Search Results (112)

Severe soil salinization and low fertility significantly constrain sustainable agricultural development in the Yellow River Delta, one of the three major estuarine deltas in China. Despite their ecological importance, the regional-scale spatial interactions between soil salinity and nutrients, particularly regarding their vertical variability, remain poorly understood. This study analyzed 228 soil samples from 76 sites distributed across a distinct salinity gradient, which was determined by constructing a spatial salinity distribution map after sampling. Samples were collected at three depths (0–15, 15–30, and 30–45 cm) to investigate the spatial distribution of soil organic carbon (SOC), total nitrogen (TN), and the C/N ratio, along with their underlying driving factors. SOC and TN exhibited similar spatial patterns, with higher values distributed along both banks of the Yellow River. Horizontally, SOC and TN in the 0–15 cm layer decreased gradually from west to east, whereas the 15–30 cm and 30–45 cm layers showed an opposite trend, increasing eastward. Vertically, SOC and TN contents declined significantly with soil depth (p < 0.05), although the magnitude of this decline varied regionally: the 0–15 cm layer in the western area contained markedly higher nutrient levels than deeper layers, while vertical variation was less pronounced in the eastern and estuarine regions. Both variables were positively associated with total phosphorus (TP), available potassium (AK), soil moisture content (MC), clay content, and pH, but negatively correlated with electrical conductivity (EC), particularly in the 0–15 cm layer. Our results highlight that soil texture, moisture, and salinity affect the spatial heterogeneity and vertical decline of SOC and TN in the Yellow River Delta. Future research should focus on the long-term temporal distribution of the coupling of multiple elements under changing hydrological and salinity regimes. Full article

Larval fish assemblages provide critical insights into reproductive dynamics, biodiversity baselines, and ecosystem resilience, yet remain poorly documented in the Colombian Pacific. This study analyzed ichthyoplankton diversity and spatial turnover across six neritic localities sampled between 2008 and 2022. Standardized plankton tows yielded 43,277 larvae representing 291 morphospecies, 150 genera, 66 families, and 38 orders. The richness observed accounts for ~34% of fish species listed for the Eastern Tropical Pacific and 15% of adult bony fishes reported for the Colombian Pacific, exceeding previous records. Diversity patterns revealed pronounced spatial heterogeneity: Cupica emerged as a biodiversity hotspot, Pizarro and Tortugas were dominated by few taxa, and Sanquianga exhibited high evenness despite moderate richness. Beta diversity analyses indicated turnover exceeding 60% and dissimilarity surpassing 70%, underscoring strong locality identity shaped by oceanographic gradients, geomorphology, and estuarine dynamics. Dominance patterns highlighted contrasting ecological strategies, with cosmopolitan taxa such as Cetengraulis mysticetus coexisting alongside habitat-restricted species of Labrisomus. These findings establish the Colombian Pacific neritic zone as a reservoir of genetic and functional diversity, with high richness and turnover reinforcing its role in sustaining ecosystem functioning and fisheries productivity. Methodological handicaps—including reliance on morphology-based identification, formalin preservation limiting molecular analyses, and uneven temporal coverage—constrain taxonomic resolution, yet the ecological patterns observed provide a robust foundation for conservation planning. Future research integrating molecular tools, trait-based approaches, and long-term monitoring will be essential to refine diversity estimates and strengthen adaptive management under scenarios of climate variability and increasing anthropogenic pressures in the Eastern Tropical Pacific. Full article

Urban rivers face increasing degradation from wastewater, runoff, and land-use change, yet multi-season tropical estuarine datasets remain scarce. This study compared physicochemical water quality, metals, and salinity dynamics over one year in the Juan Díaz and Pacora rivers, two contrastingly urbanized Panama Bay watersheds. Juan Díaz showed higher nutrient concentrations, lower dissolved oxygen, and greater variability than Pacora. Dissolved oxygen in Juan Díaz fell below 5 mg/L in five of nine campaigns and ammonia nitrogen exceeded 3.7 mg/L in all three dry-season campaigns, versus two of seven campaigns below 5 mg/L in Pacora. Total dissolved solids exceeded 500 mg/L in four of nine Juan Díaz campaigns, all in the wet season, but stayed compliant in Pacora. Total nitrogen and total phosphorus were up to 10-fold and seven-fold higher, respectively, in Juan Díaz during the dry season. Cu exceeded its USEPA criterion in two of three detections; Cd was detected once, in Juan Díaz, below its saltwater criterion (0.0079 mg/L). Salinity confirmed stronger tidal influence in Juan Díaz (up to 24.7 g/kg) than Pacora (0.03–2.74 g/kg). PCA separated the two rivers along a nutrient–oxygen gradient explaining 53.6% of variance. Overall, Juan Díaz shows greater degradation, while Pacora remains less contaminated but requires continued monitoring amid rapid urbanization. Full article

