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Chapter 1 - Núria BONADA

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Local scale: Distribution patterns in Trichoptera<br />

reaches of rivers (k-means 3 and 4), characterized by intermediate altitude and channel width<br />

and lower riparian structure. Conductivity is also similar between both midstream groups<br />

although the higher percentage of sedimentary basins mainly composed by marls in group 3<br />

and the dominance of pools with a lower IASPT, suggest us to consider it as a group<br />

of samples with rambla type features. In contrast, group 4 would correspond to common<br />

GROUP 1: CALCAREOUS/SILICEOUS HEADWATERS<br />

Calcareous and siliceous basin with a small area. Medium altitude.<br />

Low stream order and narrow channel. High biological quality and<br />

riparian structure. Riffles dominant with low substrate diversity<br />

and high heterogeneity elements. Water with low conductivity.<br />

GROUP 2: SILICEOUS HEADWATERS<br />

Mainly siliceous basins with small area. High altitude. Medium<br />

stream order and narrow channel. High biological quality and<br />

riparian structure. Riffles dominant with high substrate diversity<br />

and heterogeneity elements. Water with very low conductivity.<br />

GROUP 3: SEDIMENTARY-MARLS MIDSTREAMS<br />

Mainly sedimentary-marls basin with medium basin area. Mediumlow<br />

altitude. High stream order and narrow channel. High biological<br />

quality and medium riparian structure. Low IASPT. Pools dominant<br />

with medium substrate diversity and scarce heterogeneity elements.<br />

Water with high natural conductivity.<br />

GROUP 4: CALCAREOUS/SEDIMENTARY MIDSTREAMS<br />

Calcareous and sedimentary basin with large basin area. Mediumlow<br />

altitude. Medium stream order and narrow channel. High<br />

biological quality and medium riparian structure. Medium IASPT.<br />

Riffles and pools dominant with medium substrate diversity and<br />

heterogeneity elements. Water with high conductivity.<br />

GROUP 5: CALCAREOUS/SEDIMENTARY LOWLAND REACHES<br />

Calcareous and sedimentary basins with very large basin area. Low<br />

altitude. High stream order and wide channel. Low biological quality<br />

and riparian structure. Riffles and pools dominant with medium<br />

substrate diversity and scarce heterogeneity elements. Water with<br />

high conductivity.<br />

Figure 7. Groups significance according to the results obtained from discriminant analysis.<br />

281

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