Wh. Thomas et B. Duval, SIERRA-NEVADA, CALIFORNIA, USA, SNOW ALGAE - SNOW ALBEDO CHANGES, ALGAL BACTERIAL INTERRELATIONSHIPS, AND ULTRAVIOLET-RADIATION EFFECTS, Arctic and alpine research, 27(4), 1995, pp. 389-399
In the Tioga Pass area (upper Lee Vining Creek watershed) of the Sierr
a Nevada (California), snow algae were prevalent in the early summers
of 1993 and 1994. Significant negative correlations were found between
snow albedo and algal cell numbers, and between albedo and snow water
content. However, red snow caused by algal blooms did not decrease me
an albedos in representative snowfields. This was due to algal patchin
ess; mean albedos would not decrease over the whole water catchment ba
sin; and water supplies would not be affected by the presence of algae
. Albedo was also reduced by dirt on the snow, and wind-blown dirt may
provide a source of allochthonous organic matter for snow bacteria. H
owever, several observations emphasize the importance of an autochthon
ous source for bacterial nutrition. Bacterial abundances and productio
n rates were higher in red snow containing algae than in noncolored sn
ow. Bacterial production was about two orders-of-magnitude lower than
photosynthetic algal production. Bacteria were also sometimes attached
to algal cells. In experiments where snow algae were contained in UV-
transmitting quartz tubes, ultraviolet radiation inhibited red snow (c
ollected from open, sunlit areas) photosynthesis about 25%, while gree
n snow (collected from forested, shady locations) photosynthesis was i
nhibited by 85%. Methanol extracts of red snow algae had greater absor
bances in blue and UV spectral regions than did algae from green snow.
These differences in UV responses and spectra may be due to habitat (
sun vs. shade) differences, or may be genetic, since different species
were found in the two snow types. However, both habitat and genetic m
echanisms may be operating together to cause these differences.