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EXECUTIVE SUMMARY - UNESCO World Heritage

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

Stelzbuche in the Jasmund<br />

National Park<br />

Beech forests of Jasmund<br />

started developing as late<br />

as 800 years ago.<br />

Kreidefelsen auf Rügen, 1818<br />

(Caspar David Friedrich)<br />

The present forests of<br />

Jasmund have been forests<br />

for 1,000 years.<br />

2.b.1 Jasmund<br />

Forest history<br />

Following the fi nal retreat of the glaciers of<br />

the last ice age, over 3,000 years would<br />

pass before the late glacial tundra vegetation<br />

gave way to permanent woodlands in the<br />

Preboreal period. Another 3,000 years saw<br />

the vegetation cover being dominated by<br />

pine forests with birch and aspen, later on<br />

with hazel and elm. During the following<br />

six and a half millennia, the property was<br />

covered with various types of mixed oak<br />

forest.<br />

In Jasmund, so called the mixed oak forests<br />

(the lime Tilia cordata was the main tree)<br />

would develop into beech forests as late as<br />

some 800 years ago. Th ey have ever since<br />

been dominating all forest-compatible mineral<br />

soil sites in Jasmund without restrictions,<br />

while alder and ash trees continue to<br />

be prevalent in wet sites. At the same time,<br />

Jasmund’s steep coast was carved by coast<br />

adjustment processes of the intermittently<br />

rising sea level. Special sites developed<br />

where photophilic and thermophilic plants<br />

could spread together with the beech.<br />

Human interference<br />

With insular clearances and thinning out of<br />

the mixed oak forests, the neolithic colonisa-<br />

tion about 5,000 years ago had a fi rst lasting<br />

impact on Jasmund’s forests. With the extension<br />

of the settlement during the Bronze<br />

Age (3,800 – 2,600 BP), which is testifi ed<br />

by 389 burial mounds in the national park,<br />

the forest was pushed back. Th e Iron<br />

Age (2,600 – 1,350 BP) saw an increase in<br />

wood demand caused by iron production and<br />

smelting. Th e Migration period, 1,600 –<br />

1,350 BP was a time of recovery for the forest.<br />

In medieval times however, the area was<br />

the "wood basket" of the almost unwooded<br />

island of Rügen, in the process of which<br />

the coastal slope forests were spared. Wood<br />

harvest was restricted as early as in the<br />

16th century. From 1648 to 1815, Jasmund<br />

was a Swedish crown forest which was<br />

managed gently. After Rügen had fallen to<br />

Prussia, the old customary laws of forest<br />

grazing and free wood removal were gradually<br />

abolished. 1,500 hectares of forest became<br />

a preserve in 1929. Stubnitz became a<br />

nature conservation area in 1935. After 1945,<br />

large-area wood harvest took place within<br />

the scope of reparations, which had a<br />

massive impact on Jasmund’s beech forest.<br />

In the context of a treatment directive,<br />

the 1960s saw the designation of a fi rst strict<br />

forest reserve of 256 ha that included the<br />

slope forests, the brook valleys of Kiel and<br />

Brisnitz, and the Herthasee surroundings.<br />

Following the political turning point in 1990,<br />

the area was designated as national park<br />

with 3,003 ha of total land area within the<br />

scope the national park programme of<br />

the GDR. Jasmund is legally protected as<br />

national park and Natura 2000 territory.<br />

Th e area of the present national park Jasmund<br />

is of outstanding signifi cance also<br />

in terms of cultural history. Th e chalk coast<br />

has been providing artists, philosophers,<br />

and scientist with inspiring motives since<br />

the 19th century. Th e most famous exponent<br />

is Caspar David Friedrich, whose

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