Thesis (M.S.)--Naval Postgraduate School, 1975. / Includes bibliographical references (leaves 72-75).

University, Diss., 2005--Kiel.

abstract: Phytoplankton comprise the base of the marine food web, and, along with heterotrophic protists, they are key players in the biological pump that transports carbon from the surface to the deep ocean. In the world's subtropical oligotrophic gyres, plankton communities exhibit strong seasonality. Winter storms vent deep water into the euphotic zone, triggering a surge in primary productivity in the form of a spring phytoplankton bloom. Although the hydrographic trends of this "boom and bust" cycle have been well studied for decades, community composition and its seasonal and annual variability remains an integral subject of research. It is hypothesized here that proportions of different phytoplankton and protistan taxa vary dramatically between seasons and years, and that picoplankton represent an important component of this community and contributor to carbon in the surface ocean. Monthly samples from the Bermuda Atlantic Time-series Study (BATS) site were analyzed by epifluorescence microscopy, which permits classification by morphology, size, and trophic type. Epifluorescence counts were supplemented with flow cytometric quantification of Synechococcus, Prochlorococcus, and autotrophic pico- and nanoeukaryotes. Results from this study indicate Synechococcus and Prochlorococcus, prymnesiophytes, and hetero- and mixotrophic nano- and dinoflagellates were the major players in the BATS region plankton community. Ciliates, cryptophytes, diatoms, unidentified phototrophs, and other taxa represented rarer groups. Both flow cytometry and epifluorescence microscopy revealed Synechococcus to be most prevalent during the spring bloom. Prymnesiophytes likewise displayed distinct seasonality, with the highest concentrations again being noted during the bloom. Heterotrophic nano- and dinoflagellates, however, were most common in fall and winter. Mixotrophic dinoflagellates, while less abundant than their heterotrophic counterparts, displayed similar seasonality. A key finding of this study was the interannual variability revealed between the two years. While most taxa were more abundant in the first year, prymnesiophytes experienced much greater abundance in the second year bloom. Analyses of integrated carbon revealed further stark contrasts between the two years, both in terms of total carbon and the contributions of different groups. Total integrated carbon varied widely in the first study year but displayed less fluctuation after June 2009, and values were noticeably reduced in the second year. / Dissertation/Thesis / M.S. Microbiology 2010

Coastal hydrodynamics regulate population dynamics through the distribution and dispersal of the meroplankton of many benthic invertebrates. I examined the hydrodynamics at four different sites on the south-east coast of South Africa and coupled them with larval sampling done at high temporal and spatial resolution. Day and night sampling was done at all four sites and a continuous 24 hour study was done in one site, both forms of sampling were carried out in autumn and spring. Samples were taken at two stations, 900 metres offshore and 300 metres apart, within each site. Water properties measured were depth, temperature and current velocity and direction. Plankton samples were collected using a plankton pump at various depths, from the surface, bottom and either side of the thermocline when present. A wide range of taxa (mostly bryozoans, bivalves, barnacles and decapods) was examined. 2-way ANOVAs were used to test the effects of time and depth on each taxon. In addition, multiple regression analyses were performed on each taxon to investigate the effects of hydrodynamics on the distribution of larvae. Bryozoanlarvae proved to be positively phototactic whilst bivalve veligers, barnacle larvae and decapod zoeae performed diel vertical migration. Turbulence and temperature had an effect on the vertical distribution/migration of decapod zoeae. These results highlight the role of taxon-specific responses to flow and the potential differential effects on larval retention and ultimately connectivity of benthic populations.

