Accumulation rates of organic matter associated with different successional stages from open water to carr forest in former turbaries

This paper investigates the rates of peat accumulation associated with different phases in the succession from open water to carr forest in shallow ponds created by peat dredging in The Netherlands. Four phases had been recognized in a previous study of aerial photographs for the period 1937–1990, i.e. open water (Aq), reed swamp (SA), brownmoss quaking fen (BM) and carr forest (CF). Peat accumulation rates were estimated by relating the amounts of organic matter stored to the data on the successional history for 21 different sites.The organic matter accumulation rates were highest in the SA phase (1.12 kg m^-2 y^-1 on a dry weight basis), intermediate in the BM and CF phases (0.49 and 0.58 kg m^-2 y^-1), and lowest in the Aq phase (0.26 kg m^-2 y^-1). These values are high in comparison with values determined for fen ecosystems with stratigraphic methods in combination with radiocarbon dating. The accumulation rates were inversely related to the average duration of the successional phases, suggesting that peat accumulation is a major driving force behind the succession.