Soil drying and active layer deepening decrease productivity across
ecotypes of a dominant Arctic sedge
Abstract
Arctic warming is outpacing the global rate of climate change, with up
to 11 degrees C of warming projected by the year 2100 if greenhouse gas
emissions follow their current trajectories. Increasing temperatures are
expected to result in permafrost thaw, and the combined effects of
precipitation changes, soil warming, and active layer deepening are
expected to result in net soil drying. While there is widespread
agreement that increasing temperatures and active layer depth will
release carbon from soils, the effect on vegetative C cycling is less
certain. In 2017, we conducted an experiment to examine the effects of
soil drying and active layer deepening on primary productivity in
Eriophorum vaginatum, a dominant circumpolar Arctic sedge, and the
extent to which those effects vary across ecotypes. We harvested E.
vaginatum tussocks from three sites along a latitudinal gradient in the
Alaskan Arctic, placed them in pots filled with peat soil, and assigned
each to one of three drying treatments. In one treatment, the soils were
kept saturated with water through the growing season. In the second
treatment, rain was excluded in alternating two-week cycles. In the
third treatment, rain was also excluded in alternating two-week cycles,
and the soil column was approximately doubled in depth to allow deeper
drainage. We measured soil moisture, leaf water potential, leaf area
index (LAI), leaf-level phenology, and photosynthetic capacity (Amax) in
each of the tussocks. We found that the southern ecotype was affected
most severely by drying, with reductions in LAI, maximum leaf length,
and Amax. We found that effects were greater with rain exclusion and
soil column deepening than with rain exclusion alone. However, we found
no difference in leaf water potential between populations or treatments,
suggesting that E. vaginatum leaves function within a fairly narrow
range of moisture conditions. These results demonstrate that changes in
soil moisture may affect carbon storage in Arctic vegetation, but that
the magnitude of the effect may vary depending on region and ecotype.