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Search Results (430)

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18 pages, 1908 KiB  
Article
A Decade of Protecting Insect Biodiversity: The Impact of Multifunctional Margins in an Intensive Vegetable System
by Francisco Javier Peris-Felipo, Fernando Santa, Oscar Aguado-Martin, Ana Lia Gayan-Quijano, Rodrigo Aguado-Sanz, Luis Miranda-Barroso and Francisco Garcia-Verde
Insects 2025, 16(2), 118; https://doi.org/10.3390/insects16020118 - 24 Jan 2025
Viewed by 352
Abstract
The intensification of agriculture over the past 80 years has led to significant changes in farm management, resulting in the creation of large-scale fields and the elimination of ecological structural elements. The loss of these areas has dramatically affected natural communities. This study [...] Read more.
The intensification of agriculture over the past 80 years has led to significant changes in farm management, resulting in the creation of large-scale fields and the elimination of ecological structural elements. The loss of these areas has dramatically affected natural communities. This study aimed to test whether the implementation of floral margins generates significant differences in insect abundance over time. The study was carried out on an intensive vegetable farm in Spain over a ten-year period (2013–2022) where a floral margin was sown and maintained over the years. The results showed a clear linear increase in insect individuals, with a total increase of 403.33% from 2013 to 2022. The number of species increased by 138.80% overall, with most growth occurring in the first three years before stabilising (0.63% increase from 2016 to 2022). The analysis of community structure demonstrates a gradual evolution in the insect population dynamics aligned significantly with both log-series and log-normal distributions (p-value > 0.05). This long-term study demonstrates that floral margins are an essential tool for fostering insect biodiversity in intensive agricultural areas. The steady, rather than abrupt, shift in the ecosystem suggests that sustained implementation of floral margins can effectively prevent or reverse insect decline over time. Full article
(This article belongs to the Section Insect Ecology, Diversity and Conservation)
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<p>Floral margin on a farm in Águilas (Murcia) and its location in Spain.</p>
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<p>Scatterplot of the number of species and insects across the years. (<b>a</b>) Number of species. (<b>b</b>) Number of insects.</p>
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<p>Scatterplot of the α-diversity indices: Shannon’s <span class="html-italic">H</span> (<b>a</b>), species richness (<b>b</b>), and Pielou’s evenness <span class="html-italic">J</span> across years (<b>c</b>).</p>
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<p>Correlation matrices of the number of species and insects between years. (<b>a</b>) Number of species. (<b>b</b>) Number of insects.</p>
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<p>Changes of the species by abundance classes throughout the study (the arrows indicate the direction of change).</p>
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19 pages, 7452 KiB  
Article
Responses of Typical Riparian Vegetation to Annual Variation of River Flow in a Semi-Arid Climate Region: Case Study of China’s Xiliao River
by Xiangzhao Yan, Wei Yang, Zaohong Pu, Qilong Zhang, Yutong Chen, Jiaqi Chen, Weiqi Xiang, Hongyu Chen, Yuyang Cheng and Yanwei Zhao
Land 2025, 14(1), 198; https://doi.org/10.3390/land14010198 - 19 Jan 2025
Viewed by 719
Abstract
In semi-arid basins, riparian vegetation is an important part of the river ecosystem. However, with the decrease in river runoff caused by human activities and the continuous changes in climate, riparian vegetation has gradually degraded. To identify the main influencing factors of riparian [...] Read more.
In semi-arid basins, riparian vegetation is an important part of the river ecosystem. However, with the decrease in river runoff caused by human activities and the continuous changes in climate, riparian vegetation has gradually degraded. To identify the main influencing factors of riparian vegetation changes, we extracted the river flow indicators, climate indicators, and riparian vegetation indicators of a Xiliao River typical section from 1985 to 2020 in spring and summer, and established a random forest model to screen the key driving factors of riparian vegetation. Then, we simulated the response characteristics of riparian vegetation to the key driving factors in spring and summer based on nonlinear equations. The results showed that the contribution of river flow factors to riparian vegetation was higher than that of climate factors. In spring, the key driving factors of riparian vegetation were the average flow in May and the average flow from March to May; in summer, the key driving factors were the average flow in May, the maximum 90-day average flow, and the average flow from March to August. Among them, the average flow in May contributed more than 50% to the indicators of riparian vegetation in both spring and summer. The final conclusion is that in the optimal growth range of plants, increasing the base flow and pulse flow of rivers will promote seed germination and plant growth, but when the river flow exceeds this threshold, vegetation growth will stagnate. The research results improve the existing knowledge of the influencing factors of riparian vegetation in semi-arid basins, and provide a reference for improving the natural growth of riparian vegetation and guiding the ecological protection and restoration of rivers in semi-arid areas. Full article
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<p>Geographical location of study area and image of surrounding terrain.</p>
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<p>Significance analysis for vegetation indicators and driving factors in riparian zones in May. Abbreviations: <span class="html-italic">CP</span>, cumulative precipitation; <span class="html-italic">CSR</span>, cumulative solar radiation; <span class="html-italic">CST</span>, cumulative surface temperature; <span class="html-italic">FVC</span>, fractional vegetation cover; k<span class="html-italic">NDVI</span>, kernel normalized-difference vegetation index; <span class="html-italic">NPP</span>, net primary production.</p>
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<p>Significance analysis for vegetation indicators and driving factors in the riparian zones in August. Abbreviations: <span class="html-italic">CP</span>, cumulative precipitation; <span class="html-italic">CSR</span>, cumulative solar radiation; <span class="html-italic">CST</span>, cumulative surface temperature; <span class="html-italic">FVC</span>, fractional vegetation cover; k<span class="html-italic">NDVI</span>, kernel normalized-difference vegetation index; <span class="html-italic">NPP</span>, net primary production.</p>
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<p>Fitting results for relationship between riparian vegetation indicators and key driving factors in May: (<b>a</b>) kernel normalized-difference vegetation index (k<span class="html-italic">NDVI</span>); (<b>b</b>) fractional vegetation cover (<span class="html-italic">FVC</span>); (<b>c</b>) net primary production (<span class="html-italic">NPP</span>). All regressions were statistically significant (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Fitting results for relationships between riparian vegetation indicators and key driving factors in August: (<b>a</b>) kernel normalized-difference vegetation index (k<span class="html-italic">NDVI</span>); (<b>b</b>) fractional vegetation cover (<span class="html-italic">FVC</span>); (<b>c</b>) net primary production (<span class="html-italic">NPP</span>). All regressions were statistically significant (<span class="html-italic">p</span> &lt; 0.05).</p>
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30 pages, 5648 KiB  
Article
Sub-District Level Spatiotemporal Changes of Carbon Storage and Driving Factor Analysis: A Case Study in Beijing
by Yirui Zhang, Shouhang Du, Linye Zhu, Tianzhuo Guo, Xuesong Zhao and Junting Guo
Land 2025, 14(1), 151; https://doi.org/10.3390/land14010151 - 13 Jan 2025
Viewed by 488
Abstract
Analyzing the current trends and causes of carbon storage changes and accurately predicting future land use and carbon storage changes under different climate scenarios is crucial for regional land use decision-making and carbon management. This study focuses on Beijing as its study area [...] Read more.
