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Biological Nitrogen Fixation in Two Tropical Forests: Ecosystem-Level Patterns and Effects of Nitrogen Fertilization

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TLDR
In this article, the authors estimated inputs of N via BNF by free-living microbes for two tropical forests in Puerto Rico, and assessed the response to increased N availability using an on-going N fertilization experiment.
Abstract
Humid tropical forests are often characterized by large nitrogen (N) pools, and are known to have large potential N losses. Although rarely measured, tropical forests likely maintain considerable biological N fixation (BNF) to balance N losses. We estimated inputs of N via BNF by free-living microbes for two tropical forests in Puerto Rico, and assessed the response to increased N availability using an on-going N fertilization experiment. Nitrogenase activity was measured across forest strata, including the soil, forest floor, mosses, canopy epiphylls, and lichens using acetylene (C2H2) reduction assays. BNF varied significantly among ecosystem compartments in both forests. Mosses had the highest rates of nitrogenase activity per gram of sample, with 11 ± 6 nmol C2H2 reduced/g dry weight/h (mean ± SE) in a lower elevation forest, and 6 ± 1 nmol C2H2/g/h in an upper elevation forest. We calculated potential N fluxes via BNF to each forest compartment using surveys of standing stocks. Soils and mosses provided the largest potential inputs of N via BNF to these ecosystems. Summing all components, total background BNF inputs were 120 ± 29 μg N/m2/h in the lower elevation forest, and 95 ± 15 μg N/m2/h in the upper elevation forest, with added N significantly suppressing BNF in soils and forest floor. Moisture content was significantly positively correlated with BNF rates for soils and the forest floor. We conclude that BNF is an active biological process across forest strata for these tropical forests, and is likely to be sensitive to increases in N deposition in tropical regions.

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Community and ecosystem responses to elevational gradients: processes, mechanisms and insights for global change

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Linking N2O emissions from biochar-amended soil to the structure and function of the N-cycling microbial community

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Functional Ecology of Free-Living Nitrogen Fixation: A Contemporary Perspective

TL;DR: It is shown that recent research and analytical advances have generated a wealth of new information that provides novel insight into the ecology of N2 fixation as well as raises new questions and priorities for future work.
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Nutrition of mangroves

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References
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Journal ArticleDOI

Nitrogen cycles: past, present, and future

TL;DR: In this paper, the authors compared the natural and anthropogenic controls on the conversion of unreactive N2 to more reactive forms of nitrogen (Nr) and found that human activities increasingly dominate the N budget at the global and at most regional scales, and the terrestrial and open ocean N budgets are essentially dis-connected.
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The Acetylene-Ethylene Assay for N2 Fixation: Laboratory and Field Evaluation

TL;DR: This assay was successfully applied to measurements of N(2) fixation by other symbionts and by free living soil microorganisms, and was also used to assess the effects of light and temperature on the N( 2) fixing activity of soybeans.
Journal ArticleDOI

Nutrient cycling in moist tropical forest

TL;DR: Variations in mineral cycling nonetheless follow coherent, explicable patterns in tropical forests, and the cycling of nitrogen, phosphorus, potassium, calcium, and magnesium are the best-studied soil-derived nutrients, and they are the nutrients most likely to limit primary production and other ecosystem functions.
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