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. 2018 Jun 28;9:2530. doi: 10.1038/s41467-018-04995-y

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.5759;
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