Figure 5
From: Convergence of soil nitrogen isotopes across global climate gradients
Relationships between soil carbon concentrations and texture.
Shown are the percentages of (A,D) sand, (B,E) silt and (C,F) clay vs. (A–C) soil carbon (mg g−1) as well as (D–F) residual log10-transformed soil carbon (mg g−1) after accounting for MAT, log10MAP and average depth. All points represent soil values averaged to 0.1° latitude and longitude.
