Absorption and utilization of irradiance by cyanobacterial mats in two ice-covered Antarctic lakes with contrasting light climates

We investigated the under-ice light climate and the efficiency with which l ight was absorbed and utilized by benthic algal mats in Lakes Hoare and Van da, two perennially ice-covered lakes in the McMurdo Dry Valleys area of So uthern Victoria Land, Antarctica. The ice cover and water column of Lake Va nda were much more transparent than those of Lake Hoare (18% vs. 2% transmi ssion though ice and attenuation coefficients for downwelling irradiance of 0.05 vs. 0.12 m(-1), respectively). In both lakes the under-ice spectra we re dominated by blue-green wavelengths. The benthic flora under perennial i ce covers of both lakes comprised thick mucilaginous mats, dominated by cya nobacteria. The mats were well suited to absorb the dominant blue-green wav elengths of the under-ice light, with phycoerythrin being present at high c oncentrations. The pigment systems of the benthic mats absorbed 30%-50% of the light that reached them, varying with depth and lake. There was a tende ncy for the percentage of absorption to increase as ambient irradiance decr eased. The efficiency of utilization of absorbed irradiance was examined by constructing absorbed irradiance/oxygen evolution curves to estimate commu nity quantum yield. Mats from 13 m in Lake Hoare showed the highest quantum yields, approaching 1 mol of carbon fixed for every 8 mol quanta absorbed under Light-limiting conditions. Lake Vanda mats had lower quantum yields, but these increased with depth. Calculated in situ irradiance occasionally exceeded the measured saturating irradiance for oxygen evolution in both la kes, thus efficiency in situ was below the maximum at times. As in other en vironments, optimization strategies allowed efficient capture and utilizati on of the lower and middle ranges of experienced irradiance but led to a co mpromised capacity to use the highest irradiances encountered at each depth .