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EXECUTIVE SUMMARY - UNESCO World Heritage

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Altitudinal zones<br />

Planar<br />

Colline-submontane<br />

Montane-altomontane/subalpine<br />

Kellerwald<br />

2.a Description of Property<br />

Biogeography<br />

Th e nominated component parts are charac<br />

teristic of the beech forests in Europe.<br />

While Jasmund, Serrahn, and Grumsin<br />

occupy the lowland at heights of 0 m to<br />

a maximum of 140 m above sea level,<br />

Hainich and Kellerwald are situated in the<br />

colline to submontane altitudinal zone<br />

(200 – 626 m above sea level), thus extending<br />

the Carpathian <strong>World</strong> Natural <strong>Heritage</strong>,<br />

the greater part of which being located at<br />

levels between 600 and 1,000 m above sea<br />

level (max. 1,940 m above sea level) and<br />

consequently at the montane to subalpine<br />

altitude level, by essential altitudinal zones<br />

to give a com prehensive illustration of the<br />

post glacial development process (fi g. 2.3).<br />

Th e various altitudinal forms of beech forest<br />

are characterised by the occurrence of altitudinal<br />

diff erential species. While oaks<br />

(Quercus petraea and Q. robur), Hornbeam<br />

(Carpinus betulus), Small-leaved Lime (Tilia<br />

Serrahn<br />

Hainich<br />

Jasmund<br />

Grumsin<br />

Primeval Beech Forests<br />

of the Carpathians<br />

cordata), and Field Maple (Acer campestre)<br />

occur as mixed tree species in the planar<br />

and colline beech forests and the nominated<br />

component parts (BOHN & GOLLUB<br />

2007), the (alto-)montane zone is naturally<br />

mixed with Rowan (Sorbus aucuparia),<br />

Sycamore Maple (Acer pseudoplatanus),<br />

White Fir (Abies alba), and Norway Spruce<br />

(Picea abies).<br />

Th e nominated component parts are located<br />

in a typical temperate climate zone with<br />

mild winters, moderately warm, at times<br />

hot summers and rather evenly distributed<br />

pre cipitation. Th is is the central climatic<br />

range of the mesophytic deciduous broadleaf<br />

forests, complementing the Carpathian<br />

mountain climate with its long, cold winters<br />

and a relatively brief growing season by relevant<br />

growth types (fi g. 2.4).<br />

Th e nominated component parts are markedly<br />

diff erent in terms of soil base content.<br />

Th e soils of Jasmund and Hainich are<br />

base-rich in consequence of the high lime<br />

2. DESCRIPTION<br />

Fig. 2.3: Altitudinal zonation of<br />

European beech forests (BOHN<br />

et al. 2002 / 2003) in planar<br />

(-colline), colline-submontane,<br />

and montane-altomontane forms,<br />

including position of the nominated<br />

component parts and the <strong>World</strong><br />

Natural <strong>Heritage</strong> “Primeval<br />

Beech Forests of the Carpathians”<br />

The German beech forests<br />

will extend the Carpathian<br />

<strong>World</strong> Natural <strong>Heritage</strong><br />

by essential altitudinal<br />

zones to give a comprehensive<br />

illustration of<br />

the post glacial development<br />

process.<br />

The temperate climate of<br />

the German beech forests<br />

is complementary to<br />

the Carpathian mountain<br />

climate.<br />

Nationale<br />

Naturlandschaften<br />

31

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