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The 3500-year-long lake-dwelling tradition comes to an end: what is to blame?Menotti, Francesco January 2015 (has links)
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Razna National Park : - a selection of excursion destinationsZandén Ljungmark, Mimi January 2012 (has links)
Different areas in Latvias youngest National Park Rāzna has been visited and analyzed. One objectivewas to find out if ecotourism is a possibility and what improvements need to be made. Latvia has avery old history of nature conservation. Objectives to protect valuable species and habitats for thefuture are influenced by factors such as economy and politics. The laws and regulations concerningenvironmental care are dependent on the processes and conditions that have contributed to formingthem. What is considered normality in Sweden can be completely different in Latvia eventhough theintentions and wished results are the same. The conclusion is that there is potential for ecotourism,although many factors must be considered and disadvantageous situations be avoided in the natureprotecting process.
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Effects of Air Temperature and Lake Ice on Snowfall on the South Shore of Lake SuperiorMaki, Angela Pelkie 15 May 2009 (has links)
Lake Superior is a forcing factor for local weather systems, causing substantial amounts of lake effect snow in the winter (particularly on the south shore). This study assesses decreasing ice cover of Lake Superior and its effects upon synoptic weather factors. Data were collected from eleven National Weather Service (NWS) stations located on the south shore of the lake. Rainfall and snowfall amounts from December to May were regressed on percent ice coverage and average monthly temperatures from 1972-2002. Ice coverage and average monthly temperature had a negative relationship with snowfall and rainfall.
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Recovery of Marsh Vegetation at Malheur Lake Following an Extended FloodSpencer, Sherry Vlasta 10 February 1994 (has links)
Water levels of Malheur Lake in southeastern Oregon fluctuate widely with seasonal and cyclic climatic changes. Seven years of severe flooding from 1978 to 1984 produced the highest water levels in recorded history and covered almost all marsh vegetation. Seven years of drought followed the flooding, and by 1992 the water level had dropped to the lowest point in nearly 60 years. A survey of vegetation colonizing the lakeshore as flood water receded was conducted from 1989 to 1992 to describe the reestablishment of marsh vegetation. Six transects were placed in three different ecological units of the lake. Frequency and cover data for each plant species were recorded. Recruitment from seed banks produced germination the first year of annual, mud flat species followed the second year by perennial emergent seedlings. The emergent seedlings generally did not survive the drought as water levels continued to recede. The seeds of introduced Eurasian species were distributed by wind, became lodged in the cracks of drying mud flats and then germinated following winter rains. The central ecological unit, fed by both the Blitzen and Silvies Rivers, did not show severe effects of drought and species of emergent vegetation grew without apparent signs of drought stress.
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Landscape evolution of the Umbum Creek Catchment, Western Lake Eyre, Central Australia.Waclawik, Victor G. January 2006 (has links)
Landscape evolution is important for mineral and petroleum exploration concepts, especially in dryland continental settings. This study seeks to understand the main issues and controls on landscape evolution that have produced the regolith and young sediments around the western side of Lake Eye, in the arid heart of Australia. Several methods were employed including satellite image analysis, geomorphometry, geological mapping, regolith mapping and surveying. Outcomes indicate that the underlying structural fabric of the basement has controlled the development of the surface morphology of the Umbum Creek Catchment. The arrangement of basement faults is reflected in the distribution of surface landforms and in the topography of the land surface. Significant deformation of the Etadunna and Eyre formations indicate tectonic activity occurred at the end of the Miocene and was probably related to movement in the Lake Eyre Fault Zone. Pleistocene faulting is expressed as minor blind faulting associated with pre - existing basement faults. These faults remain active and current seismic activity is driven by changes in hydrostatic pressure (hydroseismicity). The scale of Pleistocene faulting and modern seismic activity demonstrates that since the Pliocene tectonic activity has been subdued. Climate change caused landforms developed under wet conditions during the Palaeogene and Neogene to be preserved by the development of aridity in the Pleistocene. High erosion rates associated with tectonism and the onset of aridity in the Pleistocene led to topographic inversion of many features. Palaeo-Proterozoic inliers formed inselbergs, silcrete outcrops formed capstones, gypsum hardpans protected underlying sediment from erosion creating plateaux of gypsum patterned ground and palaeo-channels on the Neales Fan were eroded to make heavily armoured mounds and associated sand dunes and sand sheets. The dominant factor influencing the evolution of the landscape in the Umbum Creek Catchment was the deposition of sedimentary sulphides within the Bulldog Shale. The excess sulphur that this sediment supplied to the landscape over time created the necessary conditions for the formation of a range of landscape features that would not otherwise exist. Weathering, oxidation and leaching of the sedimentary sulphides led to the development of silcrete. Subsequent weathering and tectonic activity led to the breakdown of the silcrete and the distribution of silcrete pebbles widely across the landscape forming gibber plains. Sulphur from the Bulldog Shale continued to contribute to the landscape forming intra-formational gypsum and precipitating as gypsum hardpans. This study has implications for petroleum exploration in dryland continental settings as potential reservoirs may be affected by secondary diagenetic processes, such as the formation of gypsum or silcretes, that could act as baffles or result in reduced porosity within the reservoir. The broad-scale architecture of fluvial systems, like the Neales Fan, may not conform to traditional fan-shaped models being, instead, comprised of structurally rearranged channels. In terms of earthquake risk assessment, the identification of hydroseismicity active within the Lake Eye Basin allows for a new level of predictability of earthquake behaviour within Central Australia. / http://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1260856 / Thesis (Ph.D.) -- School of Earth and Environmental Sciences, 2006
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Effects of a threadfin shad introduction upon black crappie and smallmouth buffalo pupulations in Roosevelt LakeBeers, Gary Delman, 1942- January 1965 (has links)
No description available.
