A detailed limnological study of Clark's Borrow Pit Pond (SW* Sec. 30 T22N R9E, Delaware County, IN) was conducted from the spring of 1978 through the fall of 1979 to ascertain what factors regulate the abundance of Volvox aureus, a major phytoplanktor of the pond. This algal species often dominates the spring and sometimes fall phytoplankton blooms that occur annually, but disappears fran the plankton throughout the remainder of the year.Laboratory growth experiments suggest that the spring peak of V. aureus (105 colonies ml-l in 1978) is most likely induced by the high nutrient levels in the pond (total P = 4.6 µmoles ℓ-1; NO3 - N + NH3 - N = 11.8 Wholes 2-1) and warming temperatures. Competition from other algal species is reduced at this time by the presence of the zooplanktor Da hnia ambigua which effectively grazes all but the V. aureus colonies. Decreased nutrient levels in the summer months (total P = 1.0 µmoles Z-1 N03 - N + NH3 - N = 1.3 µmoles Z-1 ) restrict the abundance of V. aureus, and other algal species (notably blue-greens) dominate. Two of these species, Oscillatoria sp. and Microcystis sp., were shown to exhibit no allelopathic influences on the growth of V. aureus. However, experiments suggested a heat labile inhibitor or inhibitors of V. aureus may periodically affect its growth in the pond. Increasing nutrient levels in the fall sometimes induce a second V. aureus bloom, but this declines rapidly as the water temperature drops below 10° C. Consequently, the abundance of V. aureus in Clark's Pond is influenced mainly by abiotic factors (nutrient availability and water temperature) and only to a lesser degree by biotic factors (grazing and competition).

The impacts of oil sands processed materials (OSPM) on phytoplankton and periphyton community growth and stable carbon and nitrogen isotopes were examined. Estimates of plankton and periphyton community growth, measured as chl a and dry weight, were low and similar in reference and OSPM reclamation wetlands. The use of stable isotope analyses revealed higher δ15N of plankton and periphyton in OSPM wetlands than reference wetlands, possibly due to increased TN concentrations in some OSPM wetlands. In the laboratory, water-soluble fractions (WSF) of two types of OSPM (mature fine tailings, MFT and consolidated tailings, CT) and an amendment material (peat-mineral mixture), potential fill materials in wetland or end pit lake reclamation, were examined for phytoplankton community growth and stable carbon and nitrogen isotopes. All WSF treatments had higher chl a compared to reference water and maximum growth was observed at a 50:50 ratio of peat:CT or peat:MFT. In general, WSFs of peat had the highest concentration of total nitrogen (TN) whereas WSFs of MFT had the highest total phosphorus (TP; 3x higher). The results suggested that the addition of peat as an amendment to OSPM (particularly for MFT), contributing additional TN, could improve phytoplankton community growth in oil sands reclamation. At higher percentages of MFT WSF, there was increased turbidity due to fine clay particles that likely contributed to reduced phytoplankton growth. Turbidity could be an important factor limiting phytoplankton growth and thus reducing dietary resources and biological detritus (via sedimentation) in the initial development of an end pit lake. The WSFs also promoted the unfavourable growth of filamentous algae, highest at intermediate concentrations of peat and CT WSFs and inhibited in MFT WSFs due to light limitation. Stable N isotopes of plankton and filamentous algae suggests that 15N enrichment of algae could be a useful indicator of nutrient inputs, including OSPM seepage into natural aquatic systems, for oil sands regional monitoring programs.

Several lines of evidence suggest small alpine lakes and ponds are sensitive to nitrogen deposition. Paleolimnological studies, nutrient bioassays, and mesocosm experiments show the positive effects of nitrogen on aquatic alpine primary producers. In particular, alpine pond ecosystems have been inferred to be nitrogen-limited based on low availability of dissolved inorganic nitrogen relative to total phosphorus. However, nitrogen-limitation of alpine ponds has never been tested at the whole-ecosystem level. I performed a replicated in situ whole-pond experiment, consisting of two crossed treatments (2 nitrogen x 2 phosphorus levels) applied across 16 natural alpine ponds (n = 4) immediately following ice-out in 2008. Surprisingly, neither nutrient amendment stimulated phytoplankton or zooplankton abundance although subtle shifts in community composition were detected over a two-month period. Intensive grazing pressure exerted by high densities (> 100 individuals/ m2) of herbivorous Branchinecta paludosa (fairy shrimp) may have suppressed planktonic responses to nutrient additions. Another ecological explanation for the lack of a positive effect of nutrients on phytoplankton abundance was competition from periphyton, which are comparatively more abundant in most shallow ponds on an areal basis. Therefore, density-dependent ecological interactions (competition and predation) may mediate the responses of phytoplankton to nitrogen deposition over ponds situated in extreme environments. / Ecology

Graduation date: 1987

The present study, planned as a quantitative investigation of the phytoplankton of Kaneohe Bay, Hawaii, over a period of one year, was undertaken to supplement present knowledge of seasonal, distributional, floristic, and ecological features of the phytoplankton in Kaneohe Bay. The objectives of this study were: 1. To identify and enumerate phytoplankton collected at selected stations at re~ular intervals over a period of one year 2. To attempt to determine the factors that control variations in the qualitative and quantitative makeup of the phytoplankton 3. To relate the quantitative data obtained in this study with other ecological data obtained by other investigators in a concurrent study. / Typescript. Thesis (M. S.)--University of Hawaii at Manoa, 1972. Bibliography: leaves [106]-109.

