On the relations between water regime, mass accretion and formation of ombrotrophic conditions in Sphagnum mires
(1) I explore the hypothesis that the water regime is one of the major determinants of the difference between bog and fen in Sphagnum mires because of its effects on the decay loss and the mass accretion rate. This article deals with the recent mass balance and water regime and the variation in mass accretion rate during the last millennium, studied at two mires in southern Sweden. (2) At one bog