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1

Bowling, LC. "Heat contents, thermal stabilities and Birgean wind work in Dystrophic Tasmanian Lakes and Reservoirs." Marine and Freshwater Research 41, no. 3 (1990): 429. http://dx.doi.org/10.1071/mf9900429.

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Values of whole-lake standard energy parameters (heat content, thermal stability and Birge's work of the wind) for ten dystrophic standing waters from western Tasmania were lower than expected for lakes of their depth and area. Although controlled principally by morphometric factors, the degree of shelter from wind and the extent of each lake's dystrophy also had considerable effects. These factors allowed only surface waters to contribute to the annual heat exchange cycle, thereby reducing the magnitude of each lake's heat budgets and influencing stability and wind work values. The lakes show
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2

Fiłoc, Magdalena, and Mirosława Kupryjanowicz. "Non-Pollen Palynomorphs Characteristic for the Dystrophic Stage of Humic Lakes in the Wigry National Park, Ne Poland." Studia Quaternaria 32, no. 1 (2015): 31–41. http://dx.doi.org/10.1515/squa-2015-0003.

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Abstract The numerous dystrophic (humic) lakes are a very important feature of Wigry National Park, NE Poland. As the most recent palaeoecological data indicate, at the beginning of its development (in the Late Glacial and Early and Middle Holocene) these water bodies functioned as harmonious lakes, and their transformation into dystrophic lakes and the stabilization of the trophic state took place at the beginning of the Subboreal. Palynological analysis of sediments from two such lakes (Lake Ślepe and Lake Suchar II), with special emphasis on non-pollen palynomorphs (NPPs), was aimed at a de
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3

Karpowicz, Maciej, Agnieszka Pasztaleniec, Magdalena Grabowska, and Anna Pietryczuk. "Deep chlorophyll maximum in temperate lakes with different trophic conditions − a rare or common phenomenon?" Knowledge & Management of Aquatic Ecosystems, no. 425 (2024): 1. http://dx.doi.org/10.1051/kmae/2023024.

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Deep chlorophyll maxima (DCM) are a common phenomenon in low-trophic stratified lakes, and there is much less information about the occurrence of DCM in eutrophic and dystrophic lakes. Therefore, we performed in situ continuous measurements of chlorophyll concentration by a submersible spectrofluorometer in 23 temperate lakes with different trophic conditions (mesotrophic, eutrophic, and dystrophic). We perform chemical analyses of available nutrient forms to better understand the mechanism of DCM formation. We found the highest concentration of phytoplankton in the metalimnion or upper hypoli
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4

Earle, J. Chris, Hamish C. Duthie, and David A. Scruton. "Analysis of the Phytoplankton Composition of 95 Labrador Lakes, with Special Reference to Natural and Anthropogenic Acidification." Canadian Journal of Fisheries and Aquatic Sciences 43, no. 9 (1986): 1804–11. http://dx.doi.org/10.1139/f86-224.

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Phytoplankton abundances and accompanying morphometric, physical, and chemical data from 95 Labrador lakes were subjected to statistical analysis to determine the structure of the phytoplankton communities and to relate environmental factors to the patterns observed. Factor analysis of the 22 measured physical and chemical variables reduced the data to six derived environmental factors: hardness, dystrophy, lake size, salinity, oligotrophy, and seasonality. The analysis showed that the low-pH lakes are associated with dystrophy and hence are likely to be naturally acidic. There was no evidence
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5

Adamec, Ludomír. "Why do aquatic carnivorous plants prefer growing in dystrophic waters?" Acta Biologica Slovenica 55, no. 1 (2012): 3–8. http://dx.doi.org/10.14720/abs.55.1.15520.

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The majority of aquatic carnivorous plants (ACPS; Aldrovanda, Utricularia) usually grow in shallow dystrophic waters. In these habitats, rootless ACPs usually grow together with rooted aquatic non-carnivorous plants (N-ACPs). Yet species diversity of rooted N-ACPs in dystrophic lakes is relatively poorer than that of abundant ACPs. If generally true, why do rootless ACPs prefer growing in shallow dystrophic waters and why is the occurrence of rooted N-ACPs in these waters limited? These questions are elucidated on the basis of different specific adaptive traits of both functional groups and a
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6

Parkman, Helena, and Markus Meili. "Mercury in Macroinvertebrates from Swedish Forest Lakes: Influence of Lake Type, Habitat, Life Cycle, and Food Quality." Canadian Journal of Fisheries and Aquatic Sciences 50, no. 3 (1993): 521–34. http://dx.doi.org/10.1139/f93-061.

