. The effects of different CO2 concentrations in the acrotelm pore water on
the development of Sphagnum magellanicum monoliths grown in wet conditions
in the laboratory are reported here.
. Decomposition processes result in much higher CO2 concentrations in bog a
crotelms than atmospheric concentrations. We therefore hypothesized that th
is substrate-derived carbon provides an important carbon source for Sphagnu
m.
. S. magellanicum hummocks developed only when CO2 concentrations in the ac
rotelm water were high. Plants in the low CO2 treatment appeared to be carb
on-limited; they had increased nutrient concentrations and decreased ratios
of carbon to other nutrients. Chlorophyll concentrations were much higher
in these plants, probably allowing them to harvest more CO2 but the allocat
ion of carbon to structural tissues was lower, resulting in weak stems that
were unable to remain upright. As a result of carbon-limitation, net bioma
ss and height increases of the monoliths were much lower in the low CO2 tre
atment.
. Results indicate that, at least in wet conditions, atmospheric CO2 alone
is not sufficient to enable S. magellanicum to develop its normal vertical
growth pattern. We conclude that the role of substrate-derived CO2 as a car
bon source for Sphagna is underestimated and requires reconsideration.