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海洋氮循环:新发展与全球变化。

The marine nitrogen cycle: new developments and global change.

机构信息

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

出版信息

Nat Rev Microbiol. 2022 Jul;20(7):401-414. doi: 10.1038/s41579-022-00687-z. Epub 2022 Feb 7.

Abstract

The ocean is home to a diverse and metabolically versatile microbial community that performs the complex biochemical transformations that drive the nitrogen cycle, including nitrogen fixation, assimilation, nitrification and nitrogen loss processes. In this Review, we discuss the wealth of new ocean nitrogen cycle research in disciplines from metaproteomics to global biogeochemical modelling and in environments from productive estuaries to the abyssal deep sea. Influential recent discoveries include new microbial functional groups, novel metabolic pathways, original conceptual perspectives and ground-breaking analytical capabilities. These emerging research directions are already contributing to urgent efforts to address the primary challenge facing marine microbiologists today: the unprecedented onslaught of anthropogenic environmental change on marine ecosystems. Ocean warming, acidification, nutrient enrichment and seawater stratification have major effects on the microbial nitrogen cycle, but widespread ocean deoxygenation is perhaps the most consequential for the microorganisms involved in both aerobic and anaerobic nitrogen transformation pathways. In turn, these changes feed back to the global cycles of greenhouse gases such as carbon dioxide and nitrous oxide. At a time when our species casts a lengthening shadow across all marine ecosystems, timely new advances offer us unique opportunities to understand and better predict human impacts on nitrogen biogeochemistry in the changing ocean of the Anthropocene.

摘要

海洋是一个多样化且代谢方式多样的微生物群落的家园,这些微生物进行着复杂的生化转化,推动着氮循环,包括氮固定、同化、硝化和氮损失过程。在这篇综述中,我们讨论了从宏蛋白质组学到全球生物地球化学建模等多个学科以及从生产力高的河口到深海深渊等各种环境中丰富的新海洋氮循环研究。有影响力的最近发现包括新的微生物功能群、新的代谢途径、新颖的概念视角和开创性的分析能力。这些新兴的研究方向正在为解决海洋微生物学家目前面临的主要挑战做出贡献:人为环境变化对海洋生态系统的前所未有的冲击。海洋变暖、酸化、营养富化和海水分层对微生物氮循环有重大影响,但广泛的海洋缺氧对参与好氧和厌氧氮转化途径的微生物来说可能是最具影响的。反过来,这些变化又反馈到二氧化碳和氧化亚氮等温室气体的全球循环中。在我们这个物种在所有海洋生态系统中都投下越来越长的阴影的时候,及时的新进展为我们提供了独特的机会,使我们能够了解并更好地预测人类对人类世变化中的海洋氮生物地球化学的影响。

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