21.12.2012 Views

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

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

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

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Chapter 3 Aboveground–Belowground Linkages, Ecosystem Development, <strong>and</strong> Ecosystem <strong>Restoration</strong> 55<br />

Figure 3.3 A forested isl<strong>and</strong> in Lake Hornavan in northern Sweden.<br />

this is a marked reduction in both plant st<strong>and</strong>ing biomass <strong>and</strong> NPP (Wardle<br />

et al. 2003). The isl<strong>and</strong> system thus represents a retrogressive succession with<br />

prolonged absence of disturbance leading to aboveground decline in biomass<br />

<strong>and</strong> productivity (Wardle et al. 2004b). <strong>Restoration</strong> of a natural fire regime<br />

would reverse this succession <strong>and</strong> thus promote biomass <strong>and</strong> productivity of<br />

these forests.<br />

The shifts in vegetation composition aboveground have important corresponding<br />

effects belowground. For example, soils on the small isl<strong>and</strong>s contain<br />

higher concentrations of polyphenols than those on the large isl<strong>and</strong>s, presumably<br />

because of domination by Picea <strong>and</strong> Empetrum (Wardle et al. 1997).<br />

The quality of litter entering soils on the small isl<strong>and</strong>s is also inferior (Wardle<br />

et al. 2003). Although N inputs from N2 fixation by cyanobacteria associated<br />

with bryophytes (the main agent of N input to these forests; De Luca et al.<br />

2002b) is much greater on the small isl<strong>and</strong>s (Lagerström, Wardle, Nilsson, <strong>and</strong><br />

Zackrisson, unpublished), <strong>and</strong> soils on small isl<strong>and</strong>s have a higher N concentration<br />

(Wardle et al. 1997), this N is of reduced biological availability largely<br />

because it is tightly bound in polyphenolic complexes. The net consequence of<br />

this is reduced biomass <strong>and</strong> activity of decomposer microbes, lower rates of decomposition<br />

<strong>and</strong> N mineralization, <strong>and</strong> lower concentrations of available forms<br />

of N on the small isl<strong>and</strong>s. Concomitant with this is reduced availability of P, a<br />

characteristic of retrogressive successions that span thous<strong>and</strong>s of years (Wardle<br />

et al. 2004b). The reduction in soil biological activity <strong>and</strong> nutrient availability<br />

creates aboveground feedbacks, ultimately reducing plant nutrient acquisition,<br />

st<strong>and</strong>ing plant biomass, <strong>and</strong> NPP (Wardle et al. 1997 <strong>and</strong> 2003). <strong>Restoration</strong><br />

of the natural fire regime in these forests to reverse or arrest this retrogressive<br />

succession would in turn promote soil biological activity <strong>and</strong> nutrient supply

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!