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Mercury concentrations in lacustrine macroinvertebrates were concurrently studied in eight remote Swedish forest lakes of differing dystrophy, acidity, and eutrophy. The aim was to assess the influence of ecological factors (taxon, habitat, and feeding habits), chemical factors (characterizing different types of lakes), and regional and climatic factors (Hg deposition and mean temperature) on the accumulation of Hg. Concentrations varied from <50 to >5000 ng Hg∙g dry weight−1. A large part of this high variability could be ascribed to differences in water and sediment chemistry, ecologic
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7

Cudowski, Adam, Andrzej Stefan Górniak, and Marta Hryniewicka. "Boron and manganese fractions in dystrophic lake waters (Wigry National Park, NE Poland)." Limnological Review 13, no. 2 (2013): 79–86. http://dx.doi.org/10.2478/limre-2013-0009.

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Abstract Physicochemical studies in four dystrophic lakes (Suchar Wielki, Suchar II, Suchar IV, and Wądołek) were carried out in Wigry National Park, NE Poland. Total manganese concentrations oscillated within the range of 386.6-647.5 μg Mn dm-3, while those of soluble reactive manganese, 112.5-328.2 μg Mn dm-3. Fairly high boron contents were recorded in the studied lakes, which amounted to 0.09-2.20 mg B dm-3. The increase in dissolved reactive manganese (DRMn) and decrease in dissolved boron concentration with the lake depth were observed. Almost half (47%) of the total manganese pool was c
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8

Pakulnicka, J., and A. Zawal. "Model of disharmonic succession of dystrophic lakes based on aquatic beetle fauna (Coleoptera)." Marine and Freshwater Research 70, no. 2 (2019): 195. http://dx.doi.org/10.1071/mf17050.

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Directional changes in environmental conditions during individual stages of the succession of lakes should determine the character of the aquatic beetle fauna inhabiting them. Can changes in environmental conditions lead to degradation of fauna and to a deterioration of the ecological quality of lakes? We analysed this problem in 40 lakes. The fauna of the lakes proved to be rich and diverse in terms of species. Deterioration of species richness along successional stages was not observed, but distinct changes were noted in faunal composition. The eurytopic component proved stable, whereas chan
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9

Petrov, Vladimir N., and Anastasija J. Karpaeva. "The role of diatoms algae in phytoplankton of dystrophic lakes." Issues of modern algology (Вопросы современной альгологии), no. 2(32) (2023): 170–71. http://dx.doi.org/10.33624/2311-0147-2023-2(32)-170-171.

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The paper presents seasonal indicators of the abundance and biomass of the dominant groups of algae in the phytoplankton of lakes Kurganistoye and Yazhginya. In both lakes the largest values of summer abundance and biomass are formed by cryptophyte algae. A group of diatoms formed the peaks of only the May values of the abundance and biomass of phytoplankton in Lake Yazhginya.
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10

Górniak, A., E. Jekatierynczuk-Rudczyk, and P. Dobrzyń. "Hydrochemistry of Three Dystrophic Lakes in Northeastern Poland." Acta hydrochimica et hydrobiologica 27, no. 1 (1999): 12–18. http://dx.doi.org/10.1002/(sici)1521-401x(199901)27:1<12::aid-aheh12>3.0.co;2-x.

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11

Earle, J. C., H. C. Duthie, and David A. Scruton. "Factors Influencing the Distribution of Phytoplankton in 97 Headwater Lakes in Insular Newfoundland." Canadian Journal of Fisheries and Aquatic Sciences 44, no. 3 (1987): 639–49. http://dx.doi.org/10.1139/f87-078.

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Phytoplankton samples collected from 97 headwater lakes throughout insular Newfoundland were analyzed and used as a basis for a statistical evaluation of the environmental factors influencing species distributions. A selected subset of 77 taxa were clustered using a complete-linkage cluster analysis. The final 12 clusters represent the associations of species found occurring together in insular Newfoundland. Physical, chemical, and morphometric data collected with the phytoplankton served to characterize the environment. Factor analysis simplified the original variables, many of which were hig
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12

Molenda, Tadeusz, Beata Kostka, Ireneusz Malik, Paweł Lejwoda, Wiktor Radziejowski, and Joanna Kidawa. "Polyhumous Dystrophic Pit Lakes: Hydrographic and Hydrochemical Characteristics on the Example of Reservoirs in the Włoszczowska Basin, Central Poland." Energies 15, no. 7 (2022): 2681. http://dx.doi.org/10.3390/en15072681.

