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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98 Joachim Schrautzer et al.<br />
Figure 5.3 Mowed foreground <strong>and</strong> ab<strong>and</strong>oned background (successional stage III with<br />
dominant Urtica dioica) wet meadow (Molinietalia) in Schmalensee, central Schleswig-<br />
Holstein, Germany.<br />
wet meadow), labeled Sere B, <strong>and</strong> for 4B (eutrophic wet meadow), labeled Sere<br />
C. Stage 1 of each of the ab<strong>and</strong>oned sites had a l<strong>and</strong>-use history of cattle grazing<br />
<strong>and</strong> mowing for hay.<br />
All stage II sites are wet sites <strong>and</strong> are characterized by an increase in tall clonal<br />
species such as Calamagrostis canescens, Carex acutiformis, Carex acuta, Filipendula<br />
ulmaria, Glyceria maxima, Juncus acutiflorus, Juncus subnodulosus,<br />
or Phalaris arundinacea. These species were already present in stage I, but<br />
became dominant only after ab<strong>and</strong>onment.<br />
In sere (A), stage III develops from stage II through immigration <strong>and</strong> establishment<br />
of herbaceous species (Phragmites australis). In seres (B) <strong>and</strong> (C),<br />
ruderal species such as Urtica dioica, Galium aparine, <strong>and</strong> Galeopsis tetrahit<br />
agg. increase in dominance (Fig. 5.3). These species seldom occur in vegetation<br />
of stage I. Stage IV in all seres results from the immigration <strong>and</strong> establishment<br />
of woody species (Alnus glutinosa, Betula pubescens).<br />
Site factors <strong>and</strong> vegetation parameters in all investigated seres differed in a<br />
characteristic way (Table 5.4). Groundwater tables increase <strong>and</strong> groundwater<br />
amplitudes decrease from stages I to II <strong>and</strong> vice versa from stages III to IV.<br />
St<strong>and</strong>ing crop <strong>and</strong> LAI increase significantly from stages I to III (cf. Schrautzer<br />
<strong>and</strong> Jensen 2006). The lowest st<strong>and</strong>ing crop (105 g m −2 ) <strong>and</strong> LAI (2.5) values<br />
were detected in st<strong>and</strong>s of stage I of sere A.<br />
Even though the vegetation trends for the ab<strong>and</strong>onment seres have been<br />
shown in several successional studies, it is impossible to predict the time when<br />
one successional stage passes over to the next. This is due to differences in<br />
surrounding vegetation <strong>and</strong> l<strong>and</strong>-use history resulting in a specific seed bank<br />
composition <strong>and</strong> potentials for the immigration of new species. However, data<br />
from the Biological Station of Steinfurt (unpublished) show the transition from<br />
stage I up to stage III occurs more quickly at eutrophic sites than at mesotrophic