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固氮作用:淡水 - 海洋连续体中一个了解甚少的过程。

Nitrogen fixation: a poorly understood process along the freshwater-marine continuum.

作者信息

Marcarelli Amy M, Fulweiler Robinson W, Scott J Thad

机构信息

Department of Biological Sciences, Michigan Technological University.

Department of Earth and Environment, Boston University.

出版信息

Limnol Oceanogr Lett. 2022 Feb;7(1):1-10. doi: 10.1002/lol2.10220. Epub 2021 Oct 29.

Abstract

Although N fixation is a major component of the global N cycle and has been extensively studied in open-ocean and terrestrial ecosystems, rates and ecological dynamics remain virtually unknown for the inland and coastal aquatic ecosystems (lakes, wetlands, rivers, streams, estuaries) that connect terrestrial and marine biomes. This is due to the diversity of these habitats, as well as the traditional paradigm that N fixation rates were low to nonexistent, and therefore not important, in these ecosystems. We identify three major research themes to advance understanding of aquatic N fixation: 1) the biological diversity of diazotrophs and variability of N fixation rates, 2) the ecological stoichiometry of N fixation, and 3) the upscaling of N fixation rates from genes to ecosystems. Coordinating research across these areas will advance limnology and oceanography by fully integrating N fixation into ecological dynamics of aquatic ecosystems from local to global scales.

摘要

尽管固氮是全球氮循环的一个主要组成部分,并且在公海和陆地生态系统中已经得到了广泛研究,但对于连接陆地和海洋生物群落的内陆和沿海水生生态系统(湖泊、湿地、河流、溪流、河口),其固氮速率和生态动态实际上仍然未知。这是由于这些栖息地的多样性,以及传统观念认为这些生态系统中的固氮速率很低或不存在,因此不重要。我们确定了三个主要研究主题,以促进对水生固氮的理解:1)固氮微生物的生物多样性和固氮速率的变异性,2)固氮的生态化学计量,3)固氮速率从基因到生态系统的尺度放大。通过将固氮完全整合到从局部到全球尺度的水生生态系统的生态动态中,协调这些领域的研究将推动湖沼学和海洋学的发展。

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