Chilean Grassland Gradient

Samples of mineral topsoils from a 2300 km long gradient of Chilean grasslands help us to address questions surrounding the dynamics of soil organic matter (SOM).

  • How and why does SOM accumulate?
  • How does soil microbial community composition link to SOM quantity and quality?
  • How do SOM and microbial community composition link with soil functioning?
Enlarged view: Grassland gradient chile
Grassland gradient Chile (Daniel Wasner)

      

The gradient allows to link soil microbial processes and SOM quantity and quality with soil physicochemical properties, which are shaped over long time scales in the course of soil formation. The sampling was designed to maximize climatic and soil physicochemical contrasts, while constraining the analysis to a coherent type of ecosystem. We apply methods to quantify relevant SOM pools, gross and net fluxes, enzymatic activities and soil physicochemical parameters, as well as sequencing based characterization of soil microbial communities. The gradient is very well characterized, and we actively promote collaboration on this data set.

References:
Daniel Wasner, Rose Abramoff, Marco Griepentrog et al. Systematic and predictable variation of soil carbon reservoirs along a geoclimatic gradient, 10 May 2023, PREPRINT (Version 1) available at Research Square, external pagehttps://doi.org/10.21203/rs.3.rs-2856937/v1

 

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