scholarly journals Dark microbial CO2 fixation in temperate forest soils increases with CO2 concentration

Author(s):  
Marie Spohn ◽  
Karolin Müller ◽  
Carmen Höschen ◽  
Carsten W. Müller ◽  
Sven Marhan

<p>Dark, that is, nonphototrophic, microbial CO<sub>2</sub> fixation occurs in a large range of soils.<br>However, it is still not known whether dark microbial CO<sub>2</sub> fixation substantially contributes<br>to the C balance of soils and what factors control this process. Therefore,<br>the objective of this study was to quantitate dark microbial CO<sub>2</sub> fixation in temperate<br>forest soils, to determine the relationship between the soil CO<sub>2</sub> concentration and<br>dark microbial CO<sub>2</sub> fixation, and to estimate the relative contribution of different<br>microbial groups to dark CO<sub>2</sub> fixation. For this purpose, we conducted a <sup>13</sup>C-CO<sub>2</sub> labeling<br>experiment. We found that the rates of dark microbial CO<sub>2</sub> fixation were positively<br>correlated with the CO<sub>2</sub> concentration in all soils. Dark microbial CO<sub>2</sub> fixation<br>amounted to up to 320 μg C kg<sup>−1</sup> soil day<sup>−1</sup> in the Ah horizon. The fixation rates were<br>2.8–8.9 times higher in the Ah horizon than in the Bw1 horizon. Although the rates of<br>dark microbial fixation were small compared to the respiration rate (1.2%–3.9% of the<br>respiration rate), our findings suggest that organic matter formed by microorganisms<br>from CO<sub>2</sub> contributes to the soil organic matter pool, especially given that microbial<br>detritus is more stable in soil than plant detritus. Phospholipid fatty acid analyses<br>indicated that CO<sub>2</sub> was mostly fixed by gram-positive bacteria, and not by fungi. In<br>conclusion, our study shows that the dark microbial CO<sub>2</sub> fixation rate in temperate<br>forest soils increases in periods of high CO<sub>2</sub> concentrations, that dark microbial CO<sub>2</sub><br>fixation is mostly accomplished by gram-positive bacteria, and that dark microbial<br>CO<sub>2</sub> fixation contributes to the formation of soil organic matter.</p><p>Reference</p><p>Spohn M, Müller K, Höschen C, Mueller CW, Marhan S. Dark microbial CO<sub>2</sub> fixation in temperate forest soils increases with CO<sub>2</sub> concentration.<br>Glob Change Biol. 2019;00:1–10. https ://doi.org/10.1111/gcb.14937</p>

2017 ◽  
Vol 427 (1-2) ◽  
pp. 53-69 ◽  
Author(s):  
Simon Stahr ◽  
Markus Graf-Rosenfellner ◽  
Wantana Klysubun ◽  
Robert Mikutta ◽  
Jörg Prietzel ◽  
...  

2015 ◽  
Vol 124 (1-3) ◽  
pp. 273-290 ◽  
Author(s):  
Andreas Schindlbacher ◽  
Werner Borken ◽  
Ika Djukic ◽  
Christian Brandstätter ◽  
Christoph Spötl ◽  
...  

2018 ◽  
Vol 126 ◽  
pp. 22-30 ◽  
Author(s):  
Kazumichi Fujii ◽  
Takahiro Yamada ◽  
Chie Hayakawa ◽  
Asami Nakanishi ◽  
Shinya Funakawa

2012 ◽  
Vol 9 (8) ◽  
pp. 3013-3028 ◽  
Author(s):  
C. A. Sierra ◽  
S. E. Trumbore ◽  
E. A. Davidson ◽  
S. D. Frey ◽  
K. E. Savage ◽  
...  

Abstract. Representing the response of soil carbon dynamics to global environmental change requires the incorporation of multiple tools in the development of predictive models. An important tool to construct and test models is the incorporation of bomb radiocarbon in soil organic matter during the past decades. In this manuscript, we combined radiocarbon data and a previously developed empirical model to explore decade-scale soil carbon dynamics in a temperate forest ecosystem at the Harvard Forest, Massachusetts, USA. We evaluated the contribution of different soil C fractions to both total soil CO2 efflux and microbially respired C. We tested the performance of the model based on measurable soil organic matter fractions against a decade of radiocarbon measurements. The model was then challenged with radiocarbon measurements from a warming and N addition experiment to test multiple hypotheses about the different response of soil C fractions to the experimental manipulations. Our results showed that the empirical model satisfactorily predicts the trends of radiocarbon in litter, density fractions, and respired CO2 observed over a decade in the soils not subjected to manipulation. However, the model, modified with prescribed relationships for temperature and decomposition rates, predicted most but not all the observations from the field experiment where soil temperatures and nitrogen levels were increased, suggesting that a larger degree of complexity and mechanistic relations need to be added to the model to predict short-term responses and transient dynamics.


2018 ◽  
Vol 501 ◽  
pp. 86-94 ◽  
Author(s):  
Jun Jiang ◽  
Ying-Ping Wang ◽  
Mengxiao Yu ◽  
Nannan Cao ◽  
Junhua Yan

Author(s):  
Cecilia A Pérez ◽  
Martín R. Carmona ◽  
José M. Fariña ◽  
Juan J. Armesto

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