Aim The objective of this work was to determine if the existence of ancient
forests on cliffs was specific to the Niagara Escarpment, Canada, or part
of a globally widespread pattern.
Location Sixty-five cliff sites were visited in five countries in the tempe
rate climatic zone, and trees were sampled for age and growth rate on forty
-six of these.
Methods Two hundred and twenty-four core samples or cross-sections were tak
en from trees on cliffs that varied in height, aspect, rock-type, and expos
ure. General observations were also made of regeneration of the tree specie
s forming the mature canopy, and other habitat conditions.
Results The evidence shows that ancient slow-growing forest occurs on most
cliffs. Age and growth rate distributions were similar at all treed sites.
Small-statured Thuja, Juniperus, or Taxus stems with age estimates in exces
s of 1000 years were found in the United States, the United Kingdom and Fra
nce, and small Pinus and Quercus stems nearly 400 years in Germany. There w
as a high rate of recurrence of plants in the genera Polypodium, Asplenium,
Cystopteris, Campanula, Rosa, Prunus, Hedera, and Sorbus. Most of the site
s appear to be habitats of completely natural origin.
Conclusions We conclude that ancient natural forest is a normal feature of
cliffs, at least in the temperate zone.