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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To restore ab<strong>and</strong>oned l<strong>and</strong> there are two potential constraints, high pH <strong>and</strong><br />
high nutrient supplies (usually P), both linked to past fertilizer/lime additions.<br />
There are a variety of techniques available for reducing soil pH such as the<br />
addition of elemental or pelleted S or addition of acidic plant materials. The<br />
most effective has been the addition of S, either directly (Owen et al. 1999),<br />
or as pyrite-rich peat (Davy et al. 1998). Experience has shown that application<br />
rates need to be calculated empirically for individual sites (Owen et al.<br />
1999).<br />
When attempting to set back succession on heathl<strong>and</strong>s where succession has<br />
proceeded to woodl<strong>and</strong> stages, it is essential to remove the woodl<strong>and</strong> species<br />
(in Europe these are usually Betula spp., Pinus sylvestris, Pteridium aquilinum,<br />
Rhododendron ponticum) <strong>and</strong> especially their litter. Control of the colonizing<br />
species is essential (Marrs et al. 1998a). Control of conifers such as P. sylvestris<br />
is done easily by cutting, because it does not regenerate from cut stumps, but for<br />
all other colonizing species, either mechanical treatment needs to be repeated<br />
on a regular basis (e.g., Pteridium aquilinum control; Marrs et al. 1998a),<br />
or a herbicide should be included in the strategy (Marrs 1988). One of the<br />
techniques used in heathl<strong>and</strong>s is “sod cutting <strong>and</strong> removal,” <strong>and</strong> subsequent<br />
restoration proceeds in a nutrient-poor, subsurface layer (Werger et al. 1985,<br />
Diemont 1994). This approach has been commonly used in The Netherl<strong>and</strong>s<br />
<strong>and</strong> Belgium.<br />
Like grassl<strong>and</strong>s, heathl<strong>and</strong>s require manipulation in the Secondary Management<br />
Phase, <strong>and</strong> usually this will include grazing, cutting, <strong>and</strong> burning.<br />
However, young heathl<strong>and</strong> plants are very sensitive to grazing, <strong>and</strong> they need<br />
protection from grazing until they become established (Gimingham 1992).<br />
6.4.2.3 Wetl<strong>and</strong>s<br />
Highly dynamic systems such as river floodplains have high nutrient turnover<br />
rates <strong>and</strong> are normally very productive. In Europe, such systems were once<br />
dominated by species such as Carex spp., Phragmites australis, <strong>and</strong> Typha spp.<br />
in the wettest parts <strong>and</strong> soft- <strong>and</strong> hardwood forests in less-flooded parts. Because<br />
of their fertility, the majority of such sites are exploited for agriculture <strong>and</strong><br />
pristine floodplains are now amongst the most endangered ecosystems worldwide<br />
(Olson <strong>and</strong> Dinerstein 1998). After ab<strong>and</strong>onment, restoration to sedge<br />
or reed beds <strong>and</strong> softwood forests (e.g., Salix spp., Populus spp.) can proceed<br />
quickly but a conversion to hardwood forests (e.g., Quercus spp., Ulmus spp.,<br />
Frangula spp.) is less common. Existing evidence of hardwood development<br />
comes mainly from North America <strong>and</strong> results suggest that unassisted succession<br />
takes at least 50–100 years, depending on site conditions <strong>and</strong> proximity<br />
to seed sources (Collins <strong>and</strong> Montgomery 2002). Planting native tree mixtures<br />
can accelerate this process somewhat but even after 50 years there were considerable<br />
differences in the understory composition of planted woodl<strong>and</strong> <strong>and</strong><br />
historic bottoml<strong>and</strong> forests (Shear et al. 1996).<br />
Wet systems with less dynamic water regimes (see Chapter 5) usually exhibit<br />
lower site fertility, because organic matter decomposes slowly <strong>and</strong> is deposited<br />
as peat. The nutrient stocks of such mires are large but nutrient availability is low<br />
(Koerselman <strong>and</strong> Verhoeven 1995). Human interference almost always involves<br />
drainage, with a consequent initial large release of stored nutrients (Grootjans<br />
et al. 1985). Even after just a short drainage period <strong>and</strong> soil structural change,<br />
Chapter 6 Manipulation of <strong>Succession</strong> 135