Les symbioses ont un role majeur dans le fonctionnement et l'equilibre des ecosystemes. Dans les oceans, qui couvrent pres de 70 % de la surface de la planete, vivent une multitude d'organismes incapables de lutter contre les courants et la plupart sont microscopiques, il s'agit du plancton. Les organismes du plancton, comme ceux d'autres ecosystemes, entretiennent des symbioses, mais la nature et l'ampleur de ces interactions sont encore mal connues dans le plancton du fait la petite taille de ces organismes et de la difficulte d'echantillonnage des ecosystemes planctoniques, surtout dans les zones les plus eloignees des cotes. Les principaux objectifs de cette these sont de donner un apercu global de la place occupee par ces symbioses dans le plancton et de proposer des methodes originales permettant leur detection. Les travaux presentes dans ce manuscrit s'appuient sur l'analyse des donnees generees lors de l'expedition Tara Oceans (2009-2013) pendant laquelle 210 stations oceaniques ont ete echantillonnees a travers le monde. Ils concernent plus precisement le jeu de donnees environnemental obtenu grace au sequencage a haut debit (Illumina) de la region hypervariable V9 (130 nucleotides) de la sousunite 18S de l'ADN ribosomique des organismes eucaryotes (metabarcoding). Dans un premier temps, un etat des lieux de la diversite et de la structure des communautes du pico-nano-micro-mesoplancton (0,8-2000 μm) eucaryote de la zone photique des oceans temperes a tropicaux est realise. Il met en evidence la place importante occupee par les symbiotes au sein de ces communautes. Ensuite, l'etude de deux cas de symbiose (Blastodinium- Copepodes et Symbiodinium-Tiarina) montre les difficultes inherentes a la detection de couples symbiotiques a partir d’un jeu de donnees issue d'etudes par metabarcoding du plancton (flexibilite de la specificite des symbioses dans le plancton), mais aussi la possibilite de distinguer les differentes phases de vie des symbiotes (libres et symbiotiques) lorsque les echantillons etudies ont ete fractionnes. Enfin, un ensemble de methodes est propose afin d'ameliorer l'efficacite de la detection de symbioses dans le cadre d'etudes par reseau de cooccurrences des communautes planctoniques. L'analyse de la distribution des metabarcodes le long des fractions de taille (piconano- (0.8-5 μm), nano- (5-20 μm), micro- (20-180 μm), et meso-plancton (180-2000 μm)) permet de differencier ceux provenant d'organismes symbiotiques de ceux d'organismes libres, sans a priori. De plus la comparaison de l'abondance de groupes genetiques definis a differents niveaux de resolution permet de detecter des associations symbiotiques peu specifiques et d'apprecier leur niveau de specificite. / The oceans, which cover nearly 70 % of the earth's surface, is host to a myriad of mostly microscopic organisms that drift with the currents and are collectively called plankton. As in other ecosystems, symbioses play a major role in the functioning and equilibrium of the plankton. But the exact nature and strength of those symbiotic interactions are still poorly known, not only due to the small size of most planktonic organisms, but also because of the inherent difficulty of sampling planktonic ecosystems, especially in the high-seas. The main goals of this thesis are to give a global view of the importance of planktonic symbioses and to propose novel methods for their detection. The work presented in this manuscript is based on analyses of data generated during the Tara Oceans expedition (2009-2013), during which sea water was collected and size fractionated by filtration at 210 sampling locations distributed across the world's oceans. The data analyses presented herein mostly focus on an environmental metabarcoding dataset obtained from next-generation sequencing (Illumina) of the V9 hypervariable region (~130 nucleotides long) of the 18S small ribosomal subunit of eukaryotic organisms. We begin by assessing the diversity and structure of pico-, nano-, micro and meso-planktonic eukaryotic communities (0.8-2000 μm) in the photic zone of tropical to temperate sea regions. Then, we present two cases of symbioses (Blastodinium-Copepods and Symbiodinium-Tiarina) to illustrate both the difficulties encountered when trying to detect symbiotic relationships using metabarcoding data due to varying specificities of symbiotic relationships, but also the potential solutions offered by size-fractionated sampling to distinguish between the different stages of the life cycle of symbiotic organisms (free living and symbiotic stages). Finally, we propose a set of methods to improve the detection of symbioses by studying the co-occurrence of organisms in planktonic communities: we use the distribution of metabarcodes along size fractions ((piconano- (0.8-5 μm), nano- (5-20 μm), micro- (20-180 μm), and meso-plancton (180-2000 μm)) to distinguish likely free living organisms from those that have a symbiotic life style, and we compare the abundance of genetic groups constructed by clustering metabarcodes at different resolution levels, which allows us to detect interactions occurring above the species level and to evaluate their level of specificity.

