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Characterization of Prochlorococcus clades from iron-depleted oceanic regions

机译:贫铁海洋地区原球菌进化枝的特征

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摘要

Prochlorococcus describes a diverse and abundant genus of marine photosynthetic microbes. It is primarily found in oligotrophic waters across the globe and plays a crucial role in energy and nutrient cycling in the ocean ecosystem. The abundance, global distribution, and availability of isolates make Prochlorococcus a model system for understanding marine microbial diversity and biogeochemical cycling. Analysis of 73 metagenomic samples from the Global Ocean Sampling expedition acquired in the Atlantic, Pacific, and Indian Oceans revealed the presence of two uncharacterized Prochlorococcus clades. A phylogenetic analysis using six different genetic markers places the clades close to known lineages adapted to high-light environments. The two uncharacterized clades consistently cooccur and dominate the surface waters of high-temperature, macronutrient-replete, and low-iron regions of the Eastern Equatorial Pacific upwelling and the tropical Indian Ocean. They are genetically distinct from each other and other high-light Prochlorococcus isolates and likely define a previously unrecognized ecotype. Our detailed genomic analysis indicates that these clades comprise organisms that are adapted to iron-depleted environments by reducing their iron quota through the loss of several iron-containing proteins that likely function as electron sinks in the photosynthetic pathway in other Prochlorococcus clades from high-light environments. The presence and inferred physiology of these clades may explain why Prochlorococcus populations from iron-depleted regions do not respond to iron fertilization experiments and further expand our understanding of how phytoplankton adapt to variations in nutrient availability in the ocean.
机译:原绿球菌描述了海洋光合微生物的多样性和丰富的属。它主要存在于全球的贫营养水中,在海洋生态系统的能量和养分循环中起着至关重要的作用。分离菌的丰富,全球分布和可获得性使Prochlorococcus成为理解海洋微生物多样性和生物地球化学循环的模型系统。对来自大西洋,太平洋和印度洋的全球海洋采样远征队的73个宏基因组学样本进行的分析表明,存在两个未鉴定的原球藻球菌进化枝。使用六种不同遗传标记的系统发育分析表明进化枝靠近适合高光环境的已知谱系。赤道东太平洋上升流和热带印度洋的高温,大量营养丰富和低铁区域的两个表层水质始终一致并占主导地位。它们在遗传上彼此不同,也与其他高强度原球菌分离,因此可能定义了以前无法识别的生态型。我们详细的基因组分析表明,这些进化枝包含通过减少几种含铁蛋白的含量而减少其铁定额的方式,从而适应了贫铁环境,这些铁蛋白可能会在高光照下其他Prochlorococcus进化枝中的光合途径中充当电子沉环境。这些进化枝的存在和推测的生理现象可能解释了为什么缺铁地区的原球菌种群对铁肥实验没有反应,并进一步扩大了我们对浮游植物如何适应海洋养分利用率变化的理解。

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