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Current trends toward warmer air temperatures and longer ice free seasons in Hudson Bay are expected to cause changes in Arctic marine ecosystem dynamics. Ringed seals (Phoca hispida) will likely experience changes in levels of predation, competition, and prey availability. The purpose of this thesis was to investigate seasonal, inter-annual, and spatial variation in Hudson Bay ringed seal feeding ecology. Fatty acid composition, δ15N, and δ13C varied significantly by season, suggesting seasonal changes in foraging habitat and diet. Spatial differences in ringed seal stable isotope ratios occurred between western and eastern Hudson Bay, and there was a strong relationship between spring air temperature and δ15N. Peak δ15N occurred within a range in spring air temperatures between approximately -5°C and -2°C. I propose that the high δ15N observed in ringed seals within this temperature range is indicative of relatively greater importance of capelin (Mallotus villosus) in the ringed seal diet.

Trophic ecology is a key component in describing patterns of variation between and within populations, particularly in Arctic marine systems wherein climate change is impacting food webs. This thesis investigates the trophic ecology of Arctic char (Salvelinus alpinus) in the Cumberland Sound region using a multi-indicator approach. My data show trophic niche differences between resident and anadromous ecotypes and evidence for estuarine feeding by residents. I document a shift in the marine diet of Arctic char from zooplankton to capelin (Mallotus villosus) – a novel prey species in this region – that has occurred in less than a decade. Changes in Arctic char growth imply population-level effects of this shift; however, more research is required. Finally, I find lipid effects on δ13C and lipid-extraction effects on δ15N and δ34S for Arctic char muscle tissue. Lipid-correction models did not provide adequate δ13C estimates; thus, chemical extraction or ecotype-specific validation of models is recommended.

Over the past two decades, Lake Winnipeg has been experiencing increasingly rapid eutrophication, and large cyanobacterial blooms now form in the North Basin in most years in late summer or fall. Cyanobacteria are considered a relatively poor food source compared with other phytoplankton, but the impacts of these blooms upon the primary consumers in the lake have not previously been researched. A microscopic analysis of whole water samples found cyanobacteria to be scarcely present in summer 2012, with nitrogen-fixing and non-fixing cyanobacteria comprising 11.2% and 8.4% of the basin-wide biovolume, respectively, and all but absent in fall. Gut content analysis of chironomids found that cyanobacteria made up an almost negligible part of their diet. Stable isotope analysis revealed that nitrogen-fixing cyanobacteria reduced phytoplankton δ15N values, and that this same reduction could be traced through the zooplankton, but not down to the sediments or chironomids.

A reconstruction of regional climate variability in southern West Virginia that spans the last glacial/interglacial transition is presented. Paleoclimate interpretations obtained from the 50-cm long stalagmite provide key insights regarding the timing, magnitude, and forcing mechanisms responsible for past climate variability. Stable isotopic (δ18O and δ13C) and trace element (Ba, Sr, Mg) signatures from samples contiguously milled along the growth-axis of a 230Th-dated stalagmite which grew between approximately 20 and 5 thousand years before present (kyr BP) provide critical constraints for above-cave mean annual temperature, seasonality of moisture mean annual precipitation, and potential vegetation shifts. Specifically, the stalagmite record reveals subcentennial-scale variations in the proxy records, and strong multimillennial-scale features that correlate to well-known patterns of sea-surface variability in the North Atlantic Ocean (i.e., Bond cycles). The large-scale glacial/interglacial transition is sufficiently resolved to show that regional climate changes largely paralleled climatic transitions preserved in low-latitude (Chinese monsoon records; Cariaco Basin) and high-latitude (Greenland Ice Sheet) paleo-archives. However, the Younger Dryas interval in the south-central Appalachian Mountains is not as prominent a feature as in other records.

Three small (< 1 ha) mountain wetlands located in eastern Kentucky, host populations of two rare orchids, the white fringeless orchid, Platanthera integrilabia, and the crested yellow orchid, Platanthera cristata. Recently, concern has arisen about the persistence of the orchids. To better understand these wetlands and determine if hydrology is affecting the orchid populations, a hydrologic characterization study was initiated in 2009. Each wetland was equipped with a well nest consisting of piezometers, tensiometers, and a shallow well with a data logging pressure transducer. Chemistry and stable isotopes analysis (deuterium and 18O) of groundwater and precipitation were analyzed, and soil, topographic and channel cross-section surveys were conducted. Hydrology data suggest the primary source of water is precipitation and the primary output is evapotranspiration. Between 10 and 30 cm below the soil surface soil and tensiometer data revealed the presence of a weak fragipan, which likely contributes to seasonal ponding at the site. Management recommendations include thinning and construction of debris dams to increase the hydroperiod, surface area, and total potential volume of the wetlands.

