Warming can boost denitrification disproportionately due to altered oxygen dynamics.

BACKGROUND: Global warming and the alteration of the global nitrogen cycle are major anthropogenic threats to the environment. Denitrification, the biological conversion of nitrate to gaseous nitrogen, removes a substantial fraction of the nitrogen from aquatic ecosystems, and can therefore help to...

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Main Authors: Annelies J Veraart, Jeroen J M de Klein, Marten Scheffer
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2011-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3069112?pdf=render
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spelling doaj-1a3d5e61b3f44bdda092857cc31d39bb2020-11-25T01:44:56ZengPublic Library of Science (PLoS)PLoS ONE1932-62032011-01-0163e1850810.1371/journal.pone.0018508Warming can boost denitrification disproportionately due to altered oxygen dynamics.Annelies J VeraartJeroen J M de KleinMarten SchefferBACKGROUND: Global warming and the alteration of the global nitrogen cycle are major anthropogenic threats to the environment. Denitrification, the biological conversion of nitrate to gaseous nitrogen, removes a substantial fraction of the nitrogen from aquatic ecosystems, and can therefore help to reduce eutrophication effects. However, potential responses of denitrification to warming are poorly understood. Although several studies have reported increased denitrification rates with rising temperature, the impact of temperature on denitrification seems to vary widely between systems. METHODOLOGY/PRINCIPAL FINDINGS: We explored the effects of warming on denitrification rates using microcosm experiments, field measurements and a simple model approach. Our results suggest that a three degree temperature rise will double denitrification rates. By performing experiments at fixed oxygen concentrations as well as with oxygen concentrations varying freely with temperature, we demonstrate that this strong temperature dependence of denitrification can be explained by a systematic decrease of oxygen concentrations with rising temperature. Warming decreases oxygen concentrations due to reduced solubility, and more importantly, because respiration rates rise more steeply with temperature than photosynthesis. CONCLUSIONS/SIGNIFICANCE: Our results show that denitrification rates in aquatic ecosystems are strongly temperature dependent, and that this is amplified by the temperature dependencies of photosynthesis and respiration. Our results illustrate the broader phenomenon that coupling of temperature dependent reactions may in some situations strongly alter overall effects of temperature on ecological processes.http://europepmc.org/articles/PMC3069112?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Annelies J Veraart
Jeroen J M de Klein
Marten Scheffer
spellingShingle Annelies J Veraart
Jeroen J M de Klein
Marten Scheffer
Warming can boost denitrification disproportionately due to altered oxygen dynamics.
PLoS ONE
author_facet Annelies J Veraart
Jeroen J M de Klein
Marten Scheffer
author_sort Annelies J Veraart
title Warming can boost denitrification disproportionately due to altered oxygen dynamics.
title_short Warming can boost denitrification disproportionately due to altered oxygen dynamics.
title_full Warming can boost denitrification disproportionately due to altered oxygen dynamics.
title_fullStr Warming can boost denitrification disproportionately due to altered oxygen dynamics.
title_full_unstemmed Warming can boost denitrification disproportionately due to altered oxygen dynamics.
title_sort warming can boost denitrification disproportionately due to altered oxygen dynamics.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2011-01-01
description BACKGROUND: Global warming and the alteration of the global nitrogen cycle are major anthropogenic threats to the environment. Denitrification, the biological conversion of nitrate to gaseous nitrogen, removes a substantial fraction of the nitrogen from aquatic ecosystems, and can therefore help to reduce eutrophication effects. However, potential responses of denitrification to warming are poorly understood. Although several studies have reported increased denitrification rates with rising temperature, the impact of temperature on denitrification seems to vary widely between systems. METHODOLOGY/PRINCIPAL FINDINGS: We explored the effects of warming on denitrification rates using microcosm experiments, field measurements and a simple model approach. Our results suggest that a three degree temperature rise will double denitrification rates. By performing experiments at fixed oxygen concentrations as well as with oxygen concentrations varying freely with temperature, we demonstrate that this strong temperature dependence of denitrification can be explained by a systematic decrease of oxygen concentrations with rising temperature. Warming decreases oxygen concentrations due to reduced solubility, and more importantly, because respiration rates rise more steeply with temperature than photosynthesis. CONCLUSIONS/SIGNIFICANCE: Our results show that denitrification rates in aquatic ecosystems are strongly temperature dependent, and that this is amplified by the temperature dependencies of photosynthesis and respiration. Our results illustrate the broader phenomenon that coupling of temperature dependent reactions may in some situations strongly alter overall effects of temperature on ecological processes.
url http://europepmc.org/articles/PMC3069112?pdf=render
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