Mary Jane Carmichael

Mn(II)-Oxidizing Bacteria Are Abundant And Environmentally Relevant Members Of Ferromanganese Deposits In Caves Of The Upper Tennessee River Basin

The upper Tennessee River Basin contains the highest density of our nations caves; yet, little is known regarding speleogenesis or Fe and Mn biomineralization in these predominantly epigenic systems. Mn:Fe ratios of Mn and Fe oxide-rich biofilms, coatings, and mineral crusts that were abundant in several different caves ranged from ca. 0.1 to 1.0 as measured using ICP-OES. At sites where the Mn:Fe ratio approached 1.0 this represented an order of magnitude increase above the bulk bedrock ratio, suggesting that biomineralization processes play an important role in the formation of these cave ferromanganese deposits. Estimates of total bacterial SSU rRNA genes in ferromanganese biofilms, coatings, and crusts measured approximately 7×107–9×109 cells/g wet weight sample. A SSU-rRNA based molecular survey of biofilm material revealed that 21% of the 34 recovered dominant (non-singleton) OTUs were closely related to known metal-oxidizing bacteria or clones isolated from oxidized metal deposits. Several different isolates that promote the oxidation of Mn(II) compounds were obtained in this study, some from high dilutions (10–8–10–10) of deposit material. In contrast to studies of caves in other regions, SSU rRNA sequences of Mn-oxidizing bacterial isolates in this study most closely matched those of Pseudomonas, Leptothrix, Flavobacterium, and Janthinobacterium. Combined data from geochemical analyses, molecular surveys, and culture-based experiments suggest that a unique consortia of Mn(II)-oxidizing bacteria are abundant and promoting biomineralization processes within the caves of the upper Tennessee River Basin.

Increased Abundance Of Gallionella Spp., Leptothrix Spp. And Total Bacteria In Response To Enhanced Mn And Fe Concentrations In A Disturbed Southern Appalachian High Elevation Wetland

The Sorrento wetland hosts several Fe- and Mn-rich seeps that are reported to have appeared after the area was disturbed by recent attempts at development. Culture-independent and culture-based analyses were utilized to characterize the microbial community at the main site of the Fe and Mn seep. Several bacteria capable of oxidizing Mn(II) were isolated, including members related to the genera Bacillus, Lysinibacillus, Pseudomonas, and Leptothrix, but none of these were detected in clone libraries. Most probable number assays demonstrated that seep and wetland sites contained higher numbers of culturable Mn-oxidizing microorganisms than an upstream reference site. When compared with quantitative real time PCR (qPCR) assays of total bacteria, MPN analyses indicated that less than 0.01% of the total population (estimated around 109 cells/g) was culturable. Light microscopy and fluorescence in situ hybridization (FISH) images revealed an abundance of morphotypes similar to Fe- and Mn-oxidizing Leptothrix spp. and Gallionella spp. in seep and wetland sites. FISH allowed identification of Leptothrix-type sheath-forming organisms in seep samples but not in reference samples. Gallionella spp. and Leptothrix spp. cells numbers were estimated using qPCR with a novel primer set that we designed. Results indicated that numbers of Gallionella, Leptothrix or total bacteria were all significantly higher at the seep site relative to the reference site (where Gallionella was below detection). Interestingly, numbers of Leptothrix in the seep site were estimated at only 107 cells/g and were not statistically different in the late summer versus the late winter, despite dramatic changes in sheath abundance (as indicated by microscopy). qPCR also indicated that Gallionella spp. may represent up to 10% (3 × 108 cells/g) of the total bacteria in seep samples. These data corroborate clone library data from samples taken in October 2008, where 11 SSU rRNA sequences related to Gallionella spp. were detected out of 77 total sequences (roughly 10–15%), and where Leptothrix sequences were not detected. Analysis of this SSU rRNA clonal library revealed that a diverse microbial community was present at seep sites. At a 3% difference cutoff, 30 different operational taxonomic units were detected out of 77 sequences analyzed. Dominant sequence types clustered among the beta- and gamma- Proteobacteria near sequences related to the genera Ideonella, Rhodoferax, Methylotenera, Methylobacter, and Gallionella. Overall, results suggest that high metal concentrations at the seep sites have enriched for Fe- and Mn-oxidizing bacteria including organisms related to Gallionella and Leptothrix species, and that members of these genera coexist within a diverse microbial community.