Analyzing the current trends and causes of carbon storage changes and accurately predicting future land use and carbon storage changes under different climate scenarios is crucial for regional land use decision-making and carbon management. This study focuses on Beijing as its study area and introduces a framework that combines the Markov model, the Patch-based Land Use Simulation (PLUS) model, and the Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) model to assess carbon storage at the sub-district level. This framework allows for a systematic analysis of land use and carbon storage spatiotemporal evolution in Beijing from 2000 to 2020, including the influence of driving factors on carbon storage. Moreover, it enables the simulation and prediction of land use and carbon storage changes in Beijing from 2025 to 2040 under various scenarios. The results show the following: (1) From 2000 to 2020, the overall land use change in Beijing showed a trend of “Significant decrease in cropland area; Forest increase gradually; Shrub and grassland area increase first and then decrease; Decrease and then increase in water; Impervious expands in a large scale”. (2) From 2000 to 2020, the carbon storage in Beijing showed a “decrease-increase” fluctuation, with an overall decrease of 1.3 Tg. In future carbon storage prediction, the ecological protection scenario will contribute to achieving the goals of carbon peak and carbon neutrality. (3) Among the various driving factors, slope has the strongest impact on the overall carbon storage in Beijing, followed by Human Activity Intensity (HAI) and Nighttime Light Data (NTL). In the analysis of carbon storage in the built-up areas, it was found that HAI and DEM (Digital Elevation Model) have the strongest effect, followed by NTL and Fractional Vegetation Cover (FVC). The findings from this study offer valuable insights for the sustainable advancement of ecological conservation and urban development in Beijing. Full article
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<p>Location of the study area. Hebei–Beijing location map (<b>a</b>), Beijing location map (<b>b</b>), and remote sensing image of Beijing (<b>c</b>).</p>
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<p>Flowchart of this study.</p>
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<p>Land use map of Beijing from 2000 to 2020.</p>
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<p>Conversion between various land use types in Beijing from 2000 to 2020.</p>
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<p>Changes in the amount of various carbon storage and the total carbon storage in Beijing from 2000 to 2020.</p>
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<p>Changes in carbon storage in various regions of Beijing, 2000–2020.</p>
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<p>Spatial distribution of carbon density in Beijing from 2000 to 2020.</p>
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<p>Standard deviation ellipse result. The change in the middle point represents the shift in the center of gravity of the carbon storage.</p>
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<p>Results of carbon storage changes of different sub-districts using the Sen + MK model.</p>
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<p>Result of the factors’ impact on overall carbon storage in Beijing.</p>
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<p>Result of the factors’ impact on carbon storage in the built-up areas of Beijing.</p>
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<p>Result of the factors’ impact on carbon storage in Beijing by GTWR.</p>
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<p>Spatial distribution prediction under three scenarios of land use in Beijing in 2025–2040.</p>
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23 pages, 7550 KiB  
Article
Spatiotemporal Changes in Evapotranspiration and Its Influencing Factors in the Jiziwan Region of the Yellow River from 1982 to 2018
by Wenting Liu, Rong Tang, Ge Zhang, Jiacong Xue, Baolin Xue and Yuntao Wang
Remote Sens. 2025, 17(2), 252; https://doi.org/10.3390/rs17020252 - 12 Jan 2025
Viewed by 443
Abstract
Evapotranspiration (ET) is a critical process in the interaction between the terrestrial climate system and vegetation. In recent years, ET has undergone significant changes in the Jiziwan region of the Yellow River Basin, primarily due to the implementation of ecological restoration programs and [...] Read more.
Evapotranspiration (ET) is a critical process in the interaction between the terrestrial climate system and vegetation. In recent years, ET has undergone significant changes in the Jiziwan region of the Yellow River Basin, primarily due to the implementation of ecological restoration programs and the dual impacts of climate change. As a result, hydrological cycle processes have been profoundly affected, making it crucial to accurately capture trends in ET and its components, as well as to identify the key drivers of these changes. In this study, we first systematically analyzed the dynamic evolution of ET and its components in the Jiziwan of the Yellow River area between 1982 and 2018 from the perspective of land use change. To achieve accurate ET simulations, we introduced a multiple linear regression algorithm and quantitatively evaluated the specific contributions of five climate factors, including precipitation, temperature, wind speed, specific humidity, and radiation, as well as the normalized difference vegetation index (NDVI), a vegetation factor, to ET and its components. On this basis, we explored the combined influence mechanism of climate change and vegetation change on ET in detail. The results revealed that the structure of ET in the Jiziwan of the Yellow River area has changed significantly and that vegetation evapotranspiration has gradually replaced soil evaporation, occupies a dominant position, and has become the main component of ET in this area. Among the many factors affecting ET, the contribution of climate change is the most significant, with an average contribution rate of approximately 59%. Moreover, the influence of human activities on total ET and its components is also high. The factors that had the greatest impact on total ET, soil evaporation, and vegetation transpiration were precipitation, radiation, and the NDVI, respectively. In terms of spatial distribution, the eastern part of Jiziwan was more significantly affected by environmental changes, and the trends of the ET changes were more dramatic. This study not only enhances our scientific understanding of the changes in ET and their driving mechanisms in the Jiziwan area of the Yellow River but also provides a solid scientific foundation for the development of water resource management and ecological restoration strategies in the region. Full article
(This article belongs to the Special Issue Quantitative Remote Sensing of Vegetation and Its Applications)
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<p>Map of the study area.</p>
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<p>Schematic representation of the method.</p>
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<p>(<b>a</b>,<b>b</b>) Verification of the accuracy of GLEAM data at flux sites; (<b>c</b>) verification of the accuracy of the GLEAM data versus the simulated values of evapotranspiration, expressed as R<sup>2</sup>.</p>
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<p>Interannual trends in evapotranspiration and its components in the Jiziwan area.</p>
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<p>Annual average and trend of evapotranspiration and its components in the Jiziwan area of the Yellow River. Subplots (<b>a</b>–<b>d</b>) show the annual average spatial patterns of ET, Es, Ei, and Ec, respectively, and subplots (<b>e</b>–<b>h</b>) display their corresponding annual trends.</p>
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<p>Changes in land use area in Jiziwan, Yellow River Basin, 1985–2020.</p>
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<p>Sankey diagram of the land use transfer matrix for 1985–2020 in the Jiziwan area.</p>
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<p>Interannual changes in ET for different land cover types, 1985–2020.</p>
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<p>Spatial distributions of the effects of climate and vegetation factors and nonvegetated subsurface factors on ET and its components. Subplots (<b>a</b>–<b>d</b>) illustrate the influence of climatic and vegetation factors on evapotranspiration and its components, while subplots (<b>e</b>–<b>h</b>) represent the influence of non-vegetation underlying surface factors on evapotranspiration and its components.</p>
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<p>Spatial distributions of the relative contributions of ET and its component drivers. The (<b>a</b>–<b>d</b>), (<b>e</b>–<b>h</b>), and (<b>i</b>–<b>l</b>) of subplots represent the impacts of climate change, vegetation change, and other factors on evapotranspiration and its components, respectively.</p>
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<p>Spatial distributions of the relative contributions of meteorological factors to ET and its components. The (<b>a</b>–<b>d</b>), (<b>e</b>–<b>h</b>), (<b>i</b>–<b>l</b>), (<b>m</b>–<b>p</b>) and (<b>q</b>–<b>t</b>) of subplots represent the contributions of temperature, precipitation, wind speed, specific humidity, and radiation to evapotranspiration and its components, respectively, with values ranging from 0 to 100.</p>
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<p>Contribution of ET and its components to influencing factors. (<b>a</b>–<b>c</b>) illustrate the differences in the dominant factors of E, Es, and Ec.</p>
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<p>Plot of the NDVI and its trend during the study period in the Jiziwan area.</p>
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23 pages, 12794 KiB  
Article
Effects of Forest Swamp Succession and Soil Depth on Distribution Pattern of Soil Nematode Communities
by Liqiang Xuan, Lina Che and Luhe Wan
Forests 2025, 16(1), 133; https://doi.org/10.3390/f16010133 - 12 Jan 2025
Viewed by 633
Abstract
The forest swamp ecosystem, as a special wetland ecosystem, is a key link in the material cycle and an important carbon sink in the carbon cycle. The global carbon cycle is of great significance, but the impact of forest swamp succession and soil [...] Read more.