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The article presents the hydrographic and hydrochemical characteristics of post-exploitation reservoirs formed in peat excavations. Two natural bog lakes were selected as the control objects for the study. The research indicated that both the waters of post-exploitation peat reservoirs and natural bog lakes show low electrolytic conductivity (&lt;100 µS/cm) and acidic water reaction (pH &lt; 5.5). The concentration of major cations and anions is also very low. The concentration of calcium and magnesium does not exceed a few mg/L. Hydrochemically, all post-exploitation peat reservoirs are bi-io
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13

Bowling, LC, and K. Salonen. "Heat uptake and resistance to mixing in small humic forest lakes in Southern Finland." Marine and Freshwater Research 41, no. 6 (1990): 747. http://dx.doi.org/10.1071/mf9900747.

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The annual heat budgets and maximum thermal stabilities achieved by small Finnish forest lakes are considerable for lakes of their size. Heat uptake is rapid during the brief period of vernal circulation, with the latent heat of fusion of ice contributing substantially to this. Heating then slows, with maximum heat contents and thermal stabilities occurring around early August. Absorption of solar radiation by the dystrophic waters, effective shelter from wind-induced turbulence, and considerable relative depths all combine to prevent mixing of heat much below the surface 2 m of most study lak
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14

Pakulnicka, Joanna, and Andrzej Zawal. "Effect of changes in the fractal structure of a littoral zone in the course of lake succession on the abundance, body size sequence and biomass of beetles." PeerJ 6 (September 26, 2018): e5662. http://dx.doi.org/10.7717/peerj.5662.

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Dystrophic lakes undergo natural disharmonic succession, in the course of which an increasingly complex and diverse, mosaic-like pattern of habitats evolves. In the final seral stage, the most important role is played by a spreading Sphagnum mat, which gradually reduces the lake’s open water surface area. Long-term transformations in the primary structure of lakes cause changes in the structure of lake-dwelling fauna assemblages. Knowledge of the succession mechanisms in lake fauna is essential for proper lake management. The use of fractal concepts helps to explain the character of fauna in r
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15

Aquino, Regimeire Freitas, José Maria de Lima, Ciro Augusto de Souza Magalhães, Bruno Montoani Silva, Renato Fráguas de Carvalho, and Luiz Roberto Guimarães Guilherme. "Atrazine in a corn cultivated area and its relation with the landscape position." Ciência e Agrotecnologia 37, no. 5 (2013): 389–96. http://dx.doi.org/10.1590/s1413-70542013000500001.

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Atrazine is still being used in no-till corn production in Brazil. This herbicide can be moved by overland flow and leached in the soil profile. In both ways, it can pollute water, either by reaching the groundwater or lakes and streams close to the crop field. This study evaluated the presence of atrazine in a dystrophic Yellow-Red Argisol and a dystrophic Melanic Gleisol in a corn field, where atrazine has been applied for 11 years. Overland flow was the main process of atrazine transport on hillslope and leaching was the most important process in the floodplain. Frequency and location of at
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16

Strüder-Kypke, Michaela C. "Periphyton and sphagnicolous protists of dystrophic bog lakes (Brandenburg, Germany)." Limnologica 29, no. 4 (1999): 393–406. http://dx.doi.org/10.1016/s0075-9511(99)80047-4.

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17

Strüder-Kypke, Michaela C., and Wilfried Schönborn. "Periphyton and sphagnicolous protists of dystrophic bog lakes (Brandenburg, Germany)." Limnologica 29, no. 4 (1999): 407–24. http://dx.doi.org/10.1016/s0075-9511(99)80049-8.

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18

Lauster, George H., Paul C. Hanson, and Timothy K. Kratz. "Gross primary production and respiration differences among littoral and pelagic habitats in northern Wisconsin lakes." Canadian Journal of Fisheries and Aquatic Sciences 63, no. 5 (2006): 1130–41. http://dx.doi.org/10.1139/f06-018.

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Net ecosystem production (NEP) trends among lakes have been ascribed to differences in nutrient and allochthonous carbon inputs, but little is known on how different habitats within lakes contribute to these trends. We sampled pelagic and littoral surface waters using sonde (i.e., free-water) and bottle methods concurrently in lakes spanning a range of trophic conditions. We considered whether the typically higher metabolism estimates found with sonde methods are due to contributions from littoral habitats not reflected by bottle estimates. We sought the source of littoral contributions by sel
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19

Watras, C. J., K. A. Morrison, and N. S. Bloom. "Mercury in remote Rocky Mountain lakes of Glacier National Park, Montana, in comparison with other temperate North American regions." Canadian Journal of Fisheries and Aquatic Sciences 52, no. 6 (1995): 1220–28. http://dx.doi.org/10.1139/f95-119.

