<sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study

Globally, peatlands have been recognized as important carbon sinks while only covering approximately 3% of the earth’s land surface. Root exudates are known key drivers of C cycling in soils and rhizosphere priming effects have been studied extensively in terrestrial ecosystems. Their role for decom...

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Main Authors: Raphael Müller, Andreas Maier, Erich Inselsbacher, Robert Peticzka, Gang Wang, Stephan Glatzel
Format: Article
Language:English
Published: MDPI AG 2022-09-01
Series:Diversity
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Online Access:https://www.mdpi.com/1424-2818/14/9/735
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author Raphael Müller
Andreas Maier
Erich Inselsbacher
Robert Peticzka
Gang Wang
Stephan Glatzel
author_facet Raphael Müller
Andreas Maier
Erich Inselsbacher
Robert Peticzka
Gang Wang
Stephan Glatzel
author_sort Raphael Müller
collection DOAJ
description Globally, peatlands have been recognized as important carbon sinks while only covering approximately 3% of the earth’s land surface. Root exudates are known key drivers of C cycling in soils and rhizosphere priming effects have been studied extensively in terrestrial ecosystems. Their role for decomposition of peat still remains unclear, as little research about their fate and potential priming effects in peat exists. In this study, we aimed to evaluate pathways of root exudates and their short-term priming effects by daily determination of stable carbon isotope fluxes of <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub></mrow></semantics></math></inline-formula> and <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>H</mi><mn>4</mn></msub></mrow></semantics></math></inline-formula>. As the drainage of peatlands strongly alters processes of decomposition, we included measurements after drainage as well. Results revealed the immediate respiration of root exudates in peat, mainly as <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub></mrow></semantics></math></inline-formula>, while <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>H</mi><mn>4</mn></msub></mrow></semantics></math></inline-formula> release was associated with a lag time of several days. However, the largest proportion of added root exudates remained in the solid and liquid phase of peat. In conclusion, our findings suggest that no priming occurred as added substrates remained immobile in peat.
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spelling doaj.art-8403af4f566e4d02a9f4f9d7965ed1072023-11-23T15:52:42ZengMDPI AGDiversity1424-28182022-09-0114973510.3390/d14090735<sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm StudyRaphael Müller0Andreas Maier1Erich Inselsbacher2Robert Peticzka3Gang Wang4Stephan Glatzel5Department of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaDepartment of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaDepartment of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaDepartment of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaDepartment of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaDepartment of Geography and Regional Research, Geoecology, Faculty of Earth Sciences, Geography and Astronomy, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, AustriaGlobally, peatlands have been recognized as important carbon sinks while only covering approximately 3% of the earth’s land surface. Root exudates are known key drivers of C cycling in soils and rhizosphere priming effects have been studied extensively in terrestrial ecosystems. Their role for decomposition of peat still remains unclear, as little research about their fate and potential priming effects in peat exists. In this study, we aimed to evaluate pathways of root exudates and their short-term priming effects by daily determination of stable carbon isotope fluxes of <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub></mrow></semantics></math></inline-formula> and <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>H</mi><mn>4</mn></msub></mrow></semantics></math></inline-formula>. As the drainage of peatlands strongly alters processes of decomposition, we included measurements after drainage as well. Results revealed the immediate respiration of root exudates in peat, mainly as <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub></mrow></semantics></math></inline-formula>, while <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>C</mi><msub><mi>H</mi><mn>4</mn></msub></mrow></semantics></math></inline-formula> release was associated with a lag time of several days. However, the largest proportion of added root exudates remained in the solid and liquid phase of peat. In conclusion, our findings suggest that no priming occurred as added substrates remained immobile in peat.https://www.mdpi.com/1424-2818/14/9/735root exudatespriming effectpeat<i>CO</i><sub>2</sub><i>CH</i><sub>4</sub>stable carbon isotopes
spellingShingle Raphael Müller
Andreas Maier
Erich Inselsbacher
Robert Peticzka
Gang Wang
Stephan Glatzel
<sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
Diversity
root exudates
priming effect
peat
<i>CO</i><sub>2</sub>
<i>CH</i><sub>4</sub>
stable carbon isotopes
title <sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
title_full <sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
title_fullStr <sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
title_full_unstemmed <sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
title_short <sup>13</sup>C-Labeled Artificial Root Exudates Are Immediately Respired in a Peat Mesocosm Study
title_sort sup 13 sup c labeled artificial root exudates are immediately respired in a peat mesocosm study
topic root exudates
priming effect
peat
<i>CO</i><sub>2</sub>
<i>CH</i><sub>4</sub>
stable carbon isotopes
url https://www.mdpi.com/1424-2818/14/9/735
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