Apparatus has been designed and developed for determining the response of the plankton Crustacean Simocephalus serrulatus (Koch) to horizontal gradients of light and temperature. These factors were varied independently or combined under standardized conditions. The temperature preferendum for this organism, cultured in a constant environment, was found to be 19.13°C, for animals previously held at 19°C. for 14 hours. The steepness of a temperature gradient was shown to influence the rate of aggregation at a preferendum temperature. At a constant temperature (temperature preferendum) reactions to light were then studied. Light intensity, gradients of light intensity, light quality, and gradients of light quality were considered. Animals were positively phototactic to the range of visible light intensities considered, but became indifferent to light on the addition of chemical substances to the water medium. An absolute optimum light intensity was demonstrated, at which the response to light is greatest in magnitude. The rate of rise of light intensity was shown to be directly related to the magnitude of the response and indirectly related to the time for the response to reach a peak up to the absolute optimum light intensity. The intensity of illumination was inversely related to the time for adaptation to occur. The magnitude of the light response was inversely related to the intensity of a pre-adaptation light stimulus. Wave lengths in the region of 3000 to 3500 Å, with a mean value of approximately 3300 Å, were shown to reverse the primary sign of the phototactic response. The spectral sensitivity curve for the positive phototactic response to visible light extended from 4000 to 6400 Å. Finally, light factors were applied to the animals in a temperature gradient and quantitative data on the response obtained. The interaction of the two factors produced a response which is the resultant of the factors acting in opposition. / Science, Faculty of / Zoology, Department of / Graduate

The SELECT model (Frost, 1982) is analyzed, criticized, and extended to embrace new information about the feeding behaviour of copepods and the structure of the planktonic food web in a series of alternative models. Diel variations in photosynthesis, grazing, and predation on copepods (temporal structure) and patchiness of zooplankton and their predators (spatial structure) are modelled in other variants. It is observed that the vertical, temporal, and (horizontal) spatial structure of the planktonic ecosystem are important components of ecosystem models that can not safely be ignored. It is further observed that a convincing mechanism for the termination of diatom blooms is lacking and should be a subject of intensive research, and that the status of chlorophyll-containing microflagellates as phototrophs is questionable and should be reconsidered. / Science, Faculty of / Zoology, Department of / Graduate

This thesis presents a quantitative model of interactions among phytoplankton, nutrients, bacteria and grazers in an enclosed marine ecosystem. The enclosed system was a 23 m deep, 9.6 m diameter column of surface water in Saanich Inlet, British Columbia. Dynamics of large- and small-celled diatoms and flagellates in response to observed irradiance and zooplankton numbers and observed or simulated nitrogen and silicon concentrations were modelled over a simulated 76-day period between July 12 and September 26. The model's predictions poorly matched the observed events in Controlled Experimental Ecosystem 2 (CEE2), but nevertheless provided some important insights into system behavior. Ciliate grazing probably prevented small-celled phytoplankton from increasing to large concentrations in CEE2. By virtue of their tremendous numbers, colourless flagellates were potentially the most important grazers on bacteria, much more important than larvaceans or metazoan larvae. Whereas small-celled phytoplankton were limited by grazers, large phytoplankton dynamics were not markedly affected by grazing. The average observed rate of 14C fixation in the surface 8 m was roughly consistent with an interpretation in which artificial additions of nitrogen contributed 62% of inferred net uptake of nitrogen by phytoplankton, mixing from subsurface water contributed 18%, bacterial remineralization 12%, and zooplankton excretion 9%. However, independent observations of rapid activity by microheterotrophs (presumably bacteria) suggested that 1*C fixation considerably underestimated net primary production. This yielded an alternative interpretation in which nutrient additions contributed 46% of inferred net uptake of nitrogen in the surface layer, mixing 13%, bacteria 35%, and zooplankton 7%. Dissolution of silica was responsible for the observed accumulation of silicic acid below 8 m depth in CEE2, but the importance of silica dissolution as a source of Si for diatom growth in the surface 8 m is uncertain. The model's major failing was its assumption of unchanging maximum growth rates of phytoplankton, and unchanging rates of exudation, sinking, and respiration. Physiological parameter values which accounted for the huge bloom of Stephanopyxis in CEE2 could not account for the ensuing collapse. Traditional modelling assumptions of slowly changing internal physiology, although adequate for marine systems dominated by physical factors such as seasonality or water movement, cannot capture the behavior of biologically dominated systems like the enclosed system considered here. / Science, Faculty of / Zoology, Department of / Graduate

This problem was undertaken to determine a suitable combination of fertilizers that would increase the food in a lake, resulting in increased yield of bass and crappie.

No description available.