Table 1.
Compilation N outputs estimates from biocrusts to subsurface soil from various location worldwide and the respective percentage of Archean land crust cover needed to reach the modern N land-to-ocean export flux
Location | Net N outputs from crusts to subsurface soil (m−2 yr−1) | Percentage of Archean land coverage needed to reach the modern N export flux | |
---|---|---|---|
Johnson et al.43 | Colorado Plateau | 2.080–8.820a | 1.13–0.27% |
Thiet et al.46 | Lake Michigan | 0.020–0.800a | 117.8–2.94% |
Rychert & Skujins49; West & Skujins50 |
Cold desert | 0.19–1.9 | 12.4–1.24% |
Rychert et al.51 | Australia | 0.025 | 94.2% |
Evans & Johansen52 | Sonoran Desert | 0.133–0.342 | 17.71–6.88% |
Evans & Lange53; Belnap54, 55; Russow et al.56; Stewart et al.57–59; Caputa et al.60 |
Global | 0.0133–1.9 | 177–1.24% |
Elbert et al.42 | Global | 0.144b | 16.35% |
The modern export flux is set to 0.15 Tmol yr−1 based on N/C data from shales and continental organics15. Detailed calculations are described in the methods section and available in Supplementary Table 1
aDirect estimate of N export fluxes from modern biocrusts, all other values of N outputs from crusts to subsurface soil are extrapolated from the nitrogen import fluxes
bGeometric mean value given by Elbert et al.42