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We determined concentrations of mercury (Hg) and methylmercury (MeHg) in 12 pristine lakes of Glacier National Park (GNP) and compared our observations with data from published studies of remote lakes in north-central Wisconsin and the Adirondack region of New York. Despite marked differences in water chemistry, biology, and hydrogeology, concentrations of Hg and MeHg in all regions were strongly correlated with dissolved organic carbon (DOC). Variables related to the acid–base status of lake waters had secondary effects on the concentration of waterborne mercury species. Although Hg and MeHg
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20

Kalinowska, K., A. Napiórkowska-Krzebietke, D. Ulikowski, E. Bogacka-Kapusta, K. Stawecki, and P. Traczuk. "Under-ice environmental conditions, planktonic communities and ichthyofauna in dystrophic lakes." European Zoological Journal 88, no. 1 (2021): 340–51. http://dx.doi.org/10.1080/24750263.2021.1889054.

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21

Strzałka, Małgorzata, Katarzyna Kozakiewicz, and Tomasz Postawa. "Does water quality matter? Foraging activity of Daubenton’s bat (Myotis daubentonii) over three lakes with different trophy." Theriologia Ukrainica 2024, no. 28 (2024): 161–70. https://doi.org/10.53452/tu2814.

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The trophic parameters of water bodies, especially the content of biogenic components, may have an impact on invertebrate communities, both those strictly aquatic and those using the water bodies periodically. Among this group, insects are highly relevant, the density of which can affect the attractiveness of the water body as foraging habitat of water-surface forager bats. The present paper presents the results of a study measuring the foraging activity of Myotis daubentonii (Kuhl, 1917) in linear transects over three water bodies: an oligotrophic, eutrophic, and dystrophic lake located withi
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22

Rychert, Krzysztof, Magdalena Wielgat-Rychert, Anna Matviikiv, Yana Kryvoshei, and Anastasiia Parfeniuk. "Planktonic communities in a small post-peat reservoir (Ustka Forest District, Poland)." Folia Forestalia Polonica 63, no. 3 (2021): 260–66. http://dx.doi.org/10.2478/ffp-2021-0026.

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Abstract The aim of this study was to evaluate the present state of a small (area of 0.2 ha), shallow (mean depth of 2 m) and approximately 30-year-old post-peat reservoir located in Bruskowskie Bagno, a Baltic raised mire in northern Poland. The study was conducted during all seasons of the year (August 2019–July 2020). The reservoir was characterised by a yellow to brown water colour, low pH (5.4) and quite low conductivity (40.4 μS cm-1), which are the main features of dystrophic water bodies. Similar to natural, dystrophic lakes and ponds, the phytoplankton was mainly composed of mixotroph
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23

Croome, RL, and PA Tyler. "Structure and ecology of the flagellate Scourfieldia caeca (Korsh.) Belcher & Swale in two meromictic lakes in Tasmania." Marine and Freshwater Research 36, no. 3 (1985): 413. http://dx.doi.org/10.1071/mf9850413.

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The minute green flagellate S. caeca occurs in large numbers in two dystrophic meromictic lakes in Tasmania, constantly occupying a narrow stratum immediately above the chemocline, where physical and chemical conditions change dramatically with depth and where available light is less than 1% of surface radiation and restricted to red wavelengths. In its ultrastructure, S. caeca resembles cultured material described previously but differs in the structure and size of its chloroplast and in the structure of its diagnostic keel of starch.
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24

Kostrzewska-Szlakowska, Iwona, and Bartosz Kiersztyn. "Microbial Biomass and Enzymatic Activity of the Surface Microlayer and Subsurface Water in Two Dystrophic Lakes." Polish Journal of Microbiology 66, no. 1 (2017): 75–84. http://dx.doi.org/10.5604/17331331.1234995.

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Nutrient and organic matter concentration, microbial biomass and activities were studied at the surface microlayers (SML) and subsurface waters (SSW) in two small forest lakes of different water colour. The SML in polyhumic lake is more enriched with dissolved inorganic nitrogen (0.141 mg l–1) than that of oligohumic lake (0.124 mg l–1), the former also contains higher levels of total nitrogen (2.66 mg l–1). Higher activities of lipase (Vmax 2290 nmol l–1 h–1 in oligo- and 6098 in polyhumic) and glucosidase (Vmax 41 nmol l–1 h–1 in oligo- and 49 in polyhumic) were in the SMLs in both lakes. Ph
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25

Sepulveda-Jauregui, A., K. M. Walter Anthony, K. Martinez-Cruz, S. Greene, and F. Thalasso. "Methane and carbon dioxide emissions from 40 lakes along a north–south latitudinal transect in Alaska." Biogeosciences Discussions 11, no. 9 (2014): 13251–307. http://dx.doi.org/10.5194/bgd-11-13251-2014.

