Water velocity, growth-form and diffusion resistances to photosynthetic CO2 uptake in aquatic bryophytes

Abstract. Boundary-layer resistances of aquatic bryophytes for CO₂ diffusion in water were estimated from wind tunnel measurements of evaporation of aniline in air, using the principle of dynamic similarity. The results indicated resistances at water velocities between 0.02 and 0.2 m s ⁻¹ ranging from about 35 to 5 s mm⁻¹ and 70 to 9 s mm⁻¹, respectively, for the mat-forming liverworts Nardia compressa and Scapania undulata , measured on a projected area (canopy) basis. Over a range of velocities from 0.01 to 0.2 m s⁻¹ the estimated CO₂ boundary-layer resistance of the streamer-like shoots of the moss Fontinalis antipyretica is between about 180 and 15 s mm⁻¹. Comparison with experiments on photosynthetic ¹⁴CO₂-uptake at a range of water velocities suggests that boundary-layer resistance limits photosynthesis at velocities below about 0.01 m s^−l in Fontinalis and below about 0.1 m s⁻¹ in the mat-forming species. It is suggested that high leaf-area index allows the mat growth form more effectively to exploit the low boundary-layer resistance at high velocities while remaining relatively invulnerable to drag. By contrast, the streamer form allows Fontinalis to maximize surface area under conditions where boundary-layer resistance is limiting.     

Evidence for a possible extinction debt in Swiss wetland specialist plants

1. Habitat loss leading to smaller patch sizes and decreasing connectivity is a major threat to global biodiversity. While some species vanish immediately after a change in habitat conditions, others show delayed extinction, that is, an extinction debt. In case of an extinction debt, the current species richness is higher than expected under present habitat conditions.
2. We investigated wetlands of the canton of Zürich in the lowlands of Eastern Switzerland where a wetland loss of 90% over the last 150 years occurred. We related current species richness to current and past patch area and connectivity (in 1850, 1900, 1950, and 2000). We compared current with predicted species richness in wetlands with a substantial loss in patch area based on the species‐area relationship of wetlands without substantial loss in patch area and studied relationships between the richness of different species groups and current and historical area and connectivity of wetland patches.
3. We found evidence of a possible extinction debt for long‐lived wetland specialist vascular plants: in wetlands, which substantially lost patch area, current species richness of long‐lived specialist vascular plants was higher than would have been expected based on current patch area. Additionally and besides current wetland area, historical area also explained current species richness of these species in a substantial and significant way. No evidence for an extinction debt in bryophytes was found.
4. The possible unpaid extinction debt in the wetlands of the canton of Zürich is an appeal to nature conservation, which has the possibility to prevent likely future extinctions of species through specific conservation measures. In particular, a further reduction in wetlands must be prevented and restoration measures must be taken to increase the number of wetlands.

     

Analysis of temporal variability in the concentrations of some elements in the terrestrial moss Pseudoscleropodium purum

The uptake of contaminants by moss is a complex process that depends on the nature and characteristics of the contaminants and on the physicochemical and biological processes that affect the moss. All of these factors in turn depend on environmental variables that may vary within a short time. It can therefore be assumed that the uptake of elements varies in such short periods that it is very difficult to obtain temporally representative results in biomonitoring studies with terrestrial moss. In order to investigate the temporal variability and the implications that it may have on the interpretation of the results obtained in this type of study, the tissue concentrations of 12 elements were determined in samples of the moss Pseudoscleropodium purum collected from two sampling sites in Galicia (NW Spain), during a long term survey with a high frequency of sampling. The results showed that the concentrations of the elements in the moss varied greatly within very short periods, and that the error associated with the temporal variability in the results was high. In accordance with these findings, and taking into account that the technique enabled contaminated and uncontaminated sites to be distinguished, we recommend that the results of biomonitoring studies should be regarded as qualitative or semiqualitative, rather than attempting to provide absolute data, which may not be temporally representative, and may have a high degree of uncertainty associated with them.