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23 pages, 8057 KiB  
Article
Hydrochemical Dynamics and Water Quality Assessment of the Ramsar-Listed Ghodaghodi Lake Complex: Unveiling the Water-Environment Nexus
by Ganga Paudel, Ramesh Raj Pant, Tark Raj Joshi, Ahmed M. Saqr, Bojan Đurin, Vlado Cetl, Pramod N. Kamble and Kiran Bishwakarma
Water 2024, 16(23), 3373; https://doi.org/10.3390/w16233373 (registering DOI) - 23 Nov 2024
Viewed by 437
Abstract
Human activities and climate change increasingly threaten wetlands worldwide, yet their hydrochemical properties and water quality are often inadequately studied. This research focused on the Ghodaghodi Lake Complex (GLC) and associated lakes in Nepal, a Ramsar-listed site known for its biodiversity and ecological [...] Read more.
Human activities and climate change increasingly threaten wetlands worldwide, yet their hydrochemical properties and water quality are often inadequately studied. This research focused on the Ghodaghodi Lake Complex (GLC) and associated lakes in Nepal, a Ramsar-listed site known for its biodiversity and ecological significance. The study was conducted to assess seasonal water quality, investigate the factors influencing hydrochemistry, and assess the lakes’ suitability for irrigation. Forty-nine water samples were collected from the GLC in pre-monsoon and post-monsoon periods. Nineteen physicochemical parameters, such as dissolved oxygen (DO), total dissolved solids (TDS), and major ions (calcium ‘Ca2+’, magnesium ‘Mg2+’, and bicarbonate ‘HCO3’), were analyzed using standard on-site and laboratory methods. Statistical methods, including analysis of variance (ANOVA), T-tests, and hydrochemical diagrams, e.g., Piper, were adopted to explore spatial and seasonal variations in water quality, revealing significant fluctuations in key hydrochemical indicators. Results showed marked seasonal differences, with pre-monsoon TDS levels averaging 143.1 mg/L compared to 78.9 mg/L post-monsoon, underscoring evaporation and dilution effects. The hydrochemical analysis identified Ca2+-HCO3 as the dominant water type, highlighting the influence of carbonate weathering on GLC’s water composition. Gibbs, mixing, and Piper diagram analysis supported these findings, confirming the predominance of HCO3, with Ca2+ and Mg2+ as the main cations. Additionally, sodium adsorption ratio (SAR) values were consistently below 1, confirming excellent irrigation quality. These findings provided critical data for policymakers and stakeholders, supporting sustainable wetland management and aligning with the United Nations’ Sustainable Development Goals relevant to environmental conservation, i.e., clean water and life on land. Full article
(This article belongs to the Special Issue Water Quality Assessment of River Basins)
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Graphical abstract

Graphical abstract
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<p>Study area region illustrating Ghodaghodi Lake and its adjacent lakes, including sampling sites: (<b>i</b>) A global map illustrating the study area, marked by a red polygon; (<b>ii</b>) A map of the Kailali District highlighting Ghodaghodi Municipality in yellow and the Ramsar site encompassing the Ghodaghodi Lake complex (GLC) in red; (<b>iii</b>) A map of the GLC-Ramsar site, depicting the locations of Ghodaghodi Lake and its associated lakes, classified into Section ‘A’ and Section ‘B’ with delineations; (<b>iv</b>) Locations of Bichka Chaita, Budhiya Nakhrod, Ramphal, and Sanopokhari Lakes along with their respective sampling sites BC1–BC5, BN1–BN5, R1–R5, and SP1–SP5, and (<b>v</b>) Locations of Ghodaghodi and Ojahuwa Lakes with their corresponding sampling sites G1–G24 and OH1–OH5.</p>
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<p>Land use/land cover map of the study area region illustrating different categories adjacent to sampling points of the lakes.</p>
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<p>Piper diagram for the classification of lake water types in Ghodaghodi and its associated lakes (Ojahuwa, Bichka Chaita, and Sanopokhari) during the pre-monsoon season, featuring three plots: anionic, cationic, and diamond plots.</p>
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<p>Piper diagram for the classification of lake water types in Ghodaghodi and its related lakes (Ojahuwa, Bichka Chaita, Budhiya Nakhrod, Ramphal, and Sanopokhari) during the post-monsoon season, featuring three plots: anionic, cationic, and diamond plots.</p>
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<p>Gibbs diagrams illustrating the fluctuation of the weight ratio of Na<sup>+</sup>/(Na<sup>+</sup> + Ca<sup>2+</sup>) and Cl<sup>−</sup>/(Cl<sup>−</sup> + HCO<sup>3−</sup>) concerning TDS (pre-monsoon) throughout all examined lakes (Ghodaghodi, Ojahuwa, Bichka Chaita, and Sanopokhari).</p>
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<p>Gibbs diagrams illustrating the fluctuation of the weight ratio of Na<sup>+</sup>/(Na<sup>+</sup> + Ca<sup>2+</sup>) and Cl<sup>−</sup>/(Cl<sup>−</sup> + HCO<sup>3−</sup>) concerning TDS (post-monsoon) throughout all examined lakes (Ghodaghodi, Ojahuwa, Bichka Chaita, Budhiya Nakhrod, Ramphal, and Sanopokhari).</p>
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<p>Mixing diagrams illustrating the roles of carbonate, silicate, and evaporates in the hydrochemistry of Ghodaghodi and associated lakes (Ojahuwa, Bichka Chaita, and Sanopokhari) during the pre-monsoon season. (<b>a</b>) represents HCO<sub>3</sub><sup>−</sup>/Na<sup>+</sup> vs Ca<sup>2+</sup>/Na<sup>+</sup> and (<b>b</b>) represents Mg<sup>2+</sup>/Na<sup>+</sup> vs Ca<sup>2+</sup>/Na<sup>+</sup> of mixing diagram.</p>
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<p>Mixing diagrams illustrating the roles of carbonate, silicate, and evaporates in the hydrochemistry of Ghodaghodi and its associated lakes (Ojahuwa, Bichka Chaita, Budhiya Nakhrod, Ramphal, and Sanopokhari) during the post-monsoon season. (<b>a</b>) represents HCO<sub>3</sub><sup>−</sup>/Na<sup>+</sup> vs Ca<sup>2+</sup>/Na<sup>+</sup> and (<b>b</b>) represents Mg<sup>2+</sup>/Na<sup>+</sup> vs Ca<sup>2+</sup>/Na<sup>+</sup> of mixing diagram.</p>
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<p>Wilcox diagram depicting the irrigation water quality based on SAR and EC for Ghodaghodi Lake and three related lakes (Ojahuwa, Bichka Chaita, and Sanopokhari) during the pre-monsoon period.</p>
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<p>Wilcox diagram depicting the irrigation water quality based on SAR and EC for Ghodaghodi Lake and five related lakes (Ojahuwa, Bichka Chaita, Sanopokhari, Budhiya Nakhrod, and Ramphal) during the post-monsoon period.</p>
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<p>Hydrochemical dynamics, sustainable development goals (SDGs) impact, and conservation strategies for Ghodaghodi Lake Complex (GLC).</p>
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13 pages, 3260 KiB  
Article
Reconstruction of Surface Water Temperature in Lakes as a Source for Long-Term Analysis of Its Changes
by Mariusz Sojka and Mariusz Ptak
Water 2024, 16(23), 3347; https://doi.org/10.3390/w16233347 - 21 Nov 2024
Viewed by 293
Abstract
One of the key parameters of lakes is water temperature, which influences many physical and biochemical processes. In Poland, in situ temperature measurements are or have been conducted in only about 30 lakes, whereas there are over 3000 lakes with an area larger [...] Read more.
