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Exploring cyanobacterial diversity in Antarctica Blog

3 Posts tagged with the nostoc tag
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Most of the cyanobacterial mats that we have found were orange pigmented and the macroscopic structure was flaky to cohesive. The orange colour is due to carotenoids which are an protection against UV and oxidative stress.

 

I had a small light micrscope with me in the field and the genus Leptolyngbya dominated the orange mats. Leptolyngbya are filamentous non-branching cyanobacteria belonging to the order Oscillatoriales. They are mostly between 0.5-3 micrometre thick. However, the lower side of the orange layers sometimes had green pigmentation, which besides the Leptolyngbya also had some Phormidium. The genus Phormidium also belong to the order Oscillatoriales, but they are thicker with a width of around 5 micrometres.

 

   Flaky orange-pigmented cyanobacterial mats dominated by Leptolyngbya

Cyano1.jpg

 

Cohesive orange-pigmented cyanobacterial mats

Cyano2.jpg

 

green lower side of cyanobacterial mat with Phormidium

Cyano3.jpg

Interestingly, we also found some cyanobacterial mats which were dark purple to black. This colour is due to the UV-screening Scytonemin. We found the genus Schizothrix sp. (Oscillatoriales)  in the mats which is known to produce Scytonemin. We also found several ponds with large accumulations of the genus Nostoc, which belongs to the order Nostocales and has specialist cells called heterocysts for nitrogen-fixation.

 

Cyanobacterial mats with the Scytonemin-producing genus Schizothrix

Cyano5.jpg

 

Nostoc accumulations in a meltwater pond

Cyano4.jpg

 

We also found a few ponds with green algae. Green algae biofilms are easy to distinguish from cyanobacteria as green algae are very bright green.

                                                                                              

Green algae

Algae1.jpg

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Today we went to an area that is classified as Antarctic Specially Protected Area or ASPA. These are sites that are of special historic or ecological significance and a permit is required for entry.

 

The area comprises sloping ice-free ground with summer ponds and small meltwater streams draining from the Canada Glacier to Lake Fryxell. It is  is on the other side of the Canada Glacier and  the hike took ca 1.5 hours including the crossing of Canada Glacier.

 

                                                                             Canada_glacier.jpg                                             

 

 

The Canada Glacier stream area has high biomass accumulations in comparison to most other regions of the Dry Valleys. Several moss species (Bryum argenteum, Hennediella heimii and Bryum pseudotriquetrum), lichens (Lecanora expectans, Caloplaca citrina) and freshwater algae (Prasiola calophylla, Tribonema elegans) have been described from the stream area (Management Plan for Antarctic Specially Protected Area No. 131).

 

         

                                                                                                      Canada stream and Lake Fryxell

                                                                                stream.jpg

 

 

Cyanobacterial mats are also abundant. Oscillatoria, Leptolyngbya, Phormidium, Calothrix, Nostoc and Gloeocapsa are the common cyanobacterial genera the mats growing in the streams.

 

 

                                                                                                   Cyanobacerial mats

 

                                                                                 Mat.jpg

 

                                                                                       Nostoc and other cyanobacteria growing on moss

                                                                                     moss.jpg

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In Lake Hoare the mats are vertically stratified. Each year one layer is formed and they can be used as indicators of growth and environmental conditions just like tree rings. Similar to microbial mats in other lakes the layers have different pigmentations for light capturing and protection.

 

                                                                                Cyanobacterial mats in Lake Hoare

 

                                                                      LHmat1.jpg

 

After the divers had brought up mat samples from a depth of ca 10 m, we went back to the lab and identified the diversity using light microscopy. The microbial mats contained different cyanobacteria including the genera Oscillatoria, Phormidium, Leptolyngbya and Nostoc.

 

After returning to the Natural History Museum, we will carry out DNA-based methods to characterise their evolutionary relationship to other Antarctica cyanobacteria.



Anne D Jungblut

Anne D Jungblut

Member since: Sep 2, 2010

I'm Anne Jungblut from the Botany Department. Join me as I head to Antarctica to study cyanobacterial diversity in ice-covered lakes of the Dry Valleys and Ross Island where already scientists on Scott's and Shakleton's expeditions made many discoveries.

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