The forest swamp ecosystem, as a special wetland ecosystem, is a key link in the material cycle and an important carbon sink in the carbon cycle. The global carbon cycle is of great significance, but the impact of forest swamp succession and soil depth on soil active organic matter and nematode community structure and diversity is unclear. This study used the “space instead of time” method to investigate the succession process of forest swamps from grasslands (WC) and shrubs (WG) to forests (WS) in national nature reserves. The results showed that during the forest succession process, the dominant nematode communities in the WC and WG stages were dominated by the genera Apis and Labroidei, while the dominant genera increased in the WS stage. The total abundance of nematodes increased, and the number of groups was ordered WG > WC > WS. The diversity in soil nematode communities according to Shannon–Wiener (H′), Pielou (J), and Trophic diversity (TD) was WS > WG > WC, which is related to vegetation, soil physical and chemical properties, and microbial community structure. The maturity index (MI) was WG > WS > WC. The soil food web was dominated by bacterial channels and had characteristics in forest metabolic activity and regulation ability. At different soil depths, there were significant differences in the community, with species such as the spiny cushioned blade genus being key. The number and group size of nematodes varied from 0–10 cm > 10–20 cm > 20–30 cm. The relative abundance of feeding nematodes changed with depth, while diversity indices such as H′, J, and TD decreased with depth. Ecological function indices such as MI and PPI showed depth variation patterns, while basic indices (BI) and channel indices (CI) showed significant differences. In terms of soil variables, during the forest succession stage, soil organic carbon (SOC), soluble organic nitrogen (DON), easily oxidizable organic carbon (ROC), microbial biomass carbon (MBC), and microbial biomass nitrogen (MBN) showed a gradually increasing trend with WC-WG-WS, while total nitrogen (TN), soluble organic carbon (DOC), soil temperature (ST), and soil moisture (SM) showed opposite changes. There were significant differences in soil ST, SM, and DON values with succession (p < 0.05). At different soil depths, except for DON and ROC, which increased first and then decrease with depth, the values of other physical and chemical factors and active carbon and nitrogen components at depths of 0–10 cm were higher than those at other depths and decreased with depth. An analysis of variance showed significant differences in MBC and MBN values at different soil depths (p < 0.05), which is of great significance for a deeper understanding of the mechanism of soil nematode community construction and its relationship with the environment. Full article
(This article belongs to the Section Forest Soil)
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<p>Location of study area.</p>
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<p>The difference of nematode community structure at different forest succession stages and depths: (<b>A</b>) quantitative composition of nematode communities at different successional stages; (<b>B</b>) composition of nematode communities at different soil depths; (<b>C</b>) differences in soil nematode community structure at different succession stages; (<b>D</b>) differences in nematode community structure at different soil depths; WC: grassy meadow; WG: shrub; WS: forest; different depths: 0–10 cm, 10–20 cm, and 20–30 cm; Tenu: <span class="html-italic">Tenunemellus</span>; Tyle1: <span class="html-italic">Tylenchus</span>; Cosl: <span class="html-italic">Coslenchus</span>; Agle: <span class="html-italic">glenchus</span>; Bole: <span class="html-italic">Boleodorus</span>; Male: <span class="html-italic">Malenchus</span>; Parl: <span class="html-italic">Ptylenchus</span>; Pale: <span class="html-italic">Pararotylenchus</span>; Dity: <span class="html-italic">Ditylenchus</span>; Aphe1: <span class="html-italic">Aphelenchus</span>; Aphe2: <span class="html-italic">Aphelenchoides</span>; Ceph: <span class="html-italic">Cephalobus</span>; Pana: <span class="html-italic">Panagrolaimus</span>; Tera: <span class="html-italic">Teratocephalus</span>; Eute: <span class="html-italic">Euteratocephalus</span>; Laim: <span class="html-italic">Laimydorus</span>; Eula: <span class="html-italic">Eudorylaimus</span>; Epla: <span class="html-italic">Epidorylaimus</span>; Thon: <span class="html-italic">Thonus</span>; Labr: <span class="html-italic">Labronema</span>; Long: <span class="html-italic">Longidorella</span>; Park: <span class="html-italic">Parkellus</span>; Nygo: <span class="html-italic">Nygolaimus</span>; Apor: <span class="html-italic">porcelaimellus</span>; Tyle2: <span class="html-italic">Tylencholaimus</span>; Para: <span class="html-italic">Paratrichodorus</span>; Tric: <span class="html-italic">Trichodorus</span>; Pris: <span class="html-italic">Prismatolaimus</span>; Alai: <span class="html-italic">Alaimus</span>; Trip: <span class="html-italic">Tripyla</span>; Bast: <span class="html-italic">Bastiania</span>; Anap: <span class="html-italic">Anaplectus</span>; Plec: <span class="html-italic">Plectus</span>; Wils: <span class="html-italic">Wilsonema</span>.</p>
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<p>The distribution characteristics of nematode communities and groups in different succession sequences and different soil depths were as follows: (<b>A</b>) total number of nematodes in different succession stages; (<b>B</b>) number of genera of nematodes in different successional stages; (<b>C</b>) total number of nematodes at different soil depths; (<b>D</b>) number of nematode genera in different soil depths; WC: grassy meadow; WG: shrub; WS: forest; different depths: 0–10 cm, 10–20 cm, and 20–30 cm; different lowercase letters indicate a significant difference in soil depth and forest succession stage (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>The relative abundance of nematode trophic groups at different succession stages and different soil depths: (<b>A</b>) relative abundance of trophic groups at different succession stages; (<b>B</b>) relative abundance of different soil depth nutrient groups; WC: grassy meadow; WG: shrub; WS: forest; different depths: 0–10 cm, 10–20 cm, and 20–30 cm; PP: plant parasites; BF: bacterivores; FF: fungivores; OP: predators–omnivores; the difference between different letters of the same color is significant (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Soil nematode community diversity in different stages of forest succession and at different soil depths: (<b>A</b>–<b>C</b>) soil nematode community ecological indices at different succession stages and different soil depths; (<b>D</b>–<b>F</b>) ecological indices of soil nematode communities at different depths; WC: grassy meadow; WG: shrub; WS: forest; different depths: 0–10 cm, 10–20 cm, and 20–30 cm; H′: Hannon–Wiener; λ: Simpson; J: Pielou; SR: Margalef; TD: trophic diversity; MI: free nematode maturity index; PPI: plant-parasitic nematode index; NCR: nematode channel index; WI: Wasilewska index; BI: basal index; EI: enrichment index; SI: structure index; CI: channel index; the difference among different lowercase letters is significant at <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Metabolic footprints of nematode communities at different forest succession stages and different soil depths: (<b>a</b>) metabolic footprints of different forest succession nematodes; (<b>b</b>) metabolic footprints of nematodes at different soil depths; (<b>c</b>) floristic analysis of metabolic footprints of nematodes at different successional stages; (<b>d</b>) floristic analysis of the metabolic footprint of nematodes at different soil depths. WC: grassy meadow; WG: shrub; WS: forest; different depths: 0–10 cm, 10–20 cm, and 20–30 cm; BFMF: bacterial feeder metabolic footprint; FFMF: fungal feeder metabolic footprint; PPMF: plant parasite metabolic footprint; OPMF: omnivore–predator metabolic footprint; TNMF: complex metabolic footprint; Fe: integrated metabolic footprint; Fs: structural metabolic footprint; FMF: functional metabolic footprint; In figures (<b>c</b>,<b>d</b>) (A–D represents different quadrants). The difference among different lowercase letters is significant at <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Redundancy analysis of nematode communities and organic carbon components and physicochemical properties at different succession stages and depths: ((<b>A</b>): WC), ((<b>B</b>): WG), and ((<b>C</b>): WG): WS represents correlations of organic carbon components and physicochemical properties at different succession stages; ((<b>D</b>): 0–10 cm), ((<b>E</b>): 10–20 cm), and ((<b>F</b>): 20–30 cm) represent correlations of organic carbon components and physicochemical properties at different stages; the species and physical and chemical properties of nematode communities are the same as those in <a href="#forests-16-00133-f002" class="html-fig">Figure 2</a> and <a href="#forests-16-00133-f006" class="html-fig">Figure 6</a>.</p>
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<p>Mantel test of the relationship between community structure and diversity of soil nematodes, metabolic footprint, and soil physicochemical properties. Environmental drivers of soil nematode community structure and diversity assessed by partial Mantel tests based on Bray–Curtis distance. Pairwise comparisons of environmental and biological factors are shown in the lower left area; the width and color of the edges represent Mantel’s R-value and statistical significance, respectively; and pairwise Pearson correlations between environmental factors are represented by color gradients. Ns: nematode community structure; Nd: nematode community diversity; Nnd: nematode nutritional diversity; Nlhd: nematode life history diversity; Fdn: functional diversity of nematode; Lhmf: life history metabolic footprint; Nmf: nutritional metabolic footprint; ((<b>A</b>): WC), ((<b>B</b>): WG), and ((<b>C</b>): WG): WS represents correlations of organic carbon components and physicochemical properties at different succession stages; ((<b>D</b>): 0–10 cm), ((<b>E</b>): 10–20 cm), and ((<b>F</b>): 20–30 cm) represent correlations of organic carbon components and physicochemical properties at different stages; the physical and chemical properties are as shown in <a href="#forests-16-00133-f006" class="html-fig">Figure 6</a>.</p>
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25 pages, 30285 KiB  
Article
The Analysis of Spatiotemporal Changes in Vegetation Coverage and Driving Factors in the Historically Affected Manganese Mining Areas of Yongzhou City, Hunan Province
by Jinbin Liu, Zexin He, Huading Shi, Yun Zhao, Junke Wang, Anfu Liu, Li Li and Ruifeng Zhu
Land 2025, 14(1), 133; https://doi.org/10.3390/land14010133 - 10 Jan 2025
Viewed by 544
Abstract
Manganese ore, as an important strategic metal resource for the country, was subject to unreasonable mining practices and outdated smelting technologies in early China, leading to severe ecological damage in mining areas. This study examines the trends in vegetation cover change in the [...] Read more.