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Distribution and Abundance of Larval Lake Whitefish (Coregonus clupeaformis) in Stokes Bay, Lake HuronRyan, Kathleen 29 November 2012 (has links)
Lake whitefish (Coregonus clupeaformis) are an ecologically, culturally and economically important species throughout the Great Lakes. Studying the larval period of ontogeny is important to increasing knowledge of population dynamics and monitoring ecological changes in lake whitefish populations. Larval lake whitefish have been studied across the Great Lakes since the 1930’s; however, there are major gaps in our understanding of the factors that affect distribution and abundance of larval lake whitefish. The goal of this study was to investigate the distribution and abundance of larval lake whitefish in a Great Lakes embayment, using Stokes Bay, Lake Huron as a case study. Plankton samples and environmental data were collected from mid-spring to early summer during 2011 and 2012. Plankton tows in 2011 (n=71, 21 April-03 June) revealed relatively high densities of larval lake whitefish as compared to other Great Lakes studies. Overall there was little relationship between environmental variables (temperature, dissolved oxygen, conductivity, depth) and larval lake whitefish distribution and abundance. Plankton tows in 2012 (n=25, 25 April-23 May) revealed a virtual absence of larval lake whitefish in Stokes Bay. The apparent 2012 year-class failure was concurrent with unseasonably warm temperatures and reduced ice coverage. Temperature-related hypotheses are evaluated in context with other possible explanations of a general year-class failure of lake whitefish during early life history. / Saugeen Ojibway Nation (SON)
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Aspects of the biology and population dynamics of freshwater mussels in Lake Kariba and Lake McIlwaine.Kenmuir, Dale Harold Stafford. January 1982 (has links)
Following preliminary observations in 1975 the
Lake Kariba Fisheries Research Institute implemented a research
program in March 1976 to investigate various aspects of the
biology and population dynamics of the mussel crop of Lake
Kariba, with a view to greater understanding of their status
in the lake, and establishing a basis for management, if
required. Aspects investigated were densities, distribution,
species composition, predation by fish, reproduction, age and
growth, gross biochemical composition and crude production
rates. The mussel community comprised four species, a small
pill clam, Corbicula africana, and three mussels, Caelatura
mossarnbicensis, Aspatharia wahlbergi and Mutela dubia. Only
the latter three were studied. Mussel beds occupied all the
gently shelving cleared and uncleared areas, and the bulk of
the populations occurred from 3 m - 9 m depth, but extending
to 11 m. Predation by fish was found to be extremely low.
The reproduction study showed two species bred all year
C. mossambicensis and M. dubia, whereas A. wahlbergi bred
seasonally during the rainy season. The two year-round
breeders were repetitive spawners, capable of breeding several
times a year. Indications are that A. wahlbergi is essentially
a fluviatile species, with a life cycle adapted to taking
advantage of riverine conditions. Sex ratios in all three
species were approximately 1 : 1 , with females predominating
slightly. Fecundity in one species, C. mossambicensis, was
investigated. The complete parasitic cycle of M. dubia was
elucidated and found to be similar to that of M. bourguignati,
as described by Fryer (1961). Host species were noted amongst the cichlid and mormyrid families, and the conclusion drawn
that the species is not host specific. various aspects of the
life-cycles of the other two species were noted, but complete
life-cycles were not successfully elucidated. population
composition according to age showed the most common species,
c. mossambicensis, to be comprised mainly of 2 - 5 year-old
individuals, indicating a young and vigorous population.
