotope; Seasonal variations; sediment trap; South China Sea; suspended particle; Synecology; Thermocline; Water column
• ISSN: 0886-6236; 1944-9224
• DOI: 10.1029/2011GB004091

Particulate nitrogen (PN) dynamics in the oligotrophic northern South China Sea (around the SouthEast Asian Time‐series Study (SEATS) station) was explored by examining the isotopic compositions of suspended PN in the top 200 m over 3 years and sinking PN collected by sediment traps. The PN inventory (IPN) in the upper 100 m is larger than in the lower 100 m, exhibiting stronger seasonality. Both layers reveal significant seasonality in meanδ15NPN, yet, the mean in the upper 100 m (2.0 to 5.3‰) is consistently smaller than that in the lower 100 m, implying the occurrence of vertical biological fractionation and/or an addition of 15N‐depleted N from the atmosphere. Theδ15NPN surges in winter, when the mixed layer is deeper, indicate an intensified nitrate supply from thermocline, during which relatively stronger downward transfer efficiency was inferred by a small IPN gradient. The largest vertical gradient in IPN appeared during intermonsoon periods, corresponding with weak vertical mixing, low δ15NPN, and high N* values. N fixation is likely the cause for the intermonsoon δ15NPN lows. The δ15NPNvalues of trapped material at 374 m and 447 m range from 3.3 to 7.3‰ with a flux‐weighted mean of 5.6‰ resembling theδ15NO3of upwelled sources. By using a mass‐isotope balance model under the assumption of no atmospheric N deposition, we obtained an N fixation input of ∼20 ± 26 mmol N m−2 yr−1. This value accounts for only ∼5–10% of the new production on an annual basis. Key Points Isotopic constraints on particulate nitrogen dynamics in surface ocean Low downward transfer efficiency of N fixation signal Isotopic correlations between suspended and sinking particles