Biogeography of N-2 fixation influenced by the western boundary current intrusion in the South China Sea Lu, Y. Y. Wen, Z. Z. Shi, D. L. Lin, W. F. /Bonnet, Sophie Dai, M. H. Kao, S. J. 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. 2019 text https://www.documentation.ird.fr/hor/fdi:010077125 fdi:010077125 Lu Y. Y., Wen Z. Z., Shi D. L., Lin W. F., Bonnet Sophie, Dai M. H., Kao S. J.. Biogeography of N-2 fixation influenced by the western boundary current intrusion in the South China Sea. 2019, 124 (10), 6983-6996 EN MER DE CHINE