Treatment wetlands play an important role in reducing nitrogen content in wastewater and agricultural run-off water. The main removal process is denitrification and the removal efficiency depends on the hydrological and microbiological features of the wetland, especially in terms of water residence times and denitrification rates. The aim of this thesis was to increase the understanding of the coupled hydrological and microbiological processes regulating the denitrification capacity. This was done by applying a broad spectrum of analyses methods, including tracer experiment, water flow modeling, denitrification rate measurements, and analyses of the microbial community structures. The tracer experiment and flow modeling revealed that the wetland design, especially the vegetation, largely can affect the water residence time distributions in wetlands. In the investigated wetland, vegetation dominated the water flow, explaining 60-80% of the variance in water residence times, whereas basin shape only explained about 10% of the variance, but also mixing phenomena significantly affected the residence times and could considerably delay solutes. Measured potential denitrification rates in the wetland exhibited significant spatial variations, and the variations were best described by concentration of nitrogen in sediments and water residence time. Analyses of the denitrifying bacteria populations indicated that a few key populations dominated and that the community diversity increased with decreasing nutrient levels and increasing water residence times. Moreover, it was found that denitrification rates in terms of Menten and first order kinetics can be evaluated by fitting a mathematical expression, considering denitrification and other nitrogen transforming processes to measured product formation in nitrate limited experiments. / QC 20101110

Understanding the impacts of climate change is critical for improving the conservation and management of ecosystems worldwide. Ecosystems vary along a precipitation and temperature gradient, ranging from tropical jungles to arid deserts. The Great Basin is a semi-arid eco-region that is found within the western United States. Plant communities within the Great Basin range from sagebrush valleys to sub-alpine conifer forests found at high elevation areas. It is predicted that the Great Basin will experience prolonged periods of drought, more intense fires, and greater variability in average annual and monthly precipitation, all in response to changes in climate patterns. At the lower elevations, sagebrush communities are expected to experience less suitable habitat conditions, however, less is understood about vegetation response at upper elevations. Understanding forest composition and structure at these upper elevations within the Great Basin will help us better understand potential impacts from climate change. In chapter 1, we characterized Pinus longaeva (Great Basin bristlecone pine D.K. Bailey) forest structure and composition. We mapped this tree species distribution and characterized forest structure and composition using a sampling protocol that included both biophysical variables and individual tree characteristics. We collected data from 69 mixed and homogenous P. longaeva stands found within the Great Basin and Colorado Plateau. Results suggest that P. longaeva forest structure and composition exhibit high structural variability in tree characteristic measurements like density, basal area, growth rate, age, and in biophysical variables such as substrate type, slope, aspect, elevation, average monthly temperature and precipitation, latitude, and longitude. This study also found that variability in forest composition and structure in P. longaeva forests allows for greater flexibility in the breadth of life-history strategies and probable resiliency to climate change. In chapter 2 we used remote sensing images with high spatial resolution to identify 685 unique P. longaeva stands on 42 mountain ranges. Pinus longaeva was found on the White Mountains on the western edge of the Great Basin to the Colorado Plateau's Henry Mountain and West Tavaputs Plateau in the East, and from the Spring Mountains in the South to the Ruby and Spruce Mountains in the North. Stands covered 113,886 ha across the geographic distribution. A comparison between our maps and those produced by David Charlet found a total of 36% overlap of P. longaeva. We mapped 58 unique stands that the control dataset lacked and 11 stands that we did not include. We believe that this is the most comprehensive P. longaeva distribution map created to date.

