Mesoscale eddies shape Prochlorococcuscommunity structure and dynamics in the oligotrophic open ocean

Uri Sheyn, Kirsten E Poff, John M Eppley, Andy O Leu, Jessica A Bryant, Fuyan Li, Anna E Romano, Andy Burger, Benedetto Barone, Edward F DeLong
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Abstract

Mesoscale eddies, horizontally rotating currents sometimes referred to as “ocean weather,” influence open ocean macronutrient distributions, primary production, and microbial community structure. Such eddies impact ecosystems like the North Pacific Subtropical Gyre, where year-round thermal stratification limits the mixing of subsurface macronutrients with surface waters. Populations of the dominant primary producer Prochlorococcusin the North Pacific Subtropical Gyre consist of genetic variants with differential adaptive traits to light intensity, temperature, and macronutrient availability. How Prochlorococcuspopulation variants respond to transient, localized environmental changes, however, remains an open question. Leveraging microbial community phylogenetic, metagenomic, and metatranscriptomic data, we report here a consistent, specific enrichment of Prochlorococcushigh-light I ecotypes around the deep chlorophyll maximum in cyclonic eddies, but not adjacent anticyclonic eddies. The shallower deep chlorophyll maximum depths of cyclones had lower temperatures, higher light intensities, and elevated nutrient concentrations compared to adjacent anticyclones, which favored Prochlorococcushigh-light I ecotype proliferation. Prochlorococcushigh-light I ecotypes in the cyclone deep chlorophyll maximum exhibited unique genetic traits related to nitrogen metabolism and were enriched in gene transcripts associated with energy production, cell replication, and proliferation. Prochlorococcusgene transcripts involved in amino acid transport, metabolism, and biosynthesis were also elevated in the cyclone. These results suggest the potential importance of nitrogen metabolism in Prochlorococcushigh-light I ecotype proliferation in cyclonic eddies. Our findings demonstrate how mesoscale eddies shape microbial community structure in the oligotrophic ocean and how Prochlorococcuscommunities respond to short-term localized environmental variability.
中尺度涡旋影响寡营养开阔海域原绿球菌群落结构和动态
中尺度涡旋,即有时被称为“海洋天气”的水平旋转洋流,影响着开阔海洋的大量营养物质分布、初级生产和微生物群落结构。这样的涡旋会影响像北太平洋亚热带环流这样的生态系统,在那里全年的热分层限制了地下大量营养物质与地表水的混合。北太平洋副热带环流原绿球藻的优势初级生产者群体由对光强、温度和大量养分有效性具有不同适应特征的遗传变异组成。然而,原绿球菌种群变异如何对短暂的局部环境变化作出反应仍然是一个悬而未决的问题。利用微生物群落系统发育、宏基因组学和元转录组学数据,我们在这里报告了在气旋涡旋中,原绿球菌高光I生态型在深叶绿素最大值周围一致、特异性富集,而不是在邻近的反气旋涡旋中富集。与邻近的反气旋相比,气旋较浅的深层叶绿素最大深度具有较低的温度、较高的光强和较高的营养物质浓度,有利于原绿球藻高光I生态型的增殖。气旋深叶绿素区原绿球藻高光I生态型表现出与氮代谢相关的独特遗传性状,并富含与能量产生、细胞复制和增殖相关的基因转录物。参与氨基酸运输、代谢和生物合成的原绿球藻基因转录物也在气旋中升高。这些结果表明氮代谢在原绿球藻高光I型生态型在旋涡中的增殖中具有潜在的重要性。我们的研究结果证明了中尺度涡旋如何塑造寡营养海洋中的微生物群落结构,以及原绿球菌群落如何响应短期局部环境变化。
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