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Abstract. Uncertainties in the magnitude and seasonality of various gas emission modes, particularly among different lake types, limit our ability to estimate methane (CH4) and carbon dioxide (CO2) emissions from northern lakes. Here we assessed the relationship between CH4 and CO2 emission modes in 40 lakes along a latitudinal transect in Alaska to physicochemical limnology and geographic characteristics, including permafrost soil type surrounding lakes. Emission modes included Direct Ebullition, Diffusion, Storage flux, and a newly identified Ice-Bubble Storage (IBS) flux. We found that all
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26

Krzysztof, Rychert, Wielgat-Rychert Magdalena, Matviikiv Anna, Kryvoshei Yana, and Parfeniuk Anastasiia. "Planktonic communities in a small post-peat reservoir (Ustka Forest District, Poland)." FOLIA FORESTALIA POLONICA, SERIES A – FORESTRY 63, no. 3 (2021): 260–66. https://doi.org/10.2478/ffp-2021-0026.

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The aim of this study was to evaluate the present state of a small (area of 0.2 ha), shallow (mean depth of 2 m) and approximately 30-year-old post-peat reservoir located in Bruskowskie Bagno, a Baltic raised mire in northern Poland. The study was conducted during all seasons of the year (August 2019&ndash;July 2020). The reservoir was characterised by a yellow to brown water colour, low pH (5.4) and quite low conductivity (40.4 &mu;S cm<sup>-1</sup>), which are the main features of dystrophic water bodies. Similar to natural, dystrophic lakes and ponds, the phytoplankton was mainly composed o
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27

Eiler, Alexander, Sara Beier, Christin S�wstr�m, Jan Karlsson, and Stefan Bertilsson. "High Ratio of Bacteriochlorophyll Biosynthesis Genes to Chlorophyll Biosynthesis Genes in Bacteria of Humic Lakes." Applied and Environmental Microbiology 75, no. 22 (2009): 7221–28. http://dx.doi.org/10.1128/aem.00960-09.

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ABSTRACT Recent studies highlight the diversity and significance of marine phototrophic microorganisms such as picocyanobacteria, phototrophic picoeukaryotes, and bacteriochlorophyll- and rhodopsin-holding phototrophic bacteria. To assess if freshwater ecosystems also harbor similar phototroph diversity, genes involved in the biosynthesis of bacteriochlorophyll and chlorophyll were targeted to explore oxygenic and aerobic anoxygenic phototroph composition in a wide range of lakes. Partial dark-operative protochlorophyllide oxidoreductase (DPOR) and chlorophyllide oxidoreductase (COR) genes in
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28

Myrstener, Erik, Harald Biester, Christian Bigler, et al. "Environmental footprint of small-scale, historical mining and metallurgy in the Swedish boreal forest landscape: The Moshyttan blast furnace as microcosm." Holocene 29, no. 4 (2019): 578–91. http://dx.doi.org/10.1177/0959683618824741.

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The history of mining and smelting and the associated pollution have been documented using lake sediments for decades, but the broader ecological implications are not well studied. We analyzed sediment profiles covering the past ~10,000 years from three lakes associated with an iron blast furnace in central Sweden, as an example of the many small-scale furnaces with historical roots in the medieval period. With a focus on long-term lake-water quality, we analyzed multiple proxies including geochemistry, pollen and charcoal, diatom composition and inferred pH, biogenic silica (bSi), visible nea
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29

Howell, Nathan, Alexander Krings, and Richard Braham. "Guide to the littoral zone vascular flora of Carolina bay lakes (U.S.A.)." Biodiversity Data Journal 4 (April 5, 2016): e7964. https://doi.org/10.3897/BDJ.4.e7964.

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Carolina bays are elliptic, directionally aligned basins of disputed origin that occur on the Atlantic Coastal Plain from the Delmarva Peninsula to southern Georgia. In southeastern North Carolina, several large, natural, lacustrine systems (i.e., Carolina bay lakes) exist within the geomorphological features known as Carolina bays. Within the current distribution of Carolina bays, Bladen and Columbus counties (North Carolina) contain the only known examples of Carolina bay lakes. The Carolina bay lakes can be split into two major divisions, the "Bladen Lakes Group" which is characterized as b
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30

Khilchevskyi, V. K., and M. R. Zabokrytska. "MAIN ASPECTS OF THE MORPHOMETRY AND HYDROCHEMISTRY OF SHATSK LAKES." Hydrology, hydrochemistry and hydroecology, no. 3 (58) (2020): 92–100. http://dx.doi.org/10.17721/2306-5680.2020.3.9.

