The present-day Rhine alluvial hardwood forest (Querco-Ulmetum minoris, Issler 24) in the upper Rhine valley
(France/Germany) is comprised of three vegetation units, one still flooded by calm waters (F) and the two others
unflooded, one for 30 years (UF30) (after the river canalisation) and the other for about 130 years (UF130)
(after river straightening and embankment work in the middle nineteenth century). In the three stands, species
composition, structure and diversity of vegetation and nutrient content of mature leaf, leaf litter and soil have been
studied. Fungi (Macromycetae) were only studied in two stands (F and UF130). The intensity of nutrient recycling
was exemplified by comparing the chemical composition of rainwater, flood, throughfall, mature leaf, leaf litter,
soil and groundwater in two of these stands (F and UF30).
The elimination of floods has caused a change in floristic composition, tree density and plant diversity. Tree
density was higher in the two unflooded stands and was related to a large increase in sapling (< 6 cm dbh) density
more than to a change of stem (> 6 cm dbh) density. Sapling density increased 2 times and three times in the
UF30 and the UF130 respectively, whereas the stem density increased only 12% in the first stand and decreased
29% in the second one. The saprophytic macromycete communities have been supplemented with mycorrhizal
species