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浮游植物产生细胞外活性氧:过去与未来的方向

Production of extracellular reactive oxygen species by phytoplankton: past and future directions.

作者信息

Diaz Julia M, Plummer Sydney

机构信息

Department of Marine Sciences, Skidaway Institute of Oceanography, University of Georgia, Savannah, GA, USA.

出版信息

J Plankton Res. 2018 Nov;40(6):655-666. doi: 10.1093/plankt/fby039. Epub 2018 Sep 26.

DOI:10.1093/plankt/fby039
PMID:30487658
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6247811/
Abstract

In aquatic environments, phytoplankton represent a major source of reactive oxygen species (ROS) such as superoxide and hydrogen peroxide. Many phytoplankton taxa also produce extracellular ROS under optimal growth conditions in culture. However, the physiological purpose of extracellular ROS production by phytoplankton and its wider significance to ecosystem-scale trophic interactions and biogeochemistry remain unclear. Here, we review the rates, taxonomic diversity, subcellular mechanisms and functions of extracellular superoxide and hydrogen peroxide production by phytoplankton with a view towards future research directions. Model eukaryotic phytoplankton and cyanobacteria produce extracellular superoxide and hydrogen peroxide at cell-normalized rates that span several orders of magnitude, both within and between taxa. The potential ecophysiological roles of extracellular ROS production are versatile and appear to be shared among diverse phytoplankton species, including ichthyotoxicity, allelopathy, growth promotion, and iron acquisition. Whereas extracellular hydrogen peroxide likely arises from a combination of intracellular and cell surface production mechanisms, extracellular superoxide is predominantly generated by specialized systems for transplasma membrane electron transport. Future insights into the molecular-level basis of extracellular ROS production, combined with existing high-sensitivity geochemical techniques for the direct quantification of ROS dynamics, will help unveil the ecophysiological and biogeochemical significance of phytoplankton-derived ROS in natural aquatic systems.

摘要

在水生环境中,浮游植物是超氧化物和过氧化氢等活性氧物质(ROS)的主要来源。许多浮游植物类群在培养的最佳生长条件下也会产生细胞外ROS。然而,浮游植物产生细胞外ROS的生理目的及其对生态系统尺度营养相互作用和生物地球化学的更广泛意义仍不清楚。在这里,我们综述了浮游植物产生细胞外超氧化物和过氧化氢的速率、分类多样性、亚细胞机制和功能,以期为未来的研究方向提供参考。模式真核浮游植物和蓝细菌产生细胞外超氧化物和过氧化氢的细胞标准化速率跨越几个数量级,在分类群内部和之间均如此。细胞外ROS产生的潜在生态生理作用是多方面的,似乎在不同的浮游植物物种中都有体现,包括对鱼类的毒性、化感作用、促进生长和获取铁元素。细胞外过氧化氢可能源于细胞内和细胞表面产生机制的结合,而细胞外超氧化物主要由跨质膜电子传递的特殊系统产生。未来对细胞外ROS产生的分子水平基础的深入了解,结合现有的用于直接量化ROS动态的高灵敏度地球化学技术,将有助于揭示浮游植物衍生的ROS在天然水生系统中的生态生理和生物地球化学意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a16/6247811/788f949e85a9/fby039f02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a16/6247811/ddae3e46b80f/fby039f01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a16/6247811/788f949e85a9/fby039f02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a16/6247811/ddae3e46b80f/fby039f01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a16/6247811/788f949e85a9/fby039f02.jpg

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