Protected estuaries provide reference conditions for assessing coastal biodiversity, but information on swimming crab assemblages in such systems remains limited. This study evaluated the composition, dominance structure, diversity, body size, and spatio-seasonal variation in Callinectes swimming crab assemblages in the Una do Prelado River estuary, within the Barra do Una Sustainable Development Reserve, south-eastern Brazil. Seasonal sampling was conducted at four sites along the estuarine gradient using baited traps. Species composition, abundance, diversity indices and multivariate patterns were analyzed in relation to site and climatic season. A total of 146 individuals from four species were recorded: Callinectes exasperatus, C. danae, C. sapidus and C. bocourti. The assemblage was strongly dominated by C. exasperatus, which represented 81.5% of the total catch. Species richness was low, consistent with the restricted taxonomic scope and environmental filtering expected in estuaries. Abundance varied more clearly than species composition, with higher catches in autumn and at the intermediate estuarine site. Diversity indices indicated low evenness where C. exasperatus was dominant, whereas multivariate analyses detected no significant compositional differences among sites or seasons. As the first study conducted in this protected estuary, our findings provide a baseline for future monitoring of this system. Given the spatial and temporal scope of the study, these results should not be generalized to other protected estuarine systems. Full article

The Jobos Bay National Estuarine Research Reserve (JBNERR) includes the largest bay on the southern coast of Puerto Rico. The reserve includes diverse habitats ranging from mangrove forests, shallow lagoons, seagrass beds, cays and coral reefs, with a broad range of environmental gradients between the populated coastal plain and the oligotrophic Caribbean Sea. As the only research reserve in the region, resource managers seek cost-effective and reliable processes to restore and promote ecosystem health in the reserve. Benthic foraminiferal assemblages are widely applied bioindicators for assessing coastal environments, notably coral reefs and seagrass ecosystems. This study evaluated the applicability of three indices, the FoRAM Index (FI), the Epiphytic FoRAM Index (FI′), and the Long vs. Short Life-Span Index (I_LS), to assess bayside and reef habitats bordering three cays of Jobos Bay. Surficial sediment samples were collected in 2018 and 2019. Environmental data included sediment composition (e.g., texture, total organic content) and water quality (e.g., nutrients and pH). From a total of 57 samples, 4671 individuals were counted, representing 35 genera. Cluster analysis based on genus-level relative abundances revealed four main groups: Dominant (>10%), Common (5–10%), Occasional (1–4%), and Rare (<1%). Dominant genera included Quinqueloculina (24%) and Amphistegina (18%). Common taxa included smaller rotaliids such as Rotorbinella (6%) and miliolids such as Pyrgo (5%). Twelve genera were occasional, including Triloculina (4%) and Elphidium (3%). Tests of 16 genera occurred rarely (<1%), including agglutinated taxa such as Textularia and stress-tolerant forms like Bolivina. In total, FI values ranged from 1.3 to 9.6, FI′ from 1.9 to 9.7, and I_LS from 0.5 to 30.6. Bayside samples scored generally lower compared to reef samples. In summary, foraminiferal assemblages and associated bioindices indicated that environmental conditions supported Foraminifera that host algal symbionts in the reef environments and the prevalence of macroalgae and seagrass in the bayside benthos. Full article

Suspended sediment concentration (SSC) is a critical proxy for coastal water quality, geomorphological evolution, and biogeochemical cycles. In shallow macro-tidal embayments like Sanmen Bay (SMB), China, surface SSC exhibits highly dynamic spatiotemporal variations driven by intense, multi-scale tidal forcing. Using Sentinel-2 MSI imagery processed with the ACOLITE Dark Spectrum Fitting (DSF) algorithm, this study reconstructs the spatial distribution of surface SSC across the embayment. We then introduce the normalized Suspended Sediment Concentration Asymmetry Index ($A_{ssc}$) to quantitatively diagnose asymmetrical sediment responses across spring–neap and flood–ebb cycles. The results reveal a spatially divergent, dual-control mechanism governing sediment transport across the embayment’s hydro-geomorphic gradients. Quantitative trend-surface fittings and stratified regressions demonstrate that net sediment transport in deep bedrock channels is primarily governed by tidal pumping. Conversely, sediment dynamics on intertidal mudflats and shallow subtidal shoals are modulated by geomorphic resistance, exhibiting high morphodynamic sensitivity to minute water depth variations. By bridging process-based estuarine tidal theory with discrete satellite observations, this reproducible framework transforms multi-temporal remote sensing snapshots into spatially continuous diagnostics, providing a practical decision-support paradigm for coastal engineering and ecosystem management in dynamically analogous macro-tidal environments. Full article

