Relevant bibliographies by topics / Lake hoare

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Lake hoare'

Author: Grafiati
Published: 4 June 2021
Last updated: 4 February 2022

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Journal articles on the topic "Lake hoare"

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Dowling, Carolyn B., Robert J. Poreda, and W. Berry Lyons. "The effects of high meltwater on the limnology of Lake Fryxell and Lake Hoare, Taylor Valley, Antarctica, as shown by dissolved gas, tritium and chlorofluorocarbons." Antarctic Science 26, no. 4 (2014): 331–40. http://dx.doi.org/10.1017/s095410201300062x.

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AbstractSmall changes in the availability of liquid water can have profound effects on the water levels, aqueous chemistry and biogeochemical dynamics of the closed-basin, perennially ice-covered lakes of the McMurdo Dry Valleys, Antarctica. We have compiled the published and unpublished data on dissolved gas, tritium and chlorofluorocarbons (CFCs) for Lake Fryxell and Lake Hoare to determine the effects of a high meltwater year (2001–02 summer) on the lakes. The dissolved gas, tritium and CFC data indicate that the pulse of freshwater that flowed onto the surfaces of the lakes did not mix extensively with the upper water column. At the bottom of Lake Hoare, the measurable CFC and lower dissolved gas values suggest that the recent meltwater may have mixed with bottom waters. The probable mechanism for this transportation is weak density currents withc. 0.1–1.5% surface water being transported downwards in Lake Hoare. This deep water input, while not constant, may have a significant effect on the chemistry of the bottom waters in Lake Hoare over time. In Lake Fryxell, the tritium and CFC data indicate that the recent meltwater did not significantly affect the bottom water chemistry; therefore, weak density currents may not be present in Lake Fryxell.
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Neumann, Klaus, W. Berry Lyons, and David J. Des Marais. "Inorganic carbon-isotope distribution and budget in the Lake Hoare and Lake Fryxell basins, Taylor Valley, Antarctica." Annals of Glaciology 27 (1998): 685–89. http://dx.doi.org/10.3189/1998aog27-1-685-689.

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One of the unusual features of Lakes Fryxell and Hnare in Taylor Valley, southern Victoria Land, Antarctica, is their perennial ice cover. This ice cover limits gas exchange between the atmosphere and the lake water, and causesa very stable stratification of the lakes. We analyzed a series of water samples from profiles of these lakes and their tributaries for δ13C of the dissolved inorganic carbon (DIC) in order to qualify the carbon flux from the streams into the lakes, and to investigate the carbon cycling with in the lakes. Isotopic values in the uppermost waters (δ13C = +l.3‰ to 5.3‰ in Lake Hoare, +0.4‰ to +3.0‰ in Lake Fryxell) are close to the carbon-isotope values encountered in the streams feeding Lake Fryxell, but distinctively heavier than in streams feeding Lake Hoare (δ13C= — 2.3%n to 1.4%). These ratios are much heavier than ratios found in the moat that forms around the lakes injanuary February (δC = -10.1%). in the oxic photic zones of the lakes, photosynthesis clearly influences the isotopic composition, with layers of high productivity having enriched carbon-isotope signatures δ13C= +2.7‰ to +6.1‰). in both lakes, the isotopic values become lighter with depth, reaching minima of 3.2‰ and 4.0% in Lakes Fryxell and Hoare, respectively. These minima are caused by the microbial remineralization of isotopically light organic carbon. We present DIC flux calculations that help to interpret the isotopic distribution. For example, in Lake Hoare the higher utilization of CO2aq, and a substantially smaller inflow of CO2 from streams cause the heavier observed isotopic ratios. Differences in the hydrology and stream morphologies of the tributaries also greatly influence the carbon budgets of the basins.
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Lyons, W. B., S. W. Tyler, R. A. Wharton, D. M. McKnight, and B. H. Vaughn. "A Late Holocene desiccation of Lake Hoare and Lake Fryxell, McMurdo Dry Valleys, Antarctica." Antarctic Science 10, no. 3 (1998): 247–56. http://dx.doi.org/10.1017/s0954102098000340.

