scholarly journals In situabundance and carbon fixation activity of distinct anoxygenic phototrophs in the stratified seawater lake Rogoznica

2019 ◽  
Author(s):  
Petra Pjevac ◽  
Stefan Dyksma ◽  
Tobias Goldhammer ◽  
Izabela Mujakić ◽  
Michal Koblížek ◽  
...  
Keyword(s):  
Inorganic Carbon ◽  
Carbon Fixation ◽  
Green Sulfur Bacteria ◽  
Purple Sulfur Bacteria ◽  
Purple Sulfur Bacterium ◽  
Anoxygenic Phototrophs ◽  
Flow Cytometric ◽  
Sulfur Bacteria ◽  
Chlorobium Phaeobacteroides ◽  
Green Sulfur

AbstractSulfide-driven anoxygenic photosynthesis is an ancient microbial metabolism that contributes significantly to inorganic carbon fixation in stratified, sulfidic water bodies. Methods commonly applied to quantify inorganic carbon fixation by anoxygenic phototrophs, however, cannot resolve the contributions of distinct microbial populations to the overall process. We implemented a straightforward workflow, consisting of radioisotope labeling and flow cytometric cell sorting based on the distinct autofluorescence of bacterial photo pigments, to discriminate and quantify contributions of co-occurring anoxygenic phototrophic populations toin situinorganic carbon fixation in environmental samples. This allowed us to assign 89.3 ±7.6% of daytime inorganic carbon fixation by anoxygenic phototrophs in Lake Rogoznica (Croatia) to an abundant chemocline-dwelling population of green sulfur bacteria (dominated byChlorobium phaeobacteroides), whereas the co-occurring purple sulfur bacteria (Halochromatiumsp.) contributed only 1.8 ±1.4%. Furthermore, we obtained two metagenome assembled genomes of green sulfur bacteria and one of a purple sulfur bacterium which provides the first genomic insights into the genusHalochromatium, confirming its high metabolic flexibility and physiological potential for mixo-and heterotrophic growth.

scholarly journals Long-Term Population Dynamics of Phototrophic Sulfur Bacteria in the Chemocline of Lake Cadagno, Switzerland

2005 ◽  
Vol 71 (7) ◽  
pp. 3544-3550 ◽  
Author(s):  
Mauro Tonolla ◽  
Raffaele Peduzzi ◽  
Dittmar Hahn
Keyword(s):  
Major Change ◽  
Green Sulfur Bacteria ◽  
Purple Sulfur Bacteria ◽  
Phototrophic Sulfur Bacteria ◽  
Sulfur Bacteria ◽  
Large Fluctuations ◽  
Order Of Magnitude ◽  
Chlorobium Phaeobacteroides ◽  
Green Sulfur ◽  
Different Populations

ABSTRACT Population analyses in water samples obtained from the chemocline of crenogenic, meromictic Lake Cadagno, Switzerland, in October for the years 1994 to 2003 were studied using in situ hybridization with specific probes. During this 10-year period, large shifts in abundance between purple and green sulfur bacteria and among different populations were obtained. Purple sulfur bacteria were the numerically most prominent phototrophic sulfur bacteria in samples obtained from 1994 to 2001, when they represented between 70 and 95% of the phototrophic sulfur bacteria. All populations of purple sulfur bacteria showed large fluctuations in time with populations belonging to the genus Lamprocystis being numerically much more important than those of the genera Chromatium and Thiocystis. Green sulfur bacteria were initially represented by Chlorobium phaeobacteroides but were replaced by Chlorobium clathratiforme by the end of the study. C. clathratiforme was the only green sulfur bacterium detected during the last 2 years of the analysis, when a shift in dominance from purple sulfur bacteria to green sulfur bacteria was observed in the chemocline. At this time, numbers of purple sulfur bacteria had decreased and those of green sulfur bacteria increased by about 1 order of magnitude and C. clathratiforme represented about 95% of the phototrophic sulfur bacteria. This major change in community structure in the chemocline was accompanied by changes in profiles of turbidity and photosynthetically available radiation, as well as for sulfide concentrations and light intensity. Overall, these findings suggest that a disruption of the chemocline in 2000 may have altered environmental niches and populations in subsequent years.

