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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Lakes -- Economic aspects -- Europe -- Congresses. ; Electronic books.
    Description / Table of Contents: This book examines the problems regarding the present status of European large lakes and discusses the directions of change. It also considers threats caused by direct human impact and by climate change, protection needs and restoration measures.
    Type of Medium: Online Resource
    Pages: 1 online resource (270 pages)
    Edition: 1st ed.
    ISBN: 9781402083792
    Series Statement: Developments in Hydrobiology Series ; v.199
    DDC: 577.63094
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 50 (2004), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Lake Võrtsjärv (270 km2, mean depth 2.8 m, Estonia) is an eutrophic and turbid lake (Secchi depth 0.5–1 m) with a high nutrient load (total nitrogen 1–2 mg N l−1, total phosphorus ∼50 μg P l−1) leading to a highly productive phytoplankton population (average chlorophyll a concentration 24 μg l−1). Seasonal dynamics of the main members of pelagic microbial loop – phyto-, bacterio- and protozooplankton – has been studied for several years (1993–1998) in lake. The most prominent characteristic of this naturally eutrophic, turbid shallow lake is an inter-annual water level fluctuation (3.2 m) which is in the range of its average depth. Bacterioplankton growth was favored by high water level whereas phytoplankton growth was favored by low water level. In autumn and sometimes in winter bacterioplankton production (BP) was unbalanced with respect to primary production (PP) (gross BP 20–90% higher than PP) suggesting to additional sources of organic carbon. The main grazers of bacteria were probably various ciliates. In contrast to most eutrophic and stratified lakes, the relative prevalence of the microbial loop over the linear phagotrophic food chain was obvious in this eutrophic shallow lake. The bacterioplankton showed a pronounced seasonal succession with low diversity at high production periods in summer and with high diversity at low biomass and production periods in winter and spring.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1420-9055
    Keywords: Key words: Sedimentation, resuspension, nitrogen, phosphorus, suspended solids, shallow lake.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract: Phytoplankton primary production measurements and sediment trapping in the large (270 km2) shallow (mean depth 2.8 m) Lake Võrtsjärv were performed during ice-free periods in 1995-1996. Sedimentation rate varied from 26 to 700 g DWm-2d-1 (DW=dry weight), with a mean value of 170 g DWm-2d-1. Under the influence of prevailing westerly and south-westerly winds, the sedimentation rate was higher in the northern part, and lower in the western and southern parts of the lake. An increasing trend towards autumn could be followed in both years. The mean sedimentation rates in the dry year 1996 with a low lake water level exceeded those of the “normal” 1995 by a factor of more than two. New sedimentation formed 10-15 % of the downward sediment flux in 1995 and 4-6 % in 1996, while the major part of entrapped matter originated from resuspended bottom sediments. The dynamics of gross sedimentation showed no relation to the primary production but correlated significantly with the concentration of suspended solids, with the average wind speed and with the mean depth of the lake during trap exposition.¶The composition of entrapped matter did not show seasonal variation but differed between the sampling stations. The amount of particulate organic matter (POM) per DW varied from 11 % at places where the bottom sediment consisted of moraine or sand to 28 % at places with muddy bottom. N:POM was rather stable (45-61 mgg-1, Cvar = 6 %). The variability of P:POM (3.5-7.1, Cvar = 20 %) exceeded that of P:DW (0.75-1.31 mgg-1, Cvar = 10 %) showing the essential role of mineral-bound P in the settling material. In these conditions, the N:P ratio was determined by the POM content of settling matter. POM:DW in settling material was generally higher than in the 0-2 cm layer of bottom sediments.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 338 (1996), S. 91-103 
    ISSN: 1573-5117
    Keywords: Lake Peipsi-Pihkva ; large shallow eutrophic lake ; plankton ; ATP ; chlorophyll ; pheopigments ; carotenoids
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The material for pigment analysis was collected 1–3 times a year from Lake Peipsi-Pihkva in 1983, 1987, 1988, 1991 and 1992–1995. Concentrations of chlorophyll a, b and c (Chla, Chlb, Chlc), pheopigment (Pheo) and adenosine triphosphate (ATP) were measured biweekly in 1985–1986. The mean of all Chla values was 20.2 mg m−1 (median 13.3 mg m−1) indicating the eutrophic state of the lake. Average Chlb, Chlc, Pheo and carotenoid (Car) contents were 3.7 mg m−3, 4.1 mg m−3, 3.0 mg m−3 and 4.8 mg m−3, respectively. The average Chlb/Chla ratio was 22.9%, Chlc/Chla 23.4%, Pheo/Chla 38%, Car/Chla 37% and ATP/Chla 3%, the medians being 14.3, 13.6, 17.5, 39.4 and 1.9%, respectively. The proportion of Chla in phytoplankton biomass was 0.41%, median 0.32%. There were no significant differences in temperature, oxygen concentration, Chla, and ATP between the surface and bottom water; the lake was polymictic during the vegetation