Abstract. Predicted changes to the precipitation regime in many parts of the world
include intensifying the distribution into lower frequency, large magnitude
events. The corresponding alterations to the soil moisture regime may affect
plant growth and soil respiration, particularly in peatlands, where large
stores of organic carbon are due to gross ecosystem productivity (GEP)
exceeding ecosystem respiration (ER). This study uses lab monoliths
corroborated with field measurements to examine the effect of changing
rainfall frequency on peatland moisture controls on CO2 uptake in an
undisturbed cool temperate poor fen. Lab monoliths and field plots containing
mosses, sedges, or shrubs received either 2.3, 1, or 0.5 precipitation
events per week, with total rainfall held constant. Decreasing rain frequency led to lower
near-surface volumetric moisture content (VMC), water table (WT), and soil
tension for all vegetation types, with minimal effect on evapotranspiration.
The presence of sedges in particular led to soil tensions of ≥100 cm of
water for a sizeable duration (37 %) of the experiment. Altered rainfall
frequencies affected GEP but had little effect on ER; overall, low-frequency
rain led to a reduced net CO2 uptake for all three vegetation types.
VMC had a strong control on GEP and net ecosystem exchange (NEE) of the
Sphagnum capillifolium monoliths, and decreasing rainfall frequency
influenced these relationships. Overall, communities dominated by mosses
became net sources of CO2 after 3 days without rain, whereas
sedge communities remained net sinks for up to 14 days without rain. The results
of this study demonstrate the hydrological controls of peatland CO2
exchange dynamics influenced by changing precipitation frequency; furthermore, they suggest
these predicted changes in frequency will lead to increased sedge GEP but
limit the carbon-sink function of peatlands.