Efficiency of photosynthesis in a Chl d-utilizing cyanobacterium is comparable to or higher than that in Chl a-utilizing oxygenic species

The cyanobacterium Acaryochloris marina uses chlorophyll d to carry out oxygenic photosynthesis in environments depleted in visible and enhanced in lower-energy, far-red light. However, the extent to which low photon energies limit the efficiency of oxygenic photochemistry in A. marina is not known. Here, we report the first direct measurements of the energy-storage efficiency of the photosynthetic light reactions in A. marina whole cells, and find it is comparable to or higher than that in typical, chlorophyll a-utilizing oxygenic species. This finding indicates that oxygenic photosynthesis is not fundamentally limited at the photon energies employed by A. marina, and therefore is potentially viable in even longer-wavelength light environments.     

Multiple mechanisms of uranium immobilization by Cellulomonas sp. strain ES6

Removal of hexavalent uranium (U(VI)) from aqueous solution was studied using a Gram‐positive facultative anaerobe, Cellulomonas sp. strain ES6, under anaerobic, non‐growth conditions in bicarbonate and PIPES buffers. Inorganic phosphate was released by cells during the experiments providing ligands for formation of insoluble U(VI) phosphates. Phosphate release was most probably the result of anaerobic hydrolysis of intracellular polyphosphates accumulated by ES6 during aerobic growth. Microbial reduction of U(VI) to U(IV) was also observed. However, the relative magnitudes of U(VI) removal by abiotic (phosphate‐based) precipitation and microbial reduction depended on the buffer chemistry. In bicarbonate buffer, X‐ray absorption fine structure (XAFS) spectroscopy showed that U in the solid phase was present primarily as a non‐uraninite U(IV) phase, whereas in PIPES buffer, U precipitates consisted primarily of U(VI)‐phosphate. In both bicarbonate and PIPES buffer, net release of cellular phosphate was measured to be lower than that observed in U‐free controls suggesting simultaneous precipitation of U and PO. In PIPES, U(VI) phosphates formed a significant portion of U precipitates and mass balance estimates of U and P along with XAFS data corroborate this hypothesis. High‐resolution transmission electron microscopy (HR‐TEM) and energy dispersive X‐ray spectroscopy (EDS) of samples from PIPES treatments indeed showed both extracellular and intracellular accumulation of U solids with nanometer sized lath structures that contained U and P. In bicarbonate, however, more phosphate was removed than required to stoichiometrically balance the U(VI)/U(IV) fraction determined by XAFS, suggesting that U(IV) precipitated together with phosphate in this system. When anthraquinone‐2,6‐disulfonate (AQDS), a known electron shuttle, was added to the experimental reactors, the dominant removal mechanism in both buffers was reduction to a non‐uraninite U(IV) phase. Uranium immobilization by abiotic precipitation or microbial reduction has been extensively reported; however, the present work suggests that strain ES6 can remove U(VI) from solution simultaneously through precipitation with phosphate ligands and microbial reduction, depending on the environmental conditions. Cellulomonadaceae are environmentally relevant subsurface bacteria and here, for the first time, the presence of multiple U immobilization mechanisms within one organism is reported using Cellulomonas sp. strain ES6. Biotechnol. Bioeng. 2011;108: 264–276. © 2010 Wiley Periodicals, Inc.     

Relative stability of the S2 isomers of the oxygen evolving complex of photosystem II

Photosynthesis Research - The oxidation of water to O2 is catalyzed by the Oxygen Evolving Complex (OEC), a Mn4CaO5 complex in Photosystem II (PSII). The OEC is sequentially oxidized from state S0...     

