Se. Frolking et al., RELATIONSHIP BETWEEN ECOSYSTEM PRODUCTIVITY AND PHOTOSYNTHETICALLY ACTIVE RADIATION FOR NORTHERN PEATLANDS, Global biogeochemical cycles, 12(1), 1998, pp. 115-126
We analyzed the relationship between net ecosystem exchange of carbon
dioxide (NEE) and irradiance (as photosynthetic photon flux density or
PPFD), using published and unpublished data that have been collected
during midgrowing season for carbon balance studies at seven peatlands
in North America and Europe. NEE measurements included both eddy-corr
elation tower and clear, static chamber methods, which gave very simil
ar results. Data were analyzed by site, as aggregated data sets by pea
tland type (bog, poor fen, rich fen, and all fens) and as a single agg
regated data set for all peatlands. In all cases, a fit with a rectang
ular hyperbola (NEE = alpha PPFD P-max/(alpha PPFD + P-max) + R) bette
r described the NEE-PPFD relationship than did a linear fit (NEE = bet
a PPFD + R). Poor and rich fens generally had similar NEE-PPFD relatio
nships, while bogs had lower respiration rates (R = -2.0 mu mol m(-2)s
(-1) for bogs and -2.7 mu mol m(-2)s(-1) for fens) and lower NEE at mo
derate and high light levels (P-max = 5.2 mu mol m(-2)s(-1) for bogs a
nd 10.8 mu mol m(-2)s(-1) for fens). As a single class, northern peatl
ands had much smaller ecosystem respiration (R = -2.4 mu mol m(-2)s(-1
)) and NEE rates (alpha = 0.020 and P-max = 9.2 mu mol m(-2)s(-1)) tha
n the upland ecosystems (closed canopy forest, grassland, and cropland
) summarized by Ruimy et al. [1995]. Despite this low productivity, no
rthern peatland soil carbon pools are generally 5-50 times larger than
upland ecosystems because of slow rates of decomposition caused by li
tter quality and anaerobic, cold soils.