4.6 Article

Comparison of Diazotrophic Composition and Distribution in the South China Sea and the Western Pacific Ocean

Journal

BIOLOGY-BASEL
Volume 10, Issue 6, Pages -

Publisher

MDPI
DOI: 10.3390/biology10060555

Keywords

diazotroph; Proteobacteria; Trichodesmium; unicellular cyanobacteria; South China Sea; Western Pacific Ocean

Categories

Funding

  1. National Key Research and Development Project of China [2019YFC1407805]
  2. National Natural Science Foundation of China [41876134, 41676112, 41276124, 41406155]
  3. Key Project of Key Laboratory of Integrated Marine Monitoring and Applied Technologies for Harmful Algal Blooms [MATHAB201805]
  4. Key Project of Natural Science Foundation for Tianjin [17JCZDJC40000]
  5. Tianjin 131 Innovation Team Program [20180314]
  6. Changjiang Scholar Program of Chinese Ministry of Education [T2014253]

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This study investigated the spatial variation of diazotrophic communities in the South China Sea and Western Pacific Ocean. The dominant diazotrophs were Proteobacteria in the SCS and Cyanobacteria in the WPO. Temperature, dissolved inorganic nitrogen, and dissolved inorganic phosphate were significantly correlated with variations in diazotroph composition.
Simple Summary Diazotrophs are important contributors of bioavailable nitrogen that is essential to maintaining biological productivity in marine ecosystems. In this study, surface water samples were analyzed to explore the spatial variation of the diazotrophic community in the upper seawater of the South China Sea (SCS) and the Western Pacific Ocean (WPO). The well-conserved gene nifH, which is considered an important marker gene, was used for analyzing the phylogeny, diversity, and abundance of diazotrophs in this study. Our results showed that Proteobacteria was the main diazotroph in the SCS, while Cyanobacteria accounted for the largest proportion in the diazotroph community in the WPO. In addition, high abundances of diazotrophs in the subequatorial WPO indicated the occurrence of diazotrophs blooming. Variation in the composition of diazotrophs was significantly correlated with temperature, dissolved inorganic nitrogen, dissolved inorganic phosphate, and spatial variables between these regions. Our results provide insights into the ecological success and biogeochemical importance of diazotrophic communities in changing environments. The variation of diazotrophs has been elusive in multiple SCS and WPO regions due to insufficient data. Therefore, the dynamics of diazotrophic composition and distribution were investigated in this study, based on high-throughput sequencing and quantitative PCR of the nifH gene. We found that Proteobacteria dominated the diazotrophic community in the river-impacted SCS and cyanobacteria and Proteobacteria were more abundant in the ocean-dominated SCS and WPO. The qPCR analysis showed that cyanobacterial Trichodesmium was abundant in the Pearl River plume and in the SCS basin influenced by the Kuroshio intrusion, and it also thrived in the subequatorial region of the WPO. Unicellular cyanobacteria UCYN-A were mainly detected in the river-impacted area, UCYN-B was abundant in the WPO, UCYN-C had a relatively high abundance in the ocean-dominated area, and a preponderance of gamma-Proteobacteria gamma-24774A11 was observed in the ocean-dominated SCS and pelagic WPO. Diazotrophic communities had significant distance-decay relationships, reflecting clear biogeographic patterns in the study area. The variations of diazotrophic community structure were well explained by dissolved inorganic nitrogen, dissolved inorganic phosphate by an eigenvector spatial variable PCNM1. These results provide further information to help determine the ecological mechanism of elusive diazotrophic communities in different ocean ecosystems.

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