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Plankton in an acidified ocean

机译:浮游生物在海洋酸化

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摘要

The pH of the'ocean is expected to drop 0.3 units in the next century. This change is well within the pH range that plankton experience at present, but research suggests that changes in acidity near their cell surface could be larger.We may all recognize that organisms can modify their environment to suit their needs, but we generally think of large, complex organisms in this context. Beaver, for example, dramatically transform streams into large wetland systems. Plants modify soil chemistry at the soil-root interface to enhance the dissolution of mineral nutrients. However, active modification of the environment is not limited to thesebig organisms. Microscopic organisms also have both small and large impacts on their environment. At the level of individual cells, aquatic microorganisms practise low-impact living, limiting their influence to the thin boundary layer around the cell. Writing in Nature Climate Change, Flynn et al. report on a modelling study of oceanic plankton that looks at metabolic modifications to the pH and C02 chemistry in the boundarylayer surrounding the cell and how this 'microzone' may change over the next century as the oceans become more acidic.
机译:的pH值'ocean预计将下降0.3个单位在接下来的世纪。浮游生物的经验目前的pH值范围,但研究表明,酸度的变化在细胞表面可能会更大。所有生物体可以修改他们的认识环境,以适应他们的需求,但我们一般认为大型的、复杂的有机体上下文。将流转换成大型湿地系统。在soil-root植物修改土壤化学接口来提高矿物的溶解营养。环境是不限于thesebig生物。微生物也有小和对环境的影响。单个细胞,水生微生物实行绿色环保生活,限制他们影响周围的薄边界层细胞。海洋的人报告造型研究浮游生物,看着代谢修改boundarylayer pH值和二氧化碳化学周围的细胞和这个“microzone”如何可能改变在下个世纪海洋酸性更强。

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