period. The Chla concentration had its first peak in May followed by a decrease in June and July. In late summer Chla increased again achieving its seasonal maximum in late autumn. The ATP concentration was the highest during spring and early summer, decreasing drastically in autumn together with the decline of primary production. ATP/Chla was the highest during the “clear water period” in June and early July, which coincided also with the high proportion of Chla in phytoplankton biomass. The highest Chla occurred in November (average 37.2 mg m−3) when Secchi transparency was the lowest (1.05 m). Concentrations of Chlb, Chlc and carotenoids were the highest in August, that of Pheo in June. Concentrations of Chla and other pigments were the lowest in the northern part of Lake Peipsi (mean 14.7 mg m−3, median 12.5 mg m−3) and the highest in the southern part of Lake Pihkva (mean 47.9 mg m−3, median 16.3 mg m−3). An increase of Chla and decrease of Secchi depth could be noticed in 1983–1988, while in 1988–1994 the tendency was opposite.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 338 (1996), S. 105-112 
    ISSN: 1573-5117
    Keywords: Lake Peipsi-Pihkva ; large shallow eutrophic lake ; zooplankton ; species composition ; biomass ; trophic state index ; long- term changes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract 164 taxa were identified in the net zooplankton of the pelagial of L. Peipsi-Pihkva in 1909–1987, including 3 species of protozoans, 74 species of rotifers, 58 species of cladocerans, 28 species of copepods and 1 mollusc. One rotifer species, Ploesoma peipsiense Mäemets et Kutikova, has been described as new for science here. The zooplankton of L. Peipsi-Pihkva is remarkably rich in species including rarities in Estonia: Limnosida frontosa, Drepanothrix dentata, Bythotrephes longimanus, B. cederstroemi etc. Due to its large surface area, L. Peipsi-Pihkva provides a large scale of biotopes of a diverse trophic state and humic content, which support species with different ecological requirements. Most of the aquatory of the lake has lately been mesotrophic, favouring the coexistence of indicators of oligo- and mesotrophic state and species preferring a higher trophic state. The occurrece of 10 species of the genus Bosmina including B. berolinensis, B. gibbera, B. lilljeborgi, B. thersites and B. crassicornis, sparse in Estonian lakes, is the most noteworthy feature of the zooplankton of L. Peipsi-Pihkva. The coexistence of B. coregoni and B. berolinensis, B. gibbera, B. lilljeborgi etc. which were earlier regarded as subspecies of B. c. coregoni proves that they are different species producing usually no hybrids. The species composition was subjected to certain changes during the years under consideration. Larvae of Dreissena were first found in zooplankton in 1962. The oligo-mesotrophic indicator Holopedium gibberum occurred in the lake in 1909–1964, but was lacking in later samples.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 342-343 (1997), S. 175-184 
    ISSN: 1573-5117
    Keywords: zooplankton ; phytoplankton ; interactions ; grazing ; nutrient regeneration ; shallow eutrophic lake
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Zooplankton-phytoplankton interactions have been studied inthreeshallow lakes of different trophic state. In stronglyeutrophic,large and very shallow Lake Võrtsjärv the grazing doesnotplay a leading role in controlling phytoplankton productionand itsstanding stock. Small-size zooplankton can not eat filamentousblue-greens. The nutrient regeneration by zooplankton has aweakimpact on phytoplankton, the latter being limited rather byunderwater light than by nutrient availability. In largemoderatelyeutrophic Lake Peipsi the presence of concentrated zooplanktoninthe experimental vessel mostly stimulated steady-statephytoplankton growth and negative grazing values weremeasured.Most probably the nutrients (N, P), excreted by zooplankton ingrazing chamber stimulated the growth of larger phytoplanktonwhichdominated because of heavy grazing pressure on edible forms.InLake Peipsi phytoplankton seems to be nutrient-limited andheavilycontrolled by zooplankton community. In eutrophic,macrophyte-dominated Lake Yaskhan zooplankton in grazingchamberalso mainly stimulated the growth of phytoplankton communitywhichseemed to be nutrient-limited because of strong competitionwithmacrophytes.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 380 (1998), S. 93-102 
    ISSN: 1573-5117
    Keywords: diel dynamics ; bacterioplankton ; primary production ; algal exudates ; ciliate biomass ; shallow lake