One of the key parameters of lakes is water temperature, which influences many physical and biochemical processes. In Poland, in situ temperature measurements are or have been conducted in only about 30 lakes, whereas there are over 3000 lakes with an area larger than 10 hectares. In many cases, the length of existing observation series is not always sufficient for long-term analysis. Using artificial neural networks of the multilayer perceptron network (MLP) type, the reconstruction of average monthly water temperatures was carried out for nine lakes located in northern Poland. During the validation stage of the reconstruction results, BIAS values were obtained in the range of −0.33 to 0.44 °C, the mean absolute error was 0.46 °C, and the root mean square error was 0.61 °C. The high quality of the reconstructed data allowed for an assessment of water temperature changes in the analyzed lakes from 1993 to 2022 using the Mann–Kendall and Sen tests. It was found that, on an annual basis, the water temperature increased by an average of 0.50 °C per decade, ranging from 0.36 °C per decade to 0.64 °C per decade for individual lakes. For specific months, the largest increase was observed in November, about 0.99 °C per decade, and the smallest in May, 0.07 °C per decade. The obtained results confirm previous studies in this field while adding new data from lakes, which are particularly significant for the western part of Poland—a region with a previously limited number of monitored lakes. According to the findings, the analyzed lakes have undergone significant warming over the past three decades, which is important information for water management authorities. Full article
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<p>Location of study sites.</p>
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<p>Validation results of MLP-type neural networks presented in a Taylor diagram.</p>
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<p>Variability of mean annual water temperatures in lakes in the period 1993–2022.</p>
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<p>Variability of average monthly water temperatures in Lakes Morzycko and Rospouda Filipowska.</p>
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<p>Changes in average monthly water temperatures in lakes: (<b>a</b>) significance of changes; and (<b>b</b>) value of changes.</p>
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<p>Average change of water temperature regime in Lakes Komorze, Morzycko, Sławianowskie, and Ostrowite.</p>
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15 pages, 12303 KiB  
Essay
Characteristics and Genesis of Collophane in Organic-Rich Shale of Chang 7 Member in Ordos Basin, North China
by Yu Zhang, Chaocheng Dai, Congsheng Bian, Bin Bai and Xingfu Jiang
Minerals 2024, 14(12), 1184; https://doi.org/10.3390/min14121184 - 21 Nov 2024
Viewed by 244
Abstract
(1) Background: The Ordos Basin is one of the sedimentary basins in China that is richest in oil and gas resources. The Chang 7 member of the Yanchang Formation is a set of organic-rich shale, abundant in collophane. (2) Methods: The observation and [...] Read more.
(1) Background: The Ordos Basin is one of the sedimentary basins in China that is richest in oil and gas resources. The Chang 7 member of the Yanchang Formation is a set of organic-rich shale, abundant in collophane. (2) Methods: The observation and analysis of rock thin sections, combined with major elements, trace elements, electron probes, and other technical means, the characteristics and genesis mechanism of collophane in the organic-rich shale of the Chang 7 member of the Yanchang Formation in the Ordos Basin were studied. (3) Results: Collophane are divided into oolitic collophane, red-yellow aggregate collophane, and apatite-containing crystalline collophane; the main chemical compositions of the collophane were CaO, P2O5, FeO, Al2O3, and MgO. (4) Conclusions: Phosphorus elements of collophane in the organic-rich shale of the Chang 7 member of the Ordos continental lake basin are mainly derived from the nutrients carried by the volcanic ash sediments around the basin and the hydrothermal fluid at the bottom of the lake. The formation of collophane is divided into two periods: during the sedimentary period, the phosphorus released by the aerobic decomposition of phytoplankton to the mineralization and degradation of organic matter, and the death of phosphorus-rich organisms is preserved in the sediment by adsorption and complexation with iron oxides and then combined with calcium and fluoride plasma to form collophane; during the early diagenesis process, collophane underwent recrystallization, forming a colloidal, cryptocrystalline, and microcrystalline apatite assemblage. Full article
(This article belongs to the Section Mineral Geochemistry and Geochronology)
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<p>(<b>a</b>) Regional geological map of the Ordos Basin (modified from [<a href="#B22-minerals-14-01184" class="html-bibr">22</a>]); (<b>b</b>) Distribution map of sedimentary facies in the Chang 7 member of the Ordos Basin, modified from [<a href="#B23-minerals-14-01184" class="html-bibr">23</a>]; (<b>c</b>) Comprehensive strata log diagram of the Yanchang Formation in the Ordos Basin [<a href="#B24-minerals-14-01184" class="html-bibr">24</a>,<a href="#B25-minerals-14-01184" class="html-bibr">25</a>].</p>
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<p>(<b>a</b>–<b>c</b>) Oolitic collophane, brownish-brown, in individual strip form, distributed along bedding, with surface development of crack patterns, cryptocrystalline, surrounded by a fishbone-like shell, under plane-polarized light; (<b>d</b>–<b>f</b>) Red-yellow aggregate collophane, red-yellow mixed, and dark red collophane filled with large amounts of orange-yellow collophane, single polarized light; (<b>g</b>–<b>i</b>) Apatite crystal type collophane, in the edge or interior of cryptocrystalline collophane, forms lamellar and columnar apatite crystals under plane-polarized light.</p>
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<p>Relationship diagram of the oxide content of major elements in the organic-rich shale of the Chang 7 member, Ordos Basin, with respect to Al<sub>2</sub>O<sub>3</sub> content.</p>
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<p>Relationship diagram of TFe<sub>2</sub>O<sub>3</sub> and P<sub>2</sub>O<sub>5</sub> content with U content in organic-rich shale of Chang 7 member, Ordos Basin.</p>
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<p>(<b>a</b>) Comparison of major element contents in different lithofacies of the study area with PAAS major element contents; (<b>b</b>) Trace element PAAS normalization diagram for different lithofacies of the Chang 7 member in the Ordos Basin.</p>
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<p>Evolution map of major and trace elements in the organic-rich shale of the Chang 7 member of the Ordos Basin (Well Z40).</p>
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<p>(<b>a</b>) Depositional pattern of organic-rich shale in the Chang 7 member of the Yanchang Formation in the southern Ordos Basin (modified from [<a href="#B53-minerals-14-01184" class="html-bibr">53</a>]); (<b>b</b>) Formation of collophane.</p>
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15 pages, 3033 KiB  
Article
Congruent and Hierarchical Intra-Lake Subdivisions from Nuclear and Mitochondrial Data of a Lake Baikal Shoreline Amphipod
by Risto Väinölä, Tytti Kontula, Kazuo Mashiko and Ravil M. Kamaltynov
Diversity 2024, 16(11), 706; https://doi.org/10.3390/d16110706 - 20 Nov 2024
Viewed by 238
Abstract
A central goal of molecular studies on ancient lake faunas is to resolve the origin and phylogeny of their strikingly diverse endemic species flocks. Another equally intriguing goal is to understand the integrity of individual morphologically diagnosed species, which should help to perceive [...] Read more.