The light-harvesting antenna of Chlorobium tepidum: Interactions between the FMO protein and the major chlorosome protein CsmA studied by surface plasmon resonance

Green sulfur bacteria possess two external light-harvesting antenna systems, the chlorosome and the FMO protein, which participate in a sequential energy transfer to the reaction centers embedded in the cytoplasmic membrane. However, little is known about the physical interaction between these two antenna systems. We have studied the interaction between the major chlorosome protein, CsmA, and the FMO protein in Chlorobium tepidum using surface plasmon resonance (SPR). Our results show an interaction between the FMO protein and an immobilized synthetic peptide corresponding to 17 amino acids at the C terminal of CsmA. This interaction is dependent on the presence of a motif comprising six amino acids that are highly conserved in all the currently available CsmA protein sequences.     

Microbial acceleration of aerobic pyrite oxidation at circumneutral pH

Pyrite (FeS₂) is the most abundant sulfide mineral on Earth and represents a significant reservoir of reduced iron and sulfur both today and in the geologic past. In modern environments, oxidative transformations of pyrite and other metal sulfides play a key role in terrestrial element partitioning with broad impacts to contaminant mobility and the formation of acid mine drainage systems. Although the role of aerobic micro‐organisms in pyrite oxidation under acidic‐pH conditions is well known, to date there is very little known about the capacity for aerobic micro‐organisms to oxidize pyrite at circumneutral pH. Here, we describe two enrichment cultures, obtained from pyrite‐bearing subsurface sediments, that were capable of sustained cell growth linked to pyrite oxidation and sulfate generation at neutral pH. The cultures were dominated by two Rhizobiales species (Bradyrhizobium sp. and Mesorhizobium sp.) and a Ralstonia species. Shotgun metagenomic sequencing and genome reconstruction indicated the presence of Fe and S oxidation pathways in these organisms, and the presence of a complete Calvin–Benson–Bassham CO₂ fixation system in the Bradyrhizobium sp. Oxidation of pyrite resulted in thin (30–50 nm) coatings of amorphous Fe(III) oxide on the pyrite surface, with no other secondary Fe or S phases detected by electron microscopy or X‐ray absorption spectroscopy. Rates of microbial pyrite oxidation were approximately one order of magnitude higher than abiotic rates. These results demonstrate the ability of aerobic microbial activity to accelerate pyrite oxidation and expand the potential contribution of micro‐organisms to continental sulfide mineral weathering around the time of the Great Oxidation Event to include neutral‐pH environments. In addition, our findings have direct implications for the geochemistry of modern sedimentary environments, including stimulation of the early stages of acid mine drainage formation and mobilization of pyrite‐associated metals.     

Terrestrial natural sources of trichloromethane (chloroform, CHCl3) – An overview

The widespread use of volatile chlorinatedcompounds like chloroform, trichloroethene andtetrachloroethene in industrialized societiescauses a large annual release of thesecompounds into the environment. Due to theirrole as a source for halogen radicals involvedin various catalytic atmospheric reactioncycles, including the regulation of thestratospheric and tropospheric ozone layers,these compounds also constitute a risk fordrinking water resources as they can betransported to the groundwater fromcontaminated field sites or even fromatmospheric deposition. Therefore,identification and investigation of sources andsinks of volatile chlorinated compounds are ofparticular interest. Chloroform, a majorcontributor to natural gaseous chlorine, wasfound to be emitted by several anthropogenicand natural sources including the oceans andterrestrial areas. The origin of chloroform inthe terrestrial environment can beanthropogenic point sources, atmosphericdeposition, release by vegetation andproduction directly in the soil. The calculatedannual biogenic global chloroform emission is700 Gg, and marine and terrestrial environmentsare nearly equal contributors. The estimatedemissions from anthropogenic sources accountfor less than 10% of the estimated totalemissions from all sources. Among terrestrialsources, forests have recently been identifiedas contributing to the release of chloroform intothe environment. With the data available,annual emissions of chloroform to theatmosphere from forest sites were calculatedand compared to other natural sources. Atpresent knowledge, forests are only a minorsource in the total biogenic flux ofchloroform, contributing less than 1% to theannual global atmospheric input. However, itshould be noted that data are available forNorthern temperate forests only. The largetropical forest areas may provide a yet unknowninput of chloroform.