Micrometeorological measurements of carbon dioxide exchange were made
in an open peatland in north central Minnesota during two growing seas
ons (1991 and 1992). The vegetation at the site was dominated by Sphag
num papillosum, Scheuchzeria palustris, and Chamaedaphne calyculata. T
he objective of the study was to examine the diurnal and seasonal vari
ations in canopy photosynthesis (P) and develop information on the net
ecosystem CO2 exchange. The two seasons provided contrasting microcli
matic conditions: as compared with 1991, the 1992 season was significa
ntly wetter and cooler. Canopy photosynthesis was sensitive to changes
in light, temperature, and moisture stress (as indicated by water tab
le depth and atmospheric vapor pressure deficit). Under moderate condi
tions (temperature 18-28 degrees C, vapor pressure deficit 0.7-1.5 kPa
, and water table near the surface) during the peak growth period, mid
day (averaged between 1000-1400 hours) P values ranged from 0.15 to 0.
24 mg m(-2) s(-1). Under high-temperature (30 degrees-34 degrees C) an
d moisture stress (water table 0.16-0.23 m below the surface and vapor
pressure deficit 2.2-3.0 kPa) conditions, midday P was reduced to abo
ut 0.03-0.06 mg m(-2) s(-1). There was a high degree of consistency in
the values of P under similar conditions in the two seasons. Seasonal
ly integrated values of the daily net ecosystem CO2 exchange indicated
that the study site was a source of atmospheric CO2, releasing about
71 g C m(-2) over a 145-day period (May-October) in 1991. Over a simil
ar period in 1992, however, this ecosystem was a sink for atmospheric
CO2 with a net accumulation of about 32 g C m(-2). These results are c
onsistent with previous investigations on CO2 exchange in other northe
rn wetland sites during wet and dry periods.