A central goal of molecular studies on ancient lake faunas is to resolve the origin and phylogeny of their strikingly diverse endemic species flocks. Another equally intriguing goal is to understand the integrity of individual morphologically diagnosed species, which should help to perceive the nature and speed of the speciation process, and the true biological species diversity. In the uniquely diverse Lake Baikal amphipod crustaceans, molecular data from shallow-water species have often disclosed their cryptic subdivision into geographically segregated genetic lineages, but the evidence so far is mainly based on mitochondrial DNA. We now present a lake-wide parallel survey of both mitochondrial and multilocus nuclear genetic structuring in the common shoreline amphipod Eulimnogammarus verrucosus, known to comprise three deep, parapatric mtDNA lineages. Allele frequencies of seven nuclear allozyme loci divide the data into three main groups whose distributions exactly match the distributions of the main mitochondrial lineages S, W, and E and involve a further division of the W cluster into two subgroups. The inter-group differences involve one to four diagnostic loci and additional group-specific alleles. The transition zones are either abrupt (1 km), occur over a long segment of uninhabitable shoreline, or may be gradual with non-coincident clinal change at different loci. Mitochondrial variation is hierarchically structured, each main lineage further subdivided into 2–4 parapatric sublineages or phylogroups, and patterns of further local segregation are seen in some of them. Despite the recurring observations of cryptic diversity in Baikalian amphipods, the geographical subdivisions and clade depths do not match in different taxa, defying a common explanation for the diversification in environmental history. Full article
(This article belongs to the Special Issue Diversity and Evolution within the Amphipoda)
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<p>Index map of sampling localities. Black dots are sites for the allozyme + mtDNA data. Plain numbers represent 1993–1995 samples, with site codes from Mashiko et al. [<a href="#B14-diversity-16-00706" class="html-bibr">14</a>]; codes with a letter are adjacent sites from the same expeditions. Numbers with an asterisk are sites from 1999. Open circles are sites with mtDNA data only. A full list of the localities with sample information is presented in <a href="#app1-diversity-16-00706" class="html-app">Table S1</a>. Open squares are additional sites of Gurkov et al.’s mtDNA data [<a href="#B19-diversity-16-00706" class="html-bibr">19</a>]. The photographs display <span class="html-italic">E. verrucosus</span> E from the Chivyrkui Bay, near site 22.</p>
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<p>Principal components plot (PC1 vs. PC2) of the <span class="html-italic">Eulimnogammarus verrucosus</span> complex allozyme frequency data. Locality codes are those in <a href="#diversity-16-00706-f001" class="html-fig">Figure 1</a> and <a href="#app1-diversity-16-00706" class="html-app">Table S1</a>.</p>
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<p>NJ trees (<b>A</b>) from uncorrected <span class="html-italic">p</span>-distances from the original <span class="html-italic">Eulimnogammarus verrucosus</span> COI sequence data in this study, (<b>B</b>) from allozyme data (7-locus Euclidean distances among populations, data as in <a href="#diversity-16-00706-f002" class="html-fig">Figure 2</a>). (<b>C</b>) Distribution of the three main genetic groups S, W, and E and the subgroups of W along the shores of Baikal, congruently in the two datasets. The grey reference sequence is of <span class="html-italic">E. oligacanthus</span>.</p>
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<p>Frequencies of major alleles at each allozyme locus plotted against geographical distance along the shoreline around Baikal, clockwise from site 1 in <a href="#diversity-16-00706-f001" class="html-fig">Figure 1</a>. Samples 28, 19*, and 27 from the Olkhon and Ogoi islands in the W(a)/W(b) borderline are encircled, those from the continental strand are interconnected by the lines. Original data are given in <a href="#app1-diversity-16-00706" class="html-app">Table S2</a>.</p>
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<p>Examples of allele frequency variation at three nuclear allozyme loci. The two most common alleles and the pooled frequency of remaining minor alleles at each locus are shown in the pie diagrams; data from <a href="#app1-diversity-16-00706" class="html-app">Table S2</a>.</p>
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<p><span class="html-italic">COI</span> haplotype trees for each of the three main mitochondrial lineages of <span class="html-italic">Eulimnogammarus verrucosus</span>, color-coded for geographically demarcated sublineages or phylogroups. The topologies are examples from larger sets of equally parsimonious MP trees, and detailed local relationships are not significant. Haplogroups with restricted distribution within a phylogroup range are surrounded by a dashed line, reciprocally in the tree and on the map. Individuals clustering in a clade typical of another region are marked with the color of their own region. Apart from original sequences, the trees include data from Gurkov et al. [<a href="#B19-diversity-16-00706" class="html-bibr">19</a>] and Saranchina et al. [<a href="#B20-diversity-16-00706" class="html-bibr">20</a>] from sites indicated by open squares.</p>
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24 pages, 6742 KiB  
Article
SNP Polymorphisms Are Associated with Environmental Factors in Sockeye Salmon Populations Across the Northwest Pacific: Insights from Redundancy Analysis
by Anastasia M. Khrustaleva
Genes 2024, 15(11), 1485; https://doi.org/10.3390/genes15111485 - 19 Nov 2024
Viewed by 401
Abstract
The SNP variation in sockeye salmon across the Asian part of its range was studied in 23 samples from 16 lake–river systems of the West Pacific Coast to improve understanding of genetic adaptation in response to spawning watersheds conditions. Identification of candidate SNPs [...] Read more.
The SNP variation in sockeye salmon across the Asian part of its range was studied in 23 samples from 16 lake–river systems of the West Pacific Coast to improve understanding of genetic adaptation in response to spawning watersheds conditions. Identification of candidate SNPs and environmental factors that can contribute to local adaptations in sockeye salmon populations was carried out using redundancy analysis (RDA), a powerful tool for landscape genetics proven to be effective in genotype–environment association studies. Climatic and hydrographic indices (7 indices in total), reflecting abiotic conditions in freshwater habitats of sockeye salmon and characterizing the temperature regime in the river basin, its variability during the year, the amount of precipitation, as well as the height of the maximum tide in the estuary, were used as predictor factors. Among the 45 analyzed SNPs, several loci (ALDOB-135, HGFA, and RAG3-93) correlated with predictors gradients along the northwest Pacific coast were identified. The putative candidate loci localized in genes involved in the immune and inflammatory responses, as well as genes encoding temperature-sensitive enzymes and some hormones regulating ion homeostasis in fish during the anadromous migration and smoltification, were potentially associated with environmental conditions in natal rivers. The findings could have implications for aquaculture, conservation, and resource management in the context of global climate change. Full article
(This article belongs to the Special Issue Genetic Studies of Fish)
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<p>Map of the study area with sampling points (triangles). (<b>A</b>) schematic map of Kamchatka River watershed, (<b>B</b>) schematic map of Bolshaya River watershed The point’s annotations are given in <a href="#genes-15-01485-t001" class="html-table">Table 1</a>. The regions listed in <a href="#genes-15-01485-t001" class="html-table">Table 1</a> are shown in different colors.</p>
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<p>Flowchart of redundancy analysis steps: partial RDA, RDA with forward stepwise selection, simple RDA, and variables used in each step.</p>
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<p>PCA results showing population clustering based on (<b>A</b>) allele frequencies of 26 putative neutral SNPs (regions are marked with different colors; some populations are combined into polygons according to the region, and some are outliers), (<b>B</b>) allele frequencies of 41 polymorphic SNPs (populations are scaled chromatically by the average temperature, °C, and in size by the type of estuary/the high of tides). Matrices of correlation coefficients between allele frequencies of 41 SNPs and (<b>C</b>) the latitude of the river mouth along the all-Asian coast of the North Pacific, the East Cost (Chukotka and East Kamchatka), and the West Coast (Continental coast of the Sea of Okhotsk and West Kamchatka); (<b>D</b>) climatic and hydrographic indices reflecting abiotic conditions in the reproductive watershed.</p>
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<p>(<b>A</b>,<b>B</b>) PCA results of climate and hydrographic indices in sockeye salmon reproduction watersheds of the Asian Pacific coast. Three main components characterizing the climate in general (PC1), the degree of climate continentality (PC2), and the type of estuary (PC3) were defined. (<b>C</b>) Loading matrix for each ecological variable to PC1–PC3.</p>
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<p>(<b>A</b>) RDA triplot displaying predictor factors (3 principal components obtained by PCA analysis of climate and hydrographic indices (PC1–PC3)) (vectors), samples (named points) and dependent variables (SNP loci), and (<b>B</b>) biplot for genetic traits (loci correlated with the corresponding predictors are marked in corresponding color).</p>
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24 pages, 1655 KiB  
Article
The Spatial–Temporal Evolution and Impact Mechanism of Cultivated Land Use in the Mountainous Areas of Southwest Hubei Province, China
by Zhengxiang Wu, Qingbin Fan, Wen Li and Yong Zhou
Land 2024, 13(11), 1946; https://doi.org/10.3390/land13111946 - 18 Nov 2024
Viewed by 330
Abstract
Changes in cultivated land use significantly impact food production capacity, which in turn affects food security. Therefore, accurately understanding the spatial and temporal variations in cultivated land use is critical for strategic decision-making regarding national food security. Since the second national soil survey [...] Read more.
