A major deterrent to a full understanding of the ecological ramifications o
f river regulation at the catchment scale is a lack of fundamental knowledg
e of structural and functional attributes of morphologically intact river s
ystems. For example, both the River Continuum and the Serial Discontinuity
Concepts, in their original formulations, had the implicit assumption of a
stable, single-thread channel from headwaters to the sea. The Flume Tagliam
ento traverses a course of 172 km from its headwaters in the Italian Alps t
o the Adriatic Sea. No high dams impede the river's passage as it flows thr
ough the characteristic sequence of constrained, braided, and meandering re
aches. The Tagliamento, the only large morphologically intact Alpine river
remaining in Europe, provides insight into the natural dynamics and complex
ity that must have characterized Alpine rivers in the pristine state. The T
agliamento has a flashy pluvio-nival regime (mean Q = 109 m(3) s(-1), with
flood flows up to 4000 m(3) s(-1)). Thousands of newly-uprooted trees were
strewn across the active bed and floodplain along the river's course follow
ing a major flood in the autumn of 1996. The active floodplain is up to 2 k
m wide and contains a riparian vegetation mosaic encompassing a range of su
ccessional stages. Up to II individual channels per cross section occur in
the braided middle reaches. Islands are a prominent feature of the riverine
landscape and island dynamics are postulated to play a key role in determi
ning pattern and process across scales. Future studies will examine the rol
es of island dynamics and large woody debris in structuring biodiversity pa
tterns of aquatic biota and successional trajectories of riparian vegetatio
n. The high levels of spatiotemporal heterogeneity exhibited by the Flume T
agliamento provide a valuable perspective for regulated river ecologists an
d those engaged in conservation and restoration. Copyright (C) 1999 John Wi
ley & Sons, Ltd.