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Stable isotope data from waters of lakes in the McMurdo Dry Valleys (MDV) of southern Victoria Land, Antarctica are presented in order to establish the climatic history of this region over the past two millennia. New data from Lake Fryxell and Lake Hoare in Toylor Valley, along with previously published data from Lake Vanda, Wright Valley and Lake Bonney, Taylor Valley are used to infer the recent climatic history of MDV. Lakes Vanda, Fryxell and Bonney appear to have lost their ice covers and evaporated to small, hypersaline ponds by 1000 to ~1200 yr BP. Lake Hoare either desiccated or did not exist prior to 1200 yr BP. These data indicate a major lowering of lake level prior to ~1000 yr BP, followed by a warmer and/or more humid climate since then.
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Clocksin, Kate M., Deborah O. Jung, and Michael T. Madigan. "Cold-Active Chemoorganotrophic Bacteria from Permanently Ice-Covered Lake Hoare, McMurdo Dry Valleys, Antarctica." Applied and Environmental Microbiology 73, no. 9 (2007): 3077–83. http://dx.doi.org/10.1128/aem.00085-07.

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ABSTRACT Eight strains of chemoorganotrophic bacteria were isolated from the water column of Lake Hoare, McMurdo Dry Valleys, Antarctica, using cold enrichment temperatures. The isolates were Alpha-, Beta-, and Gammaproteobacteria and Actinobacteria spp. All isolates grew at 0°C, and all but one grew at subzero temperatures characteristic of the water column of Lake Hoare. Growth temperature optima varied among isolates, but the majority showed optima near 15°C, indicative of cold-active phenotypes. One isolate was truly psychrophilic, growing optimally around 10°C and not above 20°C. Half of the isolates grew at 2% salt while the other half did not, and all but one isolate grew at 2 atm of O2. Our isolates are the first prokaryotes from the water column of Lake Hoare to be characterized phylogenetically and physiologically and show that cold-active species of at least two major phyla of Bacteria inhabit Lake Hoare.
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Neumann, Klaus, W. Berry Lyons, John C. Priscu, David J. Desmarais, and Kathleen A. Welch. "The carbon isotopic composition of dissolved inorganic carbon in perennially ice-covered Antarctic lakes: searching for a biogenic signature." Annals of Glaciology 39 (2004): 518–24. http://dx.doi.org/10.3189/172756404781814465.

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AbstractThe stable-isotopic signature of dissolved inorganic carbon (DIC) has been routinely used in temperate lake systems to investigate the biogeochemical dynamics of carbon. We studied seven perennially ice-covered lakes in the McMurdo Dry Valleys, Antarctica, to ascertain how carbon cycling affects the δ13C of DIC in water columns of these systems. Unlike temperate lakes and, in fact, most polar lake systems, the permanent ice covers of these lakes eliminate physical mixing (turnover) and hence redistribution of DIC in the lakes, as well as minimize CO2 exchange with the atmosphere. These important and unique physical constraints have significant impact on carbon dynamics in the lakes, and important consequences for the δ13C distribution. The geochemistry in these lakes is influenced in varying amounts by landscape position, hydrologic input and their evolutionary history. Five of these lakes (both lobes of Lake Bonney, and Lakes Fryxell, Miers and Vanda) have surface water δ13C ratios of 0–4‰, Lake Hoare has more negative values, while Lake Joyce, the highest-elevation lake, has a much higher value (10.5‰). All of the lakes have upper- to mid-depth δ13C maxima reflecting biological uptake of 12C. Only four of the lakes (Lakes Vanda, Joyce, Hoare and Fryxell) have deep waters with negative values of δ13C, implying rigorous remineralization of 12C at depth. Lake Miers, the only lake that is not closed basin, has the smallest δ13C variation with depth, indicating that hydrologic exchange greatly influences the δ13C signal.
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Wagner, Bernd, Sabrina Ortlepp, Peter T. Doran, Fabien Kenig, Martin Melles, and Andy Burkemper. "The Holocene environmental history of Lake Hoare, Taylor Valley, Antarctica, reconstructed from sediment cores." Antarctic Science 23, no. 3 (2011): 307–19. http://dx.doi.org/10.1017/s0954102011000125.