Large-scale fishing bans are increasingly implemented to restore aquatic ecosystems, yet their effects on lower trophic levels remain poorly understood. As one of the world’s largest estuarine systems, the Yangtze River Estuary has been subjected to a ten-year fishing ban since 2021, providing a unique opportunity to potentially examine the response of plankton community to reduced fishing pressure along a steep salinity–nutrient gradient. This study relies on one-off environmental and plankton field surveys conducted in autumn 2024 (a sampling instead of multi-year time-series monitoring), we applied redundancy analysis, Mantel tests, and threshold indicator taxa analysis to tentatively clarify the roles of nutrients and salinity in structuring post-ban plankton communities. Species richness may have increased substantially compared with pre-ban levels, but community evenness declined and the dominance of Skeletonema costatum could have intensified, revealing a possible non-equilibrium recovery pattern. Zooplankton density increased substantially, which may not be fully consistent with the expectation under a simple top-down release scenario. Threshold analysis showed that S. costatum exhibited bidirectional responses to dissolved inorganic nitrogen and phosphate, with its positive response thresholds matching ambient nutrient concentrations in the inner estuary; this discrepancy is only a plausible inference since we lack direct measurements of fish predation and zooplankton grazing rates to verify causal trophic interactions. Our findings suggest that bottom-up forces driven by persistent eutrophication remain the dominant control on plankton community structure three years after the ban. From a watershed management perspective, our observational results provide a tentative implication that substantial reductions in nutrient loading might be required to mitigate unbalanced plankton community recovery; otherwise, the structural integrity of plankton assemblages could lag far behind the recovery of species richness under the current eutrophic background. Full article

Hypoxia and salinization increasingly co-occur in freshwater and estuarine ecosystems, yet their combined effects under fluctuating oxygen regimes remain poorly resolved. We experimentally quantified survival responses of four planktonic crustaceans (Daphnia magna, Daphnia longispina, Eurytemora velox, and Thermocyclops crassus) along a salinity gradient expressed as conductivity (0.6–7.7 mS cm⁻¹) under two oxygen regimes: sustained hypoxia and repeated short-term hypoxia over 120 h, under standardized food-deprived conditions to isolate abiotic stress effects. Under sustained hypoxia, survival declined monotonically with decreasing oxygen in all species, with marked interspecific differences at ≤2 mg L⁻¹. Under fluctuating oxygen conditions, survival peaked at low to intermediate salinity and declined sharply at elevated salinity, indicating a strong combined effect of oxygen limitation and salinity-related stress. Multivariate analysis identified a significant salinity × oxygen interaction, indicating that the effect of oxygen depletion on survival depended on salinity. Daphnia magna showed the highest tolerance, whereas D. longispina and E. velox were highly sensitive to elevated salinity; T. crassus showed intermediate tolerance. These results indicate that elevated salinity is associated with negative effects under both sustained and episodic hypoxia and that fluctuating oxygen regimes elicit strong combined stress responses. Our findings highlight the importance of combined abiotic stress effects when predicting zooplankton responses in oxygen-depleted and salinizing aquatic ecosystems. Full article

The Amazon coastal zone exhibits remarkable habitat diversity and species richness, with nutrient-rich estuaries playing a crucial role in local food webs and supporting fish and other aquatic organisms. To examine the distribution of fish larvae and juveniles in the Taperaçu Estuary and their relationship with environmental variables, monthly sampling was conducted at two fixed stations in 2008. Samples were collected during flood and ebb spring tides using 500 μm mesh nets. In situ measurements of salinity, temperature, and dissolved oxygen were recorded, while pH and turbidity were determined in the laboratory. Abiotic variables did not differ significantly between tides, but salinity and dissolved oxygen were higher during the dry season. A total of 5175 individuals were identified, representing 17 families and 37 species. The ichthyoplankton community was dominated by Rhinosardinia amazonica, Anchovia clupeoides, Stellifer stellifer, and Microgobius meeki. Stations 1 and 2 showed differing abundance ranges, with higher values at station 1 during the rainy season. Preflexion stages were abundant at both stations, indicating the estuary’s importance as a nursery and development area for several fish species. Multivariate analyses revealed spatial and seasonal structuring of larval assemblages along the estuarine gradient, driven primarily by salinity, temperature, and turbidity. Our results emphasize the role of upper estuary sectors of eastern Amazonia as areas of spawning, larval development, and subsequent juvenile settlement, contributing to the dispersal of fish species throughout the estuary and adjacent coastal environments. The present findings also reinforce the ecological value of the studied Extractive Reserve and other protected areas along the Amazon littoral as essential habitats for larval refuge and development. The need for continued monitoring and preservation of these protected zones is evident. Full article

