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Interactions between growth-dependent changes in cell size nutrient supply and cellular elemental stoichiometry of marine Synechococcus

机译:海洋Synechococcus细胞大小营养供应和细胞元素化学计量的生长依赖性变化之间的相互作用

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摘要

The factors that control elemental ratios within phytoplankton, like carbon:nitrogen:phosphorus (C:N:P), are key to biogeochemical cycles. Previous studies have identified relationships between nutrient-limited growth and elemental ratios in large eukaryotes, but little is known about these interactions in small marine phytoplankton like the globally important Cyanobacteria. To improve our understanding of these interactions in picophytoplankton, we asked how cellular elemental stoichiometry varies as a function of steady-state, N- and P-limited growth in laboratory chemostat cultures of Synechococcus WH8102. By combining empirical data and theoretical modeling, we identified a previously unrecognized factor (growth-dependent variability in cell size) that controls the relationship between nutrient-limited growth and cellular elemental stoichiometry. To predict the cellular elemental stoichiometry of phytoplankton, previous theoretical models rely on the traditional Droop model, which purports that the acquisition of a single limiting nutrient suffices to explain the relationship between a cellular nutrient quota and growth rate. Our study, however, indicates that growth-dependent changes in cell size have an important role in regulating cell nutrient quotas. This key ingredient, along with nutrient-uptake protein regulation, enables our model to predict the cellular elemental stoichiometry of Synechococcus across a range of nutrient-limited conditions. Our analysis also adds to the growth rate hypothesis, suggesting that P-rich biomolecules other than nucleic acids are important drivers of stoichiometric variability in Synechococcus. Lastly, by comparing our data with field observations, our study has important ecological relevance as it provides a framework for understanding and predicting elemental ratios in ocean regions where small phytoplankton like Synechococcus dominates.
机译:控制浮游植物内元素比例的因素,例如碳:氮:磷(C:N:P),是生物地球化学循环的关键。先前的研究已经确定了大型真核生物中有限养分的生长与元素比率之间的关系,但是对于像全球重要的蓝藻这样的小型海洋浮游植物中的这些相互作用知之甚少。为了提高我们对浮游浮游生物中这些相互作用的理解,我们询问在Syechococcus WH8102实验室化学恒温培养物中,细胞元素化学计量如何随稳态,N和P限制生长而变化。通过结合经验数据和理论模型,我们确定了一个以前无法识别的因素(细胞大小的生长依赖性变异性),该因素控制了养分限制的生长与细胞元素化学计量之间的关系。为了预测浮游植物的细胞元素化学计量,以前的理论模型依赖于传统的Droop模型,该模型声称获得单个限制营养素就足以说明细胞营养素配额与生长速率之间的关系。然而,我们的研究表明,细胞大小的生长依赖性变化在调节细胞营养配额方面具有重要作用。这种关键成分以及营养素摄取蛋白的调控,使我们的模型能够在一系列营养素限制条件下预测突触球菌的细胞化学计量。我们的分析还增加了增长率假说,表明除核酸以外的富含P的生物分子是Synechococcus中化学计量比变化的重要驱动因素。最后,通过将我们的数据与实地观测结果进行比较,我们的研究具有重要的生态意义,因为它为了解和预测以浮游生物为代表的浮游植物为主的海洋区域的元素比率提供了框架。

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