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Title: Microbial dynamics and soil physicochemical properties explain large-scale variations in soil organic carbon

Journal Article · · Global Change Biology
DOI:https://doi.org/10.1111/gcb.14994· OSTI ID:1863825
ORCiD logo [1];  [2];  [3];  [4]; ORCiD logo [5];  [4];  [4]; ORCiD logo [4];  [6]; ORCiD logo [7];  [8];  [9]; ORCiD logo [10];  [10]
  1. Le Laboratoire des Sciences du Climat et de l’Environnement, Gif‐sur‐Yvette (France); Univ. Libre de Bruxelles (Belgium)
  2. Le Laboratoire des Sciences du Climat et de l’Environnement, Gif‐sur‐Yvette (France); Univ. of Augsburg (Germany)
  3. CSIRO Oceans and Atmosphere, Aspendale (Australia)
  4. Le Laboratoire des Sciences du Climat et de l’Environnement, Gif‐sur‐Yvette (France)
  5. National Center for Atmospheric Research (NCAR), Boulder, CO (United States); Univ. of Colorado, Boulder, CO (United States)
  6. Thünen Inst. of Forest Ecosystems, Eberswalde (Germany)
  7. Curtin Univ., Perth, WA (Australia)
  8. PSL Research Univ., Paris (France)
  9. Univ. Paris‐Saclay, Thiverval‐Grignon (France)
  10. Chinese Academy of Sciences, Guangzhou (China)

Abstract First‐order organic matter decomposition models are used within most Earth System Models (ESMs) to project future global carbon cycling; these models have been criticized for not accurately representing mechanisms of soil organic carbon (SOC) stabilization and SOC response to climate change. New soil biogeochemical models have been developed, but their evaluation is limited to observations from laboratory incubations or few field experiments. Given the global scope of ESMs, a comprehensive evaluation of such models is essential using in situ observations of a wide range of SOC stocks over large spatial scales before their introduction to ESMs. In this study, we collected a set of in situ observations of SOC, litterfall and soil properties from 206 sites covering different forest and soil types in Europe and China. These data were used to calibrate the model MIMICS (The MIcrobial‐MIneral Carbon Stabilization model), which we compared to the widely used first‐order model CENTURY. We show that, compared to CENTURY, MIMICS more accurately estimates forest SOC concentrations and the sensitivities of SOC to variation in soil temperature, clay content and litter input. The ratios of microbial biomass to total SOC predicted by MIMICS agree well with independent observations from globally distributed forest sites. By testing different hypotheses regarding (using alternative process representations) the physicochemical constraints on SOC deprotection and microbial turnover in MIMICS, the errors of simulated SOC concentrations across sites were further decreased. We show that MIMICS can resolve the dominant mechanisms of SOC decomposition and stabilization and that it can be a reliable tool for predictions of terrestrial SOC dynamics under future climate change. It also allows us to evaluate at large scale the rapidly evolving understanding of SOC formation and stabilization based on laboratory and limited filed observation.

Research Organization:
Cornell Univ., Ithaca, NY (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
SC0016364; DE‐SC0016364
OSTI ID:
1863825
Alternate ID(s):
OSTI ID: 1599240
Journal Information:
Global Change Biology, Vol. 26, Issue 4; ISSN 1354-1013
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 42 works
Citation information provided by
Web of Science

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