Sustained Anthropogenic Impact In Carter Saltpeter Cave, Carter County, Tennessee And The Potential Effects On Manganese Cycling

Anthropogenic impact is a pervasive problem in heavily trafficked cave systems and fecal contamination is equally problematic in many cave and karst waters worldwide. Carter Saltpeter Cave in Carter County, Tennessee exhibits Mn(III/IV) oxide coatings associated with groundwater seeps, as well as manganese oxide growth on litter. Culturing results revealed that Mn(III/IV) oxide production on litter was associated with Mn(II)-oxidizing fungi. Immediately prior to this study, a massive Mn(II)-oxidizing biofilm bloomed at a cave seep. During the course of this study from 2009–2011, the seep exhibited a dramatic visual reduction in Mn(III/IV) oxide production, which was hypothesized to correlate with a decrease in fecal nutrient input. Molecular methods (16S rRNA gene sequencing) confirmed the presence of Bacteroides-Prevotella human fecal indicators in this seep, and most probable number assays and ion chromatography of the associated seep water confirmed nutrient loading at the site. Further, phylogenetic analysis from clone sequences suggested a strong initial human-specific fecal signature (50% of the sequences clustering with human feces sequences) in July 2009, and a weaker human signature (20% clustering) by June 2011. Most Probable Number (MPN) analyses of heterotrophic bacteria at this site suggested that Mn(II) oxidation was correlated with heterotrophic activity, due to point source exogenous nutrient loading.

Nutrient input influences fungal community composition and size and can stimulate manganese (II) oxidation in caves.

Little is known about the fungal role in biogeochemical cycling in oligotrophic ecosystems. This study compared fungal communities and assessed the role of exogenous carbon on microbial community structure and function in two southern Appalachian caves: an anthropogenically impacted cave and a near-pristine cave. Due to carbon input from shallow soils, the anthropogenically impacted cave had an order of magnitude greater fungal and bacterial quantitative-polymerase chain reaction (qPCR) gene copy numbers, had significantly greater community diversity, and was dominated by ascomycotal phylotypes common in early phase, labile organic matter decomposition. Fungal assemblages in the near-pristine cave samples were dominated by Basidiomycota typically found in deeper soils (and/or in late phase, recalcitrant organic matter decomposition), suggesting more oligotrophic conditions. In situ carbon and manganese (II) [Mn(II)] addition over 10 weeks resulted in growth of fungal mycelia followed by increased Mn(II) oxidation. A before/after comparison of the fungal communities indicated that this enrichment increased the quantity of fungal and bacterial cells, yet decreased overall fungal diversity. Anthropogenic carbon sources can therefore dramatically influence the diversity and quantity of fungi, impact microbial community function, and stimulate Mn(II) oxidation, resulting in a cascade of changes that can strongly influence nutrient and trace element biogeochemical cycles in karst aquifers.

Water Source Utilization in Taxodium distichum (L.) Rich. (baldcypress) over the Course of a Growing Season in a Restored Coastal Freshwater Wetland Vulnerable to Saltwater Incursion

ABSTRACT  Stable isotopic analysis of water use patterns in wetland vegetation can provide insight into the anticipated ecophysiological response of individual species to seasonal and/or episodic changes in water quality such as saltwater incursion into freshwater wetland ecosystems. In this study, variation in water source utilization over the course of a growing season was investigated in Taxodium distichum (baldcypress), a foundational species in both naturally occurring wetlands and regional wetland restoration projects in the southeastern United States. Over the course of the 2014 growing season, water use patterns were monitored in three baldcypress stands at the Timberlake Observatory for Wetland Restoration (TOWeR) in Tyrrell County, North Carolina, by comparing the isotopic composition (δ2H and δ18O) of xylem water extracted from plant tissue to that of the available water sources: surface water, sediment porewater, groundwater sampled from multiple locations in the region, and rainwater. Results indicate that water sources that are impacted by periodic saltwater incursion may be utilized by baldcypress at TOWeR, but the short-term health and reproductive competency of baldcypress at the site has not been negatively impacted by seasonal, episodic, surface water salinity incursions at the site.