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由磷和钼共同决定的热带雨林冠层微生物组的快速固氮作用。

Rapid nitrogen fixation by canopy microbiome in tropical forest determined by both phosphorus and molybdenum.

机构信息

Department of Ecology and Evolutionary Biology, Princeton University, Princeton, New Jersey, 08544, USA.

Department of Ecology, Evolution and Behavior, University of Minnesota-Twin Cities, Saint Paul, Minnesota, 55108, USA.

出版信息

Ecology. 2019 Sep;100(9):e02795. doi: 10.1002/ecy.2795. Epub 2019 Jul 30.

Abstract

Biological nitrogen fixation is critical for the nitrogen cycle of tropical forests, yet we know little about the factors that control the microbial nitrogen fixers that colonize the microbiome of leaves and branches that make up a forest canopy. Forest canopies are especially prone to nutrient limitation because they are (1) disconnected from soil nutrient pools and (2) often subject to leaching. Earlier studies have suggested a role of phosphorus and molybdenum in controlling biological N-fixation rates, but experimental confirmation has hitherto been unavailable. Here we present the results of a manipulation of canopy nutrient availability. Our findings demonstrate a primary role of phosphorus in constraining overall N fixation by canopy cyanobacteria, but also a secondary role of molybdenum in determining per-cell fixation rates. A conservative evaluation suggests that canopy fixation can contribute to significant N fluxes at the ecosystem level, especially as bursts following atmospheric inputs of nutrient-rich dust.

摘要

生物固氮对热带森林的氮循环至关重要,但我们对控制定殖于构成森林冠层的叶片和树枝微生物组的微生物固氮体的因素知之甚少。由于树冠(1)与土壤养分库隔绝,(2)经常受到淋洗,因此特别容易受到养分限制。早期的研究表明,磷和钼在控制生物固氮速率方面起着重要作用,但迄今尚无实验证实。在这里,我们提出了对树冠养分可利用性进行操纵的结果。我们的研究结果表明,磷在限制冠层蓝细菌的整体氮固定中起着主要作用,但钼在决定每个细胞的固定速率方面也起着次要作用。保守评估表明,树冠固定可以在生态系统水平上产生显著的氮通量,尤其是在富含营养的尘埃大气输入后的爆发期间。

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