This study investigated the spatial distribution, seasonal variation, and drivers of surface seawater alkalinity (Alk) in Zhanjiang Bay (ZJB) using high-frequency seasonal sampling in the summers and winters of 2023. Surface Alk ranged from 525.3 to 2213.3 μmol·L⁻¹, with mean values of 1373.1 ± 420.9 μmol·L⁻¹ (summer, n = 28) and 1612.3 ± 343.7 μmol·L⁻¹ (winter, n = 20). Spatially, Alk increased progressively from the estuary to the inner bay and further to the bay mouth, reflecting a typical dilution gradient. Correlation analyses showed that summer Alk was positively correlated with salinity (ρ = 0.706, p < 0.001), indicating that salinity changes associated with conservative mixing were a dominant control, whereas the weaker winter correlation (ρ = 0.473, p < 0.001) suggested that biological processes may play a more important role. Tidal forcing was significantly associated with diurnal Alk variations, particularly in the estuary and inner bay. In the estuary, high Alk occurred during high tide, consistent with tidal mixing; in the inner bay, elevated Alk was observed during low tide, suggesting a possible tidal pumping effect. These findings provide baseline data on Alk dynamics in a subtropical estuarine bay and contribute to understanding the carbonate system and buffering capacity in similar coastal systems. However, because measurements of dissolved inorganic carbon and pCO₂ were unavailable, a quantitative assessment of carbon sink capacity requires further investigation. Full article

This study develops an integrated framework combining emergy analysis, carbon footprint accounting, and long short-term memory neural network modeling to investigate the effects of nature-based solutions on coastal ecosystem services and blue carbon functions from the perspective of river–coast connectivity. Three transects along a connectivity gradient were established in the Yellow River Delta, a typical large river delta in temperate China, covering riparian zones, estuarine transition areas, intertidal wetlands, and seagrass beds, with multi-source data collected over three consecutive hydrological years. Emergy–carbon coupling analysis based on this case study indicates that the high-connectivity transect shows a higher emergy yield ratio and net carbon sink compared to the low-connectivity transect, with salt marshes being most sensitive to connectivity change. Threshold analysis, specific to this delta, identifies a three-phase response pattern of carbon burial rate with increasing sediment connectivity, and reveals that wave attenuation efficiency declines notably when hydrological connectivity falls below approximately 0.5, although this value may vary across different coastal settings. A higher sea level rise rate raises the critical connectivity level required to maintain carbon sink function. The long short-term memory neural network trained on observational data achieves better prediction accuracy for blue carbon accumulation rates than traditional statistical methods, and SHAP value analysis suggests the possible existence of synergistic effects among connectivity dimensions. Based on these findings, three optimization strategies including tiered restoration, a dynamic pathway, and spatial configuration are proposed as case-specific recommendations for the Yellow River Delta. Framework-based simulations indicate the potential for connectivity-informed strategy adjustments to improve restoration efficiency under local conditions. This study concludes that river–coast connectivity represents an important lever regulating the ecological benefits of nature-based solutions, but emphasizes that all quantitative thresholds and benefit magnitudes reported here are case-specific estimates that require recalibration when applied to other coastal systems. Full article

Understanding the internal translocation of sodium (Na) and potassium (K) within the soil–plant continuum is crucial for elucidating their mechanistic roles in plant growth adaptation. We investigated these processes in the Suaeda salsa across a natural salinity gradient in the Yellow River Delta coastal wetlands. Using field surveys, we quantified Na and K enrichment and translocation coefficients among soil, roots, stems, and leaves. The correlation analysis and Random Forest modeling were then employed to identify the key drivers linking these ion dynamics to plant morphological traits (height, density, biomass). Results revealed a pronounced Na compartmentalization, with leaves acting as the primary sink (enrichment coefficient = 5.62), exhibiting values 4.68- and 3.81-fold higher than roots and stems, respectively. In contrast, K enrichment levels remained relatively stable across plant organs (roots: 0.50; stems: 0.57; and leaves: 0.62). Internal Na⁺ loading in stems and leaves positively correlated with leaf Na enrichment. Conversely, high soil Na suppressed both leaf Na enrichment and stem-to-leaf K translocation, while elevated soil K reduced K enrichment in all organs and soil-to-root Na translocation. Critically, plant height was negatively correlated with Na-K enrichment coefficients in all organs. Population density and biomass were specifically linked to stem-related Na dynamics (stem-leaf Na translocation and stem Na enrichment), with K translocation showing no significant relationship. The Random Forest model identified the stem K enrichment coefficient, leaf K content and its enrichment coefficient, and stem Na content as the most influential coefficients governing plant growth (relative importance: 6.37~12.82%). We conclude that the growth adaptation of S. salsa in this coastal ecosystem is driven by a synergistic yet organ-specific regulation of Na and K translocation and homeostasis. These findings provide a mechanistic physiological basis for informing ecological restoration strategies of S. salsa wetlands and support the sustainable management of estuarine ecosystems. Full article