Manganese ore, as an important strategic metal resource for the country, was subject to unreasonable mining practices and outdated smelting technologies in early China, leading to severe ecological damage in mining areas. This study examines the trends in vegetation cover change in the historical manganese mining areas of Yongzhou under the influence of policy, providing technical references for mitigating the ecological impact of these legacy mining areas and offering a basis for adjusting mine restoration policies. This paper takes the manganese mining area in Yongzhou City, Hunan Province as a case study and selects multiple periods of Landsat satellite images from 2000 to 2023. By calculating the Normalized Difference Vegetation Index (NDVI) and the Fractional Vegetation Coverage (FVC), the spatiotemporal changes and driving factors of vegetation coverage in the Yongzhou manganese mining area from 2000 to 2023 were analyzed. The analysis results show that, in terms of time, from 2000 to 2012, the vegetation coverage in the manganese mining area decreased from 0.58 to 0.21, while from 2013 to 2023, it gradually recovered from 0.21 to 0.40. From a spatial perspective, in areas where artificial reclamation was conducted, the vegetation was mainly mildly and moderately degraded, while in areas where no artificial restoration was carried out, significant vegetation degradation was observed. Mining activities were the primary anthropogenic driving force behind the decrease in vegetation coverage, while effective ecological protection projects and proactive policy guidance were the main anthropogenic driving forces behind the increase in vegetation coverage in the mining area. Full article
(This article belongs to the Section Land Environmental and Policy Impact Assessment)
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<p>The geographic location of the study area.</p>
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<p>Map for classifying the vegetation coverage in the study area from 2000 to 2023.</p>
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<p>Trend of changes in the vegetation coverage in manganese mining areas from 2000 to 2023.</p>
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<p>Map for classifying the vegetation coverage changes in a typical manganese mining area from 2000 to 2012 (reference area (<b>top</b>); typical manganese mining area (<b>middle</b> and <b>bottom</b>)).</p>
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<p>Map for classifying vegetation coverage changes in a typical manganese mining area from 2013 to 2023 (reference area (<b>top</b>); typical manganese mining area (<b>middle</b> and <b>bottom</b>).</p>
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<p>Imagery of a typical mining area from 2015 (<b>left</b>) and 2022 (<b>right</b>).</p>
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<p>Imagery of the untreated manganese mining area from 2012 (<b>left</b>) and 2022 (<b>right</b>).</p>
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<p>The spatial evolution trend of vegetation cover in the manganese mining area from 2000 to 2012.</p>
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<p>The spatial evolution trend of vegetation cover in the manganese mining area from 2012 to 2023.</p>
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<p>Changes in temperature and precipitation in Yongzhou City from 2000–2022.</p>
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<p>Curve showing the comparison of Fractional Vegetation Coverage (FVC) values between manganese mining areas and the reference area.</p>
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<p>Correlation between FVC and natural factors.</p>
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14 pages, 2263 KiB  
Article
Five Years of Natural Vegetation Recovery in Three Forests of Karst Graben Area and Its Effects on Plant Diversity and Soil Properties
by Xiaorong Yang, Rouzi-Guli Turmuhan, Lina Wang, Jiali Li and Long Wan
Forests 2025, 16(1), 91; https://doi.org/10.3390/f16010091 - 8 Jan 2025
Viewed by 419
Abstract
In recent decades, excessive human activities have led to large-scale rocky desertification in karst areas. Vegetation restoration is one of the most important ways to control rocky desertification. In this study, vegetation surveys were conducted on three typical plantations in Jianshui County, Yunnan [...] Read more.
In recent decades, excessive human activities have led to large-scale rocky desertification in karst areas. Vegetation restoration is one of the most important ways to control rocky desertification. In this study, vegetation surveys were conducted on three typical plantations in Jianshui County, Yunnan Province, a typical karst fault basin area, in 2016 and 2021. The plantations were Pinus massoniana forest (PM), Pinus yunnanensis forest (PY), and mixed forests of Pinus yunnanensis and Quercus variabilis (MF). Plant diversity and soil nutrients were compared during the five-year period. This paper mainly draws the following results: The plant diversity of PM, PY, and MF increased. With the increase of time, new species appeared in the tree layer, shrub layer, and herb layer of the three forests. Tree species with smaller importance values gradually withdrew from the community. In the tree layer, the Patrick index, Simpson index, and Shannon–Wiener index of the three forests increased significantly. The Pielou index changed from the highest for PM in 2016 to the highest for PY in 2021. In the shrub layer, the Pielou index of the three forests increased. The Patrick index changed from the highest for MF in 2016 to the highest for PY in 2021. There was no significant difference in species diversity index for the herb layer. With the increase of vegetation restoration time, the soil bulk density (BD) of the three forests decreased. There was no significant difference in soil total porosity (TP), soil capillary porosity (CP), and non-capillary porosity (NCP). The pH of PM increased significantly from 5.88~6.24 to 7.24~7.34. The pH of PY decreased significantly (p < 0.05). The contents of total nitrogen (TN) and ammonium nitrogen (NH4+-N) in PY and MF decreased. The content of nitrate nitrogen (NO3-N) in the three forests increased significantly (p < 0.05). Total phosphorus (TP) content decreased in PM and MF. The content of available phosphorus (AP) in PM and PY increased. In general, with the increase of vegetation restoration time, plant diversity and soil physical and chemical properties have also been significantly improved. The results can provide important data support for vegetation restoration in karst areas. Full article
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<p>Species diversity of plant communities in different restoration years. (<b>a</b>–<b>d</b>): species diversity of tree layer; (<b>e</b>–<b>h</b>): species diversity of shrub layer; (<b>i</b>–<b>l</b>): species diversity of herb layer. Note: PM: <span class="html-italic">Pinus massoniana</span> forest; PY: <span class="html-italic">Pinus yunnanensis</span> forest; MF: mixed forest of <span class="html-italic">Pinus yunnanensis</span> and <span class="html-italic">Quercus variabilis</span>. Capital letters indicate the significance of different forest types in the same year (<span class="html-italic">p</span> &lt; 0.05). * indicates the significance of the same forest types and soil layers in different years (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Soil physical properties of different recovery years in different soil layers. Note: PM: <span class="html-italic">Pinus massoniana</span> forest; PY: <span class="html-italic">Pinus yunnanensis</span> forest; MF: mixed forest of <span class="html-italic">Pinus yunnanensis</span> and <span class="html-italic">Quercus variabilis</span>. (<b>a</b>) BD: bulk density; (<b>b</b>) TP: total porosity; (<b>c</b>) CP: capillary porosity; (<b>d</b>) NCP: non-capillary porosity. Capital letters indicate the significance of different forest types in the same year and soil layers (<span class="html-italic">p</span> &lt; 0.05); small letters indicate the significance of different soil layers in the same year and forest types (<span class="html-italic">p</span> &lt; 0.05); * indicates the significance of the same forest types and soil layers in different years (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Soil chemical properties of different recovery years in different soil layers. Note: PM: <span class="html-italic">Pinus massoniana</span> forest; PY: <span class="html-italic">Pinus yunnanensis</span> forest; MF: mixed forest of <span class="html-italic">Pinus yunnanensis</span> and <span class="html-italic">Quercus variabilis</span>. (<b>a</b>) pH: potential of hydrogen; (<b>b</b>) SOC: soil organic carbon; (<b>c</b>) TN: total nitrogen; (<b>d</b>) NH<sub>4</sub><sup>+</sup>-N: ammonium nitrogen; (<b>e</b>) NO<sub>3</sub><sup>−</sup>-N: nitrate nitrogen; (<b>f</b>) TP: total phosphorus; (<b>g</b>) AP: available phosphorus. Capital letters indicate the significance of different forest types in the same year and soil layers (<span class="html-italic">p</span> &lt; 0.05); small letters indicate the significance of different soil layers in the same year and forest types (<span class="html-italic">p</span> &lt; 0.05); * indicates the significance of the same forest types and soil layers in different years (<span class="html-italic">p</span> &lt; 0.05).</p>
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18 pages, 12209 KiB  
Article
Spatiotemporal Dynamics of Landscape Pattern and Vegetation Ecological Quality in Sanjiangyuan National Park
by Xiangbin Peng, Ruomei Tang, Junjie Li, Huanchen Tang and Zixi Guo
Sustainability 2025, 17(1), 373; https://doi.org/10.3390/su17010373 - 6 Jan 2025
Viewed by 511
Abstract
As one of China’s largest national parks, Sanjiangyuan National Park (SNP) plays a crucial role in preserving ecological security and biodiversity. Conducting a scientific evaluation of dynamic changes in vegetation ecological quality and landscape patterns within the park is essential for ensuring its [...] Read more.