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AbstractUp to 2.3 m long sediment sequences were recovered from the deepest part of Lake Hoare in Taylor Valley, southern Victoria Land, Antarctica. Sedimentological, biogeochemical, and mineralogical analyses revealed a high spatial variability of these parameters in Lake Hoare. Five distinct lithological units were recognized. Radiocarbon dating of bulk organic carbon samples from the sediment sequences yielded apparently too old ages and significant age reversals, which prevented the establishment of reliable age-depth models. However, cross correlation of the sedimentary characteristics with those of sediment records from neighbouring Lake Fryxell indicates that the lowermost two units of the Lake Hoare sediment sequences were probably deposited during the final phase of proglacial Lake Washburn, which occupied Taylor Valley during the late Pleistocene and early Holocene. High amounts of angular gravel and the absence of fine-grained material imply a complete desiccation with subaerial conditions in the Lake Hoare basin in the middle of the Holocene. The late Holocene (< c. 3300 calendar yr bp) is characterized by the establishment of environmental conditions similar to those existing today. A late Holocene desiccation event, such as proposed in former studies, is not indicated in the sediment sequences recovered.
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Dieser, Markus, Andreas Nocker, John C. Priscu, and Christine M. Foreman. "Viable microbes in ice: application of molecular assays to McMurdo Dry Valley lake ice communities." Antarctic Science 22, no. 5 (2010): 470–76. http://dx.doi.org/10.1017/s0954102010000404.

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AbstractThe permanent ice covers of the McMurdo Dry Valley lakes, Antarctica, are colonized by a diverse microbial assemblage. We collected ice cores from Lakes Fryxell, Hoare and Bonney. Propidium monoazide (PMA) was used in combination with quantitative PCR (qPCR) and denaturing gradient gel electrophoresis (DGGE) to examine membrane integrity of prokaryotes in these extreme environments. PMA selectively penetrates cells with compromised membranes and modifies their DNA resulting in the suppression of PCR amplification. Our results based on analysis of 16S rRNA genes demonstrate that despite the hostile conditions of the Dry Valleys, the permanent ice covers of the lakes support a ‘potentially viable’ microbial community. The level of membrane integrity, as well as diversity, was higher in samples where sediment was entrapped in the ice cover. Pronounced differences in the fraction of cells with intact and compromised cell membranes were found for Lake Fryxell and east lobe of Lake Bonney, both expressed in differences in DGGE banding patterns and qPCR signal reductions. Limitations in the ability to distinguish between intact or compromised cells occurred in samples from Lake Hoare and west lobe of Lake Bonney due to low DNA template concentrations recovered from the samples.
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Andersen, D. T., C. P. Mckay, and R. A. Wharton. "Dissolved gases in perennially ice-covered lakes of the McMurdo Dry Valleys, Antarctica." Antarctic Science 10, no. 2 (1998): 124–33. http://dx.doi.org/10.1017/s0954102098000170.

