04.11.2014 Views

Biodiversity, carbon storage and dynamics of old northern ... - BPAN.fi

Biodiversity, carbon storage and dynamics of old northern ... - BPAN.fi

Biodiversity, carbon storage and dynamics of old northern ... - BPAN.fi

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

In the boreonemoral <strong>and</strong> nemoral zones the human influence has<br />

been much stronger <strong>and</strong> more long-lasting than in the boreal zones (cf<br />

section 3.2 above), leading to stronger modi<strong>fi</strong>cation <strong>of</strong> the natural tree<br />

species distribution than in the boreal zone. Nevertheless, we can <strong>fi</strong>nd<br />

similar responses in the forest types to gradients in nutrient supply,<br />

with dwarf shrubs <strong>and</strong> low herbs dominating the poor to medium types<br />

which <strong>of</strong>ten have oak or beech as dominating tree species, with hazel,<br />

birch, pine, aspen or other tree species as additional frequent species. On<br />

richer soils a richer ground flora will <strong>of</strong>ten be characteristic, with oak,<br />

hornbeam, elm, lime, ash, maple, <strong>and</strong> alder constituting key species <strong>of</strong><br />

the tree layer. Under particularly poor <strong>and</strong>/or dry conditions pines may<br />

constitute the dominating tree species even in the nemoral zone. At the<br />

wet end <strong>of</strong> the moisture gradient, swamp forests with ash, common alder,<br />

birch <strong>and</strong> various willows tend to dominate in different sub-types.<br />

Figure 3.3. The distribution <strong>of</strong> boreal forest types along gradients in nutrients <strong>and</strong><br />

soil moisture<br />

Dry<br />

Cladonia<br />

forest<br />

Cladonia<br />

calcareous forest<br />

Vaccinium<br />

Empetrum<br />

forest<br />

Vaccinium myrtillus forest<br />

Low-herb<br />

forest<br />

Low-herb<br />

calcareous<br />

forest<br />

Calluna Vaccinium<br />

uliginosum forest<br />

Small-fern<br />

forest<br />

Tall-fern<br />

forest<br />

Tall-herb forest<br />

Tall-herb<br />

calcareous<br />

forest<br />

Pinus mire forest<br />

Picea/Betula swamp<br />

forest<br />

Alnus glutinosa/<br />

Salix forest<br />

Poor<br />

Rich<br />

Adapted from Larsson & Søgnen 2003, cf also Påhlsson 1994, <strong>fi</strong>g. 2:1.<br />

The national forest inventories mainly characterize natural forest variation<br />

by site quality (i.e., a scoring <strong>of</strong> the st<strong>and</strong>’s potential production <strong>of</strong> tree volume)<br />

<strong>and</strong> tree species composition (mainly based on a few dominating tree<br />

species), cf Figure 3.4 (see also Figure 5.1B for an illustration <strong>of</strong> the variation<br />

in forest productivity). The Finnish, Norwegian <strong>and</strong> Swedish forest<br />

inventories also record information on forest types based on characteristics<br />

<strong>of</strong> the ground vegetation (Figure 3.3). The Danish forest inventory collects<br />

information on the main functional groups <strong>of</strong> the forest vegetation (Nord-<br />

Larsen et al. 2008). The forest inventories also present information on forest<br />

age (Figure 3.5). This is an important reflection <strong>of</strong> the effects <strong>of</strong> forest<br />

management on the age structure <strong>of</strong> the forests. A number <strong>of</strong> other<br />

measures <strong>of</strong> forest conditions are also recorded <strong>and</strong> presented in reports<br />

<strong>Biodiversity</strong>, <strong>carbon</strong> <strong>storage</strong> <strong>and</strong> <strong>dynamics</strong> <strong>old</strong> <strong>northern</strong> forests 41

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

Saved successfully!

Ooh no, something went wrong!