Patterns of trees’ endogenous rhythmic growth (ERG) and paralleled C allocation shift between root and shoot systems have been studied, but there is still a need to understand their impact in shaping soil microbiomes. Moreover, the impact of plants on soil microbial communities can be modulated or overweighed by time-induced plant and/or seasonal changes. Thus, we intended to analyze the structure of soil microbiomes as response to simultaneous alternated host tree root and shoot flushes and time-induced changes within one vegetation period at two sites in Central Germany. In this study, we utilized oak phytometers (Quercus robur L., clone DF159) as host trees, and made use of their ERG, whereby consecutive root and shoot flushes make a complete growth cycle. We studied two complete growth cycles during the same vegetation period, performed a non-destructive soil sampling and applied high-throughput amplicon sequencing of the bacterial 16S gene and the fungal ITS2 region. As C allocation shifts between the tree root and shoot, released root exudates and consequently the nutrient availability alternate for soil microorganisms. We therefore anticipated different microbial communities in the host tree root zone along the growth cycles until autumnal leaf senescence. In our results, the bacterial community exhibited a directional change over time along the vegetation period. In contrast, the fungal community appeared sample specific. Our findings enlarge the current understanding of the temporal microbial assembly in the host tree root zone.

No description available.

No description available.

No description available.

No description available.

Soil is an important ecosystem that supports a wide variety of organisms such as bacteria, fungi, arthropods and nematodes. This sensitive ecosystem may be influenced by various factors, including agricultural management practices. With the introduction of genetically modified (GM) glyphosate-tolerant (RoundUp ® Ready: RR) crops, herbicides such as glyphosate have been increasingly used. However, little is known about the effect of glyphosate on the biological communities in these herbicide-sprayed soils. With the intimate proximity that microorganisms and nematodes have with the roots of plants, these organisms can be used to assess changes that may occur in the soil surrounding roots of RR crops. The aim of this study was to determine microbial community structure and nematode diversity, with emphasis on that of non-parasitic nematodes, in soil samples from conventional soybean (CS) - and RR- soybean fields compared to that in adjacent natural veld (NV) areas. Samples were collected from twenty three sites at six localities that are situated within the soybean-production areas of South Africa. These sites represented fields where RR and CS soybean grew, as well as surrounding NV. All RR fields have been treated with glyphosate for no less than five years. Microbial community structures of the twenty three sites in the RR, CS and NV ecosystems were determined by phospholipid fatty acid (PLFA) analyses. Nematode diversity was determined by extracting the nematodes from soil samples and conducting a faunal analysis. Soil physical and chemical properties were determined by an independent laboratory, Eco-Analytica (North West University, Potchefstroom) according to standard procedures. Results from this study indicated differences in microbial community structure between the various localities. However, there were no significant (p ≤ 0.05) differences in microbial community structures between RR- and CS ecosystems. Soils of both RR- and CS crops were primarily dominated by bacteria. Nematode identification and faunal analysis also indicated no significant (p ≤ 0.05) differences between the different non-parasitic/beneficial nematodes that were present in soils of these two ecosystems during the time of sampling. Non-parasitic nematode communities were primarily dominated by bacterivores. A faunal analysis indicated that most of the sites contained enriched, but unstructured soil food-webs. However, four of the sites showed enriched and structured food webs due to the presence of non-parasitic nematodes with high coloniser-persister (cp) values. Relationships between non-parasitic nematode – and microbial communities showed that there was a positive relationship between nematode functional groups and their corresponding microbial prey. From the results obtained in this study, it can be concluded that the community structures of both non-parasitic nematodes and microorganisms shared similarities. These community structures showed no long-term detrimental effects of glyphosate application in the soils surrounding roots of RR soybean crops. Relationships existed between non-parasitic nematode and microbial communities in the rhizosphere of soybean crops and natural veld. For example, bacterivore nematodes had a strong positive relationship with gram-negative bacteria. Similar but weaker relationships also existed between carnivores, omnivores, plantparasitic nematodes and gram-negative bacteria. A positive relationship also existed between fungivores and fungal fatty acids. This emphasises the value of these organisms as indicators of soil health and also the impact that agricultural practices can have on soils. / MSc (Environmental Sciences), North-West University, Potchefstroom Campus, 2014