Changes in cultivated land use significantly impact food production capacity, which in turn affects food security. Therefore, accurately understanding the spatial and temporal variations in cultivated land use is critical for strategic decision-making regarding national food security. Since the second national soil survey was conducted in around 1980, China has implemented major efforts, such as a nationwide soil testing and fertilization project in around 2005 and the establishment of the National Standards for Cultivated Land Quality Grading in 2016. However, limited research has focused on how cultivated land use has changed during these periods and the mechanisms driving these changes. This study, using Enshi Prefecture in the mountainous region of southwestern Hubei Province as a case study, examines the spatiotemporal changes in cultivated land use during 1980–2018. Land use data from 1980, 2005, and 2018 were combined with statistical yearbook data from Enshi Prefecture, and remote sensing and GIS technology were applied. Indicators such as the dynamic degree of cultivated land use, the relative rate of change in cultivated land use, and a Geoscience Information Atlas model were used to explore these changes. Additionally, principal component analysis was employed to examine the mechanisms influencing these changes. The results show that (1) the area of cultivated land in Enshi Prefecture increased slightly from 1980 to 2005, while from 2005 to 2018, it significantly decreased; compared with the earlier period, the transformation of land use types during 2005–2018 was more intense; (2) the increase in cultivated land area from 1980 to 2005 was mainly due to deforestation, the creation of farmland from lakes, and the reclamation of wasteland, while the decrease in land area was primarily attributed to the conversion of farmland back to forests and grassland. From 2005 to 2018, the main drivers for the increase in cultivated land were deforestation and the reclamation of wasteland, while the return of farmland to forests remained the primary reason for the decrease in land area; (3) from 1980 to 2005, the dynamic degree of cultivated land use in each county and city of Enshi Prefecture was generally low. However, between 2005 and 2018, the dynamic degree increased in most counties and cities except Enshi City and Xianfeng County; (4) there were significant variations in the relative rate of change in cultivated land utilization across counties and cities from 1980 to 2005. However, from 2005 to 2018, the relative rate of change decreased in all counties and cities compared to the previous period; (5) since 1980, nearly 50% of the cultivated land in Enshi Prefecture has undergone land classification conversion, with frequent shifts between different land classes; and (6) economic development, population growth, capital investment, food production, and production efficiency are the dominant socioeconomic factors driving changes in cultivated land use in Enshi Prefecture. The results of this study can provide a scientific basis for the protection and optimization of cultivated land resources in the mountainous regions of southwestern Hubei Province. Full article
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<p>Study area location and elevation distribution.</p>
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<p>Atlas of cultivated land use change patterns in Enshi Prefecture from 1980 to 2018.</p>
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<p>Changes in Population and Cultivated Land in Enshi Prefecture from 1980 to 2018.</p>
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<p>Economic Development and Changes in Enshi Prefecture from 1980 to 2018.</p>
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<p>Changes in the total output value of agriculture, forestry, animal husbandry, and fishery in Enshi Prefecture and the income of farmers and residents from 1980 to 2018.</p>
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21 pages, 902 KiB  
Article
Sustainable Solutions to Safety Risks on Frozen Lakes Through Effective Risk Mitigation Using Crisis Management Logistics
by Oľga Glova Végsöová and Katarína Čerevková
Sustainability 2024, 16(22), 10020; https://doi.org/10.3390/su162210020 - 17 Nov 2024
Viewed by 463
Abstract
This article addresses the critical safety risks posed by the use of frozen lakes, risks which are increasingly exacerbated by the impacts of climate change. In Slovakia, where numerous water reservoirs are legally designated for year-round recreational and sporting activities, safeguarding public health [...] Read more.
This article addresses the critical safety risks posed by the use of frozen lakes, risks which are increasingly exacerbated by the impacts of climate change. In Slovakia, where numerous water reservoirs are legally designated for year-round recreational and sporting activities, safeguarding public health and safety necessitates innovative and sustainable approaches to risk mitigation in emergency management. Using the Jazero water reservoir as a case study, this paper demonstrates that the integration of comprehensive risk assessment, the strategic selection of rescue methods, and the deployment of advanced technical equipment for rescue teams are fundamental to ensuring a robust and efficient crisis management response. Through a comparative analysis of nine access routes, validated by tactical exercises and a detailed evaluation of three distinct rescue methods combined with different equipment types, this study reveals the critical role of optimized rescue strategies in reducing response times. Rescue operations were accelerated by at least 4.5 s, a significant reduction that could be the deciding factor between life and death in real-world scenarios. The proposed sustainable strategies for the Jazero reservoir are applicable to similar natural water bodies, underscoring the vital importance of proactive, data-driven, and adaptive crisis management systems in enhancing both immediate and long-term public safety. Full article
(This article belongs to the Special Issue Sustainable Risk Management)
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<p>The process of a lake freezing.</p>
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<p>Effective resolution of a crisis situation on a frozen lake.</p>
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<p>Adjusted satellite image of the Jazero reservoir showing the possibility of access roads and parking possibilities for emergency vehicles.</p>
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<p>Adjusted satellite image of the Jazero reservoir showing available and fast routes for emergency vehicles.</p>
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20 pages, 4822 KiB  
Article
Assessment of the Impact of Meteorological Variables on Lake Water Temperature Using the SHapley Additive exPlanations Method
by Teerachai Amnuaylojaroen, Mariusz Ptak and Mariusz Sojka
Water 2024, 16(22), 3296; https://doi.org/10.3390/w16223296 - 17 Nov 2024
Viewed by 426
Abstract
The water temperature of lakes is one of their fundamental characteristics, upon which numerous processes in lake ecosystems depend. Therefore, it is crucial to have detailed knowledge about its changes and the factors driving those changes. In this article, a neural network model [...] Read more.
The water temperature of lakes is one of their fundamental characteristics, upon which numerous processes in lake ecosystems depend. Therefore, it is crucial to have detailed knowledge about its changes and the factors driving those changes. In this article, a neural network model was developed to examine the impact of meteorological variables on lake water temperature by integrating daily meteorological data with data on interday variations. Neural networks were selected for their ability to model complex, non-linear relationships between variables, often found in environmental data. Among various architectures, the Artificial Neural Network (ANN) was chosen due to its superior performance, achieving an R2 of 0.999, MSE of 0.0352, and MAE of 0.1511 in validation tests. These results significantly outperformed other models such as Multi-Layer Perceptrons (MLPs), Recurrent Neural Networks (RNNs), and Long Short-Term Memory (LSTM). Two lakes (Lake Mikołajskie and Sławskie) differing in morphometric parameters and located in different physico-geographical regions of Poland were analyzed. Performance metrics for both lakes show that the model is capable of providing accurate water temperature forecasts, effectively capturing the primary patterns in the data, and generalizing well to new datasets. Key variables in both cases turned out to be air temperature, while the response to wind and cloud cover exhibited diverse characteristics, which is a result of the morphometric features and locations of the measurement sites. Full article
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<p>Location of study objects: Sławskie Lake (<b>A</b>); Mikołajskie Lake (<b>B</b>); blue color-lakes, red color—hydrological station; green color—meteorological station.</p>
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<p>Workflow of this study.</p>
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<p>Learning rate on (<b>a</b>) MSE, (<b>b</b>) MAE, and (<b>c</b>) R<sup>2</sup> of sensitivity analysis.</p>
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<p>Yearly average observed and predicted water temperature from neural network (<b>a</b>); scatter plot of observed and predicted water temperature from neural network model for validation set (<b>b</b>) and test set (<b>c</b>) at Mikołajskie Lake.</p>
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<p>Yearly average observed and predicted water temperature from neural network (<b>a</b>); scatter plot of observed and predicted water temperature from neural network model for validation set (<b>b</b>) and test set (<b>c</b>) at Sławskie Lake.</p>
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<p>Model loss for training and validation data at Mikołajskie (<b>a</b>) and Sławskie (<b>b</b>).</p>
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<p>Feature importance based on SHAP values at Mikołajskie Lake (<b>a</b>), and Sławskie Lake (<b>b</b>). Mean Air Temperature: the average air temperature for the day; Maximum Air Temperature: the highest air temperature recorded during the day; Minimum Air Temperature: the lowest air temperature recorded during the day; Daily Air Temperature Amplitude: the difference between the maximum and minimum air temperatures for the day; Average Wind Speed: the average wind speed recorded over the day; Total Daily Rainfall: the total amount of rainfall recorded for the day; Average Daily Cloud Cover: the average cloud cover observed in octants (scale from 0 to 8); Interday Air Temperature Change: the change in air temperature between consecutive days; Interday Wind Speed Change: the change in average wind speed between consecutive days; Interday Rainfall Change: the change in total daily rainfall between consecutive days; Interday Cloud Cover Change: the change in average cloud cover between consecutive days.</p>
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15 pages, 5817 KiB  
Article
Efficacy of Feed Additives on Immune Modulation and Disease Resistance in Tilapia in Coinfection Model with Tilapia Lake Virus and Aeromonas hydrophila
by Aslah Mohamad, Jidapa Yamkasem, Suwimon Paimeeka, Matepiya Khemthong, Tuchakorn Lertwanakarn, Piyathip Setthawong, Waldo G. Nuez-Ortin, Maria Mercè Isern Subich and Win Surachetpong
Biology 2024, 13(11), 938; https://doi.org/10.3390/biology13110938 - 16 Nov 2024
Viewed by 440
Abstract
Coinfections by multiple pathogens, including viruses and bacteria, have severely impacted tilapia aquaculture globally. This study evaluated the impacts of dietary supplementation on red hybrid tilapia (Oreochromis spp.) coinfected with Tilapia lake virus (TiLV) and Aeromonas hydrophila. Fish were divided into [...] Read more.
