Hydrogen metabolism of the unicellular cyanobacterium Chroococcidiopsis thermalis ATCC29380

Abstract Hydrogenase was induced in the unicellular cyanobacterium Chroococcidiopsis thermalis ATCC29380 when grown aerobically in a medium lacking combined nitrogen. Nitrogenase, however, was only observed after incubation of cells in a microaerobic environment. Hydrogen evolution could not be detected under aerobic conditions, but upon transfer of cells to dark anaerobic conditions, large amounts of hydrogen were immediately produced. This hydrogen evolution was sensitive to light and oxygen but not to inhibitors of protein synthesis. The enzyme activity catalyzing the formation of hydrogen was not membrane-bound; some functional properties were characterized in cell-free extracts.     

中国蓝藻植物的新记录属-拟甲色球藻

拟甲色球藻(Chroococcidiopsis Geitler 1933)在全球分布广泛, 并在极端环境下多有发现, 但目前在中国尚无报道。研究在对太湖水体进行野外调查时观察到了水体中的Chroococcidiopsis, 并分离得到纯培养藻株, 编号为CHAB1690。拟甲色球藻属(Chroococcidiopsis)为我国新记录属, 本文描述了该属的特征。对16S rRNA基因进行测序分析表明: CHAB1690与拟甲色球藻属的模式种温泉拟甲色球藻(Chroococcidiopsis thermalis)基因序列相似度仅为91%, 暂未定种; CHAB1690与欧洲的两株未定种Chroococcidiopsis相似度较高, 并与大多数拟甲色球藻(Chroococcidiopsis)聚集在一起, 但仍有少数藻株聚集在距离较远的另一个类群。比较两个类群中藻株的最低相似率, 结果表明, 基于形态界定的拟甲色球藻属(Chroococcidiopsis)可能包含多个属。       

DEWFALL AS A WATER SOURCE FREQUENTLY ACTIVATES THE ENDOLITHIC CYANOBACTERIAL COMMUNITIES IN THE GRANITES OF TAYLOR VALLEY,ANTARCTICA1

Endolithic photosynthetic microorganisms like cyanobacteria and algae are well known from savannas and deserts of the world, the high Arctic, and also Antarctic habitats like the Dry Valleys in the Ross Dependency. These endolithic microbial communities are thought to be at the limits of life with reported ages in the order of thousands of years. Here we report on an extensive chasmoendolithic cyanobacterial community inside granite rocks of Mt. Falconer in the lower Taylor Valley, Dry Valleys. On average, the cyanobacterial community was 4.49 ± 0.95 mm below the rock surface, where it formed a blue‐green layer. The community was composed mainly of the cyanobacterium Chroococcidiopsis sp., with occasional Cyanothece cf. aeruginosa (Nägeli) Komárek and Nostoc sp. Mean biomass was 168 ± 44 g carbon · m^?2, and the mean chl a content was 24.3 ± 34.2 mg · m^?2. In situ chl fluorescence measurements—a relative measure of photosynthetic activity—showed that they were active over long periods each day and also showed activity the next day in the absence of any moisture. Radiocarbon dating gave a relatively young age (175–280 years) for the community. Calculations from microclimate data demonstrated that formation of dew or rime was possible and could frequently activate the cyanobacteria and may explain the younger age of microbial communities at Mt. Falconer compared to older and less active endolithic microorganisms reported earlier from Linnaeus Terrace, a higher altitude region that experiences colder, drier conditions.     

