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Recent Changes in the Riparian Forest of

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Table 2period, although it is likely that the peak in precipitationregistered in almost all the Ebro River Basin during the1970s (Abaurrea and others) of the flow regime with regard to the previous 2002) dampened the effects ofdams on the hydroperiod (Cabezas and others 2009).Likewise, the dams probably limited the provision ofsediments as well and, together with river embank-ment, they may have increased river bed incision, and
Table 1Largest damscurrently operating in the EbroRiver Basin upstream of thestudy area (Natural Reserve ofthe Alfranca Galachos, 41�360N,0�460W)
Fig. 3Localization of the1957 and numbered from14 to 26) and(colonized before 1957 andnumbered from 27 to 39),respectively
Table 3Floodplain area (ha)occupied by the differentecotopes within the 10-yearrecurrence interval floodplainin 2003
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