Coinfections by multiple pathogens, including viruses and bacteria, have severely impacted tilapia aquaculture globally. This study evaluated the impacts of dietary supplementation on red hybrid tilapia (Oreochromis spp.) coinfected with Tilapia lake virus (TiLV) and Aeromonas hydrophila. Fish were divided into three groups: a control group on a normal diet, and two experimental groups received diets supplemented with strategy A, an organic acid blend combined with a lyso-phospholipid-based digestive enhancer, and strategy B, an organic acid blend combined with natural immunostimulants and nutrients. Following exposure to both pathogens, the fish supplemented with strategies A and B showed lower cumulative mortality rates of 50.0% and 41.7%, respectively, compared to 76.3% in the control group. Notably, fish fed with strategy B-supplemented diet displayed a stronger immune response, with a lower expression of il-8, mx, and rsad2, and showed less pathological changes in the liver, spleen, and intestines, suggesting enhanced resistance to coinfection. In contrast, fish receiving strategy A did not exhibit significant changes in the immune-related gene expression or pathogen load, but demonstrate less pathological alterations, indicating intestinal protection. These findings highlight the potential of feed additives, particularly strategy B, to reduce the impact of virus-bacterial coinfections and improve outcomes in tilapia farming. Full article
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<p>Experimental design of the study. The fish were fed a control diet only or feed supplemented with additives using strategy A or B for 21 days. Groups 1 to 3 had four replicates and one tank dedicated as the control tank (sham) group. Fish were injected intraperitoneally with TiLV at 10<sup>5</sup> TCID<sub>50</sub>/mL on day 0 and <span class="html-italic">A. hydrophila</span> at 10<sup>8</sup> CFU/mL on day 3.</p>
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<p>Comparison of the cumulative mortality (%) of red hybrid tilapia coinfected with Tilapia lake virus (TiLV) and <span class="html-italic">Aeromonas hydrophila</span> from the control group and the groups that received feed additives with strategy A or B. The asterisks (*) indicate significant differences in cumulative mortality (<span class="html-italic">p</span> &lt; 0.05) compared to the control group.</p>
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<p>The external appearances and lesions of internal organs (1-liver; 2-spleen) of the fish in the control group and those that received feed additives with strategy A or B. During the challenge study (days 0 to 14), the infected fish showed haemorrhaging and congestion on the dorsal skin and fin base (indicated by red arrows) and exophthalmia (indicated by blue arrows). The common internal lesions had ascitic fluid, and a pale, yellow liver and an enlarged spleen (inset) were evident.</p>
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<p>The levels of Tilapia lake virus (TiLV) RNA in the (<b>A</b>) liver, (<b>B</b>) spleen, and (<b>C</b>) anterior kidney of the fish fed the control diet or the feed supplemented with additives using strategy A or B at 0, 3, 5, 7, and 14 days post-infection. The data from five fish are presented as the mean ± standard deviation. Different alphabets indicate statistical differences (<span class="html-italic">p</span> &lt; 0.05) between groups according to Tukey’s multiple comparison tests.</p>
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<p>Expression of the (<b>A</b>) <span class="html-italic">ifn-γ</span>, (<b>B</b>) <span class="html-italic">il-8</span>, (<b>C</b>) <span class="html-italic">mx</span>, and (<b>D</b>) <span class="html-italic">rsad2</span> genes from the anterior kidneys of the challenged fish that were fed the control and additive-supplemented diets, strategies A and B. The samples were collected at day 0 and 3, 5, 7 and 14 days post-infection following the Tilapia lake virus and bacterial challenge (<span class="html-italic">n</span> = 5). The relative fold expression of genes at each time point following infection was normalised to day 0 and is presented as the mean ± standard deviation. Significant differences (<span class="html-italic">p</span> &lt; 0.05) between groups from Tukey’s multiple comparison tests were denoted by different letters.</p>
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<p>Histopathological changes at 7 days post-infection in the liver, spleen, and intestines of red hybrid tilapia coinfected with Tilapia lake virus and <span class="html-italic">Aeromonas hydrophila</span>: comparison between the groups that received the control diet (<b>A</b>–<b>C</b>) or additive-supplemented feed (<b>D</b>–<b>I</b>) and the uninfected control group (<b>J</b>–<b>L</b>). Syncytial hepatocytes (black arrows), the presence of intracytoplasmic inclusion bodies in the liver (arrowheads, inset), the severe depletion of red blood cells, and the distinct proliferation of melanomacrophage centres in the spleen (blue arrows) are denoted.</p>
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17 pages, 5156 KiB  
Article
Identifying Alpine Lakes with Shoreline Features
by Zhimin Hu, Min Feng, Yijie Sui, Dezhao Yan, Kuo Zhang, Jinhao Xu, Rui Liu and Earina Sthapit
Water 2024, 16(22), 3287; https://doi.org/10.3390/w16223287 - 15 Nov 2024
Viewed by 360
Abstract
Alpine lakes located in high-altitude mountainous regions act as vital sentinels of environmental change. Remote-sensing-based identification of these lakes is crucial for understanding their response to climate variations and for assessing associated disaster risks. However, the complex terrain and weather conditions in these [...] Read more.
Alpine lakes located in high-altitude mountainous regions act as vital sentinels of environmental change. Remote-sensing-based identification of these lakes is crucial for understanding their response to climate variations and for assessing associated disaster risks. However, the complex terrain and weather conditions in these areas pose significant challenges to accurate detection. This paper proposes a method that leverages the high precision of deep learning for small lake and lake boundary extraction combined with deep learning to eliminate noise and errors in the identification results. Using Sentinel-2 data, we accurately identified and delineated alpine lakes in the eastern Himalayas. A total of 2123 lakes were detected, with an average lake area of 0.035 km². Notably, 76% of these lakes had areas smaller than 0.01 km². The slope data is crucial for the lake classification model in eliminating shadow noise. The accuracy of the proposed lake classification model reached 97.7%. In the identification of small alpine lakes, the recognition rate of this method was 96.4%, significantly surpassing that of traditional deep learning approaches. Additionally, this method effectively eliminated most shadow noise present in water body detection results obtained through machine learning techniques. Full article
(This article belongs to the Topic Advances in Hydrological Remote Sensing)
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<p>Geographic extent and elevation distribution of the study area.</p>
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<p>Sentinel-2 RGB true-color imagery and corresponding labels for classification.</p>
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<p>Flow diagram of the methods in the study.</p>
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<p>Training loss for different input data configurations. Input1 consists of Sentinel-2 RGB images; Input2 combines Sentinel-2 RGB images with slope data; Input3 includes Sentinel-2 RGB images with MNDWI; and Input4 integrates Sentinel-2 RGB images with both slope and MNDWI data.</p>
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<p>Distribution density map of alpine lakes in the study area.</p>
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<p>(<b>a</b>) Distribution of alpine lakes by size, (<b>b</b>) distribution of alpine lakes by elevation.</p>
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<p>Sentinel-2 RGB composite displaying alpine lakes; (<b>a</b>) shows RF method results;(<b>b</b>) shows results from the proposed method. Blue indicates alpine lakes and red represents noise.</p>
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<p>Sentinel-2 RGB composite displaying alpine lakes, with columns labeled as follows: (<b>a</b>) for the manual interpretation results, (<b>b</b>) for the ConvNeXt model segmentation results, and (<b>c</b>) for the results obtained from the proposed method.</p>
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<p>The area comparison between the dataset from this method and the manually interpreted water body dataset. (<b>a</b>–<b>c</b>) Comparison of classification results with manual interpretation for small, medium, and large alpine lakes. (<b>d</b>–<b>f</b>) Comparison of segmentation results with manual interpretation for small, medium, and large alpine lakes.</p>
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19 pages, 4174 KiB  
Article
Novel Method for Evaluating Wetland Ecological Environment Quality Based on Coupled Remote Sensing Ecological Index and Landscape Pattern Indices: Case Study of Dianchi Lake Wetlands, China
by Yilu Zhao, Aidi Huo, Zhixin Zhao, Qi Liu, Xuantao Zhao, Yuanjia Huang and Jialu An
Sustainability 2024, 16(22), 9979; https://doi.org/10.3390/su16229979 - 15 Nov 2024
Viewed by 335
Abstract
Wetlands serve as crucial ecological buffers, significantly influencing temperature reduction, carbon storage, regional climate regulation, and urban wastewater treatment. To elucidate the relationship between wetland landscape patterns and ecological environment, and to accurately assess lake ecosystems, this study proposes a semi-supervised classification method [...] Read more.
