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Chapter 1 - Núria BONADA

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<strong>Chapter</strong> 3<br />

In spite of these observed divergences between macroinvertebrate assemblage in med-region,<br />

numerous ubiquitous taxa are present, what implies the existence of similar evolutionary<br />

mechanisms of dispersion, extinction and adaptation of the taxa along time (Deacon, 1983).<br />

Because of the dispersion and colonization of one organism depends on the environmental<br />

conditions and life cycles (Cox & Moore, 1993), organisms with short life cycles, continuous<br />

reproductions and aerial phases should be easily dispersed, and therefore they will have a<br />

wider distribution (Williams & Feltmate, 1993). Baetidae, Caenidae, Leptophlebiidae,<br />

Leptoceridae, Hydropsychidae, Oligochaeta and almost all dipterans are ubiquitous taxa, and<br />

most of them have been considered as organisms easily to disperse because their<br />

morphological and reproductive traits (for example see Gray, 1981; Gray & Fisher, 1981;<br />

Fisher et al., 1982). Moreover, most of these taxa are characterized by having a very old origin<br />

(e.g., Baetidae, Caenidae and Leptophlebiidae) in contrast with others with a local distribution<br />

(e.g., Teloganodidae — Edmunds, 1972).<br />

Historical factors are important to understand taxonomical convergences and divergences, but<br />

the viability and success of one taxa in one new region will depend on the local and<br />

environmental conditions (Resh & Solem, 1996). In that sense, Ball (1975) distinguishes<br />

between an analytical (Historical Biogeography) and an empirical biogeography (Ecological<br />

Biogeography). Thus, the abundance of EPT in Northern hemisphere and Chile respect other<br />

areas could be interpreted by the mountain river typology of some rivers flowing from high<br />

mountains near the coast (Sierra Nevada in California, Andes in Chile and Sierra Nevada,<br />

Pyrenees, Apennines, Atlas,... in Med-Basin), that let the establishment of species adapted to<br />

steep, cold and fast flowing rivers. On the other hand, even though some mountainous and<br />

high gradient rivers with cold waters are present in South Africa and SAustralia, the low<br />

EPT/OCH is explained by the poor contribution of Plecoptera in these regions because of<br />

biogeographical factors (Zwick, 2000), instead of environmental ones. This difficulty to discern<br />

between ecological and historical factors has been emphasized by Endler (1982), but both have<br />

to be present to understand community structure and composition (Ricklefs, 1987; Menge &<br />

Olson, 1990).<br />

Local scale: Ecological factors and the spatio-temporal variability<br />

In our study and according to the measured factors in reference conditions (without human<br />

disturbance), pH is a key variable to diferenciate med-regions. Calcareous geology in<br />

mediterranean basin (di Castri, 1981) is the responsible of a high pH in its rivers and streams<br />

(Toro et al., (in press)), whereas heavily washed soils in South Africa and SWAustralia (Specht<br />

& Moll, 1983), provide a high acidity in reference conditions. In South Africa, fynbos vegetation<br />

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