scholarly journals Anoxygenic photo- and chemosynthesis of phototrophic sulfur bacteria from an alpine meromictic lake

2021 ◽  
Author(s):  
Francesco Di Nezio ◽  
Clarisse Beney ◽  
Samuele Roman ◽  
Francesco Danza ◽  
Antoine Buetti-Dinh ◽  
...  
Keyword(s):  
Carbon Fixation ◽  
Meromictic Lake ◽  
Purple Sulfur Bacterium ◽  
Phototrophic Sulfur Bacteria ◽  
Anaerobic Microorganisms ◽  
Sulfur Bacteria ◽  
Pure Cultures ◽  
Chlorobium Phaeobacteroides ◽  
Anoxic Environment ◽  
Dark Carbon Fixation

Abstract Meromictic lakes are interesting ecosystems to study anaerobic microorganisms due their permanent stratification allowing the formation of a stable anoxic environment. The crenogenic meromictic Lake Cadagno harbors an important community of anoxygenic phototrophic sulfur bacteria responsible for almost half of its total productivity. Besides their ability to fix CO2 through photosynthesis, these microorganisms also showed high rates of dark carbon fixation via chemosyntesis. Here, we grew in pure cultures three populations of anoxygenic phototrophic sulfur bacteria previously isolated from the lake, accounting for 72.8% of the total microbial community, and exibiting different phenotypes: 1) the motile, large-celled purple sulfur bacterium (PSB) Chromatium okenii, 2) the small-celled PSB Thiodictyon syntrophicum, and 3) the green sulfur bacterium (GSB) Chlorobium phaeobacteroides. We measured their ability to fix CO2 through photo- and chemo-synthesis, both in situ in the lake and in laboratory under different incubation conditions. We also evaluated the efficiency and velocity of H2S photo-oxidation, an important reaction in the anoxygenic photosynthesis process. Our results confirm that phototrophic sulfur bacteria strongly fix CO2 in the presence of light and that oxygen increases chemosynthesis at night, in laboratory conditions. Moreover, substancial differences were displayed between the three selected populations in terms of activity and abundance.

Occurrence of Hypolimnetic blooms of the Purple Sulfur Bacterium, Thiopedia rosea, and the Green Sulfur Bacterium, Chlorobium limicola, in an Australian Reservoir

1990 ◽  
Vol 41 (2) ◽  
pp. 223 ◽  
Author(s):  
RJ Banens
Keyword(s):  
Red Light ◽  
Secchi Depth ◽  
Extended Period ◽  
Light Regime ◽  
Purple Sulfur Bacteria ◽  
Green Sulfur Bacterium ◽  
Purple Sulfur Bacterium ◽  
Sulfur Bacteria ◽  
Inflow Event ◽  
Green Sulfur

Seasonal blooms of green and purple sulfur bacteria were found in the anoxic hypolimnion of Puddledock Reservoir, a small, eutrophic water-supply storage in north-eastern N.S.W. These blooms were dominated by the green sulfur bacterium C. limicola, and were sometimes overlain by a bloom of the purple sulfur bacterium T. rosea. They generally formed a plate just below the oxycline at a depth of between 4 and 6 m in the shallow, sulfuretted, nutrient-rich hypolimnion. The blooms increased in density from about mid summer until holomixis, when the return to oxygenated conditions killed the sulfur bacteria. Maximum bacterial chlorophyll levels varied with the light regime, but typically reached 250�g L-1, although the maximum recorded value was 410�g L-1. The Secchi transparency during summer stratification was variable, but was typically around 1.2 m, with extremes ranging from 4.5 m on one occasion to as low as 0.8 m for an extended period, as a result of epilimnetic algal levels of 40�g L-1 chlorophyll. Gilvin (g440) levels during these bacterial blooms were always less than 2.5 m-1. Sulfur bacteria were absent during one summer; this was attributed to a dramatic change in the light regime as a result of a major inflow event. The latter resulted in a Secchi depth of 0.75 m associated with very high gilvin levels of 7.5-11.0 m-1 and high inorganic turbidity levels, which would have resulted in a very dim red light regime in the hypolimnion. This study is the first report of a bloom of purple sulfur bacteria in Australian fresh waters, and the first to detail the occurrence of blooms of green and purple sulfur bacteria in a seasonally stratifying water body.

