Gene-informed decomposition model predicts lower soil carbon loss due to persistent microbial adaptation to warming

Autor: Renmao Tian, Jiajie Feng, Aifen Zhou, Zhili He, Qun Gao, Xishu Zhou, James R. Cole, Jizhong Zhou, Linwei Wu, Gangsheng Wang, Feifei Liu, Liyou Wu, Chang Gyo Jung, Lauren Hale, Zhou Shi, Lifen Jiang, Daliang Ning, Joy D. Van Nostrand, Edward A. G. Schuur, James M. Tiedje, Dejun Li, Konstantinos T. Konstantinidis, Arthur Escalas, Xue Guo, C. Ryan Penton, Yiqi Luo, Lijun Chen, Bo Wu, Mengting Yuan, Xueduan Liu, Shuli Niu, Xia Xu, Yunfeng Yang
Jazyk: angličtina
Rok vydání: 2020
Předmět:
Hot Temperature
010504 meteorology & atmospheric sciences
Acclimatization
Microbial metabolism
General Physics and Astronomy
01 natural sciences
Global Warming
Plant Roots
Soil respiration
Microbial ecology
Soil
Models
lcsh:Science
Soil Microbiology
Multidisciplinary
Ecology
Microbiota
Soil chemistry
04 agricultural and veterinary sciences
Carbon cycle
Grassland
Soil microbiology
Science
Environmental DNA
Poaceae
complex mixtures
General Biochemistry
Genetics and Molecular Biology

Article
Carbon Cycle
Environmental
Genetic
Ecosystem
Cellulose
0105 earth and related environmental sciences
Ecological modelling
Bacteria
Models
Genetic

Global warming
Fungi
General Chemistry
Soil carbon
DNA
Archaea
DNA
Environmental

Carbon
Climate Action
040103 agronomy & agriculture
0401 agriculture
forestry
and fisheries

Environmental science
Metagenome
lcsh:Q
Metagenomics
Zdroj: Nature Communications, Vol 11, Iss 1, Pp 1-12 (2020)
Nature Communications
Nature communications, vol 11, iss 1
ISSN: 2041-1723
DOI: 10.1038/s41467-020-18706-z
Popis: Soil microbial respiration is an important source of uncertainty in projecting future climate and carbon (C) cycle feedbacks. However, its feedbacks to climate warming and underlying microbial mechanisms are still poorly understood. Here we show that the temperature sensitivity of soil microbial respiration (Q10) in a temperate grassland ecosystem persistently decreases by 12.0 ± 3.7% across 7 years of warming. Also, the shifts of microbial communities play critical roles in regulating thermal adaptation of soil respiration. Incorporating microbial functional gene abundance data into a microbially-enabled ecosystem model significantly improves the modeling performance of soil microbial respiration by 5–19%, and reduces model parametric uncertainty by 55–71%. In addition, modeling analyses show that the microbial thermal adaptation can lead to considerably less heterotrophic respiration (11.6 ± 7.5%), and hence less soil C loss. If such microbially mediated dampening effects occur generally across different spatial and temporal scales, the potential positive feedback of soil microbial respiration in response to climate warming may be less than previously predicted.
Mechanisms and consequences of the acclimation of soil respiration to warming are unclear. Here, the authors combine soil respiration, metagenomics, and functional gene results from a 7-year grassland warming experiment to a microbial-enzyme decomposition model, showing functional gene information to lower uncertainty and improve fit.
Databáze: OpenAIRE