ALGAL COMMUNITY DYNAMICS AND HALOTOLERANCE IN A TERRESTRIAL, HYPERSALINE ENVIRONMENT

We studied the algal community of the Great Salt Plains (GSP), an expansive (65 km super(2)) salt flat situated in north-central Oklahoma, USA that has been designated as the Salt Plains Microbial Observatory (SPMO) by the National Science Foundation. The GSP offered a unique opportunity to study a terrestrial, hypersaline algal community that experiences wide-ranging environmental conditions. We were able to show that ammonium-N, rather than salinity, was the most important predictor of total algal biomass. However, salinity was found to be a significant controlling variable in diatom distribution at the GSP, where diatom abundance was negatively correlated with porewater salinity concentrations. Overall, chlorophytes (likely dominated by Dunaliella spp.) were the most abundant algal group at the consistently hypersaline (>300 ppt) south site. Diatom and cyanobacterial biomass were on average highest at the central site, which experienced greater fluctuations in salinity. While taxonomic diversity was limited to three algal groups (chlorophytes, diatoms, and cyanobacteria), the salinity preferences and halotolerance ranges of isolated strains were quite variable. Although porewater salinities at the GSP are commonly near saturation (>300 ppt), the large majority of isolates had halotolerance ranges below 150 ppt. This suggests that algae at the GSP rarely achieve maximum growth rates, and could only do so when intermittent rain events reduce salinity to optimal levels. Because the vast majority of our strains were isolated from salt-saturated soil samples, maintaining viability (rather than growth efficiency) appears to be the most successful adaptation to the extreme conditions at the GSP.