scholarly journals Two Genes Encoding New Carotenoid-Modifying Enzymes in the Green Sulfur Bacterium Chlorobium tepidum

2006 ◽  
Vol 188 (17) ◽  
pp. 6217-6223 ◽  
Author(s):  
Julia A. Maresca ◽  
Donald A. Bryant
Keyword(s):  
Green Sulfur Bacteria ◽  
The Other ◽  
Chlorobium Tepidum ◽  
Green Sulfur Bacterium ◽  
Gene Encoding ◽  
Anoxygenic Phototrophs ◽  
Sulfur Bacteria ◽  
Genes Encoding ◽  
Green Sulfur ◽  
Predicted Function

ABSTRACT The green sulfur bacterium Chlorobium tepidum produces chlorobactene as its primary carotenoid. Small amounts of chlorobactene are hydroxylated by the enzyme CrtC and then glucosylated and acylated to produce chlorobactene glucoside laurate. The genes encoding the enzymes responsible for these modifications of chlorobactene, CT1987, and CT0967, have been identified by comparative genomics, and these genes were insertionally inactivated in C. tepidum to verify their predicted function. The gene encoding chlorobactene glucosyltransferase (CT1987) has been named cruC, and the gene encoding chlorobactene lauroyltransferase (CT0967) has been named cruD. Homologs of these genes are found in the genomes of all sequenced green sulfur bacteria and filamentous anoxygenic phototrophs as well as in the genomes of several nonphotosynthetic bacteria that produce similarly modified carotenoids. The other bacteria in which these genes are found are not closely related to green sulfur bacteria or to one another. This suggests that the ability to synthesize modified carotenoids has been a frequently transferred trait.

scholarly journals Phototrophy and carbon fixation in Chlorobi postdate the rise of oxygen

2021 ◽  
Author(s):  
LM Ward ◽  
PM Shih
Keyword(s):  
Carbon Fixation ◽  
Iron Oxidation ◽  
Green Sulfur Bacteria ◽  
Oxygenic Photosynthesis ◽  
Comparative Genomic ◽  
Anoxygenic Photosynthesis ◽  
Earth History ◽  
Sulfur Bacteria ◽  
Green Sulfur ◽  
Global Carbon

AbstractWhile most productivity on the surface of the Earth today is fueled by oxygenic photosynthesis, during the early parts of Earth history it is thought that anoxygenic photosynthesis—using compounds like ferrous iron or sulfide as electron donors—drove most global carbon fixation. Anoxygenic photosynthesis is still performed by diverse bacteria in niche environments today. Of these, the Chlorobi (formerly green sulfur bacteria) are often interpreted as being particularly ancient and are frequently proposed to have fueled the biosphere early in Earth history before the rise of oxygenic photosynthesis. Here, we perform comparative genomic, phylogenetic, and molecular clock analyses to determine the antiquity of the Chlorobi and their characteristic phenotypes. We show that contrary to common assumptions, the Chlorobi clade is relatively young, with anoxygenic phototrophy, carbon fixation via the rTCA pathway, and iron oxidation all significantly postdating the rise of oxygen ~2.3 billion years ago. The Chlorobi therefore could not have fueled the Archean biosphere, but instead represent a relatively young radiation of organisms which likely acquired the capacity for anoxygenic photosynthesis and other traits via horizontal gene transfer sometime after the evolution of oxygenic Cyanobacteria.

scholarly journals Microbial community dynamics and coexistence in a sulfide-driven phototrophic bloom

2019 ◽  
Author(s):  
Srijak Bhatnagar ◽  
Elise S. Cowley ◽  
Sebastian H. Kopf ◽  
Sherlynette Pérez Castro ◽  
Sean Kearney ◽  
...  
Keyword(s):  
Community Dynamics ◽  
Microbial Mats ◽  
Elemental Sulfur ◽  
Green Sulfur Bacteria ◽  
Sulfur Cycle ◽  
Ecological Niches ◽  
Purple Sulfur Bacteria ◽  
Microbial Community Dynamics ◽  
Sulfur Bacteria ◽  
Green Sulfur

