Browsing by Subject "Wetland"

An abstract of a dissertation: As humans increasingly alter the surface geomorphology of the Earth, a multitude of artificial aquatic systems have appeared, both deliberately and accidentally. Human modifications to the hydroscape range from alteration of existing waterbodies to construction of new ones. The extent and ecosystem services of these systems are underexplored, but likely substantial and changing. Instead of simply accepting that artificial ecosystems have intrinsically low values, environmental scientists should determine what combination of factors, including setting, planning and construction, subsequent management and policy, and time, impact the condition of these systems. Scientists, social scientists, and policymakers should more thoroughly evaluate whether current study and management of artificial aquatic systems is based on the actual ecological condition of these systems, or judged differently, due to artificiality, and consider resultant possible changes in goals for these systems. The emerging recognition and study of artificial aquatic systems presents an exciting and important opportunity for science and society.

Irrigation ditches are ubiquitous features of water networks in rural and urban settings in drylands, and are thus potentially important habitats within the modern hydroscape. The habitat value of ditches and other artificial systems depends on whether these systems respond to local and watershed-scale land use in similar ways to natural features, or whether artificial origin inherently constrains a system's ecological condition. The ditches and creeks of Bishop, California are fed by water from the same minimally developed watershed on the Eastern slope of the Sierra Nevada Mountains, and so served to test whether artificial and natural waters in the same watershed setting and with shared water can provide similar habitat. We sampled benthic macroinvertebrates at 52 sites within the town, stratified by substrate and season. Communities varied by substrate and season as expected, but did not differ significantly between artificial and natural streams. Instead, both types of streams changed as water flowed from undeveloped desert through town, suggesting that irrigation ditches respond to local urbanization in much the same way that natural streams do. Differences in finer-scale spatial structure of community similarity suggest that community assembly processes may differ between natural and artificial channels, but potential mechanisms for these differences are unclear. This study demonstrates that artificial aquatic systems may have substantial ecological value, and suggests that the poor condition of many artificial aquatic systems may reflect stressful watershed settings rather than something intrinsic to their artificiality.

The drainage ditches of the North Carolina Coastal Plain do not merely degrade wetlands; they themselves have ecological structural characteristics of wetlands. We surveyed 32 agricultural, freeway, and forested ditch reaches across this region for hydrologic indicators, soil organic matter, and plants. All showed some hydrologic indicators and had some soil organic matter, with easterly, swampy forests having the most, though with substantial variation across all and few significant differences between types. All had hydrophytic herbaceous plant communities in the sense of at least half their percent cover belonging to obligate, facultative wetland, or facultative taxa. These herbaceous communities differed significantly across site types (F=3.25, d.f.= 2, p=0.001), and responded to both landscape-level factors like nearby development coverage and local-level factors like apparent mowing. Sample sites were not well mapped in well-used federal aquatic databases; the National Hydrography Dataset only included one on a “CanalDitch” flow line, and the National Wetlands Inventory only included two within “partially drained/ditched” areas, and none as individual “excavated” features. Others were mis-categorized, but neither database included any highway sampling sites. Despite this limited information about extent, variation and management impact suggests that human potential to impact wetland structure of these manmade aquatic ecosystems throughout the North Carolina Coastal Plain, and beyond, could be large.

Artificial lakes are a dominant aquatic ecosystem type, but the processes controlling their condition are under-explored. Here we use structural equations modeling to compare the formation of algal blooms and associated water quality issues in 1,045 artificial and 870 natural lakes in the United States using the U.S. Environmental Protection Agency’s National Lakes Assessment data. We compare chemical and physical measurements associated with water quality and the relationships between them, and find that the processes are significantly different between natural and artificial lakes, in a way that suggests impacts of interference with thermal stratification through dam management in reservoirs. However, both the overall processes and the distributions of the data are roughly similar between the two origin types, and between 2007 and 2012 sample years. Artificial lakes are lakes, and process-based explorations of their behavior can help us better know management options.

Taken together, this dissertation examines an artificial version of each of the major aquatic ecosystem types: stream, wetland, and lake. It examines the processes controlling their ecological condition with increasing intricacy with each chapter, and finds ways that artificial aquatic ecosystems are both similar to and different from natural ones. This dissertation provides a new way of looking at the constraints and opportunities that artificial waterbodies afford those in charge of them and interested in their conservation potential.

Although microbes may strongly influence wetland phosphorus (P) cycling, specific microbial communities and P metabolic processes have not been characterized in wetlands, and microbial P cycling is poorly understood across global ecosystems, especially in soils. The goal of this work is to test the effects of stress and growth factors on microbial communities in wetlands, and on microbial P metabolism and P cycling at ecosystem scales in wetland soils and beyond. I conducted field and laboratory research experiments in wetland soils, which by definition lie along gradients between terrestrial and aquatic ecosystems, and I explicitly compared results in wetlands to adjacent ecosystems to improve inference and impact.

To test relationships between microbial communities, soil stress and resource supply, I compared the distribution and abundance of uncultured bacterial communities to environmental factors across a range of wetland soils including a well-characterized P enrichment gradient, and restoration sequences on organic soils across freshwater wetland types. The strongest predictor of bacterial community composition and diversity was soil pH, which also corresponded with the abundance of some bacterial taxa. Land use and restoration were also strong predictors of bacterial communities, diversity, and the relative abundance of some taxonomic groups. Results from wetland soils in this study were similar to both terrestrial and aquatic ecosystems in the relationship of pH to microbial communities. However, patterns of biogeography I observed in wetlands differed from aquatic systems in their poor relationships to nutrient availability, and from terrestrial ecosystems in the response of microbial diversity to ecosystem restoration.

