Epy. Tang et al., CYANOBACTERIAL DOMINANCE OF POLAR FRESH-WATER ECOSYSTEMS - ARE HIGH-LATITUDE MAT-FORMERS ADAPTED TO LOW-TEMPERATURE, Journal of phycology, 33(2), 1997, pp. 171-181
Although it is generally believed that cyanobacteria have high tempera
ture optima for growth (> 20 degrees C), mat-forming cyanobacteria are
dominant in many types of lakes, streams, and ponds in the Arctic and
Antarctic. We studied the effect of temperature on growth (mu) and re
lative pigment composition of 27 isolates of cyanobacteria (mat-formin
g Oscillatoriaceae) from the Arctic, subarctic, and Antarctic to inves
tigate whether they are a) adapted to the low temperature (i.e. psychr
ophilic) or b) tolerant of the low temperature of the polar regions (i
.e. psychotrophic). We also derived a parabolic function that describe
s both the rise and the decline of cyanobacterial growth rates with in
creasing temperature. The cyanobacteria were cultured at seven differe
nt temperatures (5 degrees-35 degrees C at 5 degrees C intervals), wit
h continuous (illumination of 225 mu mol photons . m(-2). s-(1). The p
arabolic function fits the mu-temperature data with 90% confidence for
75% of the isolates. Among the 27 isolates of cyanobacteria studied t
he temperature optima (T-opt) for growth ranged from 15 degrees to 35
degrees C, with an average of 19.9 degrees C. These results imply that
most polar cyanobacteria are psychrotrophs, not psychrophiles. The cy
anobacteria grew over a wide temperature range (typically 20 degrees C
) but growth rates were low even at T-opt (average mu(max) of 0.23 +/-
0.069 d(-1)). Extremely slow growth rates at low temperature and the
high temperature for optimal growth imply that the cyanobacteria are n
ot adapted genetically to cold temperatures, which characterize their
ambient environment. Other competitive advantages such as tolerance to
desiccation, freeze-thaw cycles, and bright, continuous solar radiati
on may contribute to their dominance in polar aquatic ecosystems.