Key Laboratory of Coastal Biology and Biological Resource Utilization, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai, 264003, China; University of Chinese Academy of Sciences, Beijing, 101408, China.
Key Laboratory of Coastal Biology and Biological Resource Utilization, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai, 264003, China.
Environ Res. 2023 Dec 15;239(Pt 1):117383. doi: 10.1016/j.envres.2023.117383. Epub 2023 Oct 12.
Coastal nitrogen input has substantially increased due to human activity. However, much remains unknown about the nitrogen-driven patterns and the underlying genetic basis of coastal picoplankton. To investigate the response and mechanisms of picoplankton induced by nitrogen variation, we conducted in-situ investigations using high-throughput sequencing in the Bohai Sea and performed laboratory nitrogen simulation experiments accompanied by physiological, genomic, and transcriptomic analyses, with Synechococcus as a representative. The results of in-situ investigation revealed that Synechococcus clades I, III, WPC1, and VI of subcluster 5.1 (S5.1) are prevalent in strait areas characterized by robust water exchange with the North Yellow Sea, while clades II, VIII, and IX of S5.1, as well as subcluster 5.2 (S5.2) and subcluster 5.3 (S5.3) are more abundant in central and bay areas experiencing elevated nitrate and nitrite loads. The laboratory experiments further confirmed that inorganic nitrogen is a crucial determinant of diversity and niche partitioning of Synechococcus lineages. Besides, the raising inorganic nitrogen concentration within the current in-situ range (0.1-10 μmol L) enhances photosynthesis and carbon fixation of Synechococcus, however further escalation of inorganic nitrogen (100 μmol L) may hinder these processes instead. The phenomenon could be associated with the differential expression of genes in metabolic pathways regulating nitrogen metabolism, photosynthetic system II, and photosynthesis-antenna proteins in response to nitrogen concentration and type variation. These findings expand our understanding of the impact of macronutrient variation resulting from human activities on marine picoplankton and biogeochemical cycles.
由于人类活动,沿海地区的氮输入大大增加。然而,对于氮驱动的沿海微微型浮游生物模式和潜在的遗传基础,我们仍然知之甚少。为了研究氮变化对微微型浮游生物的响应和机制,我们在渤海进行了现场调查,使用高通量测序,并进行了实验室氮模拟实验,同时进行了生理、基因组和转录组分析,以聚球藻作为代表。现场调查的结果表明,在与北黄海水交换强烈的海峡地区,I、III、WPC1 和 VI 聚类的聚球藻群是优势种;而在硝酸盐和亚硝酸盐负荷较高的中部和海湾地区,S5.1 的 II、VIII 和 IX 聚类以及 S5.2 和 S5.3 聚类更为丰富。实验室实验进一步证实,无机氮是聚球藻谱系多样性和生态位分化的关键决定因素。此外,在当前现场范围内(0.1-10 μmol L)提高无机氮浓度可以增强聚球藻的光合作用和碳固定,但进一步提高无机氮浓度(100 μmol L)可能会阻碍这些过程。这种现象可能与氮代谢、光合系统 II 和光合作用天线蛋白相关代谢途径中基因的差异表达有关,这些基因可以响应氮浓度和类型的变化。这些发现扩展了我们对人类活动引起的宏量营养素变化对海洋微微型浮游生物和生物地球化学循环的影响的认识。