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EXECUTIVE SUMMARY - UNESCO World Heritage

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

Standing dead wood in Grumsin<br />

In Grumsin, the beech<br />

began to take hold about<br />

3,000 years ago.<br />

With the establishment of the Müritz<br />

National Park on 1 October 1990, the nominated<br />

component part was designated as<br />

core area of the national park. Th e borders<br />

of core area, which has been unmanaged<br />

ever since, reach far beyond the nominated<br />

property so that the nominated beech<br />

forests have a highly reliable, persis tently<br />

unmanaged buff er.<br />

Natural disasters<br />

Th ere have been no known natural disasters.<br />

2.b.3 Grumsin<br />

Forest history<br />

(according to SCHÄFER &<br />

HORNSCHUCH 1998)<br />

In Grumsin, the period between the Late<br />

Glacial and Preboreal periods was characterised<br />

by occurrences of birches and<br />

pines. Th e subsequent Boreal period featured<br />

large portions of hazelnut trees.<br />

Successively elm, alder, and oak with regular<br />

values appeared. During the Atlantic, lime<br />

trees were an addition to the forests. Th e<br />

northwestern part of Grumsin was characterised<br />

by a high portion of lime trees until<br />

the beginning of the 20th century (HUECK<br />

1929). Even today, the species is regularly<br />

found in the tree layer of richer sites.<br />

Th ere were sporadic beech and hornbeam<br />

occurrences already at the beginning of the<br />

Atlantic period, which, however, would not<br />

become relevant mixed tree species before the<br />

Subboreal period. Following a brief increase<br />

in pine numbers, the composition of the<br />

for est changed radically during the Older<br />

Sub atlantic. Th e pines would disappear<br />

almost entirely. Beech and hornbeam culminated.<br />

HESMER (1935) concludes that the clayey<br />

moraine sites “have been deciduous forests<br />

for thousands of years”, in which the beech<br />

has the largest share.<br />

Human interference<br />

Grumsin is an old forest site (LUTHARDT<br />

2007, 2008). Th e beech has long since<br />

been the dominant tree species. Th e nominated<br />

component part was temporarily used<br />

as forest pasture; rocks were removed from<br />

the coarse terminal moraine material. Th ere<br />

are fi nd spots in the wider area of Grumsin<br />

from the Neolithic and Bronze Age. Slavic<br />

settlement sites from the 12th and 13th<br />

century have been verifi ed. Some town<br />

names have Slavic radicals, such as Buckow<br />

(buk = beech). However, hardly any human<br />

settlements have been verifi ed around<br />

Grumsin for the period from 1500 to 1750.<br />

Hunting took centre stage in the forest.<br />

Fence keepers and guards were settled along<br />

a fence of over 70 km in length, which was<br />

set up about 1661. In so doing, the village of<br />

Grumsin was created in 1728, which even<br />

today is composed of but a few houses, and<br />

located about two kilometres from the nominated<br />

component part.<br />

By 1720, the forest showed a natural composition<br />

of tree species with the dominant<br />

beech. Existing large-crowned oaks were<br />

exempt from wood harvest so as to have the

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