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The diel dynamics of bacterio- and phytoplankton as main compartments in the pelagic foodweb were followed in order to assess the coupling between algal photosynthesis and bacterial growth during a diel cycle in Lake Võrstjärv, Estonia. Three diurnal studies were carried out, on July 12th–13th, 1994; on June 25th–26th, 1995 and on July 17th–18th, 1995 with a sampling interval of 3–4 hours. Diel variations in bacterial number, biomass and productivity, in phytoplankton primary production and extracellular release of photosynthetic products, in ciliate number and biomass were followed. Phytoplankton was dominated by filamentous species: Limnothrix redekei, Oscillatoria sp., Aulacoseira (Melosira) ambigua and Planktolyngbya limnetica. The abundance of bacteria ranged from 4.1 to 14.6 · 1012 cells m-2 (median 9.88). The production of heterotrophic bacteria varied from 0.6 to 11 mgC m-2 h-1 (median 3.65), the variation during diel cycle was high. Depth integrated values of particulate (PPpart) and extracellular primary production (PPdiss) ranged from 6 to 55 and from 17 to 90 mgC m- 2 h-1, respectively. About 50 ciliate taxa were identified among them more abundant were bacterivores, bacterivores- herbivores and omnivores. Biomass of bacterivorous ciliates (TCbact) varied from 8 to 427 mgC m-2. Bacterioplankton production constituted not more than 20% of total primary production (particulate + released), dynamics of bacterial production was related to the primary production, the correlation was negative with PPpart and positive with PPdiss. Different types of potential controlling factors of bacterioplankton (N and P nutrient control, bottom-up control by food and top-down control) are discussed.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1573-5117
    Keywords: Nutrient budget ; nutrient uptake ; shallowlake ; sedimentation ; resuspension ; denitrification
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The nutrient budget, phytoplankton primary productionand sedimentation rate were studied weekly in the large(270 km2) and shallow (mean depth 2.8 m)eutrophic Lake Võrtsjärv in 1995. The annualexternal loading was 7.7 g m™2 y™1 of totalnitrogen (TN) and 0.2 g m™2 y™1 of totalphosphorus (TP), including 7% of both inputs asdirect atmospheric precipitation. The external budgetrevealed a retention of 53% of TN and 28% of TPannual input. About 80% of the total loss of nitrogenwas accounted for by denitrification (3.3 g m™2 y™1) and only 20% was buried into the sediment.Wind-induced sediment resuspension played the majorrole in the upward nutrient flux formation and, thus,in the formation of the temporal pattern of nutrientconcentration during the ice-free season. Other fluxesas the external loading or new sedimentation ofautochthonous production were overcome and masked bythe powerful resuspension – sedimentation cycle,exceeding the former by one or two orders ofmagnitude. The intensity of upward flux of nutrients(mainly caused by resuspension) increased inaccordance to decreasing water level in autumn andcorrelated with the weekly average wind speed. Thesummer population of filamentous blue-greens dominatedby Limnothrix redekei was light-limited untilthe minima of TN:TP ratio (〈10) and DIN:TN ratio(∼ 0) in July initiated a clear peak of N_2-fixingalgae (Aphanizomenon gracile, Anabaena spp.)which lasted until September.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2021-02-08
    Description: We aimed at quantifying the importance of limnological variables in the decadal rise of cyanobacteria biomass in shallow hemiboreal lakes. We constructed estimates of cyanobacteria (blue-green algae) biomass in a large, eutrophic lake (Estonia, Northeastern Europe) from a database comprising 28 limnological variables and spanning more than 50 years of monitoring. Using a dual-model approach consisting in a boosted regression trees (BRT) followed by a generalized least squares (GLS) model, our results revealed that six variables were most influential for assessing the variance of cyanobacteria biomass. Cyanobacteria response to nitrate concentration and rotifer abundance was negative, whereas it was positive to pH, temperature, cladoceran and copepod biomass. Response to total phosphorus (TP) and total phosphorus to total nitrogen ratio was very weak, which suggests that actual in-lake TP concentration is still above limiting values. The most efficient GLS model, which explained nearly two thirds (r2 = 0.65) of the variance of cyanobacteria biomass included nitrate concentration, water temperature and pH. The very high number of observations (maximum n = 525) supports the robustness of the models. Our results suggest that the decadal rise of blue-green algae in shallow lakes lies in the interaction between cultural eutrophication and global warming which bring in-lake physical and chemical conditions closer to cyanobacteria optima.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2015-12-18
    Description: In this first worldwide synthesis of in situ and satellite-derived lake data, we find that lake summer surface water temperatures rose rapidly (global mean = 0.34°C decade −1 ) between 1985 and 2009. Our analyses show that surface water warming rates are dependent on combinations of climate and local characteristics, rather than just lake location, leading to the counterintuitive result that regional consistency in lake warming is the exception, rather than the rule. The most rapidly warming lakes are widely geographically distributed, and their warming is associated with interactions among different climatic factors—from seasonally ice-covered lakes in areas where temperature and solar radiation are increasing while cloud cover is diminishing (0.72°C decade −1 ) to ice-free lakes experiencing increases in air temperature and solar radiation (0.53°C decade −1 ). The pervasive and rapid warming observed here signals the urgent need to incorporate climate impacts into vulnerability assessments and adaptation efforts for lakes.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
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