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30 pages, 8322 KiB  
Article
The Effects of Facies Variability and Bioturbation Intensity on Permeability in a Mixed Siliciclastic–Carbonate Core from the Upper Strawn Group, Katz Field, Eastern Shelf of the Permian Basin, Texas, USA
by Jerry L. Jensen, Peter P. Flaig and Kelly E. Hattori
Geosciences 2024, 14(12), 339; https://doi.org/10.3390/geosciences14120339 - 10 Dec 2024
Viewed by 432
Abstract
For oil and gas reservoir characterization, permeability prediction is indispensable because it helps identify potential flow pathways and lowers risk. Estimating permeability in heterogeneous media is challenging due to the limited number of measurement tools, low-resolution sampling methods, and sampling bias. To combat [...] Read more.
For oil and gas reservoir characterization, permeability prediction is indispensable because it helps identify potential flow pathways and lowers risk. Estimating permeability in heterogeneous media is challenging due to the limited number of measurement tools, low-resolution sampling methods, and sampling bias. To combat these issues, we employed a probe permeameter to produce a high-resolution (4 in [10 cm] spacing) permeability dataset for cores from the Strawn Formation, Katz Field, Permian Basin, Texas, USA. We structured our sampling to record permeability changes related to facies variability and fluctuating bioturbation intensity. We compared probe permeameter data to wireline logs and core-plug porosity and permeability data recorded at larger spacings. The results show that permeability is affected by facies type, bioturbation intensity, and cementation. The effects of bioturbation are non-linear; in our study, moderate bioturbation enhances permeability by improving connections between sands while intense bioturbation decreases permeability by redistributing fines. Core-plug and probe measurements gave similar permeability values, but the number of core plugs taken in the finer-grained intervals was insufficient. The probe, however, provided better resolution and gave larger net-to-gross sand ratios than core-plug-based evaluations. Using only the core-plug porosity–permeability relationship with wireline density log porosities led to permeability predictions too large by a factor of three or more compared to averaged probe permeameter values. Full article
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<p>(<b>A</b>) CoreLabs PPP-250<sup>TM</sup> probe permeameter with its main components identified. (<b>B</b>) Instrument mounted in motorized (for up–down motion and trigger actuation) fixture for measurements, with the modified tip positioned next to the probe tip.</p>
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<p>(<b>A</b>) Regional stratigraphic nomenclature for the Eastern Shelf of the Permian/Midland Basin and location map of local oil/gas fields including the location of the Phillips Petroleum CB-Long C-16 well in the Katz Field, Stonewall County, Texas; (<b>B</b>) normalized gamma ray log and interpolated shale volume gamma ray log from the Strawn Group interval that includes the two cores described in this manuscript. VSHGR is calculated from normalized gamma ray logs using a cutoff value of approximately 125+ API for shale. Core 1 (4825 to 4925 feet) includes the First Sand (4825–4855 feet) and the upper part of the Second Sand (4880–4990 feet), whereas Core 2 (5065 to 5157 feet) covers the upper part of the Third Sand (5065–? feet). “Sand” terminology is uniquely used by Kinder Morgan for the Katz Field.</p>
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<p>Stratigraphic column for the Philips C.B. Long C-16 cores including facies designations and characteristics, bioturbation index, and the six intervals chosen for detailed permeability evaluation.</p>
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<p>Examples of each facies delineated within the CB-Long C-16 core. Facies include (<b>A</b>) KM1: 4909–4910 ft, (<b>B</b>) KS1: 4825–4826 ft, (<b>C</b>) KS2: 4865–4866 ft, (D) KS3: 4899–4900 ft, (<b>E</b>) KS4: 5153–5154 ft., (<b>F</b>) KS5: 5088–5089 ft, and (<b>G</b>) KS6 4847–4848 ft: All core are standard 4 inches (10 cm) diameter core, with a cross-sectional slice that is 3 inches (7.5 cm) wide. Scale bars are one inch (2.5 cm) in both directions. See <a href="#geosciences-14-00339-t001" class="html-table">Table 1</a> for facies descriptions, characteristics, and paleoenvironmental interpretations.</p>
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<p>Thin section photomicrographs of facies) of the Katz Field. All photos captured in plane polarized light. (<b>A</b>,<b>B</b>) Facies KM1, high-angle planar-stratified calcareous crinoid-rich sandstone. Note poor sorting: large crinoid fragments are mixed with fine-grained quartz-rich sandstone and silt. Calcite cement between grains is stained in red. (<b>C</b>,<b>D</b>) Facies KS3, herringbone cross-stratified to current ripple cross-stratified fine-grained sandstone. (<b>C</b>) shows herringbone bedding; (<b>D</b>) highlights high interparticle porosity and permeability. (<b>E</b>) Facies KS5, weakly to moderately bioturbated fine-grained sandstone with relict mud draped current ripple to modified current ripple cross-stratification. Mud-filled burrow is prominent in the center of the image. (<b>F</b>) Facies KS6, highly bioturbated fine-grained sandstone. Fine-grained quartz sand exhibits significant disturbance with large vugs left behind in burrow voids. Images (<b>E</b>,<b>F</b>) highlight the potential of burrows to either hinder or enhance flow (permeability).</p>
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<p>Comparison between the first and second measurements made with the probe permeameter at each depth. Of 359 depths measured, 62 measurement pairs differed by more than a factor of two.</p>
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<p>Core-plug and median probe permeabilities for (<b>A</b>) Intervals 4–6 and (<b>B</b>) Intervals 1–3. Depths listed on x axis are core depths. Interval indicator line shows the location of each of the intervals.</p>
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<p>Comparison of plug and probe average permeabilities for each of the six intervals (labelled 1 through 6). Error bars indicate one standard error (i.e., approximately 68% probability). Standard error is defined as the estimated standard deviation of the arithmetic average.</p>
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<p>Box and whisker plots showing permeability statistics for each facies on (<b>A</b>) logarithmic and (<b>B</b>) linear scales. <a href="#geosciences-14-00339-f009" class="html-fig">Figure 9</a>B omits some larger outlier values. Colors are consistent with facies in <a href="#geosciences-14-00339-f003" class="html-fig">Figure 3</a>.</p>
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<p>Core-plug porosity (<span class="html-italic">ϕ</span>) vs. permeability (log<sub>10</sub> (<span class="html-italic">k</span>)) relationship with linear model (black line) fit using least squares linear regression. <span class="html-italic">R</span><sup>2</sup> is the coefficient of determination.</p>
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<p>Density porosity versus probe permeability for (<b>A</b>) Intervals 4–6 and (<b>B</b>) Intervals 1–3. Depths are wireline-log density depths. The high-porosity interval (4852–4870 ft.) is a borehole enlargement where the logging tool’s pad had poor contact with the formation.</p>
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<p>Interval 5 wireline density log porosity correlation with unaveraged probe permeability and core-plug values. Due to the fissile and poorly preserved nature of the core over the interval 4857 to 4880 feet, core-plug sampling was not performed in most of that interval. Depths listed are wireline depths.</p>
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<p>Density log porosity versus logarithm of one-foot averaged permeability categorized according to facies. The dashed line is the linear model shown in <a href="#geosciences-14-00339-f010" class="html-fig">Figure 10</a>.</p>
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<p>(<b>A</b>) Average plug and (<b>B</b>) probe permeabilities and their 68% probability standard errors (left axis) versus their bioturbation index values (x-axis). Average grain sizes for the same intervals appear in red triangles (right axis).</p>
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<p>Probe-based permeability anisotropy for (<b>A</b>) the upper three intervals and (<b>B</b>) the lower three intervals. <span class="html-italic">k</span><sub>V</sub>/<span class="html-italic">k</span><sub>H</sub> ≤ 1 because the arithmetic average always exceeds or equals the harmonic average [<a href="#B42-geosciences-14-00339" class="html-bibr">42</a>] pp. 37–38.</p>
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26 pages, 1044 KiB  
Article
PredXGBR: A Machine Learning Framework for Short-Term Electrical Load Prediction
by Rifat Zabin, Khandaker Foysal Haque and Ahmed Abdelgawad
Electronics 2024, 13(22), 4521; https://doi.org/10.3390/electronics13224521 - 18 Nov 2024
Viewed by 626
Abstract
The growing demand for consumer-end electrical load is driving the need for smarter management of power sector utilities. In today’s technologically advanced society, efficient energy usage is critical, leaving no room for waste. To prevent both electricity shortage and wastage, electrical load forecasting [...] Read more.
