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Water-mediated changes in plant–plant and biological soil crust–plant interactions in a temperate forest ecosystem

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Academic year: 2020

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Figure

Figure 1. Location of the experimental station (INTA) and sam-petrum rubrumarea within apling sites of soil, inert (IM) and plant materials (a); mosaic of Em- and biological soil crust (BSC) in a natural open Nothofagus pumilio forest (b).
Figure 2. Volumetric water content of soil (VWC, in gray) and stomatal conductance of Nothofagus pumilio seedlings (gs, in black) grownin different treatments of soil cover and under conditions of full and restricted watering (control and drought, respecti
Table 1. Properties of bare soil and soils covered by biological soil crust andamong final conditions were determined using two-way ANOVA followed by Bonferroni post hoc comparisons
Figure 4. Predawn water potential (�pd) values for Nothofagus pumilio seedlings grown in different soil cover types and under conditions offull and restricted watering (control and drought, respectively)
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