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The purpose of the study was to identify the modern morphometric characteristics of Shatsk Lakes (Volyn Polissya, Ukraine), to implement their typology according to the area of the water mirror and average depths, to establish the type of water by salinity. For research, materials from the Shatsk National Nature Park, literary and archival sources, and the results of our own research were used. The typification of Shatsky Lakes was carried out in accordance with the requirements of the Water Framework Directive of the European Union (EU WFD) according to the methodology adopted in Ukraine for
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31

Nelson, Jay A., and John J. Magnuson. "Metabolic Stores of Yellow Perch (Perca flavescens): Comparison of Populations from an Acidic, Dystrophic Lake and Circumneutral, Mesotrophic Lakes." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 12 (1992): 2474–82. http://dx.doi.org/10.1139/f92-273.

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Little is known about the animals that occupy naturally acidic habitats. To better understand the physiological state of animals from temperate, naturally acidic systems, we compared metabolite stores and meristics of two yellow perch (Perca flavescens) populations in northern Wisconsin. One population originated from a naturally acidic, dystrophic lake (Acid-Lake-Perch, ALP) and had previously been shown to have enhanced tolerance to low pH. The second population came from two nearby interconnected circumneutral, mesotrophic lakes (Neutral-Lake-Perch, NLP). Perch were collected throughout the
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32

Lau, Danny C. P., Ingvar Sundh, Tobias Vrede, Jana Pickova, and Willem Goedkoop. "Autochthonous resources are the main driver of consumer production in dystrophic boreal lakes." Ecology 95, no. 6 (2014): 1506–19. http://dx.doi.org/10.1890/13-1141.1.

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33

Forsius, M., T. Saloranta, L. Arvola, et al. "Physical and chemical consequences of artificially deepened thermocline in a small humic lake – a paired whole-lake climate change experiment." Hydrology and Earth System Sciences 14, no. 12 (2010): 2629–42. http://dx.doi.org/10.5194/hess-14-2629-2010.

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Abstract. Climate change with higher air temperatures and changes in cloud cover, radiation and wind speed alters the heat balance and stratification patterns of lakes. A paired whole-lake thermocline manipulation experiment of a small (0.047 km2) shallow dystrophic lake (Halsjärvi) was carried out in southern Finland. A thermodynamic model (MyLake) was used for both predicting the impacts of climate change scenarios and for determining the manipulation target of the experiment. The model simulations assuming several climate change scenarios indicated large increases in the whole-lake monthly
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34

Reitzel, Kasper, Joakim Ahlgren, Adolf Gogoll, Henning S. Jensen, and Emil Rydin. "Characterization of phosphorus in sequential extracts from lake sediments using 31P nuclear magnetic resonance spectroscopy." Canadian Journal of Fisheries and Aquatic Sciences 63, no. 8 (2006): 1686–99. http://dx.doi.org/10.1139/f06-070.

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Phosphorus (P) compounds in three different lake surface sediments were extracted by sequential P extraction and identified by 31P nuclear magnetic resonance (31P NMR) spectroscopy. The extraction procedure primarily discriminates between inorganic P-binding sites but most extraction steps also contained P not reacting (nrP) with the molybdenum complex during P analyses. In all three lakes, the nrP dominated in the NaOH extracts. Nonreactive P from the dystrophic lake was dominated by potentially recalcitrant P groups such as orthophosphate monoesters, while the nrP in the two more productive
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35

Zawiska, Izabela, Edyta Zawisza, Michał Woszczyk, Krystyna Szeroczyńska, Waldemar Spychalski, and Alexander Correa-Metrio. "Cladocera and geochemical evidence from sediment cores show trophic changes in Polish dystrophic lakes." Hydrobiologia 715, no. 1 (2013): 181–93. http://dx.doi.org/10.1007/s10750-013-1482-0.

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36

Tonn, William M., and Cynthia A. Paszkowski. "Habitat use of the central mudminnow (Umbra limi) and yellow perch (Perca flavescens) in Umbra-Perca assemblages: the roles of competition, predation, and the abiotic environment." Canadian Journal of Zoology 65, no. 4 (1987): 862–70. http://dx.doi.org/10.1139/z87-137.