Accumulation of inorganic polyphosphate (PolyP) is a critical factor in the survival of multiple environmental stresses by bacteria and fungi. This physiological mechanism is best characterized in pure cultures, wastewater, sediments, and I used 31P-NMR experiments to test whether similar processes influence microbial P cycling in wetland soils. I surveyed PolyP accumulation in soils from different wetland types, and observed PolyP dynamics with flooding and seasonal change in field soils and laboratory microcosms. I found PolyP accumulation only in isolated pocosin peatlands, similar to patterns in the published literature. I observed rapid degradation of PolyP with flooding and anerobic conditions in soils and microcosms, and I characterized the biological and intracellular origin of PolyP with soil cell lysis treatments and bacterial cultures. While degradation of PolyP with flooding and anaerobic conditions appeared consistent with processes in aquatic sediments, some seasonal patterns were inconsistent, and experimental shifts in aerobic and anaerobic conditions did not result in PolyP accumulation in soil slurry microcosms. Similar to patterns in wetlands, I found prior observations of PolyP accumulation in published 31P-NMR studies of terrestrial habitats were limited to acid organic soils, where PolyP accumulation is thought to be fungal in origin. Fungal accumulation of PolyP may be useful as an alternative model for PolyP accumulation in wetlands, although I did not test for fungal activity or PolyP metabolism.

To evaluate relationships between microbial P metabolism and growth, I compared concentrations of P in soil microbial biomass with the soil metabolic quotient (qCO2) by compiling a large-scale dataset of the carbon (C), nitrogen (N) and P contents of soils and microbial biomass, along with C mineralization rates across global wetland and terrestrial ecosystems (358 observations). The ratios of these elements (stoichiometry) in biomass may reflect nutrient limitation (ecological stoichiometry), or be related to growth rates (Biological Stoichiometry). My results suggest that the growth of microbial biomass pools may be limited by N availability, while microbial metabolism was highly correlated to P availability, which suggests P limitation of microbial metabolism. This pattern may reflect cellular processes described by Biological Stoichiometry, although microbial stoichiometry was only indirectly related to respiration or metabolic rates. I found differences in the N:P ratios of soil microbial biomass among ecosystems and habitats, although high variation within habitats may be related to available inorganic P, season, metabolic states, or P and C rich energy storage compounds. Variation in microbial respiration and metabolic rates with soil pH suggests important influences of microbial communities and their responses to stress on metabolism and P cycling.

My dissertation research represents early contributions to the understanding of microbial communities and specific processes of microbial P metabolism in wetlands, including PolyP accumulation and Biological Stoichiometry, which underpin microbial cycling of P and C. Together, my research findings broadly indicate differences in microbial P metabolism among habitats in wetlands and other ecosystems, which suggests the prevailing paradigm of uniform P cycling by microbes will be inadequate to characterize the role of microbes in wetland P cycling and retention. While I observed some concomitant shifts in microbial communities, PolyP accumulation, and microbial stoichiometry with soil pH, land use, and habitat factors, relationships between specific microbial groups and their P metabolism is beyond the scope of this work, but represents an exciting frontier for future research studies.

Coastal wetlands are complex biogeomorphic systems that provide important ecosystem services, but our current understanding of salt marsh evolution and persistence is based on models and empirical studies of limited spatial and temporal extent. In this dissertation, I ask: How and why do coastal wetlands form and persist? Using a geospatial framework of publicly available datasets, I analyzed drivers of wetland extent along the Atlantic and Gulf coasts of the United States. Results establish that distinct modes of wetland extent (fringing and basin full wetland extent) occur at spatial scales (approximately 10^0 to 10^2 km^2) predicted by theoretical models of local feedbacks among fetch, wind erosion, and marsh building. Marsh distributions reflect interactions between these local biogeomorphic feedbacks and macroscale drivers that set boundary conditions, including estuarine-scale morphology that governs wave energy, and riverine influence affecting sediment availability and transport. These relationships varied among regions by a regionally characteristic set of factors: estuary shape complexity, depth, estuary area and relative dominance of riverine to estuary volume. Using new and existing sediment cores from tidal marshes along the Atlantic and Gulf coasts, I analyzed the timing and spatial variability of wetland formation. Although most cores formed after the stabilization of sea level subsequent to the last ice age (approximately 4000 to 6000 ybp), overwash events, connection to major riverine systems, riverine morphology and timing of peak agriculture post European settlement all created spatial and temporal variability in the age of marshes. Historic sea level rise studies dominated the literature found for this study, pointing to the need for targeted investigations of drivers of tidal marsh formation. By reimagining tidal marshes in a macroscale framework, I investigated both the spatial and temporal drivers of land-water linkages and coastal wetland formation and persistence, elucidating ultimate drivers and future impacts on coastal wetlands from environmental pressures.

Global climate is predicted to have significant impacts on the chemical, biological, and physical characteristics of wetlands and the watersheds in which they are contained. In particular, climate prediction models suggest a significant increase in extreme precipitation events - both more frequent and more intense flood and drought occurrences. A wetland model that incorporates surfacewater-groundwater interactions (WETSAND2.0) was used to investigate the potential impacts of these stochastically generated extreme events on wetland flow regimes in an urban watershed. The results predict increases in streamflow and flooding as well as drought conditions on a near yearly basis. However, the model also shows that the impact on the Sandy Creek-Duke University watershed will not be as extreme as many suggest. Although flooding will occur, it will be relatively minor and comparable to historic flows. And although droughts are also predicted, the balance of wet and dry in this wetland watershed can actually be a positive for the environment. Therefore watersheds, no matter the spatial scale, must be analyzed individually. Although some comparisons can be made between similar regions, the effects of extreme precipitation events vary greatly depending on watershed characteristics.