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Tropical Forest Soil Carbon Stocks Predicted by Nutrients and Roots, not Aboveground Plant Biomass
Published: January 02, 2018
Posted: January 31, 2018

Soil base cation availability regulates tropical soil carbon stocks via a negative relationship with fine root biomass.

The Science   
Scientists at the University of California, Los Angeles (UCLA), and the Smithsonian Institution conducted an extensive study of predictors of tropical soil carbon stocks to 1 m depth at 48 sites in Panama, including measurements of soil characteristics, plant biomass, and climate. The study revealed a nearly three-fold change in soil carbon stocks across five soil orders, with soil characteristics like fine root biomass, clay content, and nutrient base cations the strongest predictors of soil carbon stocks.

The Impact
Tropical forests are the most carbon rich ecosystems on Earth, containing 25% to 40% of global terrestrial carbon stocks. Quantification of aboveground biomass in tropical forests has improved recently, but soil carbon dynamics remains one of the largest sources of uncertainty in Earth system models. Including soil base cations in carbon cycle models, and thus emphasizing mechanistic links among nutrients, root biomass, and soil carbon stocks, will improve prediction of climate-soil feedbacks in tropical forests.

Summary
Overall, soil characteristics were the best predictors of soil carbon stocks, with no relationship to aboveground plant biomass or litterfall. The best fit model for the study's data suggested that available base cations provide an indirect control over tropical soil carbon stocks via a negative relationship with fine-root biomass. Soil clay content and rainfall also emerged as significant predictors of soil carbon. In addition to the nearly three-fold change in soil carbon stocks, the sites used here covered five soil orders, over 25 geological formations, a two-fold range in rainfall, a 20-fold range in base cations, and a 100-fold range in available phosphorus. Thus, although the data come from a relatively restricted geographic region, the diversity of environmental conditions means that the results are likely to be broadly applicable over much larger geographical ranges.

Contacts
BER Program Manager
Daniel Stover
Terrestrial Ecosystem Science, SC-23.1
Daniel.Stover@science.doe.gov (301-903-0289)

Principal Investigator
Daniela F Cusack
Assistant Professor, Department of Geography
University of California, Los Angeles
Los Angeles, CA 90095
dcusack@geog.ucla.edu

Funding
Funding was provided by the National Science Foundation (NSF) GSS Grant #BCS-1437591 and the U.S. Department of Energy (DOE) Office of Science Early Career Research Program Grant DE-SC0015898 to D. F. Cusack, and UK Research and Innovation's National Environment Research Council (NERC) Grant NE/J011169/1 to O. T. Lewis.

Publications
Cusack D.F. et al. “Soil carbon stocks across tropical forests of Panama regulated by base cation effects on fine roots.” Biogeochemistry 137, 253–66 (2018). [DOI:10.1007/s10533-017-0416-8]

Related Links
Complete data on location, rainfall, geology, soil, litterfall, aboveground and root biomass in 48 plots in central Panama, excel format

Topic Areas:

  • Research Area: Terrestrial Ecosystem Science
  • Research Area: Carbon Cycle, Nutrient Cycling
  • Cross-Cutting: Early Career

Division: SC-33.1 Earth and Environmental Sciences Division, BER

 

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