Two small subarctic lakes were eutrophicated due to wastewater discharge from 1964. In 1975, a wastewater treatment plant was built and a recovery process started. This paper will: (1) compile the 1972–1974, 1978–1980 and 1985–1988 investigation data regarding phosphorous and microalgae for one of the lakes; (2) complement with unpublished data from 1985 and 2003; and (3) introduce a discussion regarding three alternatives for future development of the lakes in their last phase of recovery. In the latest investigation, 2003, the lakes were assessed as almost recovered. They had returned to an oligotrophic state, but not fully to a pre-sewage situation. In the upper lake, more heavily polluted, the total phosphorous levels had decreased from an average of 168 µg P/L in 1972–1974 to an average of 12 µg P/L in 2003. The phytoplankton biomass had decreased twentyfold during the same period, from 11.2 mg/L to 0.6 mg/L. The Secchi depth had increased from 1.3 m to 2.8 m. The low oxygen level in late winter was still not recovered, thereby profoundly affecting residential organisms in the lakes. The low winter oxygen is assumed to remain so for a long time due to phosphorus release from sediments in the lakes.

Since the 'discovery' of the high abundance of viruses in aquatic environments, it has been generally assumed that viruses in lakes are similar to those in oceans. I directly compared these two systems using a large, robust data set. Viral abundance was significantly different among the surveyed environments. The relationship between viral and bacterial abundance indicated a fundamental difference between lakes and oceans, and suggested that viruses infecting phytoplankton may be more important in lakes. Molecular techniques (PCR & DGGE) were used to document spatial and temporal variations in the richness of viruses that infect eukaryotic phytoplankton (Phycodnaviridae) in lakes at the Experimental Lakes Area (ELA). Phycodnavirus richness was highest in the eutrophic lake, and during the spring/early summer in all the lakes. Viral richness was closely associated with phytoplankton abundance and composition. As a result, richness was influenced by trophic status, while patterns of richness were affected by regional climatic conditions. Phylogenetic analysis of environmental Phycodnavirus DNA polymerase (pol) sequences indicated that freshwater Phycodnaviruses are genetically different from cultured isolates and marine environmental sequences. A genetic distance analysis indicated that pol sequences > 7 % different infected different host species. Therefore, the 20 different freshwater sequences likely infected nine different hosts. Multivariate statistics identified seven possible phytoplankton hosts, including chlorophytes, chrysophytes, diatoms and dinoflagellates. Finally, the modified dilution experiment was evaluated as an approach for estimating viral-mediated phytoplankton mortality in two lakes at the ELA. Experiments resulted in non-significant apparent growth rate regressions. While a model analysis, indicated that the method was sensitive to poorly constrained parameters such as burst size and length of the lytic cycle, making it unsuitable for estimating mortality rates in these lakes. These studies indicate that Phycodnaviridae are a genetically rich and dynamic component of lakes. Their richness is influenced by both the chemical and physical components of their environment. Although the presence of these viruses indicates that they are a source of phytoplankton mortality, the magnitude of their impact on structuring phytoplankton communities awaits methodological advances. Nonetheless, these findings support the view that viruses infecting phytoplankton are ecologically important components of lake ecosystems.

Typescript (photocopy) / xiii, 207 leaves : ill. ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--University of Adelaide, Dept. of Botany, 1982

