3 resultados para Archaea methanogenic

em Digital Commons at Florida International University


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Poor agreement between 3H/3He ages and CFC-11 and CFC-12 ages suggests that CFCs may not be conservative tracers in the Everglades National Park. 3H/3He ages were used to calculate the expected concentration of CFC-11 and CFC-12 in groundwater from wells 2 to 73 m deep. The expected concentrations of CFCs were compared to the measured concentrations and plots of the % CFC-12 and CFC-11 remaining offered no evidence that significant CFC removal was occurring in the groundwater at depths ≥2 m, suggesting that CFC removal occurs at shallower depths. Except where CFC contamination was suspected, CFC-11, CFC-12 and CFC-113 concentrations in fresh surface water were nearly always below solubility equilibrium with the atmosphere. Measurements of CFC-11, CFC-12 and CFC-113 in pore water indicate a 50–90% decrease in concentration 5 cm below the groundwater–surface water (GW–SW) interface. In the same 5 cm interval CH4 concentrations increased by 300–1000%. This suggested that CFCs were removed at the GW–SW interface, possibly by methane-producing bacteria. CFC derived recharge ages should therefore be viewed with caution when recharging water percolates through anoxic methanogenic sediments.

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There is increasing evidence that certain microbially-derived compounds may account for part of the aquatic dissolved organic nitrogen (DON) pool. Enantiomeric ratios of amino acids were used to assess the microbial input to the DON pool in the Florida Everglades, USA. Elevated levels of d-alanine, d-aspartic acid, d-glutamic acid and d-serine indicated the presence of peptidoglycan in the samples. The estimated peptidoglycan contribution to amino acid nitrogen ranged from 2.8 ± 0.1% to 6.4 ± 0.9%, increasing with salinity from freshwater to coastal waters. The distribution of individual d-amino acids in the samples suggests additional inputs to DON, possibly from archaea or from abiotic racemization of l-amino acids.

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Dr. Kenneth Murray, Ph.D. Assistant Professor of Biology Ribonuclease P (RNase P) is an essential and ubiquitous ribonucleoprotein enzyme primarily responsible for cleaving 5' leader sequences during tRNA maturation. RNase P comprises one essential RNA, and one protein subunit in eubacteria, five proteins in archaea, and ten in humans. Due to its homology to human RNase P, its higher stability, and simpler structure; extensive studies have been conducted utilizing the enzyme from the archaeal hyperthermophile, Pyrococcus furious (Pfu). Previous studies identified only four protein subunits associated with the archaeal RNase P. This fourprotein reconstituted particle, however, had an optimal temperature of 55°C, compared to the optimal 70°C of the wild type RNase P. Additional probing of the organism's genome database revealed a fifth RNase P protein subunit, RPP38. To facilitate further investigations of Pfu RNase complexes, we sought to develop a protocol for the purification ofRPP38. Our results, presented herein, represent the first known expression.purification protocol developed for RPP38. Briefly, we synthesized an N-terminal6x-His RPP38 fusion construct, reengineered to contain a Tobacco Etch Virus (TEV) protease cleavage site. Purification was achieved via immobilized metal affinity chromatography and reversed phase high performance liquid chromatography. Following purification the 6X-His affinity tag was removed via TEV cleavage, thus regenerating the native RPP38 protein. Purity and identity of RPP38 were confirmed by sodium dodecylsulfate - polyacrylamide gel electrophoresis and mass spectrometry, respectively. Our work is expected to contribute to our understanding ofRNase P function and tRNA maturation by providing an efficient, facile technique to express and purify Pfu RNase protein RPP38 as a means to facilitate structural and functional analyses.