High denitrification and anaerobic ammonium oxidation contributes to net nitrogen loss in a seagrass ecosystem in the central Red Sea

<p>Nitrogen loads in coastal areas have increased dramatically, with detrimental consequences for coastal ecosystems. Shallow sediments and seagrass meadows are hotspots for denitrification, favoring N loss. However, atmospheric dinitrogen (<span class="inline-formula">N<sub...

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Bibliographic Details
Main Authors: N. Garcias-Bonet, M. Fusi, M. Ali, D. R. Shaw, P. E. Saikaly, D. Daffonchio, C. M. Duarte
Format: Article
Language:English
Published: Copernicus Publications 2018-12-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/15/7333/2018/bg-15-7333-2018.pdf
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Summary:<p>Nitrogen loads in coastal areas have increased dramatically, with detrimental consequences for coastal ecosystems. Shallow sediments and seagrass meadows are hotspots for denitrification, favoring N loss. However, atmospheric dinitrogen (<span class="inline-formula">N<sub>2</sub></span>) fixation has been reported to support seagrass growth. Therefore, the role of coastal marine systems dominated by seagrasses in the net <span class="inline-formula">N<sub>2</sub></span> flux remains unclear. Here, we measured denitrification, anaerobic ammonium oxidation (anammox), and <span class="inline-formula">N<sub>2</sub></span> fixation in a tropical seagrass (<i>Enhalus acoroides</i>) meadow and the adjacent bare sediment in a coastal lagoon in the central Red Sea. We detected high annual mean rates of denitrification (<span class="inline-formula">34.9±10.3</span> and <span class="inline-formula">31.6±8.9</span>&thinsp;mg&thinsp;N&thinsp;m<span class="inline-formula"><sup>−2</sup></span>&thinsp;d<span class="inline-formula"><sup>−1</sup></span>) and anammox (<span class="inline-formula">12.4±3.4</span> and <span class="inline-formula">19.8±4.4</span>&thinsp;mg&thinsp;N&thinsp;m<span class="inline-formula"><sup>−2</sup></span>&thinsp;d<span class="inline-formula"><sup>−1</sup></span>) in vegetated and bare sediments. The annual mean N loss was higher (between 8 and 63-fold) than the <span class="inline-formula">N<sub>2</sub></span> fixed (annual mean&thinsp;<span class="inline-formula">=</span>&thinsp;<span class="inline-formula">5.9±0.2</span> and <span class="inline-formula">0.8±0.3</span>&thinsp;mg&thinsp;N&thinsp;m<span class="inline-formula"><sup>−2</sup></span>&thinsp;d<span class="inline-formula"><sup>−1</sup></span>) in the meadow and bare sediment, leading to a net flux of <span class="inline-formula">N<sub>2</sub></span> from sediments to the atmosphere. Despite the importance of this coastal lagoon in removing N from the system, <span class="inline-formula">N<sub>2</sub></span> fixation can contribute substantially to seagrass growth since <span class="inline-formula">N<sub>2</sub></span> fixation rates found here could contribute up to 36&thinsp;% of plant N requirements. In vegetated sediments, anammox rates decreased with increasing organic matter (OM) content, while <span class="inline-formula">N<sub>2</sub></span> fixation increased with OM content. Denitrification and anammox increased linearly with temperature, while <span class="inline-formula">N<sub>2</sub></span> fixation showed a maximum at intermediate temperatures. Therefore, the forecasted warming could further increase the <span class="inline-formula">N<sub>2</sub></span> flux from sediments to the atmosphere, potentially impacting seagrass productivity and their capacity to mitigate climate change but also enhancing their potential N removal.</p>
ISSN:1726-4170
1726-4189