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Measurements of dissolved N2, O2, Ar, CO2, and CH4 were made in perennially ice-covered Lake Hoare. Results confirm previous reports that O2 concentrations in the upper water column exceed atmospheric equilibrium and that N2 and Ar are supersaturated throughout the water column. The mean supersaturation of N2 was found to be 2.0 (±0.37) and Ar was 3.8 (±1.1). The ratios of N2/Ar (20.3 ±3.8), and O2/Ar (22.5 ±4.0) at the ice-water interface are consistent with those previously measured, suggesting that bubble formation is the main process for removing gas from the lake. However, the saturations of N2 and Ar greatly exceed those previously predicted for degassing by bubble formation only at the ice-water interface. The data support the hypothesis that removal of gas by bubbles occurs in the water column to a depth of 11 m in Lake Hoare. CO2 concentration increases from near zero at the ice-water interface to 80–100 times saturation at and below the chemocline at c. 28 m. There is considerable variability in the gas concentrations throughout the water column; samples separated in depth by one metre may vary by more than 50% in gas content. It is likely that this phenomenon results from the lack of turbulent mixing in the water column. Methane (c. 2 μg 1−1) was detected below the chemocline and immediately above the sediment/water interface at a depth of 30 m. Samples from lakes Vanda, Joyce, and Miers, also show supersaturations of O2, N2, and Ar at levels similar to levels found in Lake Hoare.
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NEDELL, SUSAN S., DAVID W. ANDERSEN, STEVEN W. SQUYRES, and F. GORDON LOVE. "Sedimentation in ice-covered Lake Hoare, Antarctica." Sedimentology 34, no. 6 (1987): 1093–106. http://dx.doi.org/10.1111/j.1365-3091.1987.tb00594.x.

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Roberts, Emily C., John C. Priscu, and Johanna Laybourn-Parry. "Microplankton dynamics in a perennially ice-covered Antarctic lake - Lake Hoare." Freshwater Biology 49, no. 7 (2004): 853–69. http://dx.doi.org/10.1111/j.1365-2427.2004.01230.x.

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Dissertations / Theses on the topic "Lake hoare"

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Clocksin, Kate M. "Isolation and characterization of heterotrophic bacteria from Lake Hoare, McMurdo Dry Valleys, Antarctica /." Available to subscribers only, 2005. http://proquest.umi.com/pqdweb?did=1079660831&sid=1&Fmt=2&clientId=1509&RQT=309&VName=PQD.

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Thesis (M.S.)--Southern Illinois University Carbondale, 2005.<br>"Department of Molecular Biology, Microbiology and Biochemisty." Includes bibliographical references (leaves 48-54). Also available online.
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Carroll, Kelly Patrick. "Permeability of Lake Ice in the Taylor Valley, Antarctica: From Permeameter Design to Permeability Upscaling." Columbus, Ohio : Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1206545662.

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Reeves, Brian D. "Hoary-Headed Saints: the Aged in Nineteenth-Century Mormon Culture." Diss., CLICK HERE for online access, 1987. http://patriot.lib.byu.edu/u?/MTNZ,14666.

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Lindblad, Tova. "Fogdarpsfyndet : En landskapsanalys av ett depåfynd från den yngre bronsåldern." Thesis, Uppsala universitet, Arkeologi, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-385697.

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The Fogdarp hoard from Scania in Sweden is an unusual deposit from the Late Bronze Age. Unlike similar hoards this was not found in a wetland, but was buried in the ground with a rock placed on top of it. Deposits in dry land have sometimes been considered to be a hiding place for a smith’s metalwork. But since the Fogdarp hoard contains ritual bronze objects, it has been called a ritual deposit. The aim of this paper is to investigate the Fogdarp hoard by using a landscape analysis. By doing so the study will contribute to the understanding of the hoards context, and why this hoard was buried and not deposited in a wetland. The landscape analysis shows that the hoard is buried closed to the water and in a ritual landscape on the edge of a valley. The discussion will also analyze the objects in this particular hoard: their symbolic value will be elaborated in the analysis. As a comparison, this paper includes other deposits from the Late Bronze Age. My interpretation of the objects in the Fogdarp hoard is that they are a part of the sun cult of the Nordic Bronze Age, where sun-goddess and the divine twins play an important role.
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Perrin, Stéphanie. "Les trésors de vaisselle précieuse dans les Îles Britanniques à la période romaine : pratiques de déposition de la vaisselle d’argent et d’étain dans l’Antiquite Tardive." Thesis, Paris 4, 2012. http://www.theses.fr/2012PA040234.

