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Title: Enhanced decomposition of stable soil organic carbon and microbial catabolic potentials by long-term field warming

Abstract

Quantifying soil organic carbon (SOC) decomposition under warming is critical to predict carbon–climate feedbacks. According to the substrate regulating principle, SOC decomposition would decrease as labile SOC declines under field warming, but observations of SOC decomposition under warming do not always support this prediction. This discrepancy could result from varying changes in SOC components and soil microbial communities under warming. This study aimed to determine the decomposition of SOC components with different turnover times after subjected to long-term field warming and/or root exclusion to limit C input, and to test whether SOC decomposition is driven by substrate lability under warming. Taking advantage of a 12-year field warming experiment in a prairie, we assessed the decomposition of SOC components by incubating soils from control and warmed plots, with and without root exclusion for 3 years. We assayed SOC decomposition from these incubations by combining inverse modeling and microbial functional genes during decomposition with a metagenomic technique (GeoChip). The decomposition of SOC components with turnover times of years and decades, which contributed to 95% of total cumulative CO 2 respiration, was greater in soils from warmed plots. But the decomposition of labile SOC was similar in warmed plots compared to the control.more » The diversity of C-degradation microbial genes generally declined with time during the incubation in all treatments, suggesting shifts of microbial functional groups as substrate composition was changing. Compared to the control, soils from warmed plots showed significant increase in the signal intensities of microbial genes involved in degrading complex organic compounds, implying enhanced potential abilities of microbial catabolism. These are likely responsible for accelerated decomposition of SOC components with slow turnover rates. Overall, the shifted microbial community induced by long-term warming accelerates the decomposition of SOC components with slow turnover rates and thus amplify the positive feedback to climate change.« less

Authors:
ORCiD logo [1];  [2];  [3];  [3];  [4];  [3];  [5];  [3];  [3];  [6];  [7];  [7];  [3]
  1. Chinese Academy of Agricultural Sciences, Beijing (China); Univ. of Oklahoma, Norman, OK (United States)
  2. Univ. of Oklahoma, Norman, OK (United States); Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
  3. Univ. of Oklahoma, Norman, OK (United States)
  4. Center for Ecological and Environmental Sciences, Northwestern Polytechnical University, Xi'an China
  5. Chinese Academy of Agricultural Sciences, Beijing (China)
  6. Univ. of Florida, Gainesville, FL (United States)
  7. Northern Arizona Univ., Flagstaff, AZ (United States)
Publication Date:
Research Org.:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States); Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1394428
Alternate Identifier(s):
OSTI ID: 1479341
Grant/Contract Number:  
AC05-00OR22725; AC02-05CH11231
Resource Type:
Accepted Manuscript
Journal Name:
Global Change Biology
Additional Journal Information:
Journal Volume: 23; Journal Issue: 11; Journal ID: ISSN 1354-1013
Publisher:
Wiley
Country of Publication:
United States
Language:
English
Subject:
59 BASIC BIOLOGICAL SCIENCES; diversity; Geochip; incubation; inverse modeling; long‐term warming; metagenomics; microbial community; soil organic carbon; turnover

Citation Formats

Feng, Wenting, Liang, Junyi, Hale, Lauren E., Jung, Chang Gyo, Chen, Ji, Zhou, Jizhong, Xu, Minggang, Yuan, Mengting, Wu, Liyou, Bracho, Rosvel, Pegoraro, Elaine, Schuur, Edward A. G., and Luo, Yiqi. Enhanced decomposition of stable soil organic carbon and microbial catabolic potentials by long-term field warming. United States: N. p., 2017. Web. doi:10.1111/gcb.13755.
Feng, Wenting, Liang, Junyi, Hale, Lauren E., Jung, Chang Gyo, Chen, Ji, Zhou, Jizhong, Xu, Minggang, Yuan, Mengting, Wu, Liyou, Bracho, Rosvel, Pegoraro, Elaine, Schuur, Edward A. G., & Luo, Yiqi. Enhanced decomposition of stable soil organic carbon and microbial catabolic potentials by long-term field warming. United States. doi:10.1111/gcb.13755.
Feng, Wenting, Liang, Junyi, Hale, Lauren E., Jung, Chang Gyo, Chen, Ji, Zhou, Jizhong, Xu, Minggang, Yuan, Mengting, Wu, Liyou, Bracho, Rosvel, Pegoraro, Elaine, Schuur, Edward A. G., and Luo, Yiqi. Fri . "Enhanced decomposition of stable soil organic carbon and microbial catabolic potentials by long-term field warming". United States. doi:10.1111/gcb.13755. https://www.osti.gov/servlets/purl/1394428.
@article{osti_1394428,
title = {Enhanced decomposition of stable soil organic carbon and microbial catabolic potentials by long-term field warming},
author = {Feng, Wenting and Liang, Junyi and Hale, Lauren E. and Jung, Chang Gyo and Chen, Ji and Zhou, Jizhong and Xu, Minggang and Yuan, Mengting and Wu, Liyou and Bracho, Rosvel and Pegoraro, Elaine and Schuur, Edward A. G. and Luo, Yiqi},
abstractNote = {Quantifying soil organic carbon (SOC) decomposition under warming is critical to predict carbon–climate feedbacks. According to the substrate regulating principle, SOC decomposition would decrease as labile SOC declines under field warming, but observations of SOC decomposition under warming do not always support this prediction. This discrepancy could result from varying changes in SOC components and soil microbial communities under warming. This study aimed to determine the decomposition of SOC components with different turnover times after subjected to long-term field warming and/or root exclusion to limit C input, and to test whether SOC decomposition is driven by substrate lability under warming. Taking advantage of a 12-year field warming experiment in a prairie, we assessed the decomposition of SOC components by incubating soils from control and warmed plots, with and without root exclusion for 3 years. We assayed SOC decomposition from these incubations by combining inverse modeling and microbial functional genes during decomposition with a metagenomic technique (GeoChip). The decomposition of SOC components with turnover times of years and decades, which contributed to 95% of total cumulative CO2 respiration, was greater in soils from warmed plots. But the decomposition of labile SOC was similar in warmed plots compared to the control. The diversity of C-degradation microbial genes generally declined with time during the incubation in all treatments, suggesting shifts of microbial functional groups as substrate composition was changing. Compared to the control, soils from warmed plots showed significant increase in the signal intensities of microbial genes involved in degrading complex organic compounds, implying enhanced potential abilities of microbial catabolism. These are likely responsible for accelerated decomposition of SOC components with slow turnover rates. Overall, the shifted microbial community induced by long-term warming accelerates the decomposition of SOC components with slow turnover rates and thus amplify the positive feedback to climate change.},
doi = {10.1111/gcb.13755},
journal = {Global Change Biology},
number = 11,
volume = 23,
place = {United States},
year = {2017},
month = {6}
}

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Free Publicly Available Full Text
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Cited by: 9 works
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Figures / Tables:

FIGURE 1 FIGURE 1: Cumulative CO2 respiration of soils from the four field treatments over the 3-year laboratory incubation. CI: control + intact soil; WI: warm + intact soil; CC: control + collar soil; WC: warm + collar soil. Data are mean ± SE (n = 6)

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    Figures/Tables have been extracted from DOE-funded journal article accepted manuscripts.