SCYTONEMIN, A CYANOBACTERIAL SHEATH PIGMENT, PROTECTS AGAINST UVC RADIATION: IMPLICATIONS FOR EARLY PHOTOSYNTHETIC LIFE

During the Precambrian, ultraviolet (UV) radiation reaching the Earth's surface, including UVC wavelengths (190–280 nm), was considerably higher than present because of the lack of absorbing gases (e.g. O₂ and O₃) in the atmosphere. High UV flux would have been damaging to photosynthetic organisms exposed to solar radiation. Nevertheless, fossil evidence indicates that cyanobacteria-like ancestors may have evolved as early as 3.5 × 10⁹ yr ago, and were common in shallow marine habitats by 2.5 × 10⁹ years ago. Scytonemin, a cyanobacterial extracellular sheath pigment, strongly absorbs UVC radiation. Exposure to high-irradiance conditions caused cells to synthesize scytonemin and resulted in decreased UVC inhibition of photosynthetic carbon uptake. It was further demonstrated that scytonemin alone was sufficient for substantial protection against UVC damage. This represents the first experimental demonstration of biological protection against UVC radiation in cyanobacteria. These results suggest that scytonemin may have evolved during the Precambrian and allowed colonization of exposed, shallow-water and terrestrial habitats by cyanobacteria or their oxygenic ancestors.     

Epilithic and Cryptoendolithic Cyanobacteria of Clarens Sandstone Cliffs in the Golden Gate Highlands National Park,South Africa

A cryptoendolithic cyanobacterial community is described from Clarens sandstone in a montane ecosystem of the north-eastern Orange Free State, South Africa. The community is dominated by a species of the unicellular cyanobacterial genus Chroococcidiopsis. Chlorophyll_a content of the colonised sandstone ranged between 44.3 and 51.8mg m^?2. The establishment and species composition of an artificially created tintenstrich cyanobacterial community is documented. The possible contribution of cryptoendolithic cyanobacterial communities in the biological formation of hollows and caves in Clarens sandstone cliffs is discussed.     

An investigation into the effects of increasing salinity on photosynthesis in freshwater unicellular cyanobacteria during the late Archaean

The oldest species of bacteria capable of oxygenic photosynthesis today are the freshwater Cyanobacteria Gloeobacter spp., belonging to the class Oxyphotobacteria. Several modern molecular evolutionary studies support the freshwater origin of cyanobacteria during the Archaean and their subsequent acquisition of salt tolerance mechanisms necessary for their expansion into the marine environment. This study investigated the effect of a sudden washout event from a freshwater location into either a brackish or marine environment on the photosynthetic efficiency of two unicellular freshwater cyanobacteria: the salt‐tolerant Chroococcidiopsis thermalis PCC7203 and the cyanobacterial phylogenetic root species, Gloeobacter violaceus PCC7421. Strains were cultured under present atmospheric levels (PAL) of CO₂ or an atmosphere containing elevated levels of CO₂ and reduced O₂ (eCO₂rO₂) in simulated shallow water or terrestrial environmental conditions. Both strains exhibited a reduction in growth rates and gross photosynthesis, accompanied by significant reductions in chlorophyll a content, in brackish water, with only C. thermalis able to grow at marine salinity levels. While the experimental atmosphere caused a significant increase in gross photosynthesis rates in both strains, it did not increase their growth rates, nor the amount of O₂ released. The differences in growth responses to increasing salinities could be attributed to genetic differences, with C. thermalis carrying additional genes for trehalose synthesis. This study demonstrates that, if cyanobacteria did evolve in a freshwater environment, they would have been capable of withstanding a sudden washout into increasingly saline environments. Both C. thermalis and G. violaceus continued to grow and photosynthesise, albeit at diminished rates, in brackish water, thereby providing a route for the evolution of open ocean‐dwelling strains, necessary for the oxygenation of the Earth's atmosphere.     

Induction of water-stress proteins in cyanobacteria exposed to matric- or osmotic-water stress

Abstract: Specific stress polypeptides were detected in three drought-resistant cyanobacteria ( Phormidium autumnale , LPP₄ and Chroococcidiopsis sp.) subjected to matric- and osmotic-water stress. Drought stress caused the induction of at least 2–3 new polypeptides of apparent molecular masses of 30 kDa and 40–45 kDa. The polypeptide of 30 kDa was located in the thylakoid membranes, and the 45-kDa polypeptide in the cytoplasm. When these cyanobacteria were exposed to salt stress polypeptides of similar size appeared.