Wetlands serve as crucial ecological buffers, significantly influencing temperature reduction, carbon storage, regional climate regulation, and urban wastewater treatment. To elucidate the relationship between wetland landscape patterns and ecological environment, and to accurately assess lake ecosystems, this study proposes a semi-supervised classification method based on RSEI and K-Means. By integrating landscape pattern indices, the Remote Sensing Ecological Index (RSEI), and disturbance proximity, a comprehensive evaluation of the ecological quality of the Dianchi wetlands was conducted. The results indicate that the RSEI-K-Means method, with K set to 50, achieved overall accuracies (OAs) and Kappa values of 0.91 and 0.88, surpassing the SVM’s 0.85 and 0.80. This method effectively combines ecological and landscape indices without relying on extensive training samples, enhancing accuracy and speed in wetland information extraction and addressing the challenges of spatial heterogeneity. This study reveals that from 2007 to 2009, and 2013 to 2015, landscape patterns were significantly influenced by the rapid expansion of Kunming city, exacerbating wetland fragmentation. Notably, significant ecological quality changes were observed in 2009 and 2013, with gradual recovery post-2013 due to strengthened environmental protection policies. The RSEI disturbance proximity analysis indicated that the affected areas were primarily concentrated in regions of high human activity, confirming the method’s high sensitivity and effectiveness. This study can help in wetland ecosystem research and management. Full article
(This article belongs to the Special Issue Geoenvironmental Engineering and Water Pollution Control)
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<p>Geographical location map of this study.</p>
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<p>Statistics of landscape classification area of the Dianchi lake wetland; (<b>a</b>–<b>k</b>) is the wetland landscape classification result from 2003 to 2023; (<b>l</b>) is the block boundaries in the study area.</p>
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<p>OA (<b>a</b>) and Kappa (<b>b</b>) data analysis table.</p>
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<p>Statistical map of landscape classification in Dianchi lake region.</p>
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<p>Fuxian Lake Wetland RSEI-K-Means Landscape Classification.</p>
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<p>Schematic diagram of the location of the Dianchi wetland park.</p>
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<p>Characteristic map of landscape pattern index of Dianchi wetland park.</p>
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<p>Characteristic map of landscape pattern index in Dianchi wetland section.</p>
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<p>Detection of RSEI changes in Dianchi Lake.</p>
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<p>Statistical and variational characteristics of RSEI area in Dianchi wetland segmentation.</p>
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<p>Three-dimensional scattered distribution of RSEI in Dianchi wetland.</p>
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<p>The importance of landscape pattern index to RSEI.</p>
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<p>Spatial distribution of disturbed areas around Dianchi wetland.</p>
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17 pages, 4759 KiB  
Article
The Influence of Waters of Lake Baikal on the Spatiotemporal Dynamics of Phytoplankton in the Irkutsk Reservoir
by Alena Firsova, Yuri Galachyants, Anna Bessudova, Diana Hilkhanova, Lubov Titova, Maria Nalimova, Vasilisa Buzevich, Artyom Marchenkov, Maria Sakirko and Yelena Likhoshway
Water 2024, 16(22), 3284; https://doi.org/10.3390/w16223284 - 15 Nov 2024
Viewed by 354
Abstract
On a model natural object, the Lake Baikal–Angara River–Irkutsk Reservoir (IR), we studied changes in the qualitative and quantitative characteristics of phytoplankton communities over three seasons in 2023 depending on seasonal changes in habitat parameters. Of the 151 identified taxa, Chrysophyta (57), Chlorophyta [...] Read more.
On a model natural object, the Lake Baikal–Angara River–Irkutsk Reservoir (IR), we studied changes in the qualitative and quantitative characteristics of phytoplankton communities over three seasons in 2023 depending on seasonal changes in habitat parameters. Of the 151 identified taxa, Chrysophyta (57), Chlorophyta (41) and Bacillariophyta (24) predominated in diversity. Over the entire observation period, the highest values of total biomass and total abundance were detected in the IR in June (hydrological spring) at a water temperature of 10.0–12.7 °C, and the lowest in August, despite the fact that the water warmed up to 20 °C. No mass blooms of Cyanobacteria were observed. Statistical analysis of species abundance profiles revealed that phytoplankton community structure varied across time and space. The direct effect of cold lake waters on the structure of phytoplankton in the reservoir was observed only in early June. In summer and autumn, the structures of phytoplankton in the lake and in the reservoir differed, even at the same water temperature. Low concentrations of phosphates and nitrates, high species diversity, the presence of cold-water species and species with a wide range of temperature preferences formed a dynamic spatiotemporal structure of IR phytoplankton, distinct from other temperate reservoirs, including Lake Baikal. The results obtained are important for understanding the mechanisms of formation of the flora of artificial reservoirs of temperate latitudes and for their monitoring, taking into account seasonal dynamics and the context of global climate warming. Full article
(This article belongs to the Special Issue Impact of Environmental Factors on Aquatic Ecosystem)
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<p>Map of sampling in 2023. Red dot—monthly sampling during the open water period at a station 3 km from Listvyanka Village (St. 9); black dots indicate sampling in October 2023 at stations that were sampled earlier in June [<a href="#B33-water-16-03284" class="html-bibr">33</a>] and August [<a href="#B35-water-16-03284" class="html-bibr">35</a>]. Bays of Irkutsk Reservoir: 11—Kurminsky; 13—Elovy; 16—Ershovsky.</p>
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<p>Quantitative and qualitative characteristics of phytoplankton at St. 9 near the source of the Angara River during the open water period in 2023: water temperature (<b>A</b>), total abundance and biomass of phytoplankton (<b>B</b>), relative share of large taxonomic groups (divisions) of microalgae (<b>C</b>), number of species in divisions (<b>D</b>), contribution of dominant species, the number of which exceeds 20 × 10<sup>3</sup> cells L<sup>−1</sup>, to the total abundance (<b>E</b>) and the total biomass (<b>F</b>) of phytoplankton, the absolute abundance of the dominant species (<b>G</b>).</p>
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<p>Seasonal dynamics of water temperature (<b>A</b>) and phytoplankton structure (<b>B</b>–<b>D</b>) in Southern Baikal and the Irkutsk Reservoir in 2023 during the period of open water: (<b>B</b>)—total abundance and biomass, (<b>C</b>)—number of species of different taxonomic groups, (<b>D</b>)—abundance of dominant species.</p>
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<p>Cluster analysis of species abundance community profiles using affinity propagation (<b>A</b>) and heatmap (<b>B</b>) of the species abundance profiles generated with a set of the 50 most abundant species. Color annotations below the cluster dendrogram and above the heatmap describe the spatial (<b>Type</b>) and temporal (<b>Month</b>) categories of communities. Color annotation on the left of heatmap denotes the species taxonomic affiliation at the “Class” level.</p>
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<p>Correlation of environmental parameters (<b>A</b>,<b>B</b>) and exploratory analysis of environmental parameters and species abundance data (<b>C</b>,<b>D</b>): (<b>A</b>) Correlation of environmental parameters and summary numerical variables by month of sampling. Numerical values are Pearson correlation coefficients with the color legend on the right. Strikeout cells are non-significant correlations (<span class="html-italic">p</span> &gt; 0.05). Profiles eJ9, Jl9 and S9 were not analyzed. (<b>B</b>) Correlation of environmental parameters and summary numerical variables of all community profiles sampled during 2023. (<b>C</b>) Unconstrained ordination of species abundance data using tbPCA. Shape of the point designates the month of sampling, and color denotes the sampling site type: Lake Baikal or Irkutsk Reservoir (<a href="#app1-water-16-03284" class="html-app">Table S1</a>). (<b>D</b>) Constrained ordination of species abundance profiles, excluding eJ9, Jl9 and S9, using tbRDA. Color and shape of the points as in <a href="#water-16-03284-f004" class="html-fig">Figure 4</a>B. Red and green isolines show the gradient of S and pH, respectively.</p>
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<p>Venn diagram. Species composition of phytoplankton in SB and IR during different seasons in 2023.</p>
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22 pages, 10503 KiB  
Article
Dynamics of Changes in the Surface Area of Water Bodies in Subsidence Basins in Mining Areas
by Martyna A. Rzetala, Robert Machowski, Maksymilian Solarski and Mariusz Rzetala
Water 2024, 16(22), 3280; https://doi.org/10.3390/w16223280 - 15 Nov 2024
Viewed by 453
Abstract
The Silesian Upland in southern Poland is known as a place where subsidence processes induced by mining activities occur in an area of nearly 1500 square kilometres, with many water bodies that formed in subsidence basins. This study concerned the dynamics of changes [...] Read more.
