Linking Restoration and Ecological Succession (Springer ... - Inecol
Linking Restoration and Ecological Succession (Springer ... - Inecol
Linking Restoration and Ecological Succession (Springer ... - Inecol
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5<br />
<strong>Succession</strong> <strong>and</strong> <strong>Restoration</strong> of<br />
Drained Fens: Perspectives from<br />
Northwestern Europe<br />
Joachim Schrautzer, Andreas Rinker, Kai Jensen, Felix Müller, Peter Schwartze,<br />
<strong>and</strong> Klaus Dierßen<br />
90<br />
Key Points<br />
1. Changes of ecosystem features are described for several stages of retrogressive<br />
succession due to l<strong>and</strong>-use intensification <strong>and</strong> secondary progressive<br />
succession due to ab<strong>and</strong>onment in European fens.<br />
2. Agricultural intensification causes a loss of ecosystem features in fens, which<br />
in turn reduces the capacity of fens to provide multiple ecosystem services.<br />
3. Ab<strong>and</strong>onment will not always lead to the development of the desired successional<br />
stages, so technical manipulation such as rewetting, grazing, or<br />
mowing may be needed.<br />
5.1 Introduction<br />
Fens are peat-forming wetl<strong>and</strong>s that receive nutrients from upslope sources<br />
through drainage from surrounding mineral soils <strong>and</strong> from groundwater movement<br />
(EPA 2006). Fens are dominated by graminoids (grasses, sedges, <strong>and</strong><br />
reeds), which distinguishes them from bogs (the other major type of mire or<br />
peat-forming ecosystem) that are dominated by mosses. Globally, fens are a<br />
widespread type of wetl<strong>and</strong> (Mitsch <strong>and</strong> Gosselink 2000, Fraser <strong>and</strong> Keddy<br />
2005), covering large areas of the Holarctic boreal zone (North America, Sc<strong>and</strong>inavia,<br />
eastern Europe, <strong>and</strong> western Siberia). They are also regionally abundant<br />
in tropical Southeast Asia, temperate South America, <strong>and</strong> New Zeal<strong>and</strong> at high<br />
elevations. Various kinds of fens receive different amounts of precipitation <strong>and</strong><br />
different proportions of surface water <strong>and</strong> drainage water from their catchment<br />
areas. Water tables in pristine fens fluctuate near the peat surface. Due to these<br />
abiotic conditions, fens supply several important ecological services, including<br />
the ability to retain or convert nutrients. Moreover, they offer habitats for rare,<br />
hygrophilous plants <strong>and</strong> animals.<br />
In most countries of northwestern Europe (e.g., The Netherl<strong>and</strong>s, the<br />
United Kingdom, Denmark, Germany) more than 90% of fen ecosystems have<br />
been transformed into meadows <strong>and</strong> pastures during the last several decades<br />
(Rosenthal et al. 1998, Joosten <strong>and</strong> Couwenberg 2001). As a consequence, pristine<br />
fens belong to one of the most threatened ecosystems of these countries