Water chemistry of mires in relation to the poor-rich vegetation gradient and contrasting geochemical zones of the north-eastern fennoscandian Shield

Abstract

The relationship of the poor-rich vegetation gradient with water chemistry and geochemical bedrock zones was studied with a data set from 36 pristine mire sites in the middle boreal zone, Finland. The bipartition of bedrock zones into a granitoid zone and three other, more alkaline bedrock zones was clearly connected to the poor-rich gradient in the study area. Mires in the granitoid bedrock zone were predominantly bogs and poor fens, while most of the rich fen sites were located in other bedrock zones. In fens with strongly minerogenous hydrology, the geochemically distinct bedrock zones showed significant differences in concentrations of calcium, manganese, phosphorus, as well as in the total equivalent charge of base cations and the ratio of calcium and magnesium. In light of the indicator species baseda priori poor-rich classification anda posteriori correlations with vegetation ordinations and a poor-rich indicator cover index, pH showed the strongest relationship of the water chemical variables with the poor-rich gradient. High calcium concentrations only separated extremely rich fens from other categories. The poor-rich gradient of mires is considered as a primarily pH-related vegetation continuum. A more general use of pH-classes along with hydrological and vegetation based classification is suggested for mire classification instead of the “poor-rich” terminology.