AbstractPhototrophic microbial mats commonly contain multiple phototrophic lineages that coexist based on their light, oxygen and nutrient preferences. Here we show that similar coexistence patterns and ecological niches can occur in suspended phototrophic blooms of an organic-rich estuary. The water column showed steep gradients of oxygen, pH, sulfate, sulfide, and salinity. The upper part of the bloom was dominated by aerobic phototrophicCyanobacteria, the middle and lower parts were dominated by anoxygenic purple sulfur bacteria (Chromatiales) and green sulfur bacteria (Chlorobiales), respectively. We found multiple uncultured phototrophic lineages and present metagenome-assembled genomes of two uncultured organisms within theChlorobiales. Apparently, thoseChlorobialespopulations were affected byMicroviridaeviruses. We suggest a sulfur cycle within the bloom in which elemental sulfur produced by phototrophs is reduced to sulfide byDesulfuromonas sp. These findings improve our understanding of the ecology and ecophysiology of phototrophic blooms and their impact on biogeochemical cycles.

scholarly journals Niche expansion for phototrophic sulfur bacteria at the Proterozoic–Phanerozoic transition

2020 ◽  
Vol 117 (30) ◽  
pp. 17599-17606 ◽  
Author(s):  
Xingqian Cui ◽  
Xiao-Lei Liu ◽  
Gaozhong Shen ◽  
Jian Ma ◽  
Fatima Husain ◽  
...  
Keyword(s):  
Fossil Record ◽  
Carbon Fixation ◽  
Degradation Products ◽  
Major Change ◽  
Green Sulfur Bacteria ◽  
Detailed Knowledge ◽  
Sulfur Bacteria ◽  
Physiology And Biochemistry ◽  
Green Sulfur ◽  
A Minor

Fossilized carotenoid hydrocarbons provide a window into the physiology and biochemistry of ancient microbial phototrophic communities for which only a sparse and incomplete fossil record exists. However, accurate interpretation of carotenoid-derived biomarkers requires detailed knowledge of the carotenoid inventories of contemporary phototrophs and their physiologies. Here we report two distinct patterns of fossilized C40diaromatic carotenoids. Phanerozoic marine settings show distributions of diaromatic hydrocarbons dominated by isorenieratane, a biomarker derived from low-light-adapted phototrophic green sulfur bacteria. In contrast, isorenieratane is only a minor constituent within Neoproterozoic marine sediments and Phanerozoic lacustrine paleoenvironments, for which the major compounds detected are renierapurpurane and renieratane, together with some novel C39and C38carotenoid degradation products. This latter pattern can be traced to cyanobacteria as shown by analyses of cultured taxa and laboratory simulations of sedimentary diagenesis. The cyanobacterial carotenoid synechoxanthin, and its immediate biosynthetic precursors, contain thermally labile, aromatic carboxylic-acid functional groups, which upon hydrogenation and mild heating yield mixtures of products that closely resemble those found in the Proterozoic fossil record. The Neoproterozoic–Phanerozoic transition in fossil carotenoid patterns likely reflects a step change in the surface sulfur inventory that afforded opportunities for the expansion of phototropic sulfur bacteria in marine ecosystems. Furthermore, this expansion might have also coincided with a major change in physiology. One possibility is that the green sulfur bacteria developed the capacity to oxidize sulfide fully to sulfate, an innovation which would have significantly increased their capacity for photosynthetic carbon fixation.

scholarly journals Characterization and In Situ Carbon Metabolism of Phototrophic Consortia

2003 ◽  
Vol 69 (7) ◽  
pp. 3739-3750 ◽  
Author(s):  
Jens Glaeser ◽  
Jörg Overmann
Keyword(s):  
16S Rrna ◽  
16S Rrna Gene ◽  
Denaturing Gradient Gel Electrophoresis ◽  
Stable Carbon Isotope ◽  
Green Sulfur Bacteria ◽  
Purple Sulfur Bacteria ◽  
Rrna Gene ◽  
Sulfur Bacteria ◽  
Green Sulfur