Juvenile pre-adult mussels were very scarce. In the population
of A. wahlbergi, older mussels formed a greater proportion
of the biomass than in the population of c. mossambicensis, and
young were also scarce. M. dubia were not recorded in sufficiently
large numbers to estimate age composition accurately.
The production rate (whole wet mass) of the most common
species, c. mossambicensis, was calculated to be 2,45 kg
ha¯¹ day¯¹ in the sanyati East cleared area (30,5 km²), while
the overall production rate of all three species was calculated
to be 3,34 kg ha¯¹ day¯¹. Calorific values of all three
species were obtained, while gross body composition in terms
of water, fat, protein, ash and amino acid composition were
determined. The ash component of A. wahlbergi was analysed.
The Lake Kariba results were supplemented by a
follow-up study of the composition of the mussel population
of a eutrophic, highveld dam, Lake McIlwaine, in 1978/1979.
This much smaller lake was populated by only two mussel
species, M. dubia and C. mossambicensis, although A. wahlbergi
and Unio caffer were recorded in the riverine upper reaches.
Observations on seasonal breeding of the two lake species were
made. A detailed study on the draw down zone of a gently
shelving beach showed that at the time the extreme shallows had been dominated by C. mossambicensis, whereas from a depth
of approximately 1,6 m M. dubia dominated very significantly.
Fulling lake level was found to trigger off migratory responses,
thus placing a proportion of individuals in deeper water and
improving chances of survival.
The mussel composition of Lake Kariba and Lake
McIlwaine was considered in conjunction with preliminary
observations of mussel distribution a nd composition in other
water bodies, and some inferences drawn regarding the ecological
factors which appear to influence the composition and
diversity of the mussel fauna in rivers and lakes. / Thesis (Ph.D.)-University of Natal, Pietermaritzburg, 1980.
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Changes in the summer zooplankton community of the Indiana waters of Lake Michigan inshore at a Michigan City transect, 1987 and 1988Phillips, Sheri A. January 1993 (has links)
Alterations in the summer zooplankton community that have appeared since Johnson's (1972) study of a Michigan City (site M) transect in southeastern Lake Michigan were investigated. Vertical tows were made at 5, 10, 15, and 18 meters from June through August in 1987 and 1988 in order obtain data that could be compared with that of Johnson (1972).Subsamples analyzed were proportionately larger than those of Johnson (1972), in order to obtain a detailed profile of the species and numbers in the community, and to identify large, predatory zooplankton species that are believed to have been severely impacted by the explosive growth of the alewife population during the 1960's.The most common crustacean species collected were: Diacyclops thomasi, Leptodiaptomus minutus, Leptodiaptomus ashlandi, calanoid and cyclopoid nauplii and copepodids, Daphnia retrocurva, and Bosmina longirostris. The most common rotifer species collected were Keratella c. cochlearis, Keratella crassa, Kellicottia longispina, Conochilus sp., and Polyarthra sp.. Higher numbers of Epischura lacustris adults and copepodids, Leptodora kindti, Mesocyclops edax, Daphnia galeata mendotae, and the rotifers Asplanchna priodonta, Conochilus sp., Keratella crassa, and Ploesoma truncatum were recorded as compared to Johnson's 1972 data. The summer zooplankton community of this transect appears to have been represented in the summers of 1987 and 1988 by a greater number of large crustacean zooplankton species, as opposed to a 1970 community dominated by small microfiltrators and D. thomasi. / Department of Biology
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Yellow perch Perca flavescens gonadal development and spawning in the Indiana portion of Lake Michigan during 2009Walters, Justin T. 24 July 2010 (has links)
Yellow perch Perca flavescens spawning was evaluated in southern Lake Michigan during 2009 to determine the timing, location, and extent of spawning activity. Maturity state (i.e., pre-spawn/post-spawn), gonadosomatic index (GSI), mean length, length frequency distributions, and sex group proportions were also evaluated. No egg skeins were discovered during the study. The GSI decreased during the duration of the spawn. Spent females were larger than pre-spawn females. Following the spawning season another assessment was conducted to determine whether differences existed in the spawning and post-spawning population demographics. Abundance, length frequency distributions, proportions, and relative stock density were evaluated. Abundance of fish in the post-spawning period increased six-fold and paralleled a shift in length frequency distribution to larger median size. An increase in the proportion of females and relative stock density from the spawning period to post-spawning period was discovered. These data infer adult fish were spawning elsewhere, and then migrating to Indiana. / Department of Biology
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