The growing demand for consumer-end electrical load is driving the need for smarter management of power sector utilities. In today’s technologically advanced society, efficient energy usage is critical, leaving no room for waste. To prevent both electricity shortage and wastage, electrical load forecasting becomes the most convenient way out. However, the conventional and probabilistic methods are less adaptive to the acute, micro, and unusual changes in the demand trend. With the recent development of artificial intelligence (AI), machine learning (ML) has become the most popular choice due to its higher accuracy based on time-, demand-, and trend-based feature extractions. Thus, we propose an Extreme Gradient Boosting (XGBoost) regression-based model—PredXGBR-1, which employs short-term lag features to predict hourly load demand. The novelty of PredXGBR-1 lies in its focus on short-term lag autocorrelations to enhance adaptability to micro-trends and demand fluctuations. Validation across five datasets, representing electrical load in the eastern and western USA over a 20-year period, shows that PredXGBR-1 outperforms a long-term feature-based XGBoost model, PredXGBR-2, and state-of-the-art recurrent neural network (RNN) and long short-term memory (LSTM) models. Specifically, PredXGBR-1 achieves an mean absolute percentage error (MAPE) between 0.98 and 1.2% and an R2 value of 0.99, significantly surpassing PredXGBR-2’s R2 of 0.61 and delivering up to 86.8% improvement in MAPE compared to LSTM models. These results confirm the superior performance of PredXGBR-1 in accurately forecasting short-term load demand. Full article
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<p>Main steps of ARIMA and SVM.</p>
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<p>Main steps of RNN and LSTM.</p>
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<p>Working principle of the proposed <tt>PredXGBR</tt>-1 model. The model iteratively refines its prediction by minimizing residuals using successive regression trees. Each new tree improves upon the predictions of its predecessor by learning from the residuals.</p>
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<p>The original data along with the <span class="html-italic">trend</span>, <span class="html-italic">periodic</span>, and <span class="html-italic">residual</span> patterns of electrical load consumption for the PJM and Dayton datasets.</p>
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<p>Heatmaps of different temporal features of PJM dataset.</p>
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<p>Heatmaps of different temporal features of Dayton dataset.</p>
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<p>Comparative analysis of the MAPE and <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math> value of the proposed approach: <tt>PredXGBR</tt>-1.</p>
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<p>Analysis of the generalization performance of <tt>PredXGBR</tt>-1 when compared with two of the best-performing models—SVM and TCN. Models are trained with one dataset and tested with others.</p>
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<p>Analysis of the generalization performance of <tt>PredXGBR</tt>-1 when compared with two of the best-performing models—SVM and TCN. Models are trained with one dataset and tested with others.</p>
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<p>Comparative analysis of the computational complexity (FLOPS) and inference time of <tt>PredXGBR</tt>-1 (Model1).</p>
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12 pages, 2200 KiB  
Article
Primary Care for Gestational Diabetes: A Bibliometric Analysis of Publications from 1991 to 2024
by Aliya Makasheva, Lyudmila Yermukhanova, Khatimya Kudabayeva, Saule Tazhbenova, Maral Nogayeva, Aidana Tautanova and Aliya Zhylkybekova
Int. J. Environ. Res. Public Health 2024, 21(11), 1405; https://doi.org/10.3390/ijerph21111405 - 24 Oct 2024
Viewed by 1013
Abstract
Gestational diabetes mellitus (GDM) represents a significant medical complication during pregnancy, with a global prevalence ranging from 2% to 26% and increasing by over 30% in recent decades. Therefore, the aim of our study is to assess the trends and distribution of published [...] Read more.
Gestational diabetes mellitus (GDM) represents a significant medical complication during pregnancy, with a global prevalence ranging from 2% to 26% and increasing by over 30% in recent decades. Therefore, the aim of our study is to assess the trends and distribution of published studies, as well as the contributions of countries, institutions, journals, and authors to the development of primary care for pregnant women with gestational diabetes. In this bibliometric analysis, we examine the role of primary health care in GDM from 1991 to 2024. The data were sourced from Scopus and Web of Science, encompassing 276 articles from 150 sources and involving 1375 authors. The analysis reveals a steady increase in publications, with a 4.29% annual growth rate. This study identifies the USA and UK as leading countries in GDM research, and there are significant international collaborations, with the USA having 17 joint articles with other countries. The University of Eastern Finland, Ohio State University, and Harvard University are noted as the most prolific institutions, with 23, 17, and 16 articles, respectively. Additionally, the journal Diabetes Care published the highest number of articles, totaling 635. Prominent authors such as Bernstein J. and McCloskey L., with seven articles each, have made substantial contributions to the field. Our work highlights the need to pay special attention to primary care for gestational diabetes, as many negative consequences of the disease can be prevented at this stage. Innovative approaches to screening for GDM can significantly improve treatment outcomes and reduce health risks, which will have long-term positive effects both for individual patients and society as a whole. Full article
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<p>Search strategy.</p>
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<p>Global annual trend of publications on primary care for pregnant women with GDM (1991–2024).</p>
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<p>The top 10 countries with the highest number of scientific publications (<b>A</b>) and a world collaboration map (<b>B</b>). The color saturation intensity indicates the number of articles produced by each country, with darker shades representing higher publication volumes. The thickness of the connecting arrows illustrates the strength of collaboration between countries.</p>
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<p>The plot of Bradford’s law identifies ten core journals on primary care for pregnant women with GDM (1991–2024).</p>
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<p>The top 10 most relevant authors (<b>A</b>) and their publication output (<b>B</b>) in 1991–2024.</p>
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<p>TreeMap (<b>A</b>) and scatter plot (<b>B</b>) representing top ten author keywords in research on primary care for pregnant women with GDM (1991–2024).</p>
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16 pages, 1397 KiB  
Article
Genetic Insights into the Giant Keyhole Limpet (Megathura crenulata), an Eastern Pacific Coastal Endemic: Complete Mitogenome, Phylogenetics, Phylogeography, and Historical Demography
by Brenda Bonett-Calzada, Fausto Valenzuela-Quiñonez, Miguel A. Del Río-Portilla, Natalia J. Bayona-Vásquez, Carmen E. Vargas-Peralta, John R. Hyde and Fabiola Lafarga-De la Cruz
Genes 2024, 15(10), 1303; https://doi.org/10.3390/genes15101303 - 8 Oct 2024
Viewed by 1165
Abstract
Background: The giant keyhole limpet Megathura crenulata is a gastropod mollusk (Fissurella superfamily) that is endemic to the eastern Pacific coast from southern California, USA, to Baja California Sur, Mexico. M. crenulata is socioeconomically important as it produces a potent immune-stimulating protein, called [...] Read more.
Background: The giant keyhole limpet Megathura crenulata is a gastropod mollusk (Fissurella superfamily) that is endemic to the eastern Pacific coast from southern California, USA, to Baja California Sur, Mexico. M. crenulata is socioeconomically important as it produces a potent immune-stimulating protein, called Keyhole Limpet Hemocyanin, which is extracted in vivo and utilized for vaccine development. However, ecological studies are scarce and genetic knowledge of the species needs to be improved. Our objectives were to assemble and annotate the mitogenome of M. crenulata, and to assess its phylogenetic relationships with other marine gastropods and to evaluate its population genetic diversity and structure. Methods: Samples were collected for mitogenome assembly (n = 3) spanning its geographic range, Puerto Canoas (PCA) and Punta Eugenia (PEU), Mexico, and California (CAL), USA. Total DNA was extracted from gills sequenced using Illumina paired-end 150-bp-read sequencing. Reads were cleaned, trimmed, assembled de novo, and annotated. In addition, 125 samples from eight locations were analyzed for genetic diversity and structure analysis at the 16s rRNA and COX1 genes. Results: The M. crenulata mitogenomes had lengths of 16,788 bp (PCA) and 16,787 bp (PEU) and were composed of 13 protein-coding regions, 22 tRNAs, two rRNAs, and the D-Loop region. In terms of phylogeographic diversity and structure, we found a panmictic population that has experienced recent demographic expansion with low nucleotide diversity (0.002), high haplotypic diversity (0.915), and low φST (0.047). Conclusions: Genetic insights into the giant keyhole limpet provides tools for its management and conservation by delimiting fishing regions with low genetic diversity and/or genetically discrete units. Full article
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<p>Map of the mitogenome of <span class="html-italic">M. crenulata</span> from the PCA sample. Arrows indicate the direction of transcription. Protein-coding genes (PCGs) are in purple, ribosomal RNA in red, transfer RNAs in yellow, D-Loop in dark purple, and the origin of replication in blue.</p>
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<p>Inferred Bayesian phylogenetic relationships among eight species of gastropods. (<b>A</b>) Complete mitogenome analysis. (<b>B</b>) Analysis with three mitochondrial genes <span class="html-italic">ATP8</span>, <span class="html-italic">ND6</span>, and <span class="html-italic">COX3</span>. Node support values are from Bayesian bootstrap proportions.</p>
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<p>Haplotype frequency and diversity of the <span class="html-italic">16S rRNA</span> and <span class="html-italic">COX1</span> genes in eight locations of <span class="html-italic">M. crenulata</span>. California (CAL), Ensenada (ENS), San Quintín (SQT), Isla San Jerónimo (SJO), Puerto Canoas (PCA), Punta Eugenia (PEU), Bahía Asunción (BAS), and Isla Guadalupe (IGP). The circular diagrams indicate the diversity of haplotypes, colors indicate individual haplotypes. <span class="html-italic">n</span>: sample size per locality.</p>
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<p>Historical demographic analyses based on <span class="html-italic">16S rRNA-COX1</span> concatenated haplotypes of the giant limpet <span class="html-italic">M. crenulata</span> along its geographical distribution. (<b>A</b>) Mismatch distribution. The bars represent the observed values, and the line represents the expected values under a constant population size model. (<b>B</b>) Bayesian skyline plot (BSP) approach. The <span class="html-italic">y</span>-axis is on a logarithmic scale. The <span class="html-italic">x</span>-axis indicates time (years) and starts at zero, corresponding to the present day. The solid blue line shows the median effective population size over time (<span class="html-italic">Ne</span>). The upper and bottom dashed lines represent the 95% confidence interval. The shaded grey area denotes the period during the last glacial maximum (LGM), and the vertical dashed line indicates the last interglacial (LIG) ending. A substitution rate of 0.0157 substitutions/site/million years, reported for marine invertebrates, was applied [<a href="#B40-genes-15-01303" class="html-bibr">40</a>].</p>
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<p>The minimum spanning network illustrates haplotypes from eight localities of <span class="html-italic">M. crenulata</span>. The circle sizes represent haplotype frequencies, while colors indicate the respective locality: California (CAL, red), Ensenada (ENS, pink), San Quintín (SQT, orange), Isla San Jerónimo (SJO, white), Puerto Canoas (PCA, blue), Punta Eugenia (PEU, green), Bahía Asunción (BAS, brown), and Isla Guadalupe (IGP, purple). Background circles in shaded color indicate haplogroups. Black circles represent mutational steps.</p>
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26 pages, 28717 KiB  
Article
Assessing Land-Cover Change Trends, Patterns, and Transitions in Coalfield Counties of Eastern Kentucky, USA
by Suraj K C, Buddhi R. Gyawali, Shawn Lucas, George F. Antonious, Anuj Chiluwal and Demetrio Zourarakis
Land 2024, 13(9), 1541; https://doi.org/10.3390/land13091541 - 23 Sep 2024
Viewed by 990
Abstract
Surface coal mining and reclamation have greatly reshaped eastern Kentucky’s landscape affecting its socioeconomic, environmental and climatic aspects. This study examined the land-cover changes, trends and patterns in Floyd, Knott, Letcher, Magoffin, Martin, Perry, and Pike counties from 2004 to 2019. Using a [...] Read more.
