02.04.2013 Views

EXECUTIVE SUMMARY - UNESCO World Heritage

EXECUTIVE SUMMARY - UNESCO World Heritage

EXECUTIVE SUMMARY - UNESCO World Heritage

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.

90 NOMINATION DOSSIER "ANCIENT BEECH FORESTS OF GERMANY"<br />

Another striking feature is the poverty in<br />

species of the European deciduous wood<br />

fl ora: there are 53 Central European species<br />

as opposed to North America with 124<br />

species (ELLENBERG in LANG 1994).<br />

Due to its developmental history, Europe<br />

is dominated by anemophilous species.<br />

West Asia<br />

With the Colchic, Hyrcanic, Caspian, and<br />

Caucasian forests at the Black Sea, on the<br />

montane level of the Caucaus Mountains as<br />

well as on the southern edge of the Caspian<br />

Sea, West Asia is the prime relic area of<br />

Arcto-Tertiary forests in West Eurasia. Th e<br />

northern slope of the Alborz is covered by<br />

the Caspian forests, stretching over 800 km<br />

from Southern Azerbajan across North<br />

Iran almost up to the Turkmen border in a<br />

width of only some 70 km. Beech forests<br />

made up of Fagus orientalis are found in the<br />

middle and upper montane belts. Th e beech<br />

is accompanied by a host of maple species,<br />

lime trees, oaks, and hornbeams. It is assumed<br />

that the Caspian forests have developed<br />

without any interruption caused by glacial<br />

impact as opposed to other forests in the<br />

deciduous forest zone. Today, the Caspian<br />

forests in their entirety represent the most<br />

signifi cant, albeit receding remainder of<br />

primeval forests in the world’s deciduous<br />

forest zone (KNAPP 2005).<br />

North America<br />

Th e North American deciduous forest zone<br />

has seen the transformation of 50% of all<br />

forests into farmland and pastures in less<br />

than 400 years. Th e remaining deciduous<br />

forests are mostly managed and can be<br />

considered to be relatively near-natural only<br />

in terms of the composition of tree species.<br />

Fagus grandifolia is widespread in eastern<br />

North America. Th ere are, however, no largearea<br />

pure Fagus grandifolia forests. Th e<br />

natural Fagus grandifolia-Acer saccharum<br />

ranges south of the Great Lakes have been<br />

stripped of forests almost entirely and are<br />

densely populated (“corn belt” of the USA).<br />

Obviously, there are no primeval forests<br />

left with the exception of the <strong>World</strong> <strong>Heritage</strong><br />

site Great Smokey Mountains National<br />

Park in America’s eastern decid uous forest<br />

regions.<br />

East Asia<br />

East Asian deciduous forest areas have<br />

shrunken to approx. 25% of their natural distribution<br />

range. During the last approx.<br />

6,000 years of cultural history, they have<br />

been pushed back in a similar way as in<br />

Europe. Today, some major woodlands are<br />

found only in South and, in particular,<br />

Northeast China. Th ese areas saw the<br />

cutting down of all forests at the beginning<br />

of the 20th century, which left the vast<br />

region devoid of any primeval forests and<br />

with only a very few old forests. Th e forest<br />

development in the wake of said deforestation<br />

was once again suppressed in the<br />

1960s during the Cultural Revolution.<br />

Established in 1961, the Changbai Shan<br />

National Park on the Korean border<br />

comprises, in its core zone of 196,463 ha,<br />

the most important near-natural deciduous<br />

forest stands in Manchuria. However, this<br />

does not include any Fagus forests.<br />

Near-natural forests are currently found in<br />

the montane domains of Central and<br />

South Japan as well as in the lowlands of<br />

North Japan (ARCHIBOLD 1995).<br />

Forests here are dominated by Fagus crenata<br />

(SCHRÖDER 1998), which unfolds<br />

its shaping force at the montane level<br />

(WILMANNS 1989). It is associated with<br />

maple, oak, and alder, with an understorey<br />

frequently being formed by dwarf bamboo.

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

Saved successfully!

Ooh no, something went wrong!