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Linking Restoration and Ecological Succession (Springer ... - Inecol

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114 Joachim Schrautzer et al.<br />

Alder carr,<br />

mesotrophic (1A)<br />

L<strong>and</strong>-use intensification<br />

Ab<strong>and</strong>onment<br />

Rewetting<br />

Species protection (high restoration potential)<br />

Species protection (low restoration potential)<br />

mean species number<br />

NPP/transpiration<br />

NPP/soil resp.<br />

N-balance<br />

NPP<br />

100 %<br />

80<br />

60<br />

40<br />

20<br />

0<br />

-20<br />

-40<br />

C-balance<br />

Sere A Sere B Sere C Re-wetting<br />

Small sedge reed (3)<br />

Tall sedge reed,<br />

mesotrophic (2A)<br />

N-net mineralization<br />

N-leaching<br />

Denitrification<br />

Micr. soil respiration<br />

Wet meadow,<br />

mesotrophic (4A)<br />

Wet meadow,<br />

mesotrophic (SSII)<br />

Alder carr, drained,<br />

mesotr. (SS IV)<br />

Wet meadow,<br />

eutrophic (4B)<br />

Wet meadow,<br />

eutrophic (SSII)<br />

Alder carr, drained,<br />

eutr. (SS IV)<br />

Wet pasture (5)<br />

Tall sedge reed,<br />

eutrophic (2B)<br />

Alder carr,<br />

eutrophic (1B)<br />

Figure 5.11 Amoeba diagrams to illustrate changes of the indicator values representing ecosystem functions during<br />

retrogressive succession following l<strong>and</strong>-use intensification, <strong>and</strong> progressive succession following ab<strong>and</strong>onment.<br />

Stages as in Fig. 5.1. Highest parameter values for all successional stages were set as 100%. Negative values<br />

(C-, N-balances) characterize the systems as nutrient sinks. <strong>Succession</strong>al stages III of seres A, B, <strong>and</strong> C are not<br />

presented.<br />

systems to alder carrs leads to higher nitrogen <strong>and</strong> carbon losses from the soil due<br />

to increased mineralization. The higher carbon storage in the woody phytomass<br />

of the ecosystems is restricted to the initial growth phase of these forests. It is<br />

difficult to predict when the development to alder carrs starts in ab<strong>and</strong>oned wet<br />

meadows. Long-term observations have shown that late successional stages of<br />

ab<strong>and</strong>oned wet meadows can remain stable for more than five decades due to<br />

missing disturbances. On the other h<strong>and</strong>, we detected a short-term development<br />

(5–10 years) of drained alder carrs mainly in previously grazed fens. These<br />

relationships should be taken into account if the implementation of large-scale<br />

grazing in fen areas is planned, because local undergrazing, which is a target<br />

of this nature conservation concept, can lead to a quick development of alder<br />

carrs (unpublished data, B. Holsten, Ecology Centre of Kiel). Furthermore,<br />

recommended management activities, such as planting alders to enhance carbon<br />

storage capacity of fens, has to be avoided if it is not possible to raise water<br />

levels in the degraded areas.

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