Surface coal mining and reclamation have greatly reshaped eastern Kentucky’s landscape affecting its socioeconomic, environmental and climatic aspects. This study examined the land-cover changes, trends and patterns in Floyd, Knott, Letcher, Magoffin, Martin, Perry, and Pike counties from 2004 to 2019. Using a random forest classifier, land cover was categorized into seven major classes, i.e., water, barren land, developed land, forest, shrubland, herbaceous, and planted/cultivated, majorly based on Landsat images. The Kappa accuracy ranged from 75 to 89%. The results showed a notable increase in forest area from 5052 sq km to 5305 sq km accompanied by a substantial decrease in barren land from 179 sq km to 91 sq km from 2004 to 2019. These findings demonstrated that reclamation activities positively impacted the forest expansion and reduced the barren land of the study area. Key land-cover transitions included barren land to shrubland/herbaceous, forest to shrubland, and shrubland to forest, indicating vegetation growth from 2004 to 2019. An autocorrelation analysis indicated similar land-cover types clustered together, showing effective forest restoration efforts. As surface coal mining and reclamation significantly influenced the landscapes of the coalfield counties in eastern Kentucky, this study provides a holistic perspective for understanding the repercussions of these transformations, including their effects on humans, society, and environmental health. Full article
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<p>Map of study area: (<b>a</b>) contiguous USA showing KY, (<b>b</b>) Map of KY showing study area counties within blue border, (<b>c</b>) DEM of study area, (<b>d</b>) coalfield counties of study area.</p>
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<p>Study workflow.</p>
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<p>Topographic layers: (<b>a</b>) elevation, (<b>b</b>) slope, (<b>c</b>) aspect, (<b>d</b>) land capability classes of the study area.</p>
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<p>Land-cover maps of the study area for 2004 and 2019.</p>
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<p>Map showing land-cover change in the study area from 2004 to 2019.</p>
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<p>(<b>a</b>) Land-cover change trends in the study area from 2004 to 2019. (<b>b</b>) Land-cover change trends in the study area from 2004 to 2019.</p>
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<p>Graphical representation of percentage change in land-cover classes between the years 2004 and 2019 in the study area.</p>
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<p>Hot spot and cold spot mapping of herbaceous and developed land-cover change using Gi* Statistic between 2004 and 2019 in eastern Kentucky.</p>
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<p>Hot spot and cold spot mapping of forest and barren land-cover change using Gi* Statistic between 2004 and 2019 in eastern Kentucky.</p>
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<p>Hot spot and cold spot mapping of shrubland land-cover change using Gi* Statistic between 2004 and 2019 in eastern Kentucky.</p>
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<p>Validation points and training samples shown in a map of the study area for 2004 and 2019.</p>
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15 pages, 2773 KiB  
Article
Monitoring Eastern White Pine Health by Using Field-Measured Foliar Traits and Hyperspectral Data
by Sudan Timalsina, Parinaz Rahimzadeh-Bajgiran, Pulakesh Das, José Eduardo Meireles and Rajeev Bhattarai
Sensors 2024, 24(18), 6129; https://doi.org/10.3390/s24186129 - 23 Sep 2024
Cited by 1 | Viewed by 951
Abstract
Canopy foliar traits serve as crucial indicators of plant health and productivity, forming a vital link between plant conditions and ecosystem dynamics. In this study, the use of hyperspectral data and foliar traits for white pine needle damage (WPND) detection was investigated for [...] Read more.
Canopy foliar traits serve as crucial indicators of plant health and productivity, forming a vital link between plant conditions and ecosystem dynamics. In this study, the use of hyperspectral data and foliar traits for white pine needle damage (WPND) detection was investigated for the first time. Eastern White Pine (Pinus strobus L., EWP), a species of ecological and economic significance in the Northeastern USA, faces a growing threat from WPND. We used field-measured leaf traits and hyperspectral remote sensing data using parametric and non-parametric methods for WPND detection in the green stage. Results indicated that the random forest (RF) model based solely on remotely sensed spectral vegetation indices (SVIs) demonstrated the highest accuracy of nearly 87% and Kappa coefficient (K) of 0.68 for disease classification into asymptomatic and symptomatic classes. The combination of field-measured traits and remote sensing data indicated an overall accuracy of 77% with a Kappa coefficient (K) of 0.46. These findings contribute valuable insights and highlight the potential of both field-derived foliar and remote sensing data for WPND detection in EWP. With an exponential rise in forest pests and pathogens in recent years, remote sensing techniques can prove beneficial for the timely and accurate detection of disease and improved forest management practices. Full article
(This article belongs to the Section Sensing and Imaging)
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<p>(<b>a</b>) The location of the study area in Maine (<b>b</b>) the positions of the sampled trees in Bethel (central coordinates: 44.40° N, 70.79° W).</p>
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<p>The overall data processing flowchart.</p>
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<p>Average spectral signatures of the symptomatic and asymptomatic EWP needles.</p>
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<p>The variations in (<b>a</b>) EWT, (<b>b</b>) N<sub>mass</sub>, (<b>c</b>) Chl, (<b>d</b>) LMA, (<b>e</b>) N<sub>area</sub>, and (<b>f</b>) Fluorescence in asymptomatic and symptomatic EWP samples.</p>
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<p>The variations of (<b>a</b>) NDVI, (<b>b</b>) GNDVI, (<b>c</b>) REP, (<b>d</b>) NDNI, and (<b>e</b>) NDWI<sub>1240</sub> in asymptomatic and symptomatic EWP samples.</p>
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<p>The Variable Importance Plot (VIP) for (<b>a</b>) the best-performing RF model using remotely sensed SVIs and (<b>b</b>) the best RF model using field-measured traits.</p>
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32 pages, 1923 KiB  
Review
The Spectrum of Disease-Associated Alleles in Countries with a Predominantly Slavic Population
by Grigoriy A. Yanus, Evgeny N. Suspitsin and Evgeny N. Imyanitov
Int. J. Mol. Sci. 2024, 25(17), 9335; https://doi.org/10.3390/ijms25179335 - 28 Aug 2024
Viewed by 1515
Abstract
There are more than 260 million people of Slavic descent worldwide, who reside mainly in Eastern Europe but also represent a noticeable share of the population in the USA and Canada. Slavic populations, particularly Eastern Slavs and some Western Slavs, demonstrate a surprisingly [...] Read more.