Capelin is an important forage fish species in the Northwest Atlantic and the primary prey species of many top predators. Capelin undergo extensive inshore migrations (> 350 km) to coastal spawning grounds in the spring where the timing of inshore arrival is highly variable. I investigated the influence of intrinsic factors and proxies for extrinsic factors on the timing of arrival of capelin at spawning sites on the northeast coast of Newfoundland (2012 and 2013). Despite high inter-annual variation in almost all factors examined, intrinsic factors, specifically length and age, consistently varied with timing of arrival at spawning sites for both males and females, unlike proxies for extrinsic factors. These results are important for the management of this critical fish species, as selective harvesting by the capelin fishery of early-arriving fish may impact the age/size structure of the population, recruitment, and result in increased variability in the timing of spawning.

The hydrogeology, stable isotope distribution, and chemical distribution of Cl- and NO3--N within the Battersea Drainage Basin in southern Alberta were investigated. The Battersea Drainage Basin is characterized by widespread spreading of livestock manure on irrigated farmland and a high density of feedlots, creating concern about groundwater quality in the region. Past research has used conventional piezometers to study the source, distribution and fate of nitrate in the shallow groundwater. The key component of this research involved using the new technique of high-resolution profiling to determine the distribution, source, fate, and transport of nitrate in the shallow geological groundwater environment. High-resolution profiles of δ2H indicated groundwater throughout the glaciofluvial deposits and between 5.4 and 13.7 m below ground in glaciolacustrine deposits contained values > -150.0‰ and tritiated waters (> 0.08 TU). This suggested that this water recharged within the past 60 years. At depth 5.4 to 13.5 m BG, lower δ2H values did not coincide with detectable tritium, indicating the groundwater was much older and not vulnerable to agricultural contamination. High-resolution profiles of Cl- and NO3--N (solid core and squeezed pore water data) showed concentrations of these ions up to 411 and 219 mg L-1, respectively, in the glaciofluvial deposits. Concentrations of Cl- and NO3--N decreased to less than 50 mg L-1 (Cl-) and the Drinking Water Standard for NO3--N (10 mg L-1) in the underlying glaciolacustrine and glacial till deposits at most sites. Comparison to the high-resolution δ2H profiles suggested the high nitrate concentration in the glaciofluvial sediments is agricultural in origin. High concentrations for Cl- and NO3--N (up to 257 and 209 mg L-1, respectively) observed in glacial till and glaciolacustrine deposits below 6.0 m BG at two sites (LB5a and LB6) did not coincide with modern water, indicating the source of high nitrate is geologic in origin. The NO3--N to Cl- ratios suggested denitrification was not appreciable in the glaciofluvial deposits. However, denitrification may be a cause of decreased nitrate in the underlying fine textured deposits at certain sites. Interpretation of the high resolution profiles also suggested that the major conduit for nitrate migration is in near-surface glaciofluvial sediments via advection. The distributions of δ2H, Cl- and NO3--N with depth suggest that transport in the underlying glaciolacustrine and glacial till deposits is diffusion dominated, thus acting as a sink and removing nitrate from the permeable zone. However, the presence of fracturing in the oxidized zone of glacial tills and glaciolacustrine deposits suggests that transport may occur via advection through fracturing and diffusion in the material matrix. High-resolution profiling of δ2H, Cl- and NO3--N proved to be valuable in obtaining information regarding the distribution, source, and transport of groundwater and nitrate in the shallow groundwater environment at a level of detail that cannot be readily obtained through use of conventional piezometers.

Trophic ecology is a key component in describing patterns of variation between and within populations, particularly in Arctic marine systems wherein climate change is impacting food webs. This thesis investigates the trophic ecology of Arctic char (Salvelinus alpinus) in the Cumberland Sound region using a multi-indicator approach. My data show trophic niche differences between resident and anadromous ecotypes and evidence for estuarine feeding by residents. I document a shift in the marine diet of Arctic char from zooplankton to capelin (Mallotus villosus) – a novel prey species in this region – that has occurred in less than a decade. Changes in Arctic char growth imply population-level effects of this shift; however, more research is required. Finally, I find lipid effects on δ13C and lipid-extraction effects on δ15N and δ34S for Arctic char muscle tissue. Lipid-correction models did not provide adequate δ13C estimates; thus, chemical extraction or ecotype-specific validation of models is recommended.

Over the past two decades, Lake Winnipeg has been experiencing increasingly rapid eutrophication, and large cyanobacterial blooms now form in the North Basin in most years in late summer or fall. Cyanobacteria are considered a relatively poor food source compared with other phytoplankton, but the impacts of these blooms upon the primary consumers in the lake have not previously been researched. A microscopic analysis of whole water samples found cyanobacteria to be scarcely present in summer 2012, with nitrogen-fixing and non-fixing cyanobacteria comprising 11.2% and 8.4% of the basin-wide biovolume, respectively, and all but absent in fall. Gut content analysis of chironomids found that cyanobacteria made up an almost negligible part of their diet. Stable isotope analysis revealed that nitrogen-fixing cyanobacteria reduced phytoplankton δ15N values, and that this same reduction could be traced through the zooplankton, but not down to the sediments or chironomids.