Soil is an important ecosystem that supports a wide variety of organisms such as bacteria, fungi, arthropods and nematodes. This sensitive ecosystem may be influenced by various factors, including agricultural management practices. With the introduction of genetically modified (GM) glyphosate-tolerant (RoundUp ® Ready: RR) crops, herbicides such as glyphosate have been increasingly used. However, little is known about the effect of glyphosate on the biological communities in these herbicide-sprayed soils. With the intimate proximity that microorganisms and nematodes have with the roots of plants, these organisms can be used to assess changes that may occur in the soil surrounding roots of RR crops. The aim of this study was to determine microbial community structure and nematode diversity, with emphasis on that of non-parasitic nematodes, in soil samples from conventional soybean (CS) - and RR- soybean fields compared to that in adjacent natural veld (NV) areas. Samples were collected from twenty three sites at six localities that are situated within the soybean-production areas of South Africa. These sites represented fields where RR and CS soybean grew, as well as surrounding NV. All RR fields have been treated with glyphosate for no less than five years. Microbial community structures of the twenty three sites in the RR, CS and NV ecosystems were determined by phospholipid fatty acid (PLFA) analyses. Nematode diversity was determined by extracting the nematodes from soil samples and conducting a faunal analysis. Soil physical and chemical properties were determined by an independent laboratory, Eco-Analytica (North West University, Potchefstroom) according to standard procedures. Results from this study indicated differences in microbial community structure between the various localities. However, there were no significant (p ≤ 0.05) differences in microbial community structures between RR- and CS ecosystems. Soils of both RR- and CS crops were primarily dominated by bacteria. Nematode identification and faunal analysis also indicated no significant (p ≤ 0.05) differences between the different non-parasitic/beneficial nematodes that were present in soils of these two ecosystems during the time of sampling. Non-parasitic nematode communities were primarily dominated by bacterivores. A faunal analysis indicated that most of the sites contained enriched, but unstructured soil food-webs. However, four of the sites showed enriched and structured food webs due to the presence of non-parasitic nematodes with high coloniser-persister (cp) values. Relationships between non-parasitic nematode – and microbial communities showed that there was a positive relationship between nematode functional groups and their corresponding microbial prey. From the results obtained in this study, it can be concluded that the community structures of both non-parasitic nematodes and microorganisms shared similarities. These community structures showed no long-term detrimental effects of glyphosate application in the soils surrounding roots of RR soybean crops. Relationships existed between non-parasitic nematode and microbial communities in the rhizosphere of soybean crops and natural veld. For example, bacterivore nematodes had a strong positive relationship with gram-negative bacteria. Similar but weaker relationships also existed between carnivores, omnivores, plantparasitic nematodes and gram-negative bacteria. A positive relationship also existed between fungivores and fungal fatty acids. This emphasises the value of these organisms as indicators of soil health and also the impact that agricultural practices can have on soils. / MSc (Environmental Sciences), North-West University, Potchefstroom Campus, 2014