As one of China’s largest national parks, Sanjiangyuan National Park (SNP) plays a crucial role in preserving ecological security and biodiversity. Conducting a scientific evaluation of dynamic changes in vegetation ecological quality and landscape patterns within the park is essential for ensuring its sustainable development and conservation as a national ecological security barrier. This study analyzed the spatial and temporal dynamics of vegetation ecological quality index (VEQI) and Landscape Pattern Metrics (LPM) in SNP using the VEQI model and Fragstats 4.2.1, along with spatial correlation analyses spanning from 2007 to 2022. The findings indicated an overall upward trend in VEQI, with a notable increase of approximately 38.88% over the 15-year period. Particularly in the Yangtze River Source Park, VEQI exhibited the most significant increase, reaching 48.99%. Furthermore, forest and shrub cover types displayed higher VEQI values and demonstrated an increasing trend, signifying significant ecological improvement in these ecosystems. Regarding landscape patterns, patch density (PD) and landscape shape index (LSI) demonstrated an increasing trend, while average patch area and edge density (ED) gradually decreased, indicating a rising level of landscape fragmentation. High values of the largest patch index (LPI) were primarily concentrated in the Lancangjiang source park, the Yellow River source park, and the southern part of the Yangtze River source, suggesting greater ecological connectivity in these regions. Spatial autocorrelation analysis between VEQI and LPM revealed significant spatial heterogeneity. Specifically, VEQI exhibited positive correlations with LPI and mean patch area, while showing negative correlations with PD, ED, PR, TE, NP, and mean shape index. This indicates that areas with lower vegetation ecological quality tend to exhibit higher landscape fragmentation and complexity. The study’s findings highlight the increasing trend in VEQI and changing landscape fragmentation within SNP, offering a scientific foundation for ecological protection policy formulation and sustainable park development. Full article
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<p>Location of the study area (labels “The source of the Yangtze River”, “The source of the Lancang River”, and “The source of the Yellow River” refer to the entire sections of the park associated with these rivers).</p>
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<p>Temporal trends of Vegetation Ecological Quality Index (VEQI) variation between 2007 and 2022 in Sanjiangyuan National Park based on remote sensing data.</p>
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<p>Spatial distribution of Vegetation Ecological Quality Index (VEQI) and Sanjiangyuan National Park from 2007 to 2022.</p>
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<p>Spatial distribution of Landscape Pattern Metrics of Sanjiangyuan National Park from 2007 to 2022, categorized using the Natural Breaks (Jenks) method.</p>
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<p>Correlation Between Changes in Vegetation Ecological Quality Index (VEQI) and Landscape Pattern Metrics in Sanjiangyuan National Park (2007–2022). Note: The <span class="html-italic">y</span>-axis scale does not start at 0 to better highlight trends and variations.</p>
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<p>Local Bivariate LISA agglomeration of Vegetation Ecological Quality Index (VEQI) and Landscape Pattern Metric in 2007–2022.</p>
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25 pages, 27385 KiB  
Article
Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
by Jinrun He, Jinglong Fan, Zhentao Lv and Shengyu Li
Remote Sens. 2025, 17(1), 152; https://doi.org/10.3390/rs17010152 - 4 Jan 2025
Viewed by 594
Abstract
In arid regions, climatic fluctuations significantly affect vegetation structure and function. Sun-induced chlorophyll fluorescence (SIF) can quantify certain physiological parameters of vegetation but has limitations in characterizing responses to climate change. This study analyzed the spatiotemporal differences in response to climate change across [...] Read more.
In arid regions, climatic fluctuations significantly affect vegetation structure and function. Sun-induced chlorophyll fluorescence (SIF) can quantify certain physiological parameters of vegetation but has limitations in characterizing responses to climate change. This study analyzed the spatiotemporal differences in response to climate change across various ecological regions and vegetation types from 2000 to 2020 in Xinjiang. According to China’s ecological zoning, R1 (Altai Mountains-Western Junggar Mountains forest-steppe) and R5 (Pamir-Kunlun Mountains-Altyn Tagh high-altitude desert grasslands) represent two ecological extremes, while R2–R4 span desert and forest-steppe ecosystems. We employed the standardized precipitation evapotranspiration index (SPEI) at different timescales to represent drought intensity and frequency in conjunction with global OCO-2 SIF products (GOSIF) and the normalized difference vegetation index (NDVI) to assess vegetation growth conditions. The results show that (1) between 2000 and 2020, the overall drought severity in Xinjiang exhibited a slight deterioration, particularly in northern regions (R1 and R2), with a gradual transition from short-term to long-term drought conditions. The R4 and R5 ecological regions in southern Xinjiang also displayed a slight deterioration trend; however, R5 remained relatively stable on the SPEI24 timescale. (2) The NDVI and SIF values across Xinjiang exhibited an upward trend. However, in densely vegetated areas (R1–R3), both NDVI and SIF declined, with a more pronounced decrease in SIF observed in natural forests. (3) Vegetation in northern Xinjiang showed a significantly stronger response to climate change than that in southern Xinjiang, with physiological parameters (SIF) being more sensitive than structural parameters (NDVI). The R1, R2, and R3 ecological regions were primarily influenced by long-term climate change, whereas the R4 and R5 regions were more affected by short-term climate change. Natural grasslands showed a significantly stronger response than forests, particularly in areas with lower vegetation cover that are more structurally impacted. This study provides an important scientific basis for ecological management and climate adaptation in Xinjiang, emphasizing the need for differentiated strategies across ecological regions to support sustainable development. Full article
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<p>Study area of the Xinjiang arid region in northwest China (Vegetation is classified as follows: Forest (red), high coverage grassland (HCG, &gt;50%, dark green), moderate coverage grassland (MCG, 20–50%, medium green), and low coverage grassland (LCG, 5–20%, light green). The ecological regions (R1–R5) are delineated with different hatching patterns, and meteorological stations are marked with red dots. The map was created using the standard map approved by the Ministry of Natural Resources of China (review number GS (2024) 0650). The base map provided by the Ministry of Natural Resources was used without any modifications. Similarly, all other maps in this study were created using standardized methods and remain unaltered.</p>
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<p>Technical roadmap for research of vegetation responses to climate change.</p>
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<p>Temporal variation of SPEI in Xinjiang from 2000 to 2020 (<b>a</b>) Temporal variation of SPEI at a 3-month timescale (SPEI-03). (<b>b</b>) Temporal variation of SPEI at a 6-month timescale (SPEI-06). (<b>c</b>) Temporal variation of SPEI at a 12-month timescale (SPEI-12). (<b>d</b>) Temporal variation of SPEI at a 24-month timescale (SPEI-24). Each panel shows the SPEI data series (blue) and trend line (red). Statistical values, including Z-score, <span class="html-italic">p</span>-value, and slope, are provided for each timescale to indicate the trend significance and direction.</p>
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<p>Spatial distribution of multi-year average SPEI in Xinjiang from 2000 to 2020 across different timescales. (<b>a</b>) Spatial distribution of SPEI at a 3-month timescale (SPEI-03). (<b>b</b>) Spatial distribution of SPEI at a 6-month timescale (SPEI-06). (<b>c</b>) Spatial distribution of SPEI at a 12-month timescale (SPEI-12). (<b>d</b>) Spatial distribution of SPEI at a 24-month timescale (SPEI-24). Red areas indicate drier conditions, whereas blue areas represent wetter conditions.</p>
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<p>Inter-annual variation analysis of vegetation NDVI and SIF. (<b>a</b>) Annual mean NDVI with trend line and confidence interval. The trend line (red) represents the linear trend, with the equation y = 0.0012x + 0.1276y = 0.0012x + 0.1276y = 0.0012x + 0.1276 and a correlation coefficient of 0.8929. (<b>b</b>) Annual mean SIF with trend line and confidence interval. The trend line (red) shows the linear trend, with the equation y = 0.0005x + 0.0741y = 0.0005x + 0.0741y = 0.0005x + 0.0741 and a correlation coefficient of 0.7521. Blue triangles represent observed data, and the shaded area indicates the confidence interval around the trend line.</p>