ABSTRACT A dense population of the phototrophic consortium “Pelochromatium roseum” was investigated in the chemocline of a temperate holomictic lake (Lake Dagow, Brandenburg, Germany). Fluorescence in situ hybridization revealed that the brown epibionts of “P. roseum” constituted up to 37% of the total bacterial cell number and up to 88% of all green sulfur bacteria present in the chemocline. Specific amplification of 16S rRNA gene fragments of green sulfur bacteria and denaturing gradient gel electrophoresis fingerprinting yielded a maximum of four different DNA bands depending on the year of study, indicating that the diversity of green sulfur bacteria was low. The 465-bp 16S rRNA gene sequence of the epibiont of “P. roseum” was obtained after sorting of individual consortia by micromanipulation, followed by a highly sensitive PCR. The sequence obtained represents a new phylotype within the radiation of green sulfur bacteria. Maximum light-dependent H14CO3 − fixation in the chemocline in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea suggested that there was anaerobic autotrophic growth of the green sulfur bacteria. The metabolism of the epibionts was further studied by determining stable carbon isotope ratios (δ13C) of their specific biomarkers. Analysis of photosynthetic pigments by high-performance liquid chromatography revealed the presence of high concentrations of bacteriochlorophyll (BChl) e and smaller amounts of BChl a and d and chlorophyll a in the chemocline. Unexpectedly, isorenieratene and β-isorenieratene, carotenoids typical of other brown members of the green sulfur bacteria, were absent. Instead, four different esterifying alcohols of BChl e were isolated as biomarkers of green sulfur bacterial epibionts, and their δ13C values were determined. Farnesol, tetradecanol, hexadecanol, and hexadecenol all were significantly enriched in 13C compared to bulk dissolved and particulate organic carbon and compared to the biomarkers of purple sulfur bacteria. The difference between the δ13C values of farnesol, the major esterifying alcohol of BChl e, and CO2 was −7.1%, which provides clear evidence that the mode of growth of the green sulfur bacterial epibionts of “P. roseum” in situ is photoautotrophic.

scholarly journals Carotenoid biomarkers in Namibian shelf sediments: Anoxygenic photosynthesis during sulfide eruptions in the Benguela Upwelling System

2021 ◽  
Vol 118 (29) ◽  
pp. e2106040118
Author(s):  
Jian Ma ◽  
Katherine L. French ◽  
Xingqian Cui ◽  
Donald A. Bryant ◽  
Roger E. Summons
Keyword(s):  
Microbial Mats ◽  
Green Sulfur Bacteria ◽  
Purple Sulfur Bacteria ◽  
Overlying Water ◽  
Anoxygenic Photosynthesis ◽  
Anoxygenic Phototrophs ◽  
Upwelling System ◽  
Sulfur Bacteria ◽  
Benguela Upwelling ◽  
Shelf Sediments

Aromatic carotenoid-derived hydrocarbon biomarkers are ubiquitous in ancient sediments and oils and are typically attributed to anoxygenic phototrophic green sulfur bacteria (GSB) and purple sulfur bacteria (PSB). These biomarkers serve as proxies for the environmental growth requirements of PSB and GSB, namely euxinic waters extending into the photic zone. Until now, prevailing models for environments supporting anoxygenic phototrophs include microbial mats, restricted basins and fjords with deep chemoclines, and meromictic lakes with shallow chemoclines. However, carotenoids have been reported in ancient open marine settings for which there currently are no known modern analogs that host GSB and PSB. The Benguela Upwelling System offshore Namibia, known for exceptionally high primary productivity, is prone to recurrent toxic gas eruptions whereupon hydrogen sulfide emanates from sediments into the overlying water column. These events, visible in satellite imagery as water masses clouded with elemental sulfur, suggest that the Benguela Upwelling System may be capable of supporting GSB and PSB. Here, we compare distributions of biomarkers in the free and sulfur-bound organic matter of Namibian shelf sediments. Numerous compounds—including acyclic isoprenoids, steranes, triterpanes, and carotenoids—were released from the polar lipid fractions upon Raney nickel desulfurization. The prevalence of isorenieratane and β-isorenieratane in sampling stations along the shelf verified anoxygenic photosynthesis by low-light-adapted, brown-colored GSB in this open marine setting. Renierapurpurane was also present in the sulfur-bound carotenoids and was typically accompanied by lower abundances of renieratane and β-renierapurpurane, thereby identifying cyanobacteria as an additional aromatic carotenoid source.

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