There are more than 260 million people of Slavic descent worldwide, who reside mainly in Eastern Europe but also represent a noticeable share of the population in the USA and Canada. Slavic populations, particularly Eastern Slavs and some Western Slavs, demonstrate a surprisingly high degree of genetic homogeneity, and, consequently, remarkable contribution of recurrent alleles associated with hereditary diseases. Along with pan-European pathogenic variants with clearly elevated occurrence in Slavic people (e.g., ATP7B c.3207C>A and PAH c.1222C>T), there are at least 52 pan-Slavic germ-line mutations (e.g., NBN c.657_661del and BRCA1 c.5266dupC) as well as several disease-predisposing alleles characteristic of the particular Slavic communities (e.g., Polish SDHD c.33C>A and Russian ARSB c.1562G>A variants). From a clinical standpoint, Slavs have some features of a huge founder population, thus providing a unique opportunity for efficient genetic studies. Full article
(This article belongs to the Section Molecular Genetics and Genomics)
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<p>Historical dispersal of Slavic people. Approximate time of migration (years CE) is given in brackets.</p>
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<p>Minor allele frequency (MAF) of the <span class="html-italic">NBN</span> c.657del5 allele in Slavic and some non-Slavic countries (created with <a href="http://paintmaps.com" target="_blank">paintmaps.com</a>, accessed on date 27 May 2024).</p>
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29 pages, 19572 KiB  
Article
Morphology, Internal Architecture, Facies Model, and Emplacement Mechanisms of Lava Flows from the Central Atlantic Magmatic Province (CAMP) of the Hartford and Deerfield Basins (USA)
by Abdelhak Moumou, Nasrrddine Youbi, Hind El Hachimi, Khalil El Kadiri, José Madeira, João Mata, Isma Amri and Abdelkarim Ait Baha
Geosciences 2024, 14(8), 204; https://doi.org/10.3390/geosciences14080204 - 31 Jul 2024
Viewed by 928
Abstract
The morphology, internal architecture, and emplacement mechanisms of the Central Atlantic Magmatic Province (CAMP) lava flows of the Hartford and Deerfield basins (USA) are presented. The Talcott, Holyoke, and Hampden formations within the Hartford basin constitute distinct basaltic units, each exhibiting chemical, mineralogical, [...] Read more.
The morphology, internal architecture, and emplacement mechanisms of the Central Atlantic Magmatic Province (CAMP) lava flows of the Hartford and Deerfield basins (USA) are presented. The Talcott, Holyoke, and Hampden formations within the Hartford basin constitute distinct basaltic units, each exhibiting chemical, mineralogical, and structural differences corresponding to flow fields. Each flow field was the result of several sustained eruptions that produced both inflated pahoehoe flows and subaquatic extrusions: 1–5 eruptions in the Talcott formation and 1–2 in Holyoke and Hampden basalts, where simple flows are dominant. The Deerfield basin displays the Deerfield basalt unit, characterized by pillow lavas and sheet lobes, aligning chemically and mineralogically with the Holyoke basalt unit. Overall, the studied flow fields are composed of thick, simple pahoehoe flows that display the entire range of pahoehoe morphology, including inflated lobes. The three-partite structure of sheet lobes, vertical distribution of vesicles, and segregation structures are typical. The characteristics of the volcanic pile suggest slow emplacement during sustained eruptive episodes and are compatible with a continental basaltic succession facies model. The studied CAMP basalts of the eastern United States are correlated with the well-exposed examples on both sides of the Atlantic Ocean (Canada, Portugal, and Morocco). Full article
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Figure 1
<p>(<b>a</b>) location map of Africa–South America–North America, Greenland, and Europe at 201 Ma and CAMP schematic extent; (<b>b</b>) paleogeographic extent of ca 201 Ma Central Atlantic Magmatic Province (CAMP) across the central Pangean supercontinent (after McHone [<a href="#B6-geosciences-14-00204" class="html-bibr">6</a>,<a href="#B23-geosciences-14-00204" class="html-bibr">23</a>,<a href="#B28-geosciences-14-00204" class="html-bibr">28</a>]).</p>
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<p>(<b>a</b>) Early Mesozoic rift basins in eastern North America: 1, Fundy; 2, Hartford; 3, Newark; 4, Gettysburg; 5, Culpeper; 6, Danville; (<b>b</b>) Geologic sketch map of Hartford, Deerfield, and Pomperaug (Southbury) basins; (<b>c</b>) Stratigraphic column of Newark Supergroup in the Hartford basin (after [<a href="#B23-geosciences-14-00204" class="html-bibr">23</a>]).</p>
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<p>Ideal diagram showing feature structures of inflated pahoehoe sheet lobes [<a href="#B70-geosciences-14-00204" class="html-bibr">70</a>]. The left side of the column shows the characteristic three-part division of sheet lobes (<b>a</b>) and jointing styles (<b>b</b>) CRZ, crustal zone; PLZ, platy zone; CLZ, columnar zone. The right side of the column illustrates the distribution of (<b>c</b>) vesiculation structures (VZ, vesicular zone; MV, mega-vesicle; HVS, horizontal vesicle sheet; VC, vesicle cylinder; SV, segregation vesicle; PV, pipe vesicle; BVZ, basal vesicular zone), (<b>d</b>) vesiculation (non- to sparsely vesicular d = 0–5 vol%, moderately vesicular m = 10–20 vol% and vesicular v = 30–40 vol%), and (<b>e</b>) degree of crystallinity (G, hyaline; hyh, hypohyaline; hc, hypocrystalline; c, holocrystalline). The scale h/l indicates the normalized height above the base of the sheet lobe (h, height in lobe; l, total lobe thickness).</p>
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<p>Studied sections of the Talcott Basalt Formation from the Hartford Basin, Connecticut (modified from [<a href="#B34-geosciences-14-00204" class="html-bibr">34</a>,<a href="#B93-geosciences-14-00204" class="html-bibr">93</a>]). 1. Section Behind the Target store in Meriden section (N 41°33′9.34″; W 72°49′0.40″); 2. Tariffville section (N 41°54′28.73″; W 72°45′40.18″); 3. King Philip’s Cave section, Talcott Mountain State Park (N 41°50′1.99″; W 72°47′54.08″). BC: Basal Crust; LC: Lava Core; ULC: Upper Lava Crust.</p>
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<p>The large, long rock-cut behind the Target store in Meriden, Connecticut (<b>a</b>) Contact between the New Haven Formation and the first pillowed flow of the Talcott Basalt Formation. Legend: 1, Blak mudstone, contorted with flame structure and isolated pillows; 2, Contact; 3, Closely (densely) packed pillow. (<b>b</b>) Contact between the first pillowed flow and the second sheet lobe flow of the Talcott Basalt Formation. Note the occurrence of pipe vesicles in the basal crust of the second sheet lobe and the preservation of the glassy zone and radial and concentric cracks. (<b>c</b>) View of the flow units 3, 4, and 5 of the Talcott Basalt Formation. The flow unit 3 is composed of pillow breccias of 2 m gradually overcome by a horizon of 1 m with well-preserved isolated pillow and fragment pillow dispersed in an abundant hyaloclastite matrix which is covered by less than one meter of vesicular lava. The flow unit 4 is constituted by densely packed pillows. Note its compound nature. The last flow unit 5 is a vesicular lava flow. (<b>d</b>) View of the flows units 3, 4, and 5 of the Talcott Basalt Formation. Note the compound nature of the flow units 3 and 4. The flow unit 4 with densely packed pillows is emplaced in paleochannel.</p>
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<p>Plot of pillows’ horizontal (H) vs. vertical (V) dimensions from (<b>a</b>) unit 1 of Talcott Basalt from (Behind the Target outcrop (Hartford Basin); (<b>b</b>) unit 1 of the Deerfield basalt from the Springfield outcrop (Deerfield Basin).</p>
