Fig. 3: Apparent erosion rates (εapp) determined from the measured 14C, 26Al and 10Be concentrations. | Nature Communications

Fig. 3: Apparent erosion rates (εapp) determined from the measured 14C, 26Al and 10Be concentrations.

From: Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano

Fig. 3

Sample pairs offset from the 1 : 1 grey line (i.e., yellow circles and grey triangles) indicate disequilibrium due to higher 14C apparent erosion rate relative to 10Be—a signal we attribute to erosional transience. The 26Al apparent erosion rate of sample 09 is considered an outlier (see ‘Methods’). Error bars indicate ±1σ.

Back to article page