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<p>Spatial distribution of mean NDVI and SIF in Xinjiang from 2000 to 2020. (<b>a</b>) Spatial distribution of mean NDVI, representing vegetation structural conditions across Xinjiang. The color bar indicates NDVI values, with yellow to dark green representing increasing vegetation coverage from 0.0 to 1.0. (<b>b</b>) Spatial distribution of mean SIF, indicating vegetation physiological activity levels. The color bar reflects SIF values, ranging from 0.00 to 0.20 W·m<sup>−</sup><sup>2</sup>·μm<sup>−</sup><sup>1</sup>·sr<sup>−</sup><sup>1</sup>, with dark green areas showing higher fluorescence.</p>
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<p>Spatial distribution of correlation coefficients for NDVI and SIF from 2000 to 2020 in Xinjiang. (<b>a</b>) Spatial distribution of the correlation coefficient between NDVI and SPEI across pixels over the study period. (<b>b</b>) Spatial distribution of the correlation coefficient between SIF and SPEI across pixels over the study period. The color scale represents correlation values from −1 to 1, where blue areas indicate a strong positive correlation and red areas indicate a strong negative correlation. The inset bar chart shows the proportion of pixels with positive and negative correlation trends.</p>
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<p>Spatial distribution and changes in vegetation types from 2000 to 2020 in Xinjiang. (<b>a</b>) Spatial distribution of vegetation types, including forest, high-coverage grassland (HCG), moderate-coverage grassland (MCG), and low-coverage grassland (LCG). (<b>b</b>) Spatial distribution of vegetation change over the study period, identifying common, increased, and decreased areas. The bar chart inserted shows the percentage of each type.</p>
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<p>Trends in NDVI and SIF for grassland and forested areas (2000–2020). For forest areas, NDVI shows a statistically significant increasing trend (y = 0.0017x + 0.5584, Corr. = 0.569), whereas SIF displays a slight decreasing trend (y = −0.0004x + 0.1943, Corr. = −0.2389). For grassland areas, NDVI exhibits a positive trend (y = 0.0017x + 0.194, Corr. = 0.8019), with a minimal increase in SIF (y = 0.0001x + 0.0779, Corr. = 0.0712). The shaded regions indicate the confidence intervals for each regression line.</p>
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<p>Spatial distribution of maximum correlation coefficients (R<sub>max</sub>) between vegetation indices and SPEI in Xinjiang. (<b>a</b>) The spatial distribution of the maximum correlation coefficients (R<sub>max</sub>) between NDVI and SPEI across Xinjiang, with values ranging from −0.372 to 0.745, indicating varying vegetation responses to climatic changes in different ecological regions. (<b>b</b>) The spatial distribution of the maximum correlation coefficients (R<sub>max</sub>) between SIF and SPEI, with values from −0.8 to 0.9. This figure highlights the spatial variation in vegetation sensitivity to drought stress across different regions.</p>
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<p>Maximum correlation coefficients between vegetation indices and SPEI. Box plots depict the distribution of maximum correlation coefficients (R<sub>max</sub>) between NDVI and SIF with SPEI, separated by ecological regions (R1–R5) and vegetation types (Forest, HCG, MCG, and LCG). (<b>a</b>) shows NDVI correlations across ecological regions, whereas (<b>b</b>) displays SIF correlations. (<b>c</b>,<b>d</b>) present NDVI and SIF correlations, respectively, by vegetation type.</p>
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<p>Spatial distribution of the SPEI time scales corresponding to the maximum correlation coefficients between vegetation conditions represented by NDVI (<b>a</b>) and SIF (<b>b</b>) and SPEI. (<b>a</b>) NDVI and (<b>b</b>) SIF are shown with SPEI03, SPEI06, SPEI12, and SPEI24, representing the dominant timescales of vegetation response to drought. This figure illustrates the temporal dynamics of vegetation response to drought stress.</p>
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<p>Area proportion of SPEI time scales corresponding to maximum correlation coefficients between vegetation indices and SPEI across different ecological regions and vegetation types. (<b>a</b>) displays NDVI correlations by region, whereas (<b>b</b>) shows SIF correlations by region. (<b>c</b>,<b>d</b>) present NDVI and SIF correlations, respectively, by vegetation type.</p>
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15 pages, 3699 KiB  
Article
Impact of Coastal Squeeze Induced by Erosion and Land Reclamation on Salt Marsh Wetlands
by Guangzhi Zhang, Jiali Gu, Hao Hu, Maoming Sun, Jie Shao, Weiliang Dong, Liang Liang and Jian Zeng
J. Mar. Sci. Eng. 2025, 13(1), 17; https://doi.org/10.3390/jmse13010017 - 27 Dec 2024
Viewed by 499
Abstract
Salt marshes are declining due to the dual pressures of coastal erosion and land reclamation. However, there remains a lack of quantitative analysis regarding this reduction process and its driving mechanisms. This study examines the dynamics and influencing factors of salt marsh vegetation [...] Read more.
Salt marshes are declining due to the dual pressures of coastal erosion and land reclamation. However, there remains a lack of quantitative analysis regarding this reduction process and its driving mechanisms. This study examines the dynamics and influencing factors of salt marsh vegetation along the eroding coastline of Sheyang County, Jiangsu Province, China, between 1985 and 2020, using remote sensing to analyze changes in artificial coastlines, water boundaries, vegetation front edge, and its topography. Our results showed an extensive seaward movement of artificial coastlines due to reclamation, coupled with severe reductions in salt marsh area and width. Coastal erosion further caused a 10.5% decline in vegetation elevation and a 46.7% increase in slope steepness, amplifying vulnerability to wave action. Native species were largely replaced by Spartina alterniflora, reducing ecological diversity. Currently, human pressure on the landward side has been alleviated; thus, addressing coastal erosion is vital to preventing the further loss of salt marshes. Sediment retention engineering and native vegetation restoration efforts can gradually facilitate the recovery of salt marshes. This study provided critical insights for sustainable coastal management under bidirectional pressures. Full article
(This article belongs to the Section Coastal Engineering)
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<p>Location of the research area ((<b>a</b>): Location of Sheyang County and various ports/estuaries, (<b>b</b>): Location of Sheyang County along the coast of China, (<b>c</b>): North Sheyang Region, (<b>d</b>): South Sheyang Region. The base map is a Sentinel-2 image acquired on 5 August 2020, and the false color composition is based on bands 7, 4, and 3).</p>
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<p>Interannual variation of offshore distance with different boundary lines (based on the 1985 land artificial coastline, (<b>a</b>): land artificial coastline, (<b>b</b>): water boundary, (<b>c</b>): vegetation front edge).</p>
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<p>Average movement rate of different boundary lines from 1985 to 2020 (The left map is a Sentinel-2 image acquired on 5 August 2020, and false color composition is based on bands 7, 4, and 3. Numbers 1 to 7 represent the Biandan port, Kuatao estuary, Shuangyang port, Yunliang estuary, Sheyang estuary, Shagang estuary, and Xinyang port, respectively. Rectangles N and S represent the North Sheyang region and the South Sheyang region. Section ID from small to large represents the Sheyang section from north to south, (<b>a</b>) land artificial shoreline, (<b>b</b>) water boundary, and (<b>c</b>) vegetation front edge).</p>
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<p>Changes in vegetation area of salt marshes outside the artificial coastline in Sheyang County.</p>
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<p>Changes in vegetation width outside the embankment in Sheyang County.</p>
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15 pages, 2536 KiB  
Article
A CiteSpace-Based Analysis of the Impact of Sea-Level Rise and Tropical Cyclones on Mangroves in the Context of Climate Change
by Siyu Liu, Yan Zhu, He Xiao, Jingliang Ye, Tingzhi Yang, Jin Ma and Dazhao Liu
Water 2024, 16(24), 3662; https://doi.org/10.3390/w16243662 - 19 Dec 2024
Viewed by 518
Abstract
This study aims to analyze the impact of sea-level rise and tropical cyclones on mangroves in the context of global climate change from 1993 to 2023, and to explore the development status, co-operative relationships and future trends in this research field. In order [...] Read more.
