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Molybdenum limitation of asymbiotic nitrogen fixation in tropical forest soils

机译:热带森林土壤中非共生固氮的钼限制

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Nitrogen fixation, the biological conversion of di-nitrogen to plant-available ammonium, is the primary natural input of nitrogen to ecosystems(1), and influences plant growth and carbon exchange at local to global scales(2-6). The role of this process in tropical forests is of particular concern, as these ecosystems harbour abundant nitrogen-fixing organisms(1,4) and represent one third of terrestrial primary production(4,7,8). Here we show that the micronutrient molybdenum, a cofactor in the nitrogen-fixing enzyme nitrogenase, limits nitrogen fixation by free-living heterotrophic bacteria in soils of lowland Panamanian forests. We measured the fixation response to long-term nutrient manipulations in intact forests, and to short-term manipulations in soil microcosms. Nitrogen fixation increased sharply in treatments of molybdenum alone, in micronutrient treatments that included molybdenum by design and in treatments with commercial phosphorus fertilizer, in which molybdenum was a 'hidden' contaminant. Fixation did not respond to additions of phosphorus that were not contaminated by molybdenum. Our findings show that molybdenum alone can limit asymbiotic nitrogen fixation in tropical forests and raise new questions about the role of molybdenum and phosphorus in the tropical nitrogen cycle. We suggest that molybdenum limitation may be common in highly weathered acidic soils, and may constrain the ability of some forests to acquire new nitrogen in response to CO2 fertilization(9).
机译:固氮是将氮从生物态转化为植物可用的铵态氮的生物转化,是生态系统中氮的主要自然输入(1),并在局部到全球范围内影响植物的生长和碳交换(2-6)。这一过程在热带森林中的作用尤其令人关注,因为这些生态系统具有丰富的固氮生物(1,4),占陆地初级生产的三分之一(4,7,8)。在这里,我们显示微量营养素钼,固氮酶固氮酶中的辅助因子,通过低地巴拿马森林土壤中的自由生活异养细菌限制固氮。我们测量了对完整森林中长期养分操纵以及对土壤微观世界中短期操纵的固定反应。在单独的钼处理中,在设计包括钼的微量营养物处理中以及在钼是“隐性”污染物的商业化磷肥处理中,固氮作用都急剧增加。固色对未被钼污染的磷的添加没有反应。我们的研究结果表明,仅钼就可以限制热带森林中非共生性固氮作用,并提出有关钼和磷在热带氮循环中的作用的新问题。我们建议钼的限制可能在高度风化的酸性土壤中很常见,并且可能会限制某些森林响应CO2施肥而获得新氮的能力(9)。

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