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<p>Pipe vesicles and large pillow lava located in the large, long rock cut behind the Target store in Meriden, Connecticut (<b>a</b>) Internal structure of pillow lava of the first pillowed flow of the Talcott Basalt Formation (toward the top of the unit). Location: The large, long rock-cut behind the Target store in Meriden, Connecticut. (<b>b</b>) Detail of the contact between the first pillowed flow and the second sheet lobe flow of the Talcott Basalt Formation. Note the occurrence of unfilled pipe vesicles in the basal crust of the second sheet lobe.</p>
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<p>Pictures took in the large, long rock-cut behind the Target store in Meriden, Connecticut. (<b>a</b>,<b>b</b>) Closely (densely) packed pillow; the first pillowed flow of the Talcott Basalt Formation (toward the top of the unit). Note that the hyaloclastite matrix between pillows becomes more abundant. (<b>c</b>) Contact between the first pillowed flow and the second sheet lobe flow of the Talcott Basalt Formation. Note the occurrence of pipe vesicles in the basal crust of the second sheet lobe and the preservation of the glassy zone and radial and concentric cracks. (<b>c</b>) Mega-vesicles, including half-moon vesicles and horizontal vesicle sheet of the second sheet lobe flow of the Talcott Basalt Formation. Segregation structures of pahoehoe flow types are located at the top of the lava core of the love. Location: The large, long rock-cut behind the Target store in Meriden, Connecticut. (<b>d</b>) Large pillow lava with digitation form of the first pillowed flow of the Talcott Basalt Formation (toward the top of the unit).</p>
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<p>(<b>a</b>) Fluidal peperites of the Neptunian dyke of <a href="#geosciences-14-00204-f009" class="html-fig">Figure 9</a>b Photograph of jigsaw-fit clasts in basaltic breccia from the Neptunian dyke. This type of jigsaw-fit texture is a common feature of blocky and fluidal peperites and is thought to reflect in situ quench fragmentation. (<b>b</b>) Blockey peperite of the Neptunian dyke of <a href="#geosciences-14-00204-f009" class="html-fig">Figure 9</a>b arkose host sediments inject fissures of blocky juvenile clast with typical jigsaw-fit texture, indicating that the peperite has typical features of blocky peperite. Blocky peperite is formed in the background of magma, producing brittle crackings. When hot magma intrudes cold wet sediments, hot magma generates quenching distortion and forms juvenile clasts. (<b>c</b>) Neptunian dyke (clastic dyke) cross-cutting the Talcott Basalt Formation at about 3 km ESE of the quarry of Tilcon Connecticut/North Branford on Fox Road. This basalt breccia-filled fissure with an arkosic matrix and peperites (both blocky and fluidal peperites are present) shows a chilled margin and injected Arkose pocket with the Talcott Basalt. Blocky peperites and mixed blocky and fluidal peperites formed where rising melt interacted explosively with groundwater and with coarse, water-saturated sediments of the New Haven Formation, and underwent brittle quench fragmentation. See <a href="#app1-geosciences-14-00204" class="html-app">Figures S13 and S14</a> for details of peperites. (<b>d</b>) Fluidal peperites in the Contact of the Hampden Basalt with the East Berlin Fm near Berlin along the RT-9 South. (<b>e</b>) Detail of the well-developed layers of blackish spherule layers (accretionary lapilli?). (<b>f</b>) Well-developed layers of blackish spherule layers (accretionary lapilli?) that might represent basaltic lapilli occur a few cm below the first pillowed flow of the Talcott Basalt Formation located in the large, long rock-cut behind the Target store in Meriden, Connecticut.</p>
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<p>Panoramic view of the Holyoke flood-basalt flow in the North Branford Quarry, Connecticut. Note the Cuspate boundary (dashed line) separating radiating joints in entablature from vertical columnar joints in the colonnade of the Holyoke flood-basalt flow. The boundary is approximately 120 m above the base of this 200-m-thick section through the flow. The centers of the two cusps are 15 m apart.</p>
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<p>Lithostratigraphic columns across the Holyoke basalts in the Hartford and Deerfield basins (modified from [<a href="#B34-geosciences-14-00204" class="html-bibr">34</a>,<a href="#B93-geosciences-14-00204" class="html-bibr">93</a>]). 1. Section of the Tilcon quarry near North Branford Town, Connecticut (N 41°20′31.81″; W 72°47′39.28″); 2. section of Cooks Gap, Plainville, Hartford County, Connecticut (N 41°40′28.72″; W 72°49′44.95″); 3. and 4. sections of Deerfield basalt sequence at French King Highway, Gill (3) (N 41°40′28.72″; W 72°49′44.95″) and Turner Falls; (4) (N 41°40′28.72″; W 72°49′44.95″), Massachusetts. Note that each lithostratigraphic column has its scale. BC: basal crust. LCR: lava core. ULC: upper lava crust.</p>
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<p>(<b>a</b>) The two flows of the Holyoke Basalt in the Tom Holyoke Mountains Quarry, Massachusetts. (<b>b</b>,<b>c</b>) Vesicle Cylinder of the lava core of the Holyoke flood-basalt flow in the North Branford Quarry, Connecticut. (<b>d</b>) Fault/Squeez up N30–40, 75–85 SW affecting the first flow of the Holyoke Basalt in the Tom Holyoke Mountains Quarry, Massachusetts. (<b>e</b>) Segregation sheets of coarse-grained ferrodiorite of the Holyoke flood-basalt flow in the North Branford Quarry, Connecticut.</p>
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<p>Lithostratigraphic columns across the Hampden basalts in the Hartford basin (modified from Gray [<a href="#B34-geosciences-14-00204" class="html-bibr">34</a>]). 1. Section along the RT-9 South, Berlin, Connecticut (N 41°37′19.05″; W 72°44′11.07″); 2. Section of the Rock Ridge Park, Hartford, Connecticut (N 41°45′3.08″; W 72°41′36.67″).</p>
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<p>(<b>a</b>,<b>b</b>) Horizontal vesicular zone of Hampden Basalt at the Section of the Rock Ridge Park, Hartford, Connecticut; (<b>c</b>) contact of the Hampden Basalt with the East Berlin Fm. near Berlin along the RT-9 South; (<b>d</b>) contact of the Hampden Basalt with the East Berlin Fm. near Berlin along the RT-9 South with pipe vesicles; (<b>e</b>) ash bed (Pompton Tuff Bed) of the East Berlin Fm. with orange color near Berlin along the RT-9 South, Connecticut; (<b>g</b>) flow top breccia of Hampden Basalt at the Section of the Rock Ridge Park, Hartford, Connecticut; (<b>f</b>) detail of Flow top breccia of Hampden Basalt at the Section of the Rock Ridge Park, Hartford, Connecticut.</p>
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<p>(<b>a</b>) Contact between the Deerfield Basalt and the Sugarloaf Arkose Formation near Greenfield along the Mohawk Trail (RT-2A). Left side before crossing the French King Bridge and entering Greenfield. The development of peperites underlines the contact. (<b>b</b>) Horizontal vesicular zone of the Upper Crust of the second sheet lobe of the Deerfield Basalt Formation near Greenfield along the Mohawk Trail (RT-2A). Right side before reaching the French King Bridge and entering Greenfield.</p>
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17 pages, 7202 KiB  
Article
Future Range Expansions of Invasive Wasps Suggest Their Increasing Impacts on Global Apiculture
by Xueyou Zhang, Peixiao Nie, Xiaokang Hu and Jianmeng Feng
Insects 2024, 15(7), 546; https://doi.org/10.3390/insects15070546 - 19 Jul 2024
Cited by 1 | Viewed by 953
Abstract
Until now, no study has examined the future range dynamics of major invasive wasp species to assess their future impacts on global apiculture. Here, we developed 12 species distribution models to calibrate the future range dynamics of 12 major invasive Vespidae wasp species [...] Read more.