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We compared spatial distributions and diel activity patterns of three fish populations (co-occurring central mudminnows and yellow perch, and a mudminnow population in a single-species assemblage) throughout the year in two small, northern Wisconsin dystrophic lakes. In winter, all three populations were more active offshore and during the day. During spring and summer–fall all were concentrated inshore, near the bottom, and were more active around dawn and dusk. Winter distributions appeared to be responses to abiotic conditions (ice cover and low oxygen availability); overall patterns during
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37

Forsius, M., T. Saloranta, L. Arvola, et al. "Physical and chemical consequences of artificially deepened thermocline in a small humic lake – a paired whole-lake climate change experiment." Hydrology and Earth System Sciences Discussions 7, no. 3 (2010): 2915–47. http://dx.doi.org/10.5194/hessd-7-2915-2010.

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Abstract. Climate change with higher air temperatures and changes in cloud cover, radiation and wind speed alters the heat balance and stratification patterns of lakes. A paired whole-lake thermocline manipulation experiment of a small (0.047 km2) shallow dystrophic lake (Halsjärvi) was carried out in southern Finland. A thermodynamic model (MyLake) was used for both predicting the impacts of climate change scenarios and for determining the manipulation target of the experiment. The model simulations assuming several climate change scenarios indicated large increases in the whole-lake monthly
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Dvoryankin, Gennady. "BIOLOGY, ECOLOGY AND FISHERY VALUE OF RIVER PERCH (PERCA FLUVIATILIS (L.)) OF THE KENOZERSKY NATIONAL PARK." Vestnik of Astrakhan State Technical University. Series: Fishing industry 2021, no. 1 (2021): 24–30. http://dx.doi.org/10.24143/2073-5529-2021-1-24-30.

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The article describes the habitat and behavior of the river perch (Perca fluviatilis L.), which dominates the reservoirs of the Kenozero National Park (KNP). It is not found only in the dystrophic crucian lakes. In its habitats, perch is also one of the most numerous species and, as &#x0D; a result, an important object of recreational fishing. There are presented the results of studying perch populations in the main fishery reservoirs of the KNP obtained in 2007-2019 in the course of author's research. The information about biology, ecology and abundance of perch is given. The stock status and
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39

Schiff, Sherry L., and Robert F. Anderson. "Limnocorral Studies of Chemical and Biological Acid Neutralization in Two Freshwater Lakes." Canadian Journal of Fisheries and Aquatic Sciences 44, S1 (1987): s173—s187. http://dx.doi.org/10.1139/f87-293.

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Twenty-nine 1 m diameter limnocorrals were installed in two Canadian Shield lakes to examine the relative importance of individual acid neutralization processes. Once the water column alkalinity was depleted, the within-lake alkalinity production processes were confined to the lake sediments. The flocculent organic-rich sediments of a shallow dystrophic lake (Lake 114) neutralized acid at a significantly greater rate than the sandy littoral sediments of an oligotrophy lake (Lake 302). Since the water column alkalinity of Lake 114 is much lower than Lake 302, ambient alkalinity is not a good pr
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40

Croome, RL, and PA Tyler. "Distribution of silica-scaled Chrysophyceae (Paraphysomonadaceae and Mallomonadaceae) in Australian inland waters." Marine and Freshwater Research 36, no. 6 (1985): 839. http://dx.doi.org/10.1071/mf9850839.

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Thirty-two species of silica-scaled Chrysophyceae of the genera Spiniferomonas, Chrysosphaerella and Paraphysomonas, belonging to the Paraphysomonadaceae Preisig &amp; Hibberd, 1983, and Mallomonas, Mallomonopsis and Synura, belonging to the Mallomonadaceae (Diesing, 1866) Preisig &amp; Hibberd, 1983, are recognized by electron microscopy from a wide range of Australian freshwater habitats, from tropical to temperate regions, and from a range of trophic types of lake. Eleven species are reported from Australia for the first time, and three from the Southern Hemisphere for the first time. Altho
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41

Planidin, N. P., and T. E. Reimchen. "Spatial, sexual, and rapid temporal differentiation in neuromast expression on lateral plates of Haida Gwaii threespine stickleback (Gasterosteus aculeatus)." Canadian Journal of Zoology 97, no. 11 (2019): 988–96. http://dx.doi.org/10.1139/cjz-2019-0005.

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Lateral lines, a major sensory modality in fishes, are diverse among taxa, but their intraspecific variation has received limited attention. We examined numbers of superficial neuromasts on the buttressing lateral plates (LP) of 1910 threespine stickleback (Gasterosteus aculeatus Linnaeus, 1758) from 26 ecologically and morphologically diverse populations on the Haida Gwaii archipelago, western Canada. Extending from previous studies, we predicted that (i) highly stained dystrophic localities would have threespine stickleback with elevated numbers of neuromasts per plate due to a greater relia
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42

Drzymulska, Danuta, Magdalena Fiłoc, and Mirosława Kupryjanowicz. "Reconstruction of landscape paleohydrology using the sediment archives of three dystrophic lakes in northeastern Poland." Journal of Paleolimnology 51, no. 1 (2013): 45–62. http://dx.doi.org/10.1007/s10933-013-9754-2.

