Department of Biological Sciences and Wrigley Institute for Environmental Studies, University of Southern California, Los Angeles, California 90089, USA.
Nat Rev Microbiol. 2011 Jun 16;9(7):499-508. doi: 10.1038/nrmicro2594.
Biological N(2) fixation is an important part of the marine nitrogen cycle as it provides a source of new nitrogen that can support biological carbon export and sequestration. Research in the past decade has focused on determining the patterns of distribution and abundance of diazotrophs, defining the environmental features leading to these patterns and characterizing the factors that constrain marine N(2) fixation overall. In this Review, we describe how variations in the deposition of iron from dust to different ocean basins affects the limiting nutrient for N(2) fixation and the distribution of different diazotrophic species. However, many questions remain about marine N(2) fixation, including the role of temperature, fixed nitrogen species, CO(2) and physical forcing in controlling N(2) fixation, as well as the potential for heterotrophic N(2) fixation.
生物固氮是海洋氮循环的重要组成部分,因为它提供了一种新的氮源,可以支持生物碳的输出和封存。过去十年的研究重点是确定固氮菌的分布和丰度模式,确定导致这些模式的环境特征,并描述限制海洋固氮的总体因素。在这篇综述中,我们描述了从尘埃到不同海洋盆地的铁沉积变化如何影响固氮的限制营养物和不同固氮物种的分布。然而,关于海洋固氮仍有许多问题有待解决,包括温度、固定氮物种、二氧化碳和物理强迫在控制固氮中的作用,以及异养固氮的潜力。