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- Creators: School of Life Sciences
Ground cover was fairly similar among sites, with bare ground > non-colonized quartz fragments > colonized quartz fragments > non-quartz rocks. Grass was present only at the site with the highest mean annual precipitation (MAP) where it accounted for 1% of ground cover. Lichens were present only at the lowest MAP site, where they accounted for 30% of ground cover. The proportion of quartz fragments colonized generally increased with MAP, from 5.9% of soil covered by colonized hypoliths at the most costal (lowest MAP) site, to 18.7% at the most inland (highest MAP) site. There was CO2 uptake from most hypoliths measured, with net carbon uptake rates ranging from 0.3 to 6.4 μmol m-2 s-1 on well hydrated hypoliths. These carbon flux values are similar to previous work in the Mojave Desert. Our results suggest that hypoliths might play a key role in the fixation of organic carbon in hyperarid ecosystems where quartz fragments are abundant, with MAP constraining hypolith abundance. A better understanding of these extremophiles and the niche they fill could give an understanding of how microbial life might exist in extraterrestrial environments similar to hyperarid deserts.
Heliobacteria are an anaerobic phototroph that require carbon sources such as pyruvate, <br/>lactate, or acetate for growth (Sattley, et. al. 2008). They are known for having one of the <br/>simplest phototrophic systems, the central component of which is a Type I reaction center (RC) <br/>that pumps protons to generate the electrochemical gradient for making ATP. Heliobacteria <br/>preform cyclic electron flow (CEF) with the RC in the light but can also grow chemotropically in <br/>the dark. Many anaerobes like heliobacteria, such as other members of the class Clostridia, <br/>possess the capability to produce hydrogen via a hydrogenase enzyme in the cell, as protons can <br/>serve as an electron acceptor in anaerobic metabolism. However, the species of heliobacteria <br/>studied here, H. modesticaldum have been seen to produce hydrogen via their nitrogenase <br/>enzyme but not when this enzyme is inactive. This study aimed to investigate if the reason for <br/>their lack of hydrogen production was due to a lack of an active hydrogenase enzyme, possibly <br/>indicating that the genes required for activity were lost by an H. modesticaldum ancestor. This <br/>was done by introducing genes encoding a clostridial [FeFe] hydrogenase from C. thermocellum<br/>via conjugation and measuring hydrogen production in the transformant cells. Transformant cells <br/>produced hydrogen and cells without the genes did not, meaning that the heliobacteria ferredoxin <br/>was capable of donating electrons to the foreign hydrogenase to make hydrogen. Because the <br/>[FeFe] hydrogenase must receive electrons from the cytosolic ferredoxin, it was hypothesized <br/>that hydrogen production in heliobacteria could be used to probe the redox state of the ferredoxin <br/>pool in conditions of varying electron availability. Results of this study showed that hydrogen <br/>production was affected by electron availability variations due to varying pyruvate <br/>concentrations in the media, light vs dark environment, use acetate as a carbon source, and being <br/>provided external electron donors. Hydrogen production, therefore, was predicted to be an <br/>effective indicator of electron availability in the reduced ferredoxin pool.
In oxygenic photosynthesis, conversion of solar energy to chemical energy is catalyzed by the<br/>pigment-protein complexes Photosystem II (PSII) and Photosystem I (PSI) embedded within the<br/>thylakoid membrane of photoautotrophs. The function of these pigment-protein complexes are<br/>conserved between all photoautotrophs, however, the oligomeric structure, as well as the<br/>spectroscopic properties of the PSI complex, differ. In early evolving photoautotrophs, PSI<br/>exists in a trimeric organization, but in later evolving species this was lost and PSI exists solely<br/>as a monomer. While the reasons for a change in oligomerization are not fully understood, one<br/>of the 11 subunits within cyanobacterial PSI, PsaL, is thought to be involved in trimerization<br/>through the coordination of a calcium ion in an adjacent monomer. Recently published<br/>structures have demonstrated that PSI complexes are capable of trimerization without<br/>coordinating the calcium ion within PsaL.<br/>5 Here we explore the role the calcium ion plays in both<br/>the oligomeric and spectroscopic properties in PSI isolated from Synechocystis sp. PCC 6803.
