4.7 Article

Biogeography of N2 Fixation Influenced by the Western Boundary Current Intrusion in the South China Sea

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 124, Issue 10, Pages 6983-6996

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2018JC014781

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Funding

  1. National Natural Science Foundation of China [NSFC U1305233, 41376116, 41721005, 91328207]
  2. National Key Basic Research Program of China (973 Program) [2014CB953702, 2015CB954003]
  3. Scientific Research Fund of the Second Institute of Oceanography, SOA [SZ1914]

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The N-2 fixation and primary production rates were measured simultaneously using N-15(2) and C-13 incubation assays in the northern South China Sea influenced by the Kuroshio intrusion (KI) seasonally. The degree of KI (KI index, range from 0 to 1) was assessed by applying an isopycnal mixing model. The water column integrated N-2 fixation and primary production for stations with KI index larger than 0.5 were 463 +/- 260 mu mol N center dot m(-2)center dot day(-1) and 62 +/- 19 mmol C center dot m(-2)center dot day(-1), respectively, significantly higher than those for stations with KI index lower than 0.5 (50 +/- 10 mu mol N center dot m(-2)center dot day(-1) and 28 +/- 10 mmol C center dot m(-2)center dot day(-1), respectively). Trichodesmium was the dominant diazotroph at stations with KI index larger than 0.5, with 2 orders of magnitude higher nifH gene abundance than that at stations with KI index lower than 0.5. However, the highest N-2 fixation rates were found in waters with moderate KI index around 0.6, suggesting that frontal zone mixing might stimulate N-2 fixation. Our results demonstrated that diazotrophs (mainly Trichodesmium) were tightly associated with the KI, which modulated the biogeographic distribution of N-2 fixers. In summary, we found the transportation of Trichodesmium by KI, then, we quantified the fraction of KI and N-2 fixation rates in the northern South China Sea. The results suggested that KI generated a new biogeographic regime which could significantly influence the carbon and nitrogen cycles far away from the main stream.

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