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微生物与海洋全球变化。

Microorganisms and ocean global change.

机构信息

Marine and Environmental Biology, University of Southern California, Los Angeles, California 90089, USA.

出版信息

Nat Microbiol. 2017 May 25;2:17058. doi: 10.1038/nmicrobiol.2017.58.

Abstract

The prokaryotic and eukaryotic microorganisms that drive the pelagic ocean's biogeochemical cycles are currently facing an unprecedented set of comprehensive anthropogenic changes. Nearly every important control on marine microbial physiology is currently in flux, including seawater pH, p, temperature, redox chemistry, irradiance and nutrient availability. Here, we examine how microorganisms with key roles in the ocean carbon and nitrogen cycles may respond to these changes in the Earth's largest ecosystem. Some functional groups such as nitrogen-fixing cyanobacteria and denitrifiers may be net beneficiaries of these changes, while others such as calcifiers and nitrifiers may be negatively impacted. Other groups, such as heterotrophic bacteria, may be relatively resilient to changing conditions. The challenge for marine microbiologists will be to predict how these divergent future responses of marine microorganisms to complex multiple variable interactions will be expressed through changing biogeography, community structure and adaptive evolution, and ultimately through large-scale alterations of the ocean's carbon and nutrient cycles.

摘要

驱动海洋生物地球化学循环的原核生物和真核微生物目前正面临着前所未有的全面人为变化。几乎每一个对海洋微生物生理学有重要控制作用的因素都在发生变化,包括海水 pH 值、二氧化碳分压、温度、氧化还原化学、光照和营养物质的可利用性。在这里,我们研究了在地球最大的生态系统中,海洋碳氮循环中具有关键作用的微生物可能会如何应对这些变化。一些功能群,如固氮蓝藻和反硝化菌,可能是这些变化的净受益者,而其他如钙化生物和硝化生物则可能受到负面影响。其他群体,如异养细菌,可能对变化的条件相对有弹性。海洋微生物学家面临的挑战将是预测海洋微生物对复杂的多变量相互作用的这些不同未来反应将如何通过生物地理学、群落结构和适应性进化的变化表现出来,并最终通过海洋碳氮循环的大规模改变表现出来。

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