Inomura Keisuke, Wilson Samuel T, Deutsch Curtis
School of Oceanography, University of Washington, Seattle, Washington, USA
Daniel K. Inouye Center for Microbial Oceanography: Research and Education (C-MORE), University of Hawai'i at Manoa, Honolulu, Hawaii, USA.
mSystems. 2019 Aug 6;4(4):e00210-19. doi: 10.1128/mSystems.00210-19.
The cyanobacterium is an important contributor of new nitrogen (N) to the surface ocean, but its strategies for protecting the nitrogenase enzyme from inhibition by oxygen (O) remain poorly understood. We present a dynamic physiological model to evaluate hypothesized conditions that would allow to carry out its two conflicting metabolic processes of N fixation and photosynthesis. First, the model indicates that managing cellular O to permit N fixation requires high rates of respiratory O consumption. The energetic cost amounts to ∼80% of daily C fixation, comparable to the observed diminution of the growth rate of relative to other phytoplankton. Second, by forming a trichome of connected cells, can segregate N fixation from photosynthesis. The transfer of stored C to N-fixing cells fuels the respiratory O consumption that protects nitrogenase, while the reciprocal transfer of newly fixed N to C-fixing cells supports cellular growth. Third, despite lacking the structural barrier found in heterocystous species, the model predicts low diffusivity of cell membranes, a function that may be explained by the presence of Gram-negative membrane, production of extracellular polysaccharide substances (EPS), and "buffer cells" that intervene between N-fixing and photosynthetic cells. Our results suggest that all three factors-respiratory protection, trichome formation, and diffusion barriers-represent essential strategies that, despite their energetic costs, facilitate the growth of in the oligotrophic aerobic ocean and permit it to be a major source of new reactive nitrogen. is a major nitrogen-fixing cyanobacterium and exerts a significant influence on the oceanic nitrogen cycle. It is also a widely used model organism in laboratory studies. Since the nitrogen-fixing enzyme nitrogenase is extremely sensitive to oxygen, how these surface-dwelling plankton manage the two conflicting processes of nitrogen fixation and photosynthesis has been a long-standing question. In this study, we developed a simple model of metabolic fluxes of capturing observed daily cycles of photosynthesis, nitrogen fixation, and boundary layer oxygen concentrations. The model suggests that forming a chain of cells for spatially segregating nitrogen fixation and photosynthesis is essential but not sufficient. It also requires a barrier against oxygen diffusion and high rates of oxygen scavenging by respiration. Finally, the model indicates an extremely short life span of oxygen-enabling cells to instantly create a low-oxygen environment upon deactivation of photosynthesis.
蓝细菌是海洋表层新氮的重要贡献者,但其保护固氮酶免受氧抑制的策略仍知之甚少。我们提出了一个动态生理模型,以评估假设条件,这些条件将使蓝细菌能够进行固氮和光合作用这两个相互冲突的代谢过程。首先,该模型表明,控制细胞内的氧以允许固氮需要高呼吸耗氧率。能量成本相当于每日碳固定量的80%左右,这与观察到的蓝细菌相对于其他浮游植物生长速率的降低相当。其次,通过形成由相连细胞组成的藻丝,蓝细菌可以将固氮与光合作用分开。储存的碳向固氮细胞的转移为保护固氮酶的呼吸耗氧提供了能量,而新固定的氮向碳固定细胞的反向转移则支持细胞生长。第三,尽管蓝细菌缺乏异形胞物种中发现的结构屏障,但该模型预测细胞膜具有低扩散性,这一功能可能由革兰氏阴性膜的存在、胞外多糖物质(EPS)的产生以及介于固氮细胞和光合细胞之间的“缓冲细胞”来解释。我们的结果表明,所有这三个因素——呼吸保护、藻丝形成和扩散屏障——代表了基本策略,尽管它们有能量成本,但有助于蓝细菌在贫营养需氧海洋中生长,并使其成为新的活性氮的主要来源。蓝细菌是主要的固氮蓝细菌,对海洋氮循环有重大影响。它也是实验室研究中广泛使用的模式生物。由于固氮酶对氧极其敏感,这些生活在海洋表层的浮游生物如何管理固氮和光合作用这两个相互冲突的过程一直是一个长期存在的问题。在这项研究中,我们开发了一个简单的蓝细菌代谢通量模型,该模型捕捉了观察到的光合作用、固氮和边界层氧浓度的每日循环。该模型表明,形成一串细胞以在空间上分离固氮和光合作用是必不可少的,但还不够。它还需要一个防止氧扩散的屏障和高呼吸吸氧率。最后,该模型表明,产氧细胞的寿命极短,在光合作用失活后能立即创造一个低氧环境。