Géza B. Selmeczy

Presence of Potential Toxin-Producing Cyanobacteria in an Oligo-Mesotrophic Lake in Baltic Lake District, Germany: An Ecological, Genetic and Toxicological Survey

Massive developments of potentially toxic cyanobacteria in Lake Stechlin, an oligo-mesotrophic lake in the Baltic Lake District of Germany raised concerns about toxic contamination of these important ecosystems. Field samples in the phase of mass developments of cyanobacteria were used for genetic and toxicological analyses. Microcystins and microcystin genes were detected in field samples of the lake for the first time. However, the toxins were not produced by the dominant taxa (Dolichospermum circinale and Aphanizomenon flos-aquae) but by taxa, which were present only in low biomass in the samples (Microcystis cf. aeruginosa and Planktothrix rubescens). The phytoplankton successions during the study period revealed an increase of cyanobacterial populations. The findings contribute to the changes that have been investigated in Lake Stechlin since the mid-1990s. The possible reasons behind these developments may be climate change, special weather conditions and an increased nutrient pool.

Spatial- and niche segregation of DCM-forming cyanobacteria in Lake Stechlin (Germany)

At low trophic state, stable stratified water columns may provide favorable conditions for adapted phytoplankton species to form deep chlorophyll maxima (DCM). Such maxima occur regularly in Lake Stechlin, mainly contributed by the cyanobacterial species Cyanobium sp. and occasionally by Planktothrix rubescens. In the early twenty-first century, a rapid invasion by nostocalean cyanobacteria occurred in the lake and a number of Dolichospermum species together with Aphanizomenon flos-aquae appeared. As revealed by both microscopic and fluorimetric methods, during the summer stratification of 2013, a multispecific DCM was formed by Cyanobium, Planktothrix rubescens, and A. flos-aquae, however with spatial segregation. Planktothrix occurred in the upper hypolimnion, Aphanizomenon and Cyanobium dominated in the metalimnetic layer. Coexistence of these three cyanoprokaryota is possibly the consequence of different environmental factors limiting them (light, availability of N and P). This study represents a rare case when spatial niche segregation of phytoplankton species occurs in close to equilibrium conditions. DCM formed by Aphanizomenon and Cyanobium was detected by the fluoroprobe; Planktothrix with its different pigment compositions remained largely hidden. Our results indicate the necessity of parallel microscopic investigations and the need of careful calibration when fluorimetric methods are used for detecting cyanobacterial populations.

Leaf litter decomposition in Torna stream before and after a red mud disaster

The aim of the study was to estimate the breakdown of the allochthonous litter in an artificial stream running in an agricultural area and compare it with the same values following a toxic mud spill into the same stream. Litter bags were filled with three types of leaves (Quercus robur, Populus tremula and Salix alba) and placed to the bottom of the river. Ergosterol was used to detect fungal biomass. We supposed the absence of fungi and the retardation of leaf litter decomposition. Only pH and conductivity increased significantly. Leaf mass loss after the catastrophe was much slower than in 2009 and the decay curves did not follow the exponential decay model. Prior to the catastrophe, leaf mass loss was fast in Torna, compared to other streams in the area. The reason is that the stream is modified, the bed is trapezoid and covered with concrete stones. Fungal biomass was lower, than in the pre-disaster experiment, because fungi did not have enough leaves to sporulate. Leaf mass loss followed the exponential decay curve before the disaster, but after that it was possible only after a non-change period.