CYANOBACTERIAL ASSEMBLAGES IN PERMANENT ICE COVERS ON ANTARCTIC LAKES: DISTRIBUTION, GROWTH RATE, AND TEMPERATURE RESPONSE OF PHOTOSYNTHESIS

• Published in: Journal of Phycology
• Main Authors: Fritsen, Christian H., Priscu, John C.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1998
• Subjects: Antarctic; McMurdo Dry Valleys; Antarc*; Antarctica
• Online Access: http://dx.doi.org/10.1046/j.1529-8817.1998.340587.x; http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1529-8817.1998.340587.x

The proliferation of microalgae in the McMurdo Dry Valleys of Antarctica is intricately linked to the seasonal cycle involving the freezing and melting of water. Anecdotal observations and preliminary sampling have found cyanobacterial cells in ice covers on lakes in the McMurdo Dry Valleys, and several of these ice covers are known to undergo seasonal freeze–thaw cycles. Therefore, we sought to determine the distribution and abundance of cyanobacterial assemblages in several permanent ice covers throughout the McMurdo Dry Valleys and to determine their rates of growth and their photosynthetic physiologies upon encountering liquid water. We found that the majority of the permanent ice covers contained cyanobacterial assemblages in close association with sedimentary material. Cyanobacterial biomass was conspicuously absent in sediment‐free ice covers, suggesting that the seasonal interaction between the sediments, ice, and solar radiation present the necessary liquid water environment for cyanobacterial growth. All assemblages exhibited extremely low rates of photosynthesis when first exposed to liquid water. Despite the low rates of photosynthesis, a large proportion (41%) of the photosynthate was incorporated into protein, indicating that the cells were undergoing efficient net cellular growth. The short‐term response (24 h) of photosynthesis to a range of temperatures showed optimum rates occurring at temperatures >15° C, which is similar to those of psychrotrophic cyanobacteria isolates from soil and stream habitats, which we believe provides the inoculum for the in‐ ice habitats.