The Silesian Upland in southern Poland is known as a place where subsidence processes induced by mining activities occur in an area of nearly 1500 square kilometres, with many water bodies that formed in subsidence basins. This study concerned the dynamics of changes in the occurrence, boundaries and area of water bodies in subsidence basins (using orthoimagery from 1996 to 2023), as well as the assessment of the factors underlying the morphogenetic and hydrogenetic transformations of these basins. Within the subsidence basins covered by the study, water bodies occupied a total area that changed from 9.22 hectares in 1996 to 48.43 hectares in 2003, with a maximum of 52.30 hectares in 2009. The obtained figures testify to the extremely dynamic changes taking place in subsidence basins, which are unprecedented within such short time intervals in the case of other morphogenetic types of lakes and anthropogenic water bodies (for instance, from 1996 to 2003, the basin of the Brantka water body in Bytom underwent a more than two-fold change in its area, with RA values in the range of 54.4% to 131.9). A reflection of the dynamics of short-term changes in the water bodies in question in the period from 1996 to 2023 is the increase in the water area of the three studied water bodies, which was projected by linear regression to range from 0.09 hectares/year to 0.56 hectares/year. The area change trends, as determined by polynomial regression, suggest a slight decrease in the water table within the last few years, as well as within the next few years, for each of the studied basins. Full article
(This article belongs to the Section Hydrology)
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<p>Locations of studied water bodies in subsidence basins on the Silesian Upland: (<b>A</b>)—Poland; (<b>B</b>)—Silesian Upland; ➀—the Brandka water body in Bytom; ➁—the water body in the Szotkówka River valley in Połomia; ➂—the Bory water body in Sosnowiec.</p>
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<p>Conceptual models of water-body functioning in subsidence basins on the Silesian Upland: (<b>A</b>) The Brandka water body in Bytom; (<b>B</b>) the water body in the Szotkówka River valley in Połomia; (<b>C</b>) the Bory water body in Sosnowiec. 1—fluvial silts, sands and gravels (Holocene); 2—glaciofluvial sands and gravels (Pleistocene); 3—glacial sands, gravels and boulders (Pleistocene); 4—silty loam (Pleistocene); 5—silty loam on stratified sands and gravels (Pleistocene); 6—loess (Pleistocene); 7—clays, sandy clays, sands and sandstones (Neogene); 8—light-grey marly dolomites, Diplopora dolomites, ore-bearing dolomites, and banded and wavy-bedded limestones (Middle Triassic); 9—sandstones, coal, shales (Upper Carboniferous); 10—claystones, mudstones and coal (Upper Carboniferous); 11—sandstones, mudstones, conglomerates, claystones and coal (Upper Carboniferous); 12—anthropogenic forms (e.g., embankments and allochthonous sediments filling basins as a result of human activity); 13—water bodies; 14—land surface before the occurrence of continuous and discontinuous deformation processes; 15—groundwater table of the first aquifer; 16—groundwater present in lower aquifers (including those affected by mining drainage); 17—crack lines induced by mining activities; 18—former and modern mine workings; 19—trees and shrubs; 20—herbaceous vegetation; 21—rush vegetation (sedentation); 22—transportation routes; 23—various forms of evaporation; 24—precipitation; 25—surface runoff; 26—inflows (surface and underground, including debris supply); 27—outflows (surface and underground).</p>
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<p>Changes in the area of the Brandka water body from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Changes in the area of the water body in the subsidence basin in the Szotkówka River valley in Połomia from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Destroyed power-line pole within the water body in the Szotkówka River valley in Połomia in 2013 (photo: R. Machowski).</p>
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<p>Changes in the area of the Bory water body in Sosnowiec from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Flooded base of a high-voltage power-line mast and haul road within the Bory water body in Sosnowiec in 2013 (photo: R. Machowski).</p>
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<p>Trends in changes in the area of water bodies in subsidence basins on the Silesian Upland in 1996–2023 determined by linear and polynomial regression. (<b>A</b>) The Brandka water body in Bytom; (<b>B</b>) the water body in the Szotkówka River valley in Połomia; (<b>C</b>) the Bory water body in Sosnowiec.</p>
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12 pages, 4947 KiB  
Communication
Fault Kinematics of the 2022 Delingha Mw 5.6 and Mw 5.7 Earthquakes Revealed by InSAR Observations
by Xuening Wang, Donglin Wu, Lian Liu, Chenglong Li, Yongliang Bai and Xing Huang
Remote Sens. 2024, 16(22), 4237; https://doi.org/10.3390/rs16224237 - 14 Nov 2024
Viewed by 249
Abstract
Between January and April 2022, three moderate earthquakes (Mw 5.6 on 23 January, Mw 5.7 on 25 March, and Mw 5.1 on 15 April) struck the Hala Lake area of Delingha, Qinghai, China. Their seismogenic faults are poorly mapped, resulting in an unclear [...] Read more.
Between January and April 2022, three moderate earthquakes (Mw 5.6 on 23 January, Mw 5.7 on 25 March, and Mw 5.1 on 15 April) struck the Hala Lake area of Delingha, Qinghai, China. Their seismogenic faults are poorly mapped, resulting in an unclear understanding of their kinematics and regional seismotectonics. In this study, we employed Interferometric Synthetic Aperture Radar (InSAR) observations to reconstruct the coseismic deformation fields of the Mw 5.6 and 5.7 events. We then utilized a Bayesian inversion algorithm to delineate the fault geometries of the two events, and further resolved their coseismic fault slip. Our results reveal that these earthquakes ruptured different fault planes: the fault plane of the Mw 5.6 event dips westward at an angle of 60°, while the Mw 5.7 event ruptured as a nearly vertical fault with a dipping angle of 89°. The finite-fault slip inversions further demonstrate that the coseismic rupture of the Mw 5.6 event was predominantly concentrated between depths of 2 km and 7 km, with a maximum slip of 0.18 m; in contrast, the Mw 5.7 event was mainly concentrated between depths of 2 km and 9 km, with a maximum slip of 0.4 m. We calculated the coseismic Coulomb failure stress change (ΔCFS) induced by these two earthquakes. Integrating the analysis of ΔCFS and the spatial distribution of aftershocks, we argue that the sequence earthquakes were triggered by the proceeding earthquakes. Full article
(This article belongs to the Special Issue Synthetic Aperture Radar Interferometry Symposium 2024)
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<p>Seismogenic setting around the Delingha earthquake sequence. (<b>a</b>) The red triangle denotes the epicenters of the three main earthquakes. The blue rectangle indicates the location of Figure (<b>b</b>), and the gray-dotted rectangle represents the InSAR image convergences. DHNSF: Danghe Nanshan Fault; ELSF: Elashan Fault; QIL-HYF: Qilian–Haiyuan Fault; SN-QLF: Sunan–Qilian Fault; HLHF: Halahu Fault; HLHNSF: Halahu Nanshan Fault. (<b>b</b>) Red, green, and blue beach balls represent the three earthquakes, and the blue dots represent earthquakes with magnitude M3~M5 occurring nearby from 2010 to 2020 (USGS).</p>
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<p>Coseismic interferograms and deformation maps for the 2022 Mw 5.6 and Mw 5.7 earthquakes. Red and blue beach balls represent the Mw 5.6 earthquake on 23 January 2022, and the Mw 5.7 earthquake on 25 March 2022, respectively. (<b>a</b>,<b>c</b>) are the interference diagrams of the ascending and descending orbits for the Mw 5.6 earthquake. (<b>b</b>,<b>d</b>) are the deformation diagram of the ascending and descending orbits for the Mw 5.6 earthquake. (<b>e</b>,<b>g</b>) are the interference diagram of the ascending and descending orbits for the Mw 5.7 earthquake. (<b>f</b>,<b>h</b>) are the deformation diagram of the ascent and descent orbits for the Mw 5.7 earthquake.</p>
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<p>Fault geometric parameters for the Mw 5.6 and Mw 5.7 earthquakes. Strike and dip of fault planes for the Mw 5.6 and Mw 5.7 earthquakes. (<b>a</b>,<b>b</b>) are the strike and dip of fault planes, along with their marginal posterior probability distributions for the Mw 5.6 earthquake. (<b>c</b>,<b>d</b>) are the strike and dip of fault planes, along with their marginal posterior probability distributions for the Mw 5.7 earthquake.</p>
