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Influence of Temperature and CO2 On Plasma-membrane Permeability to CO2 and HCO3 - in the Marine Haptophytes Emiliania huxleyi and Calcidiscus leptoporus (Prymnesiophyceae).
Journal of Phycology ( IF 2.9 ) Pub Date : 2020-05-17 , DOI: 10.1111/jpy.13017
Sonia Blanco-Ameijeiras 1 , Heather M Stoll 1 , Hongrui Zhang 1, 2 , Brian M Hopkinson 3
Affiliation  

Membrane permeabilities to CO2 and HCO3 constrain the function of CO2 concentrating mechanisms that algae use to supply inorganic carbon for photosynthesis. In diatoms and green algae, plasma membranes are moderately to highly permeable to CO2 but effectively impermeable to HCO3. Here, CO2 and HCO3 membrane permeabilities were measured using an 18O‐exchange technique on two species of haptophyte algae, Emiliania huxleyi and Calcidiscus leptoporus, which showed that the plasma membranes of these species are also highly permeable to CO2 (0.006–0.02 cm · s−1) but minimally permeable to HCO3. Increased temperature and CO2 generally increased CO2 membrane permeabilities in both species, possibly due to changes in lipid composition or CO2 channel proteins. Changes in CO2 membrane permeabilities showed no association with the density of calcium carbonate coccoliths surrounding the cell, which could potentially impede passage of compounds. Haptophyte plasma‐membrane permeabilities to CO2 were somewhat lower than those of diatoms but generally higher than membrane permeabilities of green algae. One caveat of these measurements is that the model used to interpret 18O‐exchange data assumes that carbonic anhydrase, which catalyzes 18O‐exchange, is homogeneously distributed in the cell. The implications of this assumption were tested using a two‐compartment model with an inhomogeneous distribution of carbonic anhydrase to simulate 18O‐exchange data and then inferring plasma‐membrane CO2 permeabilities from the simulated data. This analysis showed that the inferred plasma‐membrane CO2 permeabilities are minimal estimates but should be quite accurate under most conditions.

中文翻译:

温度和CO2对海洋七足纲植物Emiliaania huxleyi和Calcidiscus leptoporus(Prymnesiophyceae)的质膜透透性对CO2和HCO3的影响。

膜渗透性至CO 2和HCO 3 -限制CO的功能2浓缩机制藻类使用用于光合作用提供无机碳。在硅藻和绿藻,质膜是中度至高度可渗透的CO 2可有效不可渗透HCO 3 - 。在此,CO 2和HCO 3 -使用测量膜渗透率18上的两个物种定鞭藻门的藻类,O型交换技术-贺Calcidiscus leptoporus,这表明,这些物质的等离子体膜也高渗透性至CO2(0.006-0.02厘米·秒-1),但最低限度地可渗透HCO 3 - 。升高的温度和CO 2通常会增加两个物种中的CO 2膜渗透性,这可能是由于脂质组成或CO 2通道蛋白的变化所致。CO 2膜通透性的变化表明与细胞周围碳酸钙可可脂的密度无关,这可能会阻止化合物的通过。八足植物对CO 2的膜渗透率略低于硅藻,但通常高于绿藻的膜渗透率。这些测量的一个警告是,用于解释18 O交换数据假定催化18 O交换的碳酸酐酶均匀分布在电池中。该假设的含义使用两室模型进行了测试,该模型具有碳酸酐酶的不均匀分布,以模拟18个O交换数据,然后从模拟数据推断出血浆膜的CO 2渗透率。该分析表明,推定的血浆膜CO 2渗透率是最小估计值,但在大多数情况下应相当准确。
更新日期:2020-05-17
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