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Les trésors de vaisselle précieuse de l’Antiquité tardive dans les îles britanniques présentent un corpus d’étude digne d’intérêt à la fois grâce à leur nombre important, à la variété des objets réunis et aux métaux employés. En effet, de nombreux ensembles de vaisselle précieuse ont été ensevelis entre le 3ème et le 5ème siècle en Bretagne romaine, tandis que d’autres dépôts issus de butins de pillage ont été trouvés en dehors des frontières de l’Empire (Écosse et Irlande actuelles). En outre, alors que les grands services d’argenterie y tiennent une part assez exceptionnelle, cette province se démarque du reste de l’Empire par une grande richesse en dépôts constitués de petits objets variés en métaux précieux (or et argent). Enfin, cette région voit se développer de façon quasiment exclusive, dès le 3ème siècle, l’industrie de l’"étain" (un alliage d’étain et de plomb dans des proportions variables), qui se prête bien à l’imitation des plats d’argenterie, donnant ainsi la possibilité à des familles moins aisées de posséder des services entiers de vaisselle de table.À partir de la constitution d’un catalogue de 229 dépôts et objets isolés, cette étude s’ouvre par une analyse typologique de la vaisselle d’argent et d’étain, comprenant l’observation des formes, des éléments décoratifs et de l’iconographie. S’ensuit l’analyse comparative du contenu de ces ensembles et de leur contexte d’enfouissement, menant à l’élaboration de tableaux typologiques et de cartes de répartition géographique. Des différenciations sont ainsi mises en évidence et permettent de tenter une interprétation de ces dépôts, témoins matériels d’une époque bouleversée<br>Several hoards of precious vessels come from Roman Britain, some of them were found outside imperial boundaries (Scotland and Ireland) and represent loots of pirates. They were deposited during all Roman period, especially during the 3rd to the 5th centuries. Though large silver treasures are very rare there, this region is very rich in hoards of small precious objects of gold and silver (spoons, strainers, toothpicks, jewellery, coins, ingots…). In the meantime pewter industry flourishes from the 3rd century and vessels of this matter are produced in great quantity and diffused through the entire island, imitating silver vessels of the same period. It is often called the "poor man's silver".Through a descriptive catalogue of 229 Roman pewter and silver vessels hoards and single finds from the British Isles, this study starts with a typological and stylistic analysis of precious vessels and their imitations (forms, decoration, and techniques). It continues with a classification of all treasures and hoards that contain silver or pewter vessels, through a comparison of what they contained and where they were buried. Some of them could be of votive origin, inherited from Bronze Age
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Book chapters on the topic "Lake hoare"

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McKnight, D. M., G. R. Aiken, E. D. Andrews, E. C. Bowles, and R. A. Harnish. "Dissolved organic material in dry valley lakes: A comparison of Lake Fryxell, Lake Hoare and Lake Vanda." In Physical and Biogeochemical Processes in Antarctic Lakes. American Geophysical Union, 1993. http://dx.doi.org/10.1029/ar059p0119.

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Wharton, Robert A., George M. Simmons, and Christopher P. McKay. "Perennially ice-covered Lake Hoare, Antarctica: physical environment, biology and sedimentation." In High Latitude Limnology. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2603-5_22.

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West, Alan. "A Late Bronze Age hoard from Feltwell." In Landscapes and Artefacts. Archaeopress Publishing Ltd, 2014. http://dx.doi.org/10.2307/j.ctvqc6j85.9.

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Scheers, Simone, and Guido Creemers. "The gold hoard of Heers." In Late Iron Age Gold Hoards from the Low Countries and the Caesarian Conquest of Northern Gaul. Amsterdam University Press, 2012. http://dx.doi.org/10.2307/j.ctt46n0nm.9.

