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April 1, 2000Ecological Applications

The Vertical Distribution of Soil Organic Carbon and Its Relation to Climate and Vegetation

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Authors

EJEstéban G. JobbágyConsejo Nacional de Investigaciones Científicas y TécnicasRJRobert B. JacksonBrigham Young University

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Implication

Global database analysis reveals plant functional types and clay content govern vertical soil organic carbon storage, highlighting deeper soil layers for carbon sequestration strategies.

Key Points

  • To determine how climate, soil texture, and plant functional types influence the vertical distribution of soil organic carbon and to calculate global carbon storage down to a depth of three meters.
  • Analyzed mineral soil layers across global profiles (N > 2700) sourced from three worldwide databases matched with climate, vegetation, and land-use data.
  • Evaluated vertical soil organic carbon (SOC) depth patterns across shrublands, grasslands, and forests while controlling for climate ranges.
  • Relative SOC depth distribution in the upper 20 cm compared to the first meter averaged 33% in shrublands, 42% in grasslands, and 50% in forests, consistently remaining deepest in shrublands across all climates (P < 0.05).
  • Total SOC content increased with precipitation and clay content but decreased with temperature, with climatic variables dominating shallow soil and clay content dominating deeper horizons.
  • Global SOC storage to 3 m depth was calculated at 2344 Pg C (56% higher than the top meter's 1502 Pg C), containing 491 Pg C and 351 Pg C in the second and third meters, respectively.

Cite This Study

Jobbágy et al. (2000) studied this question.

synapsesocial.com/papers/69d89b7233ca018b39ae3c65https://doi.org/10.1890/1051-0761(2000)010[0423:tvdoso]2.0.co;2
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