Agricultural runoff is a major non-point source of phosphorus (P) and nitrogen (N) in aquatic environments and often contributes to coastal eutrophication. Chemical extraction techniques that measure P and N in runoff and sediments have provided little information on biologically available P and N, particularly when soils/sediments move from an agricultural setting to freshwater, estuarine and marine systems. The aims of this thesis were to a) develop algal bioassay techniques for assessing bioavailability of P in marine and freshwater sediments, b) apply algal bioassays to determine the role of suspended sediments as P and N sources c) examine how sediment type and sediment load affect P bioavailability and identify the chemical analysis of soil P that best reflects bioavailable P, and d) determine nutrient bioavailability of agricultural soil runoff in estuarine and coastal marine ecosystems. An accurate and repeatable sediment bioassay was developed using non-axenic uni-algal cultures of the euryhaline diatom Skeletonema costatum and freshwater chlorophyte Selenastrum capricornutum. Bioassays were conducted in 250 mL Erlenmeyer flasks, with 100 mg L-1 of simulated sediment and 100 mL of modified growth media, which were continuously shaken. Suspended sediments were simulated from 7 major soil types of the Maroochy River catchment in Australia, a coastal catchment influenced by agriculture. Simulated sediments were used as the sole P source in replicate batch 7-14 d bioassays in which changes in in vivo Chl a fluorescence were measured. Maximum algal biomass in bioassays was significantly correlated to total sediment P content of the added sediment in marine and freshwater. Bioassay methodology was adapted to assess N as well as P bioavailability in simulated suspended sediments using Skeletonema costatum. S. costatum biomass was significantly influenced by sediment type and correlated with the Total P content of the sediment. Conversely, S. costatum response did not correlate to total nitrogen (TN), ammonium (NH4+), nitrate (NO3-) and easily mineralisable N content of the sediment. Sediment type did significantly influence response, suggesting that sorption/desorption properties of the sediment influenced N bioavailability. Suspended sediments appear to be a significant source of bioavailable P as S. costatum biomass was enhanced by their addition. Conversely, the lack of stimulation by sediments when used as a N source implies that suspended sediments are not an immediate source of bioavailable N, although they do contribute to the sediment nutrient pool once deposited. The influence of sediment type and sediment load on phosphorus (P) bioavailability was compared using Skeletonema costatum bioassays. The amount of sediment and associated P load influenced the maximum algal biomass reached, with low sediment loads (&lt 100 mg L-1) capable of stimulating high algal biomass. Maximum algal biomass correlated with sediment iron-oxide extractable inorganic P (FeO-P) and inorganic P (Pi) extracted by sodium bicarbonate for all sediment types. Total P (TP) did not discriminate at low TP concentrations and organic P (Po) extracted by sodium bicarbonate only correlated with algal biomass when bioavailable P was low. Thus FeO-P and Pi are the most representative analyses of bioavailable P. FeO-P can also be used to accurately measure rate of sediment P desorption, which significantly influences algal growth rate. Nutrient bioavailability of agricultural soil runoff was investigated in the Maroochy River catchment in southeast Queensland Australia, a coastal catchment influenced by agriculture. Suspended sediments, river and estuarine sediments and deposited sediment in the near-shore coastal zone were collected and analysed for nutrient bioavailability using chemical analyses and S. costatum bioassays. Suspended sediments in the Maroochy River, which consisted of silt and clay sized particles, had elevated FeO-P and TP concentrations comparable to fertilised soil. Similarly the deposited sediment sampled offshore to the river mouth had elevated total P, FeO-P and total N concentrations which were much greater than the underlying marine sediment. The deposited offshore sediment contained mainly silt sized particles and appeared to be terrigenous in origin as it was more similar in composition (TP, FeO-P, TN, total carbon, total aluminium, total iron, total silica) to estuarine suspended sediments and terrestrial soils, than the underlying marine sediment. This study demonstrated that fine silt sized particles, rich in bioavailable P and N, are being transported and deposited offshore during erosion events. These findings highlight the importance of effective land management and erosion control measures that reduce the suspended sediment load. Although agricultural practices are continually improving to reduce soil erosion, practices need to encompass a broader approach that emphasizes the link between land and sea. Effective management must consider agricultural productivity as well as the environmental impact or ‘algal bloom potential’ that a soil may have when eroded into a waterway. Soils high in bioavailable nutrients must be targeted and managed effectively, particularly in areas prone to erosion.

Marine phytoplankton ecophysiological state and primary production measurements have typically been controversial due to potential impacts of measurement techniques. Advances in chl-a fluorescence techniques have provided a means for rapid, non-invasive measurement of electron transport through photosystem 2 (PSII) in dilute phytoplankton suspensions. While studies on higher plants have outlined a close relationship between PSII electron transport and carbon fixation, results from studies on microalgae reveal significant variations in the relationship. Three species of phytoplankton representing three major taxonomic groups of the marine phytoplankton were used in this study: (1) Chaetoceros muelleri CS176 Lemmermann (Bacillariophyta), (2) Isochrysis galbana CS177 Parke (Haptophyta) and, (3) Nannochloropsis oculata CS179 (Droop) Hibberd (Ochrophyta, eustigmatophyte). Each species was cultured in semicontinuous culture and primary production was estimated using oxygen evolution and carbon fixation techniques and compared against predictions based on chl-a fluorescence measurements. It was found that predicted values of primary production both under-estimated and overestimated actual carbon fixation measured via radioisotope (14C) techniques. This variation was primarily explained by probable errors in the assumed values for PSII density. The relationship between oxygen evolution or carbon fixation with chl-a fluorescence-derived measures was commonly linear below the light saturation parameter, with a departure from linearity occurring at higher irradiances. This departure from linearity was greatest in cultures adapted to low light conditions. At higher light intensities alternative electron pathways such as the Mehler reaction and/or chlororespiration are likely to be more active in low light-adapted cultures, leading to this greater non-linearity. Chl-a fluorescence measurements were also found to be a useful in characterising ecophysiology using photosynthesis-versus irradiance curves. However, an important caveat on this is the measurement of PSII density (çPSII) rather than use of an assumed value as changes in çPSII can have a profound impact on light curve parameters. A field study in Fremantle Harbour found a healthy (negligible nutrient starvation), diatom dominated, phytoplankton community. Results suggest that phytoplankton are able to begin boosting photosynthetic capability just prior to morning twilight. Waters in the harbour were well mixed via tidal motion and substantial midday photoinhibition was not observed. Data suggest levels of primary production at the mouth of the harbour are similar to those of coastal waters in the plume of the Ocean Reef wastewater outfall.