Effects of temperature regime on primary producers in Icelandic geothermal streams

Eight adjacent sub-arctic streams with consistently different temperatures but broadly similar chemistry, other than some differences in conductivity and linked pH, were used to investigate effects of temperature regime on the structure of primary producer communities. Grazing by invertebrates was also taken into account to detect possible effects on the primary producers.The moss species Fontinalis antipyretica Hedw. (Bryophyta) was only observed in the warmer streams and its cover was positively linked with temperature. The liverwort Jungermannia exsertifolia (Steph.) was absent from the warmer streams and scarce in the colder streams. The biomass of F. antipyretica was inversely correlated with concentration of epilithic chlorophyll a, possibly due to shading from the bryophyte and/or competition between algae and bryophytes for nutrients. Epilithic algae and bryophyte biomass were not related to density of the main grazer, Radix peregra Müller (Gastropoda).A high biovolume of green algae (Chlorophyta) occurred in all streams. The biovolume Cyanobacteria was greatest in the coldest stream and in the two intermediately warm streams. Diatom biovolume was low compared with the biovolumes of Cyanobacteria and green algae in all streams, except in the two warmest streams, where the highest biovolume of diatom occurred.Regularized Canonical Correlation Analysis (RCCA) classification based on all primary producer assemblages and invertebrates indicated that warm streams (16.7–22.2 °C) were similar to each other. It also showed that the colder streams (6.6–13.2 °C) were different from the warmer streams and from each other because of differences in conductivity. Temperature and conductivity were the most influential variables in determining overall stream diversity.

► We examined the primary producer assemblages in eight streams. ► How does climate warming affects primary producers at high latitude streams? ► Temperature had strong influences on the stream community structure. ► Bryophytes were most abundant in warm streams. ► Epilithic algae were most abundant in colder streams. ► Climate change can have strong effects on stream primary producers at high latitudes.