This study aims to analyze the impact of sea-level rise and tropical cyclones on mangroves in the context of global climate change from 1993 to 2023, and to explore the development status, co-operative relationships and future trends in this research field. In order to analyze future research directions for mangroves in the context of climate, this study also provides an important basis and reference for the development of research related to the mitigation of natural disasters. Using CNKI and the Web of Science as data sources, this study employs the bibliometric tool CiteSpace 6.3 R1 to conduct a quantitative and visual analysis of the research field. The research findings indicate the following: (1) The volume of publications in this field has been increasing year by year; especially since 2010, the rate of increase has accelerated, indicating an increased academic interest in this area. (2) From the authorship maps of the two data sources, it can be observed that the collaboration network is dense, indicating the existence of co-operative relationships among researchers. (3) From the analysis of the keywords, it is evident that, with the rise of artificial intelligence, the focus of keywords has gradually shifted from traditional mangrove mechanism research and ecosystem studies to research on mangroves that integrates big data, artificial intelligence, and high-resolution remote sensing data. (4) As time has progressed, areas of research interest have been shifting from the study of disturbances and damage to mangrove vegetation to the study of mangrove resilience and vulnerability in the context of natural disasters, their carbon sequestration capabilities, and their protective functions against wind and waves. The use of remote sensing technology for the monitoring and conservation of mangroves has emerged as a key area of focus for future research. In future research, there will be a focus on the adaptive capacity of mangroves to varying degrees of sea-level rise and the increasing frequency of tropical cyclones, as well as on what measures can be taken to enhance the resilience of mangrove ecosystems. Quantitative and visual analysis of the development trends in this field can provide a reference for the construction of a disaster monitoring platform for mangroves affected by sea-level rise and tropical cyclones, and can aid the development of research aimed at mitigating the impacts of natural disasters. Furthermore, the integration of remote sensing technology and ecological models can facilitate more detailed research, offering more effective tools and strategies for the conservation and management of mangroves. This approach also provides a reference point for developing a monitoring platform for mangrove disasters associated with sea-level rise and the impact of tropical cyclones. Full article
(This article belongs to the Special Issue Climate Risk Management, Sea Level Rise and Coastal Impacts)
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<p>In the years 1993–2023, the (<b>a</b>) CNKI and (<b>b</b>) Web of Science annual and total number of publications on the impact of sea-level rise and tropical cyclones on mangroves; (<b>c</b>) the annual publication volume and total annual publication volume of tropical cyclones in the context of climate change in the Web of Science.</p>
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<p>A web map of the authors of the article on the impact of sea level rise and tropical cyclones on mangroves for (<b>a</b>) CNKI, and (<b>b</b>) Web of Science; node size is proportional to publication frequency; outer deep red circles represent nodes with larger degree centrality, indicating key nodes with higher publication volume in the network.</p>
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<p>Knowledge map of research hotspot keywords in sea level rise and tropical cyclones in relation to mangrove studies in (<b>a</b>) CNKI and (<b>b</b>) Web of Science; node size is proportional to the frequency of co-citation; the outer dark circle indicates that the node has a larger degree centrality, making it a key node in the network of keywords.</p>
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<p>CNKI research hot keyword timeline diagram; the size of nodes is proportional to their frequency; the graph progresses from left to right, representing the passage of time; deep red circles indicate emergent nodes, signifying a high rate of frequency change within a certain period, to some extent representing shifts in research directions.</p>
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<p>Web of Science study of the key time lines of hot spots; the size of nodes is proportional to their frequency; the graph progresses from left to right, representing the passage of time; deep red circles indicate emergent nodes, signifying a high rate of frequency change within a certain period, to some extent representing shifts in research directions.</p>
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<p>Sea-level rise and the impact of tropical cyclones on mangrove forests and hot spots.</p>
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19 pages, 11809 KiB  
Article
Synergistic Promotion of Direct Interspecies Electron Transfer by Biochar and Fe₃O₄ Nanoparticles to Enhance Methanogenesis in Anaerobic Digestion of Vegetable Waste
by Hongruo Ma, Long Chen, Wei Guo, Lei Wang, Jian Zhang and Dongting Zhang
Fermentation 2024, 10(12), 656; https://doi.org/10.3390/fermentation10120656 - 18 Dec 2024
Viewed by 735
Abstract
When vegetable waste (VW) is used as a sole substrate for anaerobic digestion (AD), the rapid accumulation of volatile fatty acids (VFAs) can impede interspecies electron transfer (IET), resulting in a relatively low biogas production rate. In this study, Chinese cabbage and cabbage [...] Read more.
When vegetable waste (VW) is used as a sole substrate for anaerobic digestion (AD), the rapid accumulation of volatile fatty acids (VFAs) can impede interspecies electron transfer (IET), resulting in a relatively low biogas production rate. In this study, Chinese cabbage and cabbage were selected as the VW substrates, and four continuous stirred tank reactors (CSTRs) were employed. Different concentrations of biochar-loaded nano-Fe3O4(Fe3O4@BC) (100 mg/L, 200 mg/L, 300 mg/L) were added, and the organic loading rate (OLR) was gradually increased during the AD process. The changes in biogas production rate, VFAs, and microbial community structure in the fermentation tanks were analyzed to identify the optimal dosage of Fe3O4@BC and the maximum OLR. The results indicated that at the maximum OLR of 3.715 g (VS)/L·d, the addition of 200 mg/L of Fe3O4@BC most effectively promoted an increase in the biogas production rate and reduced the accumulation of VFAs compared to the other treatments. Under these conditions, the biogas production rate reached 0.658 L/g (VS). Furthermore, the addition of Fe3O4@BC enhanced both the diversity and abundance of bacteria and archaea. At the genus level, the abundance of Christensenellaceae_R-7_group, Sphaerochaeta, and the archaeal genus Thermovirga was notably increased. Full article
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<p>Schematic diagram of IET; the interspecies transfer process of IFT and IHT (<b>a</b>); the interspecies transfer process via conductive substances DIET (<b>b</b>).</p>
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<p>Each of the CSTR reactors used in the experiment was equipped with its own dedicated control and detection system.</p>
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<p>Research roadmap of anaerobic fermentation process.</p>
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<p>The magnetic separation effect of Fe₃O₄@BC (after completely mixing the nanoparticles with water, placing a magnet at the bottom, and allowing it to stand for 5 min to observe the effect).</p>
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<p>(<b>a</b>) XRD patterns of the Fe<sub>3</sub>O<sub>4</sub>@BC nanospheres samples; (<b>b</b>) magnetic hysteresis loops of Fe<sub>3</sub>O<sub>4</sub>@BC nanospheres samples.</p>
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<p>FT-IR spectra of Fe₃O₄@BC.</p>
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<p>SEM images of the (<b>a</b>,<b>b</b>) Fe<sub>3</sub>O<sub>4</sub>@BC; (<b>c</b>) energy dispersive spectroscopy (EDS) spectra; (<b>d</b>) EDS elemental analysis.</p>
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<p>Daily biogas production and OLR of anaerobic fermentation of vegetable waste.</p>
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<p>Cumulative total biogas production of VW in different experimental groups.</p>
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<p>(<b>a</b>) Methane content in different experimental groups; (<b>b</b>) Change rate of methane content in different experimental groups.</p>
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<p>(<b>a</b>) pH change graph in different experimental groups; (<b>b</b>) VFAs concentration graph in different experimental groups.</p>
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<p>(<b>a</b>) pH change graph in different experimental groups; (<b>b</b>) VFAs concentration graph in different experimental groups.</p>
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<p>The abundance of bacterial communities at phylum and genus levels in different experimental groups.</p>
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<p>The abundance of archaeal communities at phylum and genus levels in different experimental groups.</p>
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<p>The abundance of archaeal communities at phylum and genus levels in different experimental groups.</p>
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13 pages, 5690 KiB  
Article
Assessment of Green Space Dynamics Under Urban Expansion of Senegalese Cities: The Case of Dakar
by Mariama Cissé, Oluwole Morenikeji, Elke Mertens, Awa Niang Fall and Appollonia Aimiosino Okhimamhe
Urban Sci. 2024, 8(4), 258; https://doi.org/10.3390/urbansci8040258 - 18 Dec 2024
Viewed by 657
Abstract
Senegalese cities have experienced rapid urbanisation, leading to profound landscape changes. Dakar, one of Senegalese’s fastest-growing cities, is experiencing rapid urban expansion, significantly reducing green spaces. These green spaces, essential for urban sustainability and resilience, have become increasingly scarce, affecting the city’s environment [...] Read more.
Senegalese cities have experienced rapid urbanisation, leading to profound landscape changes. Dakar, one of Senegalese’s fastest-growing cities, is experiencing rapid urban expansion, significantly reducing green spaces. These green spaces, essential for urban sustainability and resilience, have become increasingly scarce, affecting the city’s environment and the quality of life for its residents. This study aims to assess the spatiotemporal changes in Dakar’s green spaces from 1990 to 2022. Using satellite imagery, this study produces land use maps to quantify green space coverage over the years. The results show a gradual decline in green spaces in Dakar between 1990 and 2022. In 1990, green spaces covered an estimated 13.36% of Dakar’s area, which decreased significantly to 9.54% by 2022. In contrast, other land uses, such as built-up areas, increased significantly over this period, rising from 19.23% in 1990 to 39.34% in 2022. Moreover, built-up areas are not the sole contributor to the reduction of green spaces in Dakar. The study revealed that, between 1990 and 2022, 5.49% of green spaces were converted into bare soil due to excessive tree cutting. This pattern highlights the growing challenge of green space availability as built-up areas expand rapidly, particularly when growth is unplanned. This study underscores the importance of sustainable urban planning that integrates the protection and conservation of Dakar’s vegetation to preserve vital ecosystem services. Full article
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<p>Location map of the study area.</p>
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<p>Flowchart of processing Landsat data.</p>
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<p>Land cover classes of Dakar from 1990 (<b>A</b>) and 2002 (<b>B</b>).</p>
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<p>Land cover classes of Dakar from 2012 (<b>A</b>) and 2022 (<b>B</b>).</p>
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<p>Percentage of land use types in the city of Dakar from 1990 to 2022.</p>
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<p>Land use/cover change in Dakar from 1990 to 2002 (<b>A</b>), from 2002 to 2012 (<b>B</b>) and from 2012 to 2022 (<b>C</b>).</p>
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<p>Photos illustrating the fragmentation of green spaces in Dakar: (<b>A</b>) motorway crossing the Mbao Classified Forest and (<b>B</b>) buildings located in Hann Forest and Zoological Park.</p>
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21 pages, 4737 KiB  
Article
Duodenum and Caecum Microbial Shift Modulates Immune and Antioxidant Response Through Energy Homeostasis in Hu Sheep Fed Vegetable Waste and Rice Straw Silage
by Muhammad Hammad Zafar, Chuang Li, Zhiqi Lu, Yue Lu, Zhenbin Zhang, Ruxin Qi, Usman Nazir, Kailun Yang and Mengzhi Wang
Antioxidants 2024, 13(12), 1546; https://doi.org/10.3390/antiox13121546 - 17 Dec 2024
Viewed by 612
Abstract
The gradual decline in feed resources for livestock needs alternate ways to ensure non-stop feed supply throughout the year. The objective of this study was to evaluate the impact of vegetable waste and rice straw silage (VTRS) on immune response, antioxidant status, and [...] Read more.