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43

KOROSI, JENNIFER B., and JOHN P. SMOL. "Contrasts between dystrophic and clearwater lakes in the long-term effects of acidification on cladoceran assemblages." Freshwater Biology 57, no. 12 (2012): 2449–64. http://dx.doi.org/10.1111/fwb.12012.

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44

Kirkwood, Andrea E., Patricia Chow-Fraser, and Greg Mierle. "Seasonal mercury levels in phytoplankton and their relationship with algal biomass in two dystrophic shield lakes." Environmental Toxicology and Chemistry 18, no. 3 (1999): 523–32. http://dx.doi.org/10.1002/etc.5620180322.

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45

Fiłoc, Magdalena, Mirosława Kupryjanowicz, and Danuta Drzymulska. "Late Glacial and Holocene Vegetation Changes in the Wigry National Park, Ne Poland – New Pollen Data from Three Small Dystrophic Lakes." Studia Quaternaria 31, no. 1 (2014): 5–16. http://dx.doi.org/10.2478/squa-2014-0001.

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Abstract The main phases of the Late Glacial and Holocene development of vegetation in the Wigry National Park were reconstructed based on the pollen analysis of sediments from three small dystrophic lakes (Lake Suchar Wielki, Lake Suchar II and Lake Ślepe). At the current stage of research, the age of the studied deposits was determined by AMS radiocarbon dating of few samples only. This meant that the chronology of the investigated sections had to be estimated also indirectly using their palynological correlation with the radiometrically well-dated section from Lake Wigry. The obtained polle
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Zawisza, Edyta, Izabela Zawiska, and Alexander Correa-Metrio. "Cladocera Community Composition as a Function of Physicochemical and Morphological Parameters of Dystrophic Lakes in NE Poland." Wetlands 36, no. 6 (2016): 1131–42. http://dx.doi.org/10.1007/s13157-016-0832-x.

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47

Vanhoutte, K., E. Verleyen, W. Vyverman, V. Chepurnov, and K. Sabbe. "The freshwater diatom genus Kobayasiella (Bacillariophyta) in Tasmania, Australia." Australian Systematic Botany 17, no. 5 (2004): 483. http://dx.doi.org/10.1071/sb03035.

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Representatives of the diatom genus Kobayasiella Lange-Bertalot (Bacillariophyta) are common in benthic diatom communities of oligotrophic and dystrophic highland lakes in Tasmania Australia. A taxonomic revision of this genus revealed the presence of four unknown taxa, which are here formally described. Kobayasiella acidophila sp. nov., K.�australis sp. nov., K.�hodgsonii sp. nov. and K.�tasmanica sp. nov. differ from all described Kobayasiella species in dimensions and stria density (K.�acidophila, K.�hodgsonii), the presence of elongated areolae at the valve apex (K.�australis) or the prese
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48

Bergström, Ann-Kristin, M. Jansson, P. Blomqvist, and S. Drakare. "The influence of water colour and effective light climate on mixotrophic phytoflagellates in three small Swedish dystrophic lakes." SIL Proceedings, 1922-2010 27, no. 4 (2000): 1861–65. http://dx.doi.org/10.1080/03680770.1998.11901562.

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49

Watras, C. J., K. A. Morrison, J. T. Crawford, C. P. McDonald, S. K. Oliver, and P. C. Hanson. "Diel cycles in the fluorescence of dissolved organic matter in dystrophic Wisconsin seepage lakes: Implications for carbon turnover." Limnology and Oceanography 60, no. 2 (2015): 482–96. http://dx.doi.org/10.1002/lno.10026.

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Crapart, Camille, Tom Andersen, Dag Olav Hessen, Nicolas Valiente, and Rolf David Vogt. "Factors Governing Biodegradability of Dissolved Natural Organic Matter in Lake Water." Water 13, no. 16 (2021): 2210. http://dx.doi.org/10.3390/w13162210.

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Dissolved Natural Organic Matter (DNOM) is a heterogeneous mixture of partly degraded, oxidised and resynthesised organic compounds of terrestrial or aquatic origin. In the boreal biome, it plays a central role in element cycling and practically all biogeochemical processes governing the physico-chemistry of surface waters. Because it plays a central role in multiple aquatic processes, especially microbial respiration, an improved understanding of the biodegradability of the DNOM in surface water is needed. Here the current study, we used a relatively cheap and non-laborious analytical method
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