scholarly journals Potential Future Ranges of Tree Species in the Alps

Author(s):  
Niklaus E. ◽  
Robert Jandl ◽  
Marc Hanewinkel ◽  
Georges Kunstler ◽  
Christian Klling ◽  
...  
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2010 ◽  
Vol 161 (6) ◽  
pp. 207-215 ◽  
Author(s):  
Felix Gugerli ◽  
Christoph Sperisen

Fossil records (pollen, macroremains) and genetic structures based on molecular markers provide complementary data sets for elucidating the (post-)glacial histories of extant plant populations. Based on comparative studies using both data sources, this article focuses on the effects of postglacial recolonization on the genetic structures in common, widespread forest tree species in the Alpine range. We recall that at least at the continental level, the three large southern European peninsulas, Iberia, Italy and the Balkans, but also the Carpathians represented important refugial areas for many European tree species during the last glacial maximum. However, these refugia had a minimal impact on the recolonization of the Alpine range. In contrast, recent studies demonstrate that refugial areas in the proximity of the Alps, e.g. at their eastern and western ends, harbored prominent source populations of current occurrences of the dominant forest trees in the Alpine range. Furthermore, there is strong evidence that several species were able to maintain populations north of the Alps, such as in the Bohemian Massif. We advocate that the Alps did not necessarily represent a barrier to northward migration, since terrain for advancement from various refugia was available along the margins of this mountain range. Such migration patterns allowed diverged genetic lineages to meet, leading to increased genetic diversity in respective contact zones. This overview underlines how paleoecological and molecular genetic studies may complement each other to develop a more comprehensive vision of the postglacial history of forest trees in the Alpine range.


2010 ◽  
Vol 161 (11) ◽  
pp. 424-432 ◽  
Author(s):  
Marco Conedera ◽  
Willy Tinner

Understanding past natural and anthropogenically induced forest fires and their long-term impact on the environment is a prerequisite for modern fire management. Thanks to modern paleoecological approaches it was possible to reconstruct the long-term role of fire for ecosystems, landscape properties and functions in various parts of Switzerland. In order to test and calibrate the paleoecological approach on a local scale, we compared the forest-fire statistics of the last 70 years around the small Lago di Origlio (southern Switzerland) with the yearly charcoal influx in the lake sediments. We demonstrated that the yearly deposition of microscopic charcoal particles (0.01−0.2 mm) correlates well with the regional forest-fire frequency 20 to 50 km around the lake, whereas macroscopic charcoal particles (> 0.2 mm) matched local fire events within a 2 km distance. Furthermore, the pilot study of lake Origlio provided insights into the different origins of forest fires and their long-term impact on vegetation. Studies in other areas in Switzerland suggest that that the long-term effects of forest fire are not limited to the southern slope of the Alps, but also concern the forests of the Swiss Plateau and the Alps. There, the diffusion of fire-sensitive tree species such as Ulmus spp., Tilia spp., Fraxinus spp., Acer spp. at the colline to mountain level, as well as Abies alba and Pinus cembra at the subalpine level was significantly reduced compared to the natural environmental conditions prior to the beginning of widespread slash and burn practices. The abundance reduction of tree species during the past millennia occurred in the southern and the northern Alps, on the Swiss Plateau, but not in the fire-prone dry valleys of the central Alps, where forest fires were more frequent naturally and exerted relevant ecosystem functions. Our results show that without considering sedimentary paleoenviromental information it is hardly possible to gain correct assessments of current and future fire, environmental and forest dynamics. The implementation of paleoecological results into practical management activities is thus indispensable, especially in the view of the expected climatic changes.


2008 ◽  
Vol 159 (10) ◽  
pp. 336-343 ◽  
Author(s):  
Thomas Wohlgemuth ◽  
Marco Conedera ◽  
Andrea Kupferschmid Albisetti ◽  
Barbara Moser ◽  
Tilo Usbeck ◽  
...  

Most natural disturbances to Swiss forests are caused by climatically induced extreme events: winter storms, foehn and thunderstorms predominate in the North of the Alps, and forest fires in the Southern Alps. Many studies predict a general increase of these extreme events under continued climatic change. How resistant are Swiss forests against wind and fire disturbance, and how resilient are they after disturbance? Because in Switzerland most of the severe winds happen in the wintertime, conifers such as Norway spruce and silver fir are the most vulnerable species. Beyond gust speeds of more than 40 m/s, all tree species are damaged. The fire resistance of forests depends on the flammability, which will increase due to increasing drought frequency. Forests in the Ticino will be most affected by this development, and to a lesser extent also forests in the Central Alps and those north of the Alps. After wind and fire disturbance, forest has re-established in almost all regions of Switzerland. Results from various studies in disturbed forests show that the amount of tree regeneration decreases with increasing elevation (R2 = 0.31). After fire, the speed of regeneration depends on various factors such as tree species, drought and the transient absence of mycorrhiza. The natural regeneration process after severe forest disturbances reflects a first step towards a forest more adapted to the future. Trees that establish in big gaps and under repeated drought may resist the future climate.


2009 ◽  
Author(s):  
Hermann Alexander Berlepsch ◽  
Leslie Stephen
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2014 ◽  
Author(s):  
William John Law
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1995 ◽  
Vol 95 (3) ◽  
pp. 399-408 ◽  
Author(s):  
Elena Toll ◽  
Federico J. Castillo ◽  
Pierre Crespi ◽  
Michele Crevecoeur ◽  
Hubert Greppin

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