Les hydrocarbures aromatiques polycycliques (HAP) sont des polluants organiques, ubiquistes, potentiellement toxiques et cancérigènes. Dans les sols, la dégradation des HAP est principalement due à l'activité microbienne. Certaines études ont montré que la biodégradation des HAP pouvait être augmentée dans la rhizosphère des plantes où le nombre et l'activité microbienne sont stimulés, grâce aux exsudats racinaires. Cependant les bénéfices des plantes ne sont pas toujours observés, et les exsudats pourraient aussi modifier la biodisponibilité des HAP. Les objectifs de ce travail ont été de mieux comprendre ces interactions sol-plante-microorganismes qui conditionnent le devenir des HAP dans la rhizosphère en suivant notamment (i) les bactéries possédant les gènes codant une HAP-dioxygènase, (ii) les espèces bactériennes impliquées dans la dégradation du phénanthrène, et (iii) la disponibilité et la biodégradation des HAP dans des terres industrielles historiquement contaminées.Les expériences ont été conduites dans des dispositifs à compartiments, lesquels permettent une diffusion des exsudats racinaires dans le sol tout en retenant physiquement les racines, puis en microcosmes avec un ajout d'exsudats racinaires naturels produits à partir d'une culture hydroponique de ray-grass (Lolium perenne, L). Les expériences ont été réalisées dans un premier temps avec du sable en ajoutant du phénanthrène (PHE) et un inoculum bactérien issu d'un sol d'une ancienne cokerie puis directement avec des sols historiquement contaminés en HAP. Les nombres de copies de gènes codant pour l'ADNr 16S et pour des HAP-dioxygènases ont été quantifiés par PCR en temps réel pour estimer la proportion de bactéries dégradantes. Les structures des communautés ont été comparées par électrophorèses (TTGE). En plus de l'analyse des 16 HAP totaux, une extraction non exhaustive des HAP a été réalisée à la cyclodextrine pour en estimer la disponibilité. L'utilisation de la méthode SIP (stable isotope probing) avec du 13C-phénanthrène a permis d'identifier les bactéries directement impliqués sa dégradation dans un sol historiquement contaminé. Les expériences en dispositifs à compartiments ont confirmé que la dissipation du phénanthrène est plus importante lorsque la distance aux racines est plus faible, et montrent que le nombre de copies de gène 16S et de gène de HAP-dioxygénase varie avec l'âge des plantes et du temps de contact des compartiments latéraux avec le tapis racinaire. Mais elles montrent aussi que la dissipation du phénanthrène n'est pas plus importante dans les pots plantés, tandis que dans les expériences en microcosmes une inhibition de la dissipation du PHE a même été observée en présence d'exsudats. La présence d'exsudats racinaires a profondément modifié la structure des communautés dégradant les HAP, et l'expérience SIP a permis d'identifier les bactéries directement impliquées dans la dégradation du 13C-phénanthrène et de montrer qu'elles étaient différentes en présence ou non d'exsudats. En présence d'exsudats, la proportion des bactéries dégradantes dans la population totale est passée de 1 % dans la terre d'origine et dans les traitements sans exsudats à plus de 10 %. Même si les exsudats racinaires ralentissent la dissipation du phénanthrène, en fournissant une source de carbone plus facilement métabolisable, ils ont augmenté la quantité de HAP extractibles à la cyclodextrine dans deux des trois sols historiquement contaminés, suggérant un effet de ceux-ci sur la biodisponibilité des HAP / Polycyclic Aromatic Hydrocarbons (PAH) are organics pollutants, ubiquitous, toxics and potentially carcinogenic. In soil, PAH degradation is mainly attributed to microbial organism. Several studies have thus reported enhanced PAH degradation in soil in the presence of plants. Rhizospheric soil increase the number et the activity of microorganisms in soil by the release of roots exudates. However, bene?cial effects of plants in the remediation are not always observed and roots exudates could be limited PAH biodegradation. The object of this study was to investigate the fate of PAHs in rhizosphere, following (i) the PAH-dioxygenase genes DNA to quantify the PAH-degrading bacteria, (ii) species implicated in phenanthrene biodegradation, and (iii) PAH availability and biodegradation from industrial soils.Different experimental devices have been designed to study detailed processes in the rhizosphere. First is a compartments devices were a nylon mesh permits diffusion of plant soluble substances towards the adjacent root free compartment as a rhizosphere. Secondly microcosms were enriched with natural roots exudates from hydroponic culture of ray-grass (Lolium perenne L.). In first time, experiments were conducted using sand and bacterial inoculum from an industrially PAH-contaminated soil and then directly with a soil historically contaminated by PAH. The Real-Time PCR quantification of 16S rRNA gene copy and of functional PAH-RHD? genes permitted to assess the proportion of a degrading bacteria. Bacterial community structure was approached from Temporal Thermal Gradient gel Electrophoresis (TTGE) fingerprinting, and bands sequencing. Nonexhaustive cyclodextrin-based extraction technique provided a estimate of the ?labile? or available pool of PAH in soil. Use of stable isotope probing (SIP) technique with [13C]phenanthrene allowed a bacterial identification of directly implicated in industrial soil.The presence of exudates modified microbial community of PAH-degrading bacteria. SIP experiment showed that 13C-labelled PHE-degrading bacteria was different depending on the exudates input. Many species having to degrade phenanthrene were able to use exudates. Presence of root exudates increased the proportion of PAH-RHD? genes compared to the bulk soil at the beginning and in microcosms without exudates (respectively 10% and 1 %). However, phenanthene dissipation in sand or soil were weaker with root exudates and aged PAH concentrations has not shifted during incubation time. Nevertheless, the root exudates increased the PAH labile fraction extract with cyclodextrin solution into two in three soils historically contaminated