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<p>Trade-off curves for the Mw 5.6 and Mw 5.7 earthquakes. (<b>a</b>) Smoothing factor test for the Mw 5.6 earthquake; (<b>b</b>) smoothing factor test for the Mw 5.7 earthquake. The red dot is the preferred smoothing factor.</p>
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<p>Inversion of ascending and descending track data for the Mw 5.6 and Mw 5.7 earthquakes. The large, dashed rectangle represents the extent of the uniform-slip fault plane, with the solid line indicating the side of the fault closest to the surface. The smaller dashed rectangle shows the primary extent of the uniform-slip fault plane. (<b>a</b>–<b>c</b>) are the observed, modeled, and residual values for the ascending track of the Mw 5.6 earthquake. (<b>d</b>–<b>f</b>) are the observed, modeled, and residual values for the descending track of the Mw 5.6 earthquake. (<b>g</b>–<b>i</b>) are the observed, modeled, and residual values for the ascending track of the Mw 5.7 earthquake. (<b>j</b>–<b>l</b>) are the observed, modeled, and residual values for the descending track of the Mw 5.7 earthquake.</p>
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<p>Three−dimensional slip distribution of the Mw 5.6 and Mw 5.7 earthquakes from InSAR inversion. (<b>a</b>,<b>b</b>) show the InSAR inverted separate views of the three-dimensional slip distribution for the Mw 5.6 and Mw 5.7 earthquakes. (<b>c</b>) presents the InSAR inverted three-dimensional slip distribution for both the Mw 5.6 and Mw 5.7 earthquakes.</p>
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<p>Aftershocks and cross-fault profiles. (<b>a</b>,<b>b</b>) The distribution of relocated aftershocks for the Mw 5.6 and Mw 5.7 earthquakes. The dashed lines represent the cross-section locations. The red pentagram represents the Mw 5.6 earthquake; the blue pentagram represents the Mw 5.7 earthquake. (<b>c</b>–<b>e</b>) display the cross-sectional aftershock relocations for the Mw 5.6 earthquake. (<b>f</b>–<b>h</b>) show the relocations for the Mw 5.7 earthquake. The dashed lines indicate the dip angles determined by the Bayesian algorithm.</p>
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<p>Coseismic slip and aftershock distribution. (<b>a</b>) Slip on the fault for the Mw 5.6 earthquake. (<b>b</b>) Slip on the fault for the Mw 5.7 earthquake. Black arrows indicate the direction of the slip. (<b>a</b>) shows a blue pentagram representing the Mw 5.6 earthquake, with other blue circles indicating the distribution of its aftershocks; (<b>b</b>) shows a blue pentagram representing the Mw 5.7 earthquake, with other blue circles indicating the distribution of its aftershocks.</p>
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<p>Coulomb stress variation of Mw 5.6 and Mw 5.7 earthquakes. (<b>a</b>–<b>c</b>) represent Mw 5.6 earthquake stress variations at the depths of the three main earthquakes (4.8 km, 6.4 km, and 10.8 km), respectively. (<b>d</b>–<b>f</b>) represent Mw 5.7 earthquake stress variations at the depths of the three main earthquakes (4.8 km, 6.4 km, and 10.8 km), respectively. Red, green, and blue beach balls represent the three earthquakes.</p>
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19 pages, 4217 KiB  
Article
Midge Paleo-Communities (Diptera Chironomidae) as Indicators of Flood Regime Variations in a High-Mountain Lake (Italian Western Alps): Implications for Global Change
by Marco Bertoli, Gianguido Salvi, Rachele Morsanuto, Elena Pavoni, Paolo Pastorino, Giuseppe Esposito, Damià Barceló, Marino Prearo and Elisabetta Pizzul
Diversity 2024, 16(11), 693; https://doi.org/10.3390/d16110693 - 12 Nov 2024
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Abstract
Sediments of alpine lakes serve as crucial records that reveal the history of lacustrine basins, offering valuable insights into the effects of global changes. One significant effect is the variation in rainfall regimes, which can substantially influence nutrient loads and sedimentation rates in [...] Read more.
Sediments of alpine lakes serve as crucial records that reveal the history of lacustrine basins, offering valuable insights into the effects of global changes. One significant effect is the variation in rainfall regimes, which can substantially influence nutrient loads and sedimentation rates in lacustrine ecosystems, thereby playing a pivotal role in shaping biotic communities. In this study, we analyze subfossil chironomid assemblages within a sediment core from an alpine lake (western Italian Alps) to investigate the effects of rainfall and flood regime variations over the past 1200 years. Sediment characterization results highlight changes in sediment textures and C/N ratio values, indicating phases of major material influx from the surrounding landscape into the lake basin. These influxes are likely associated with intense flooding events linked to heavy rainfall periods over time. Flooding events are reflected in changes in chironomid assemblages, which in our samples are primarily related to variations in sediment texture and nutrient loads from the surrounding landscape. Increased abundances of certain taxa (i.e., Brillia, Chaetocladius, Cricotopus, Psectrocladius, Cricotopus/Orthocladius Parorthocladius) may be linked to higher organic matter and vegetation inputs from the surrounding landscape. Biodiversity decreased during certain periods along the core profile due to intense flood regimes and extreme events. These results contribute to our understanding of alpine lake system dynamics, particularly those associated with intense flooding events, which are still understudied. Full article
(This article belongs to the Section Biodiversity Loss & Dynamics)
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<p>(<b>a</b>) Study area and (<b>b</b>) location of the sampling site in Upper Balma Lake.</p>
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<p>Stratigraphic diagram of the sedimentological and geochemical parameters measured in core sections sampled in the Upper Balma Lake. Results of the element analysis in light blue color are also reported.</p>
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<p>Bayesian age-depth model calculated for the Upper Balma Lake, based on 4000 interactions Markov Chain Monte Carlo. The dark gray areas represent the more precise dates, those in light gray the less precise dates; the red line indicates the best estimate of age for each level, and the black dashed lines the 95% confidence intervals.</p>
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<p>Relative abundances of the chironomid taxa observed in the Upper Balma Lake core sections and trends of the main community indices calculated along the core. Time periods with high flood regimes are indicated by the light blue bands superimposed on the graphs; identification of these periods is based on Giguet-Covex et al. [<a href="#B8-diversity-16-00693" class="html-bibr">8</a>] and Wilhelm et al. [<a href="#B55-diversity-16-00693" class="html-bibr">55</a>]. Group colors highlighted by cluster analysis and used in the RDA are reported (see <a href="#diversity-16-00693-f005" class="html-fig">Figure 5</a> and <a href="#diversity-16-00693-f006" class="html-fig">Figure 6</a>a).</p>
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<p>Cluster analysis defining stratigraphic zones (groups of sections) along the core based on the chironomid assemblages in the Upper Balma Lake (<b>a</b>) and broken sticks analysis defining the proper number of groups (<b>b</b>) (<span class="html-italic">n</span> = 6). Obtained stratigraphic zones are indicated with the same colors used for RDA analysis (see <a href="#diversity-16-00693-f006" class="html-fig">Figure 6</a>a).</p>
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<p>(<b>a</b>) Redundancy Analyses (RDA) illustrate the associations between chironomid taxa and the variables under consideration and (<b>b</b>) Venn diagrams depict the results of variance partitioning analysis (VPA) for the four variable groups: nutrients (TOC and C/N ratio), trace elements (Pb, Mo), sediment characteristics (first percentile Cμ and median diameter Mμ), and the presence of fish in relation to chironomid taxa. Variance that is unexplained or accounts for less than 1% is omitted. The group colors used in the RDA analysis correspond to those in the cluster analysis (refer to <a href="#diversity-16-00693-f005" class="html-fig">Figure 5</a>).</p>
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