Stromatolites

The earliest microfossils and living 'fossils'.

Cyanobacteria and stromatolites

The Cyanobacteria comprise only one clade of photosynthetic bacteria. The Cyanobacteria differ from other clades of photosynthetic bacteria in that they utilize both photosystems I and II. Cyanobacteria perform oxygenic photosynthesis through photosystem II, so they evolve oxygen, and are generally believed responsible for the rise in atmospheric oxygen that followed their emergence at least 3450 million years ago.

The ability of Cyanobacteria renders them ecologically important both as primary producers and for their ability to fix nitrogen.

Cyanobacteria process only chlorophyll a. Their accessory pigments include carotenoids, but the presence of the phycobilins (phycoerythrin and phycocyanin) are a feature of the group. Cyanobacteria undoubtedly gave rise to the chloroplasts of eukaryotic cells through the process of endosymbiosis.

Several of the Cyanobacteria show a striking resemblance to fossil counterparts [im, image links]. It has been suggested that "exchange of genetic material for neutrally evolving genes may explain the apparent stability of cyanobacterial morphological characters, perhaps over billions of years." [R]

Two alternative views on the relationship of the major lineages (omitting viruses) of Life on Earth (left). Modern extremophiles are considered closely related to the Archaea.

Genome analysis has provided some clarification, but horizontal gene transfer between prokaryotes blurs evolutionary relationships.

Labels: , , , , , ,

| 0 Guide-Glossary

Lipophilic pigments from cyanobacterial (blue-green algal) and diatom mats in Hamelin Pool, Shark Bay, Western Australia.

Entrez PubMed: "Lipophilic pigments were examined in microbial mat communities dominated by cyanobacteria in the intertidal zone and by diatoms in the subtidal and sublittoral zones of Hamelin Pool, Shark Bay, Western Australia. These microbial mats have evolutionary significance because of their similarity to lithfied stromatolites from the Proterozoic and Early Paleozoic eras. Fucoxanthin, diatoxanthin, diadinoxanthin, beta-carotene, and chlorophylls a and c characterized the diatom mats, whereas cyanobacterial mats contained myxoxanthophyll, zeaxanthin, echinenone, beta-carotene, chlorophyll a and, in some cases, sheath pigment. The presence of bacteriochlorophyll a within the mats suggest a close association of photosynthetic bacteria with diatoms and cyanobacteria. The high carotenoids : chlorophyll a ratios (0.84-2.44 wt/wt) in the diatom mats suggest that carotenoids served a photoprotective function in this high light environment. By contrast, cyanobacterial sheath pigment may have largely supplanted the photoprotective role of carotenoids in the intertidal mats."

Palmisano AC, Summons RE, Cronin SE, Des Marais DJ. Lipophilic pigments from cyanobacterial (blue-green algal) and diatom mats in Hamelin Pool, Shark Bay, Western Australia. J Phycol. 1989;25:655-61.

Labels: , , , , , , , ,

| 0 Guide-Glossary

. . . accreting since 10/06/06