Factors affecting the concentration and flux of materials in two southern Everglades mangrove wetlands

Concentrations and fluxes of C, N, and P were measured in dwarf and fringe mangrove wetlands along the Taylor River, Florida, USA from 1996 to 1998. Data from these studies revealed considerable spatial and temporal variability. Concentrations of C, N, and P in the dwarf wetland showed seasonal trends, while water source was better at explaining concentrations in the fringe wetland. The total and dissolved organic carbon (TOC and DOC), total nitrogen (TN), and total phosphorus (TP) content of both wetlands was higher during the wet season or when water was flowing to the south (Everglades source). Concentrations of nitrate plus nitrite (NOx –), ammonium (NH4 +), and soluble reactive phosphorus (SRP) in the fringe wetland were all highest during the dry season or northerly flow (bay source). Nutrient concentrations most effectively explained patterns of flux in both wetlands. Increased wetland uptake of a given constituent was usually a function of its availability in the water column. However, the release of NOx – from the dwarf wetland was related to the NH4 + concentration, suggesting a nitrification signal. Nitrogen flux in the dwarf wetland was also related to surface water salinity and temperature. Our findings indicate that freshwater Everglades marshes are an important source of dissolved organic matter to these wetlands, while Florida Bay may be a source of dissolved inorganic nutrients. Our data also suggest that temperature, salinity, and nutrient concentrations (as driven by season and water source) influence patterns of materials flux in this mangrove wetland. Applying long-term water quality data to the relationships we extracted from these flux data, we estimated that TN and TP were imported by the dwarf wetland 87 ± 10 and 48 ± 17% of the year, respectively. With Everglades restoration, modifications in freshwater delivery may have considerable effects on the exchanges of nutrients and organic matter in these transitional mangrove wetlands.

Novel Purification of Archaeal Rnase P Protein, Pfu Rpp38, for Nmr Studies

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.