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Scheers, Simone, and Guido Creemers. "The gold hoard of Fraire." In Late Iron Age Gold Hoards from the Low Countries and the Caesarian Conquest of Northern Gaul. Amsterdam University Press, 2012. http://dx.doi.org/10.2307/j.ctt46n0nm.5.

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Manning, W. H. "A hoard of late Roman ironwork from Sibson, Huntingdonshire." In Form and Fabric. Oxbow Books, 2017. http://dx.doi.org/10.2307/j.ctvh1dtvk.38.

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"A late Roman treasure hoard buried near Thetford, Suffolk." In The Collector's Voice. Routledge, 2016. http://dx.doi.org/10.4324/9781315264462-66.

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Papazoglou-Manioudaki, Lena. "Diversity in Life and Death in Early Mycenaean Achaea." In Death in Late Bronze Age Greece. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780190926069.003.0007.

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Achaea, in the Northwest Peloponnese, is an integral part of the Mycenaean world and in the early Mycenaean period went through the same evolutionary processes as the rest of the Myceneaen world. We witness settlement growth and the rise of local elites who manifest their status in stone built and richly furnished tombs, particularly in Western Achaea. In LH IIB the building of tholos tombs reveals the existence of local principalities in Western Achaea, while a hoard of metal vases and weapons permits us to speak of a high status warrior’s burial. This early floruit comes to an end at the beginning of the Palatial period, as the destruction levels in settlements and the plundering of tholos tombs testify. Chamber tomb cemeteries are introduced in LH IIB, starting in Eastern Achaea and prevail all over Achaea in the palatial and postpalatial era.
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Roymans, Nico, and Wim Dijkman. "The gold and silver hoard of Maastricht-Amby." In Late Iron Age Gold Hoards from the Low Countries and the Caesarian Conquest of Northern Gaul. Amsterdam University Press, 2012. http://dx.doi.org/10.2307/j.ctt46n0nm.10.

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Van Impe, Luc, and Simone Scheers. "Remains of a disturbed gold hoard at Orp-le-Grand?" In Late Iron Age Gold Hoards from the Low Countries and the Caesarian Conquest of Northern Gaul. Amsterdam University Press, 2012. http://dx.doi.org/10.2307/j.ctt46n0nm.8.

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Conference papers on the topic "Lake hoare"

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Lyons, W. Berry, Brandon C. McAdams, Susan A. Welch, et al. "THE GEOCHEMISTRY AND MINERALOGY OF SEDIMENTS FROM LAKE HOARE, ANTARCTICA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285726.

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Tutayeva, Indira. "Hoard of the Late bronze age from the village of Sosnovka." In Antiquities of East Europe, South Asia and South Siberia in the context of connections and interactions within the Eurasian cultural space (new data and concepts). Institute for the History of Material Culture Russian Academy of Sciences, 2019. http://dx.doi.org/10.31600/978-5-907053-35-9-190-192.

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Loboda, Anastasiya, and Natal’ya Shishlina. "Technological aspects of Sosnovaya Maza hoard daggers of the Late Bronze Age." In Actual Archaeology 5. Institute for the History of Material Culture Russian Academy of Sciences, 2020. http://dx.doi.org/10.31600/978-5-907298-04-0-2020-112-114.

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Retivov, Vasiliy, Anastasiya Loboda, Elena Tereshchenko, Irina Kamenskikh, and Natal’ya Shishlina. "Elemental composition of the tools from the Sosnovaya Maza hoard of the Late bronze age." In Antiquities of East Europe, South Asia and South Siberia in the context of connections and interactions within the Eurasian cultural space (new data and concepts). Institute for the History of Material Culture Russian Academy of Sciences, 2019. http://dx.doi.org/10.31600/978-5-907053-35-9-192-194.

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