When cyanobacteria originated and diversified, and what their ancient traits were, remain critical unresolved problems. Here, we used a phylogenomic approach to construct a well-resolved 'core' cyanobacterial tree. The branching positions of four lineages (Thermosynechococcus elongatus, Synechococcus elongatus, Synechococcus PCC 7335 and Acaryochloris marina) were problematic, probably due to long branch attraction artifacts. A consensus genomic tree was used to study trait evolution using ancestral state reconstruction (ASR). The early cyanobacteria were probably unicellular, freshwater, had small cell diameters, and lacked the traits to form thick microbial mats. Relaxed molecular clock analyses suggested that early cyanobacterial lineages were restricted to freshwater ecosystems until at least 2.4 Ga, before diversifying into coastal brackish and marine environments. The resultant increases in niche space and nutrient availability, and consequent sedimentation of organic carbon into the deep oceans, would have generated large pulses of oxygen into the biosphere, possibly explaining why oxygen rose so rapidly. Rapid atmospheric oxidation could have destroyed the methane-driven greenhouse with simultaneous drawdown in pCO(2), precipitating 'Snowball Earth' conditions. The traits associated with the formation of thick, laminated microbial mats (large cell diameters, filamentous growth, sheaths, motility and nitrogen fixation) were not seen until after diversification of the LPP, SPM and PNT clades, after 2.32 Ga. The appearance of these traits overlaps with a global carbon isotopic excursion between 2.2 and 2.1 Ga. Thus, a massive re-ordering of biogeochemical cycles caused by the appearance of complex laminated microbial communities in marine environments may have caused this excursion. Finally, we show that ASR may provide an explanation for why cyanobacterial microfossils have not been observed until after 2.0 Ga, and make suggestions for how future paleobiological searches for early cyanobacteria might proceed. In summary, key evolutionary events in the microbial world may have triggered some of the key geologic upheavals on the Paleoproterozoic Earth.

A phylogenomic approach was used to study the evolution of traits in the Cyanobacteria. A cyanobacterial backbone tree was constructed using multiple concatenated sequences from whole genome sequences. Additional taxa were added using a separate alignment that contained morphological characters, SSU (small subunit) and LSU (large subunit) rDNA, rpoC, rpoD, tufA, and gyrB genes. A compartmentalization approach was then used to construct a robust phylogeny with resolved deep branches. Additional morphological characters (e.g. unicellular or filamentous growth, presence or absence of heterocysts) were coded, mapped onto the backbone cyanobacterial tree, and the ancestral character states inferred. Our analyses show that the earliest cyanobacterial lineages were likely unicellular coccoid/ellipsoidal/short rods that lived in terrestrial/freshwater environments. Later cyanobacterial lineages independently gained the ability to colonize brackish, marine, and hypersaline environments while acquiring a large number of more complex traits: sheath, filamentous growth, nitrogen fixation, thermophily, motility, and use of sulphide as an electron donor. Many of these adaptations would have been important in the appearance of dense microbial mats early in Earth's history. Complex traits such as hormogonia, heterocysts, and akinetes had a single ancestor. Within the Nostocales, hormogonia and heterocysts arose before akinetes.

The extent of hyperthermophilic microbial diversity associated with siliceous sinter (geyserite) was characterized in seven near-boiling silica-depositing springs throughout Yellowstone National Park using environmental PCR amplification of small-subunit rRNA genes (SSU rDNA), large-subunit rDNA, and the internal transcribed spacer (ITS). We found that Thermocrinis ruber, a member of the order Aquificales, is ubiquitous, an indication that primary production in these springs is driven by hydrogen oxidation. Several other lineages with no known close relatives were identified that branch among the hyperthermophilic bacteria. Although they all branch deep in the bacterial tree, the precise phylogenetic placement of many of these lineages is unresolved at this time. While some springs contained a fair amount of phylogenetic diversity, others did not. Within the same spring, communities in the subaqueous environment were not appreciably different than those in the splash zone at the edge of the pool, although a greater number of phylotypes was found along the pool's edge. Also, microbial community composition appeared to have little correlation with the type of sinter morphology. The number of cell morphotypes identified by fluorescence in situ hybridization and scanning electron microscopy was greater than the number of phylotypes in SSU clone libraries. Despite little variation in Thermocrinis ruber SSU sequences, abundant variation was found in the hypervariable ITS region. The distribution of ITS sequence types appeared to be correlated with distinct morphotypes of Thermocrinis ruber in different pools. Therefore, species-or subspecies-level divergences are present but not detectable in highly conserved SSU sequences.A picture of the kinds of hyperthermophilic microorganisms inhabiting slightly alkaline (pH 7.8 to 8.9) near-boiling hot springs around the world is beginning to emerge. Molecular and cultivation studies show that many of these ecosystems, including high-and low-sulfide springs in Japan, Iceland, Kamchatka, and Yellowstone National Park, are dominated by organisms belonging to the order Aquificales (11,12,13,25,29,34). Recent cultivation of Thermocrinis ruber, the pink filaments isolated from Yellowstone's Octopus Spring, indicates that primary production in these ecosystems is by chemoautotrophic hydrogen oxidation (12). Other organisms in these ecosystems belong to known bacterial divisions, including the Thermotogales, the Thermus clade, and the Thermodesulfobacterium clade. Some organisms are unrelated to any known cultured divisions; they include the Korarchaeota (found in Yellowstone's Calcite Springs and Obsidian Pool) (3, 4), the lineage clone 8 cluster III associated with silica scale in a geothermal power plant (14), EM19 from Octopus Spring (25), and several other new candidate divisions from Obsidian Pool (4, 13).The microbial communities in these near-boiling springs are closely associated with siliceous sinter (SiO 2 · nH 2 O), commonly known as geyserite. Geyserite, by definition, pre...

The status of the Archaea as one of the three primary Domains emphasizes the importance of understanding their molecular fundamentals. Basic transcription in the Archaea resembles eucaryal transcription. However, little is known about transcriptional regulation. We have taken an in vivo approach, using genetics to address transcriptional regulation in the methanogenic Archaeon Methanococcus maripaludis. We identified a repressor binding site that regulates nif (nitrogen fixation) gene expression. The repressor binding site was palindromic (an inverted repeat) and was located just after the transcription start site of nifH. Mutations that changed the sequence of the palindrome resulted in marked decreases in repression by ammonia, even when the palindromic nature of the site was retained. The same mutations greatly decreased binding to the site by components of cell extract. These results provide the first partial description of a transcriptional regulatory mechanism in the methanogenic Archaea. This work also illustrates the utility of genetic approaches in Methanococcus that have not been widely used in the methanogens: directed mutagenesis and reporter gene fusions with lacZ.