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Landscapes Forest and Global Change - ESA - Escola Superior ...

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P. Matos et al. 2010. Can lichen functional diversity be a good indicator of macroclimatic conditions<br />

65<br />

to be declining, while (sub)tropical species are invading, independent of nutrient dem<strong>and</strong>s <strong>and</strong><br />

decreasing SO 2 emissions (van Herk et al. 2002). In Western Europe, the number of epiphytic<br />

species appears to be increasing rather than declining, as a result of global warming (Aptroot<br />

<strong>and</strong> van Herk 2007). Model predictions indicate major shifts in the distribution of lichen species<br />

(Ellis et al. 2007; Giordani <strong>and</strong> Incerti 2008).<br />

Despite many authors consider that climate change will affect lichens by shifting their<br />

communities, none of them tested this hypothesis explicitly, because these studies were<br />

performed considering either total species richness or individual species response. Recent<br />

studies (Giordani <strong>and</strong> Incerti 2008) focused on functional-diversity, but used posteriori selected<br />

guilds, that were based on the pattern of environmental variables. Because it was based on<br />

posteriori classification, it is strongly dependent on local communities, <strong>and</strong> thus cannot have a<br />

broader applicability. To overcome this problem <strong>and</strong> find a more universal indicator, we have<br />

made use of a priory classification of functional-diversity based on their humidity requirements.<br />

The use of lichen functional groups was shown to be better related with several environmental<br />

gradients than total biodiversity, at least for NH 3 air pollution (Pinho et al. 2009). Moreover,<br />

functional-groups of species have been successfully used to disentangle or analyze in<br />

simultaneous the influence of multiple environmental factors (Stofer et al. 2006; Pinho et al.<br />

2008a).<br />

In this work we propose to study the effect of macroclimate on total lichen richness, abundance<br />

<strong>and</strong> on the shifts of lichen functional groups in a regional area ranging from the more humid<br />

areas in coastal central Portugal to the SE of the Alentejo in semi-arid areas. This work intends<br />

to be a first approach to find the best ecological indicators of macroclimatic changes for<br />

Mediterranean areas.<br />

2. Methodology<br />

2.1 Study area<br />

The study was conducted in three different areas of continental Portugal, covering three<br />

different macroclimatic regions (Figure 1). The area A is a Quercus faginea wood located in the<br />

west central part of Portugal, within the Natural Park of Serra d’Aire e C<strong>and</strong>eeiros. This area<br />

belongs to the Mesomediterranean belt, from the Coastal Lusitano-Andalusian province (Rivas-<br />

Martinéz <strong>and</strong> Rivas-Saenz 2009). It has an annual average temperature that ranges from 15 to<br />

17.5 ºC <strong>and</strong> an annual average precipitation between 1400 <strong>and</strong> 1600 mm (averages from 1931 to<br />

1960, (IA 2010)). The area B is located in the southwest coast of Portugal, facing the Atlantic<br />

Ocean to the west. It’s a cork oak wood (Quercus suber) with annual average temperature<br />

between 16 <strong>and</strong> 17.5 ºC, <strong>and</strong> average annual precipitation between 600 <strong>and</strong> 1000 mm (averages<br />

from years 1931 to 1960 (IA 2010)). This area is in the Termomediterranean belt, within the<br />

Coastal Lusitano-Andalusian province (Rivas-Martinéz <strong>and</strong> Rivas-Saenz 2009). The area C is a<br />

holm oak wood (Quercus ilex) located southeast from the former area. This area belongs to the<br />

Mesomediterranean belt <strong>and</strong> is placed in the Mediterranean West Iberian province (Rivas-<br />

Martinéz <strong>and</strong> Rivas-Saenz 2009) <strong>and</strong> its climate is semi-arid warm, with annual average<br />

precipitation between 500 <strong>and</strong> 600 mm <strong>and</strong> average temperatures ranging between 16 <strong>and</strong> 17.5<br />

ºC.<br />

2.2 Biodiversity data collection <strong>and</strong> calculation of lichen-diversity variables<br />

Lichen diversity was sampled in 149 sites, 29 sampling sites in the area A, 77 sampling sites in<br />

the area B (Pinho et al. 2008a,b) <strong>and</strong> 43 sampling sites in the area C. The sampling was carried<br />

according to the method described in Asta et al. (2002).<br />

For each site we calculated several lichen-variables: i) total number of species; ii) LDV, lichen<br />

diversity value, which is the sum of all species frequency within the grid. Additionally LDV<br />

<strong>Forest</strong> <strong>L<strong>and</strong>scapes</strong> <strong>and</strong> <strong>Global</strong> <strong>Change</strong>-New Frontiers in Management, Conservation <strong>and</strong> Restoration. Proceedings of the IUFRO L<strong>and</strong>scape Ecology<br />

Working Group International Conference, September 21-27, 2010, Bragança, Portugal. J.C. Azevedo, M. Feliciano, J. Castro & M.A. Pinto (eds.)<br />

2010, Instituto Politécnico de Bragança, Bragança, Portugal.

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