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DOLOMITES - Annexes 2-8 - Provincia di Udine

DOLOMITES - Annexes 2-8 - Provincia di Udine

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NOMINATION OF THE <strong>DOLOMITES</strong> FOR INSCRIPTION ON THE WORLD NATURAL HERITAGE LIST UNESCO<br />

117<br />

tween each. This is one of the main reasons for which some Universities and other research institutes<br />

have placed their laboratories and permanent monitoring stations in the Dolomites. Many of these<br />

study show that the high-altitude ecosystems (micro-thermal grasslands and forests), are particularly<br />

sensitive to environmental change. Climate change and the <strong>di</strong>rect and in<strong>di</strong>rect effects of human activity,<br />

in fact, are shown as having a strong negative impact on their structure and functioning. For<br />

that matter, the effects of environmental change seem to cause damage, to a greater or lesser extent,<br />

accor<strong>di</strong>ng to the level of the timberline. In the Tyrol, the area that has suffered the worst impact of<br />

such changes is that of the northern calcareous Alps, whereas on the south-facing mountains and<br />

particularly in the Dolomites areas, the timberline shows no marked symptoms of deterioration as<br />

yet. In some sectors, on the contrary, a progressive upward movement of the forests can be observed,<br />

which are taking over large areas of the secondary grasslands, presumably re-gaining their former altitude<br />

limit. In this sense, the Dolomites area, as a whole, is a spectacular laboratory for the study of<br />

the re-evolution of arboreal ecosystems, processes in which other collateral processes are visibly triggered<br />

off, linked to variations in temperature (perceptible also on a planetary scale) and in rainfall<br />

and soil hydration in the summer, due to the increase of intense phenomena in the summer and the<br />

reduced snowfall in the winter. The conspicuous pedologic variability (effusive or se<strong>di</strong>mentary) connected<br />

to the more superficial matrices enriches the composite framework of the re-evolving systems<br />

and adds an important and interesting element of complexity to both the interpretation of the phenomena<br />

in progress and to the changing vegetal landscape, especially at the higher altitudes. Georg<br />

Grabherr, of Vienna University, reports that at high altitudes many more plant species can now be<br />

found than in the past. He ascribes this fact to the increased altitude of the timber and vegetation<br />

lines, a process which is procee<strong>di</strong>ng, accor<strong>di</strong>ng to each case, at a rate of between 2-4 and 20-30 meters<br />

every decade.<br />

The never-en<strong>di</strong>ng battle of stones and grass constantly climbing up the scree, covered by new rockslides.<br />

The contrast between the whiteness of the shattered rock and the pale green of the vegetation is one of the most spectacular sights

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