Until now, no study has examined the future range dynamics of major invasive wasp species to assess their future impacts on global apiculture. Here, we developed 12 species distribution models to calibrate the future range dynamics of 12 major invasive Vespidae wasp species under a unified framework. An increase in their habitat suitability was identified in more than 75% of global land. Substantial range expansions were detected for all 12 species, and they were primarily induced by future climate changes. Notably, Polistes dominula and Vespa crabro had the largest potential ranges under all scenarios, suggesting their greater impact on global apiculture. Polistes chinensis and Vespa velutina nigrithorax had the highest range expansion ratios, so they warrant more urgent attention than the other species. Polistes versicolor and P. chinensis are expected to exhibit the largest centroid shifts, suggesting that substantial shifts in prioritizing regions against their invasions should be made. Europe and the eastern part of the USA were future invasion hotspots for all major invasive wasp species, suggesting that apiculture might face more pronounced threats in these regions than in others. In conclusion, given their substantial range shifts, invasive wasps will likely have increasingly negative impacts on global apiculture in the future. Full article
(This article belongs to the Section Insect Ecology, Diversity and Conservation)
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<p>Occurrences of the 12 major invasive wasp species. Occurrences were retrieved from the Global Biodiversity Information Facility (<a href="http://www.gbif.org" target="_blank">www.gbif.org</a>, accessed on 7 September 2023). A total of 19,196 occurrences were retrieved after spatial thinning.</p>
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<p>The importance of each predictor in the baseline models. Topographical, climatic, and land-use factors are shown in green, blue, and orange fonts, respectively. For each species, importance values were standardized according to the max–min method. The grayscale shading indicates the relative importance of each of the predictors, and the blanks indicate that the predictors were not inputted into the final models for the species.</p>
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<p>Overlap indices of habitat suitability of the 12 major invasive wasp species: (<b>a</b>) current scenario; (<b>b</b>) scenario of F126; (<b>c</b>) scenario of F585; (<b>d</b>) scenario of M126; (<b>e</b>) scenario of 585. High habitat suitability overlap indices in the five scenarios was detected in Europe, the eastern and western parts of the USA, and the southeastern part of Australia.</p>
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<p>Changes in overlap indices of habitat suitability of 12 major invasive wasps. (<b>a</b>) F126; (<b>b</b>) F585; (<b>c</b>) M126; (<b>d</b>) M585. Considerable increases of overlap indices of habitat suitability under F126 and M126 were mainly detected in eastern coastline regions and the eastern part of USA, North Europe, East China, Nepal, New Zealand and southeastern coastlines of Australia. Large increases in the overlap indices of habitat suitability under the scenarios of M585 and F585 were primarily identified in the eastern part of North America, western coastline regions of the North America, North Europe, western part of Russia, Nepal, India, East China and the far-east regions of Russia.</p>
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<p>Potential ranges and range dynamics of the 12 major invasive wasp species under future scenarios. The potential ranges are shown in grayscale. The range dynamics are indicated by expanding ranges in redscale, the range expansion ratios in bluescale, and the range similarity indices in yellowscale. Under most scenarios, <span class="html-italic">Polistes dominula</span>, <span class="html-italic">Vespa crabro</span>, and <span class="html-italic">Vespula germanica</span> were projected to show larger potential ranges than the other species; <span class="html-italic">Vespa velutina nigrithorax</span> and <span class="html-italic">Polistes chinensis</span> were projected to have the higher range expansion ratios; <span class="html-italic">Polistes versicolor</span> and <span class="html-italic">P. chinensis</span> were projected to have lower range similarity indices; and <span class="html-italic">Vespa velutina</span> and <span class="html-italic">Polistes dominula</span> were projected to have larger expanding ranges.</p>
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<p>Overlap indices of potential ranges of the 12 major invasive wasp species: (<b>a</b>) overlap indices of potential ranges under the current scenario; (<b>b</b>) range overlap indices under F126; (<b>c</b>) range overlap indices under F585; (<b>d</b>) range overlap indices under M126; (<b>e</b>) range overlap indices under M585. High overlap indices of potential ranges were mainly projected in Europe, the eastern part of the USA, a region to the west of the Cascade Mountain Range in the USA, the eastern part of China, Japan, the southeast part of Australia, New Zealand, Argentina, and the southeastern part of Brazil.</p>
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<p>Overlap indices of expanding ranges of the 12 major invasive wasps. (<b>a</b>) overlap indices of expanding ranges of expanding ranges under F126 scenarios; (<b>b</b>) overlap indices of expanding ranges of expanding ranges under F585 scenarios; (<b>c</b>) overlap indices of expanding ranges under M126 scenarios; (<b>d</b>) overlap indices of expanding ranges under M585 scenarios. High values of overlapping indices of expanding ranges in Europe, northeastern and northwestern parts of the United States of America, southeastern and southwestern parts of Canada, Southeast China, New Zealand, southeastern coastline regions of Australia, Japan and southern part of Chile.</p>
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14 pages, 258 KiB  
Article
Mental Health, Sleep Quality, and Psychological Well-Being during the Holy Month of Ramadan
by Danny Jandali, Abdullah Alwaleedi, Michele W. Marenus, Sarah R. Liener, Amine Sheik, Malak Elayyan and Weiyun Chen
Healthcare 2024, 12(13), 1301; https://doi.org/10.3390/healthcare12131301 - 29 Jun 2024
Viewed by 1443
Abstract
Objectives: Ramadan, a significant month for Muslims, presents unique challenges, particularly in the context of the USA. This study aimed to explore the relationship between mental health factors (depression, anxiety, and stress), sleep quality, and psychological well-being (subjective happiness and life satisfaction) during [...] Read more.
Objectives: Ramadan, a significant month for Muslims, presents unique challenges, particularly in the context of the USA. This study aimed to explore the relationship between mental health factors (depression, anxiety, and stress), sleep quality, and psychological well-being (subjective happiness and life satisfaction) during the month of Ramadan among participants and by gender. Methods: This study enlisted 163 participants (74% female, 25.7% male), with an average age of 36.8 years (SD = 13.1), mostly of Middle Eastern descent. Recruitment was conducted via flyers at local community mosques, social media, and outreach through local religious leaders. Data collection took place in the last three weeks of Ramadan, utilizing a Qualtrics survey that included the Depression Anxiety and Stress Scale (DASS-21), the Subjective Happiness Scale (SHS), Satisfaction with Life Scale (SWLS), and the Pittsburgh Sleep Quality Index (PSQI). Data were analyzed by means of descriptive statistics and multiple linear regression models using SPSS version 28. Results: The study indicates that while mental health and psychological well-being remained within normal levels during Ramadan, sleep scores indicated significant sleep disturbance among participants. Multiple linear regression models revealed that subjective happiness, sleep duration, and the global PSQI score were significant predictors of stress for the total sample (F = 9.816, p = 0.001). Life satisfaction was the only significant predictor of anxiety (F = 7.258, p = 0.001), and it, alongside subjective happiness, significantly predicted depression (F = 12.317, p = 0.001). For men, subjective happiness alone predicted stress, while life satisfaction was a predictor for both anxiety and depression (F = 4.637, p = 0.001). In women, sleep duration and medication usage were linked to stress but not anxiety. Life satisfaction and subjective happiness were, however, predictors of depression (F = 6.380, p = 0.001). Conclusion: Fostering positive affective states can serve as a protective mechanism against the potential psychological distress associated with altered sleep patterns and lifestyle changes that accompany Ramadan. This study highlights that Ramadan is a tool for bolstering happiness and life satisfaction, thereby lowering levels of stress, anxiety, and depression. In non-Muslim majority contexts like the USA, there is a need for accommodations to safeguard against potential psychological distress. Full article
22 pages, 5448 KiB  
Article
IMERG in the Canadian Precipitation Analysis (CaPA) System for Winter Applications
by Stéphane Bélair, Pei-Ning Feng, Franck Lespinas, Dikra Khedhaouiria, David Hudak, Daniel Michelson, Catherine Aubry, Florence Beaudry, Marco L. Carrera and Julie M. Thériault
Atmosphere 2024, 15(7), 763; https://doi.org/10.3390/atmos15070763 - 27 Jun 2024
Viewed by 917
Abstract
Several configurations of the Canadian Precipitation Analysis system (CaPA) currently produce precipitation analyses at Environment and Climate Change Canada (ECCC). To improve CaPA’s performance during the winter season, the impact of assimilating the IMERG V06 product (IMERG: Integrated Multi-satellitE Retrievals for GPM—Global Precipitation [...] Read more.
Several configurations of the Canadian Precipitation Analysis system (CaPA) currently produce precipitation analyses at Environment and Climate Change Canada (ECCC). To improve CaPA’s performance during the winter season, the impact of assimilating the IMERG V06 product (IMERG: Integrated Multi-satellitE Retrievals for GPM—Global Precipitation Measurement mission) into CaPA is examined in this study. Tests are conducted with CaPA’s 10 km deterministic version, evaluated over Canada and the northern part of the United States (USA). Maps from a case study show that IMERG plays a contradictory role in the production of CaPA’s precipitation analyses for a synoptic-scale winter storm over North America’s eastern coast. While its contribution appears to be physically correct over southern portions of the meteorological system, and early in its intensification phase, IMERG displays unrealistic spatial structures over land later in the system’s life cycle when it is located over northern (colder) areas. Objective evaluation of CaPA’s analyses when IMERG is assimilated without any restrictions shows an overall decrease in precipitation, which has a mixed effect (positive and negative) on the bias indicators. But IMERG’s influence on the Equitable Threat Score (ETS), a measure of CaPA’s analyses accuracy, is clearly negative. Using IMERG’s quality index (QI) to filter out areas where it is less accurate improves CaPA’s objective evaluation, leading to better ETS versus the control experiment in which no IMERG data are assimilated. Several diagnostics provide insight into the nature of IMERG’s contribution to CaPA. For the most successful configuration, with a QI threshold of 0.3, IMERG’s impact is mostly found in the warmer parts of the domain, i.e., in northern US states and in British Columbia. Spatial means of the temporal sums of absolute differences between CaPA’s analyses with and without IMERG indicate that this product also contributes meaningfully over land areas covered by snow, and areas where air temperature is below −2 °C (where precipitation is assumed to be in solid phase). Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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Figure 1
