“…The upstream-downstream gradient is probably the most well-known large-scale pattern in stream fish assemblages, and correspondingly the flow regime, temperature, food availability and substrate conditions of the river also vary from upstream to downstream areas (Rahel and Hubert, 1991;Belliard et al, 1997;Marchetti and Moyle, 2001;Grubbs et al, 2007). Any change in expected assemblages could indicate environmental changes in the area (Hughes et al, 1986), which can provide a useful framework for studying and managing streams in different subgeographic areas of certain drainage basins (Céréghino et al, 2001;Oberdorff et al, 2001).…”