The gradual decline in feed resources for livestock needs alternate ways to ensure non-stop feed supply throughout the year. The objective of this study was to evaluate the impact of vegetable waste and rice straw silage (VTRS) on immune response, antioxidant status, and microbial changes in duodenum and caecum in Hu sheep. Eight healthy male Hu sheep were randomly distributed into control (fed farm roughage) and VTRS (fed vegetable waste silage) groups for 35 days. Results had shown that silage had less mycotoxin content (p < 0.05). The VTRS increased butyrate content in duodenal digesta, while acetate, butyrate, total volatile fatty acids (TVFA), and valerate were enhanced in caecal digesta (p < 0.05). The VTRS also increased amylase activity in duodenum and ileum tissues, along with GLUT2 and SGLT1 expressions. In serum, Interleukin-10 (IL-10) concentration and total antioxidant capacity (T-AOC) were increased while malondialdehyde (MDA) was decreased. An increase in T-AOC and GSH-Px activity was also observed, along with increased IL-6, immunoglobulin A (IgA), and catalase in duodenum tissue (p < 0.05). Prevotella was increased in the duodenum and caecum, with Prevotellacae UCG-001 and Christensenellacae R-7 group representing the VTRS group in the duodenum (p < 0.05). KEGG pathway prediction also indicated the enrichment of energy metabolism-related pathways. Significant microbes had shown a significant correlation with immune parameters. It can be concluded that vegetable waste silage has the ability to improve antioxidant status, enhance energy metabolism, and balance intestinal microbiota in Hu sheep. Full article
(This article belongs to the Topic Feeding Livestock for Health Improvement)
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Graphical abstract

Graphical abstract
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<p>Schematic diagram showing outline of experiment.</p>
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<p>Fungal microbial structure in experimental diets: (<b>A</b>) PCoA plot showing beta diversity. (<b>B</b>) Species accumulation curve. (<b>C</b>) Comparison of top two phyla among groups. (<b>D</b>) Differential analysis of microbial communities at genus level. (<b>E</b>) Functional enrichment analysis showing differences among the groups. “*” on the bars shows significant difference among the groups.</p>
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<p>Bacterial diversity and phylum comparison among dietary groups in duodenum and caecum. (<b>A</b>) PCoA plot showing beta diversity for microbiota in duodenum. (<b>B</b>) PCoA plot showing beta diversity for microbiota in caecum. (<b>C</b>) Species accumulation curve showing distribution of species in duodenum. (<b>D</b>) Comparison of most abundant phyla in duodenum. (<b>E</b>) Comparison of most abundant phyla in caecum. (<b>F</b>) Species accumulation curve showing distribution of species in caecum.</p>
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<p>Differences in microbial communities of duodenum and caecum: (<b>A</b>) Differential analysis of microbial communities at phylum level in duodenum. (<b>B</b>) LeFSe analysis showing biomarkers at genus level in duodenum. (<b>C</b>) Cladogram showing differences at all taxonomic levels among the groups. (<b>D</b>) Differential analysis of microbial communities at phylum level in duodenum. (<b>E</b>) LeFSe analysis showing biomarkers at genus level in caecum. (<b>F</b>) Cladogram showing differences at all taxonomic levels among the groups in caecum.</p>
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<p>Differences in metabolic pathways enrichment among dietary treatments and correlation analysis between significant microbial communities and metabolic pathways: (<b>A</b>) Differential analysis of metabolic pathways in duodenum. (<b>B</b>) Correlation between significant microbial communities and metabolic pathways in duodenum. (<b>C</b>) Differential analysis of metabolic pathways in caecum. (<b>D</b>) Correlation between significant microbial communities and metabolic pathways in caecum.</p>
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<p>Redundancy analysis (RDA) and correlation network: (<b>A</b>) RDA analysis showing association between duodenal microbial communities and VFAs; (<b>B</b>) RDA analysis showing association between cecal microbial communities and VFAs; (<b>C</b>) Spearman correlation network between significant intestinal microbes and significant immune indices. Blue lines show significant positive correlations (<span class="html-italic">p</span> &lt; 0.05; r &gt; 0.75), and red lines represent significant negative correlations (<span class="html-italic">p</span> &lt; 0.05; r &lt; −0.75).</p>
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17 pages, 9580 KiB  
Technical Note
Detection of the Contribution of Vegetation Change to Global Net Primary Productivity: A Satellite Perspective
by Xiaoqing Hu, Huihui Feng, Yingying Tang, Shu Wang, Shihan Wang, Wei Wang and Jixian Huang
Remote Sens. 2024, 16(24), 4692; https://doi.org/10.3390/rs16244692 - 16 Dec 2024
Viewed by 572
Abstract
Exploring NPP changes and their corresponding drivers is significant for the achievement of sustainable ecosystem management and in addressing climate change. This study aimed to explore the spatiotemporal variation in NPP and analyze the effects of vegetation and climate change on the global [...] Read more.
Exploring NPP changes and their corresponding drivers is significant for the achievement of sustainable ecosystem management and in addressing climate change. This study aimed to explore the spatiotemporal variation in NPP and analyze the effects of vegetation and climate change on the global NPP from 2003 to 2020. Methodologically, the Theil–Sen and Mann–Kendall methods were used to study the spatiotemporal characteristics of global NPP change. Moreover, a ridge regression model was built by selecting the vegetation indicators of the leaf area index (LAI) and fraction vegetation coverage (FVC) and the climate factors of CO2, shortwave downward solar radiation (Rsd), precipitation (P), and temperature (T). Then, the relative contributions of each factor were evaluated. The results showed that, over the previous two decades, the global mean NPP reached 503.43 g C m−2 yr−1, with a fluctuating upward trend of 1.52 g C m−2 yr−1. The regions with a significant increase in NPP (9.22 g C m−2 yr−1) were mainly located in Central Africa, while the regions with decreasing NPP (−3.21 g C m−2 yr−1) were primarily in the Amazon Rainforest in northern South America. Additionally, CO2, the LAI, and the FVC exhibited positive contributions to the NPP trend, with the predominant factors being CO2 (relative contribution of 32.22%) and the LAI (relative contribution of 21.96%). In contrast, the contributions of Rsd and precipitation were relatively low (<10%). In addition, the contributions varied at different land cover and climate zone scales. The CO2, LAI, FVC, and temperature were the predominant factors affecting NPP across the vegetation types. At the scale of climate zones, CO2 was the predominant factor influencing changes in vegetation NPP. As the climate gradually transitioned towards temperate and cold regions, the contribution of the LAI to NPP increased. The findings of this study help to clarify the effects of vegetation and climate change on the ecosystem, providing theoretical support for ecological environmental protection and other related initiatives. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>Spatial distribution of average global NPP from 2003 to 2020 (g C m<sup>−2</sup> yr<sup>−1</sup>).</p>
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<p>Response characteristics of NPP to various vegetation types and climate zones.</p>
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<p>The global NPP’s interannual variation.</p>
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<p>Spatial distribution of global NPP trends (“+” indicates significance at <span class="html-italic">p</span> &lt; 0.05, with unit of g C m<sup>−2</sup> yr<sup>−1</sup>) and the percentage of areas showing increasing or decreasing trends.</p>
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<p>Year-to-year comparison of NPP simulations and observations during 2003 to 2020.</p>
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<p>A scatterplot of the observed and simulated NPP values from 2003 to 2020.</p>
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<p>The mean absolute values of the relative contributions of the driving factors to NPP.</p>
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<p>The percentages of areas with positive and negative contributions.</p>
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<p>The distribution characteristics of each factor’s relative contribution to NPP in spatial terms: (<b>a</b>) LAI; (<b>b</b>) FVC; (<b>c</b>) CO<sub>2</sub>; (<b>d</b>) R<sub>sd</sub>; (<b>e</b>) P; (<b>f</b>) T.</p>
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<p>The mean absolute values of the relative contributions of the driving factors to NPP variation across different vegetation types.</p>
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<p>The mean absolute values of the relative contributions of the driving factors to NPP variation in different climatic zones.</p>
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