<p>Spatial domain used in this study for the evaluation of CaPA’s precipitation analyses. The location of observations assimilated by CaPA for a specific date (1200 UTC 7 January 2022) is shown. These stations are identified with a color code indicating the network they belong to. The network partners are listed in [<a href="#B42-atmosphere-15-00763" class="html-bibr">42</a>]. Super stations refer to the combination of at least two stations that are very close to each other.</p>
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<p>Synoptic meteorological situation at 0000 UTC (<b>top panel</b>) and 1800 UTC (<b>bottom panel</b>) 17 January 2022, from ECCC’s global deterministic atmospheric analyses. The color shadings represent screen-level air temperature (°C). The full lines are for the sea-level pressure (hPa), with “H” and “L” referring to high- and low-pressure centers, respectively. The dashed lines are for 500 hPa geopotential height (dam). The arrows are for winds at the surface (m·s<sup>−1</sup>).</p>
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<p>Six-hourly precipitation (mm) between 16 January 2022 at 1800 UTC and 17 January 2022 at 0000 UTC for (<b>a</b>) CTRL analysis, (<b>b</b>) first guess, (<b>c</b>) IMERG-ALL analysis, and (<b>d</b>) IMERG product assimilated in CaPA. The discontinuity in the lower left corner of the figure is associated with the southern border of the analysis domain (<a href="#atmosphere-15-00763-f001" class="html-fig">Figure 1</a>).</p>
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<p>Same as <a href="#atmosphere-15-00763-f003" class="html-fig">Figure 3</a> but for 6-hourly precipitation (mm) between 1200 UTC and 1800 UTC on 17 January 2022.</p>
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<p>Objective evaluation of IMERG-ALL (full lines) versus CTRL (dashed lines) over the domain shown in <a href="#atmosphere-15-00763-f001" class="html-fig">Figure 1</a> for the period from 1 December 2021 to 31 March 2022. The upper panels are for POD, FAR, and ETS. The lower panels are for FBI-1 and the partial means (see <a href="#app1-atmosphere-15-00763" class="html-app">Appendix A</a> for definitions). Objective evaluation is performed with LOOCV for CaPA’s 6-hourly precipitation analyses against surface synoptic manual observations. Filled symbols indicate that the differences between the two experiments are statistically significant at the 95% confidence level, based on the bootstrap method (not the case for open symbols). It should be noted that the thresholds (“x” axis) for the partial means are different from the other panels, in order to reach asymptotic behavior for large accumulations. Horizontal lines indicate zero values for FBI-1 and partial sums.</p>
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<p>Same as <a href="#atmosphere-15-00763-f005" class="html-fig">Figure 5</a>, but for the objective evaluation of IMERG-0p4 (full red lines) versus CTRL (dashed black lines).</p>
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<p>Frequency distribution of IMERG quality index (in percentage) for the domain shown in <a href="#atmosphere-15-00763-f001" class="html-fig">Figure 1</a> and for the analysis period from 1 December 2021 to 31 March 2022. Results are shown over (<b>a</b>) land only, (<b>b</b>) water only, (<b>c</b>) land for points where snow depth is greater than 1 cm, and (<b>d</b>) land for points where air temperature is below −2 °C. The numbers in the upper-right corners indicate the percentage of grid points considered in each panel (top number) and of realizations for which the quality index is over 0.3 and 0.4 (bottom two numbers). Grid points with negative QIs are not accounted for in the histograms.</p>
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<p>Same as <a href="#atmosphere-15-00763-f005" class="html-fig">Figure 5</a> and <a href="#atmosphere-15-00763-f006" class="html-fig">Figure 6</a> but for the objective evaluation of IMERG-0p3 (full magenta lines) versus CTRL (dashed black lines).</p>
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<p>Air temperature at the screen level (°C, <b>left panels</b>), IMERG quality index (<b>middle panels</b>), and snow depth (cm) analysis from CaLDAS (right panels), temporally averaged between 1800 UTC on 16 January 2022 and 0000 UTC on 17 January 2022 (upper panels) and between 1200 UTC and 1800 UTC on 17 January 2022 (<b>lower panels</b>). The bold lines show the 1.0 mm contour for the 6-hourly CTRL precipitation analyses, consistent with <a href="#atmosphere-15-00763-f003" class="html-fig">Figure 3</a> and <a href="#atmosphere-15-00763-f004" class="html-fig">Figure 4</a>.</p>
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<p>Temporal means and sums of the IMERG contribution for winter 2022 obtained by comparing 6-hourly precipitation analyses from CTRL and IMERG-ALL experiments. The left panels show the absolute (mm, upper panel, based on Equation (<a href="#FD2-atmosphere-15-00763" class="html-disp-formula">2</a>)) and normalized (lower panel, Equation (<a href="#FD3-atmosphere-15-00763" class="html-disp-formula">3</a>)) differences between the two experiments. The panels on the right indicate the fraction (%, based on Equation (<a href="#FD7-atmosphere-15-00763" class="html-disp-formula">7</a>)) of the absolute differences that occur over areas where snow depth is greater than 1 cm (<b>upper panel</b>) and where air temperature is below −2 °C (<b>lower panel</b>).</p>
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<p>Similar to the left panels in <a href="#atmosphere-15-00763-f010" class="html-fig">Figure 10</a>. The IMERG contribution for winter 2022 is obtained by comparing 6-hourly precipitation analyses from CTRL and the IMERG-0p4 (<b>top</b>) and IMERG-0p3 (<b>bottom</b>) experiments. The absolute (mm, left panels, Equation (<a href="#FD2-atmosphere-15-00763" class="html-disp-formula">2</a>)) and normalized (right panels, Equation (<a href="#FD3-atmosphere-15-00763" class="html-disp-formula">3</a>)) differences are shown.</p>
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16 pages, 1982 KiB  
Article
Maxent Predictive Species Distribution Models and Model Accuracy Assessment for Two Species of Psilochalcis Kieffer (Hymenoptera: Chalcididae) Occurring in the Eastern Great Basin of Utah, USA
by Mark J. Petersen, Hector G. Ortiz Cano, Teresa Gomez, Robert L. Johnson, Val Jo Anderson and Steven L. Petersen
Diversity 2024, 16(6), 348; https://doi.org/10.3390/d16060348 - 16 Jun 2024
Cited by 2 | Viewed by 941
Abstract
Two species of Psilochalcis wasps (P. minuta and P. quadratis) were recently described from Utah’s eastern Great Basin. The extent of their known distributions is extremely limited, based on few data points. We developed species distribution models (SDMs) using Maxent modeling [...] Read more.
Two species of Psilochalcis wasps (P. minuta and P. quadratis) were recently described from Utah’s eastern Great Basin. The extent of their known distributions is extremely limited, based on few data points. We developed species distribution models (SDMs) using Maxent modeling software for each Psilochalcis species to identify areas of probable suitable habitat for targeted collecting to improve our knowledge of their distributions. We used six occurrence data points for P. minuta and eight occurrence data points for P. quadratis, along with ten environmental variables as inputs into the Maxent modeling software. Model-predicted areas with a potential suitable habitat value greater than 0.69 were mapped using ArcGIS Pro to help select locations for model accuracy assessment. Employing Malaise traps, eighteen sites were sampled to evaluate each SDM’s ability to predict the occurrence of Psilochalcis species. Psilochalcis minuta occurred at eight of nine juniper-dominated sample sites that were predicted as having high suitability by the model for this species. Likewise, P. quadratis occurred at two of four cheatgrass-dominated sample sites predicted by the model. Psilochalcis minuta occurred at three of nine sampled sites that were not predicted by the model, and P. quadratis occurred at seven of fourteen non-predicted sites. The Maxent SDM results yielded an AUC value of 0.70 and p-value of 0.02 for P. minuta and 0.68 and 0.02. for P. quadratis. These results were reflected in our model accuracy assessment. Of the selected environmental variables, aspect, historic fire disturbance, and elevation yielded the greatest percent contributions to both species’ models. Sympatric distributions were observed for P. minuta and P. quadratis. Elevation, vegetation type, NDVI, and soil type are the most important environmental variables in differentiating areas of optimal suitable habitat for the two species. Full article
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<p>Lateral habitus of (<b>a</b>) <span class="html-italic">Psilochalcis minuta</span> female and (<b>b</b>) <span class="html-italic">Psilochalcis quadratis</span> female. Photos from species descriptions [<a href="#B2-diversity-16-00348" class="html-bibr">2</a>].</p>
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<p>Malaise trap sampling locations and areas of suitable habitat for <span class="html-italic">Psilochalcis minuta</span> and <span class="html-italic">Psilochalcis quadratis</span> as predicted by Maxent species distribution models. Map created in ArcGIS Pro.</p>
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<p>Results of jackknife analyses of area under the receiver operating curve (AUC) for environmental variables used in predicting areas of suitable habitat for (<b>a</b>) <span class="html-italic">Psilochalcis minuta</span> and (<b>b</b>) <span class="html-italic">Psilochalcis quadratis</span>.</p>
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<p>Environmental variable responses for (<b>a</b>) aspect, (<b>b</b>) elevation, (<b>c</b>) slope, and (<b>d</b>) NDVI. Graphs created from value range counts from the estimated probability of occurrence in 10,000 data point grid. Note: Only one set of graphs is shown since the variable responses were nearly identical for both <span class="html-italic">P. minuta</span> and <span class="html-italic">P. quadratis</span>.</p>
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25 pages, 355 KiB  
Article
A Model of Core Emotional Needs and Toxic Experiences: Their Links with Schema Domains, Well-Being, and Ill-Being
by John Philip Louis, George Lockwood and Karen McDonald Louis
Behav. Sci. 2024, 14(6), 443; https://doi.org/10.3390/bs14060443 - 24 May 2024
Viewed by 1755
Abstract
This study examined the second-order schema domains of Early Maladaptive and Adaptive Schemas based on recent trends and compared them with the five theoretical second-order schema domains commonly used in schema therapy. Using six international Eastern and Western community samples—Singapore (n = [...] Read more.
