Dg. Angeler et al., The significance of water inputs to plankton biomass and trophic relationships in a semi-arid freshwater wetland (central Spain), J PLANK RES, 22(11), 2000, pp. 2075-2093
This study attempts to describe changes in plankton biomass (including bact
eria, phytoplankton, ciliates, rotifers, and crustaceans) in the semi-arid,
hypertrophic, freshwater wetland, Las Tablas de Daimiel National Park (cen
tral Spain), in relation to water inflow. An inter-annual comparison of 199
6 and 1997, with contrasting rainfall, reveals that inflows in the form of
flooding act as a bottom-up structuring force on total plankton biomass. Ho
wever, the responses of plankton biomass to flooding were different in stre
ngth between the two years, which can be attributed to shifts in plankton c
ommunity structure. Crustacean zooplankton conditioned total plankton bioma
ss in 1996, based on the relationship between the high individual biomass a
nd community development. Crustaceans decreased in 1997, while bacteria, ph
ytoplankton and rotifers increased. The quantitative increase of the latter
groups resulted in a higher total plankton biomass in 1997. The key positi
on of crustaceans in the wetland plankton is also reflected in their capabi
lity for exerting significant top-down control, which was clearly evident i
n 1996 but weaker in 1997, based on their numerical reduction. Statistical
analyses provide evidence that the decline of trophic interactions in 1997
is related to the strength of flooding in that year, thereby highlighting t
he significance of the disruptive action of physical disturbance on biotic
interactions in the plankton. Flooding and areal inundation were also shown
to be significant for spatial heterogeneity. In 1996, site-specific develo
pment took place in the absence of prolonged flooding effects, resulting in
high spatial heterogeneity. In 1997, however, remarkable homogenization of
plankton biomass occurred along the major water flow path. Thus, wetland l
andscape heterogeneity depends on inflows which condition areal inundation.
This, in turn, influences plankton dynamics.