This study examined the second-order schema domains of Early Maladaptive and Adaptive Schemas based on recent trends and compared them with the five theoretical second-order schema domains commonly used in schema therapy. Using six international Eastern and Western community samples—Singapore (n = 628), Malaysia (n = 229), USA (n = 396), South Africa (n = 390), Nigeria (n = 364), India (n = 306)—confirmatory factor analysis showed that the four second-order domains of EMSs and EASs, which ran almost parallel with each other, were the most robust models calling into question the validity of the five domain model. Given the hypothesized links between schemas and needs, these four categories of EMSs and EASs represent four categories of toxic experiences and core emotional needs, respectively. These categories were supported empirically and are useful to parents as well as to clinicians as they approach child rearing and the treatment of clients in schema therapy from the vantage point of needs. These four categories of psychological core emotional needs, as well as toxic experiences, were found, as expected, to be linked with various measures of well-being and ill-being. Full article
21 pages, 10471 KiB  
Article
Spatial and Temporal Variability in Oyster Settlement on Intertidal Reefs Support Site-Specific Assessments for Restoration Practices
by Shannon D. Kimmel, Hans J. Prevost, Alexandria Knoell, Pamela Marcum and Nicole Dix
J. Mar. Sci. Eng. 2024, 12(5), 766; https://doi.org/10.3390/jmse12050766 - 30 Apr 2024
Viewed by 1575
Abstract
As some of the most threatened ecosystems in the world, the declining condition and coverage of coastal habitats results in the loss of the myriad ecosystem services they provide. Due to the variability in physical and biological characteristics across sites, it is imperative [...] Read more.
As some of the most threatened ecosystems in the world, the declining condition and coverage of coastal habitats results in the loss of the myriad ecosystem services they provide. Due to the variability in physical and biological characteristics across sites, it is imperative to increase location-based information to inform local management projects, which will potentially help to reestablish functions of coastal habitats. Since oysters are often used in restoration projects, this study quantified spatial and temporal patterns in eastern oyster spat settlement in a bar-built estuary in northeast Florida, USA that is host to a robust population of intertidal oyster reefs. Spat settlement was found to occur from April to October with small peaks in the spring and large ones around September. Inter-annual differences in spat settlement were likely influenced by existing environmental conditions and heavily affected by large-scale events such as tropical cyclones. Variations in regional spat settlements are possibly driven by the residence times of the watersheds, the density of adult populations, and the location of the spat collectors. The results of this study illustrate place-based variability in oyster settlement patterns and underscore the importance of local monitoring for oyster resource management, restoration, and research. Full article
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<p>Map of the Guana Tolomato Matanzas National Estuarine Research Reserve boundary (black line, bottom inset: red), spat collector locations (black dots), water quality monitoring stations (black triangles, not included in insets), and regions: Tolomato River (turquoise), Guana River (pink), Salt Run (yellow), St. Augustine (orange), and Fort Matanzas (blue). Water quality stations are from the System-Wide Monitoring Program and are Pine Island (“PIWQ”), San Sebastian (“SSWQ”), and Fort Matanzas (“FMWQ”).</p>
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<p>An example of a spat tree deployed on an oyster reef in the Guana River region of the Guana Tolomato Matanzas estuary in Florida, USA.</p>
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<p>Monthly mean spat per shell for each region from 2015 to 2020 with panels broken up in two-year segments: Tolomato River (TR, green); Guana River (GR, pink); Saint Augustine (SA; orange); Salt Run (SR, yellow); and Fort Matanzas (FM, blue). Note the difference between the scales of the <span class="html-italic">y</span>-axis and missing data in September and October 2016 indicated by the gray box in upper panel. The occurrences of Hurricane Matthew (a), Hurricane Irma (b), and Hurricane Dorian (c) are denoted by lowercase letters and dashed lines.</p>
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<p>Mean spat per shell in the five regions (<b>A</b>) of the Guana–Tolomato–Matanzas estuary: Tolomato River (TR, green); Guana River (GR, pink); Saint Augustine (SA; orange); Salt Run (SR, yellow); and Fort Matanzas (FM, blue). Mean spat per shell in all regions for each year (<b>B</b>) of the study. Group means (raw and untransformed) are represented by the large black dots with the mean value presented in a call-out box next to the dot. Each smaller point represents the monthly means per spat tree between 2015 and 2020. Letters indicate Tukey’s post hoc test results and years/regions with differing letters are significantly different from each other (<span class="html-italic">p</span> &lt; 0.001).</p>
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<p>Monthly mean spat per shell with settlement period indicated as the thick dashed line between April and October for the five regions in the Guana–Tolomato–Matanzas estuary: Tolomato River (TR, green); Guana River (GR, pink); Saint Augustine (SA; orange); Salt Run (SR, yellow); and Fort Matanzas (FM, blue) based on data collected from 2015 to 2020.</p>
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<p>Monthly average water quality parameters at the Guana Tolomato Matanzas National Estuarine Research Reserve System-Wide Monitoring Program stations: Pine Island (PI, green), San Sebastian (SS, orange), and Fort Matanzas (FM, blue). Temperature (<b>A</b>), salinity (<b>B</b>), and turbidity (<b>C</b>) are all aggregated from 15 min data from continuous instruments deployed at each site. Chlorophyll <span class="html-italic">a</span> (<b>D</b>) is collected monthly in duplicate at each station as a grab sample. The occurrences of Hurricane Matthew (a), Hurricane Irma (b), and Hurricane Dorian (c) are denoted by lowercase letters and dashed lines.</p>
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<p>Water quality parameters at the Guana Tolomato Matanzas National Estuarine Research Reserve System-Wide Monitoring Program stations: Pine Island (PI, green), San Sebastian (SS, orange), and Fort Matanzas (FM, blue). (<b>A</b>) Monthly minimum salinity (PSU) and (<b>B</b>) monthly maximum turbidity (NTU) between 2015 and 2020. The occurrences of Hurricane Matthew (a), Hurricane Irma (b), and Hurricane Dorian (c) are denoted by lowercase letters and dashed lines.</p>
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8 pages, 1693 KiB  
Article
Expanded Geographical Distribution of Coleomegilla maculata lengi (Coleoptera: Coccinellidae) in North America
by Louis Hesler and Mathew Brust
Insects 2024, 15(5), 305; https://doi.org/10.3390/insects15050305 - 25 Apr 2024
Cited by 1 | Viewed by 1265
Abstract
Several species of lady beetle native to North America have declined in abundance in the last few decades, often accompanied by contractions in their geographic ranges. Coleomegilla maculata lengi is a lady beetle native to North America that is an important predator of [...] Read more.
Several species of lady beetle native to North America have declined in abundance in the last few decades, often accompanied by contractions in their geographic ranges. Coleomegilla maculata lengi is a lady beetle native to North America that is an important predator of pests in various agroecosystems. Its reported range spans the eastern half of the USA, with no sustained decline in abundance or contraction of its range reported. Indeed, we recently collected several individuals of this lady beetle in central USA roughly 500 km beyond the western edge of its reputed range. We hypothesized that new records could indicate either that previous range characterization failed to include pre-existing collection records further west or that C. maculata lengi has recently expanded its geographic range. To test these hypotheses, we searched several institutional insect collections and digital databases for records and found many earlier records of C. maculata lengi beyond its reputed geographic range, clearly showing that the previous characterization of its geographic distribution in North America was substantially underestimated. In addition, we report a new state record of C. maculata lengi from Wyoming, USA, that further indicates its geographic range expansion in North America. We discuss new records of C. maculata lengi in light of declines in native coccinelline lady beetle species in North America. Full article
(This article belongs to the Special Issue Diversity and Abundance of Predators and Parasitoids of Insect Pests)
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<p><span class="html-italic">Coleomegilla maculata lengi</span> consuming eggs of Colorado potato beetle, <span class="html-italic">Leptinotarsa decemlineata</span> (<b>A</b>); pollen of buckwheat, <span class="html-italic">Fagopyrum esculentum</span> (<b>B</b>); and dandelion, <span class="html-italic">Taraxacum officianale</span> (<b>C</b>). Photo credits: Peggy Greb (<b>A</b>), Jim Eklund (<b>B</b>), and Eric Beckendorf (<b>C</b>), all USDA-ARS.</p>
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<p>Distribution of <span class="html-italic">Coleomegilla maculata lengi</span> (gray shading, eastern North America; Gordon 1985). Original figure used by permission of the New York Entomological Society.</p>
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<p>Counties in central USA with collection records of <span class="html-italic">Coleomegilla maculata lengi</span>. Numbers depict decades of the first pre-1980 collection record in a county west of the reputed distribution. Dots depict counties with recent collection records: brown, 2008, Pennington Co., SD; red, 2010 and 2011, Dawes Co., NE; and yellow, Goshen Co., WY, 2014. Dashed line indicates western edge of reputed range in 1985. Blue line demarcates eastern and western portions of records area. ND = North Dakota, SD = South Dakota, NE = Nebraska, KS = Kansas, WY = Wyoming.</p>
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