Understanding habitat use and connectivity in estuarine fishes is essential for effective conservation and management. In this study, otolith microchemistry was applied to investigate habitat use and connectivity of the estuarine catfish Genidens genidens across three estuaries in southeastern Brazil. A total of 58 individuals were analyzed using laser ablation inductively coupled plasma mass spectrometry, focusing on strontium-to-calcium (Sr:Ca) and barium-to-calcium (Ba:Ca) ratios. Variations in elemental ratios along otolith transects were used to infer individual ontogenetic patterns along the estuarine–marine gradient. Most individuals exhibited combined use of estuarine and marine environments, while trajectories restricted to freshwater were rare. The apparent complexity of chemical profiles tended to increase with age; however, this pattern disappeared after correction for size-related bias, suggesting that age itself did not significantly influence habitat-use transitions. These patterns are consistent with ecological plasticity and partial migration within populations of G. genidens, although they may also reflect exposure to variable environmental conditions. Sr:Ca ratios were useful indicators of salinity-related transitions, whereas Ba:Ca ratios provided complementary information associated with continental influence. Overall, this study highlights the applicability of otolith microchemistry for investigating habitat-use patterns in estuarine fishes and reinforces the ecological importance of estuaries for feeding, growth, and recruitment in G. genidens, while acknowledging inherent limitations related to environmental variability and proxy interpretation. Full article

Tidal-scale wave modulation is a critical yet complex process in macro-tidal estuaries. This study investigates semidiurnal wave modulations in the Changjiang River Estuary (CRE) using unique, long-term in situ observations and high-resolution ADCIRC–SWAN coupled simulations. Pronounced semidiurnal signals are identified in significant wave height (H_s), mean wave period, and wave direction. Observational results demonstrate that the modulation intensity is highest in Hangzhou Bay and the CRE mouth, decreasing gradually offshore. A key finding is that semidiurnal H_s maxima systematically coincide with peak flood currents and precede high water by approximately three hours. Long-term records confirm that this modulation persists year-round and intensifies during energetic events such as typhoons. The expression of the tidal signal depends on wave composition: wind-sea-dominated conditions exhibit stronger period modulation, whereas swell-dominated conditions favor coherent H_s modulation as kinematic tidal effects remain more apparent in the absence of strong local wind forcing. Numerical sensitivity experiments demonstrate that tidal currents are the primary driver of the observed wave modulation, while water-level effects are largely confined to shallow shoals. The results highlight that accurately reproducing the observed frequency–directional structure requires the inclusion of current-induced Doppler shifts and refraction. Beyond the classical following-current effects, the analysis suggests that the spatial deceleration of currents along the wave path acts as a kinematic trap that focuses wave action and sustains H_s intensification. This mechanism provides a physically plausible explanation for the observed phase relationship and points to the non-local nature of estuarine wave dynamics, where the wave state appears as an integrated response to cumulative current gradients along the propagation path. These findings emphasize the necessity of incorporating wave–current coupling in future coastal modeling and hazard forecasting. Full article

Latitudinal gradients are widely recognized as a key macro-environmental driver shaping microbial biogeographic patterns; however, the spatial organization of sediment archaeal communities in estuarine ecosystems and the mechanisms underlying their assembly remain insufficiently understood. This study is based on sediment samples collected from three representative estuarine regions spanning distinct latitudes along the Chinese coastline—the North China Sea (NCS), East China Sea (ECS), and South China Sea (SCS). Based on 16S rRNA high-throughput sequencing, combined with null-model inference and molecular ecological network (MEN) analyses, we characterized latitudinal patterns in archaeal community distributions, assembly processes, and cross-regional interaction architectures. The results showed that archaeal communities exhibited obvious spatial segregation across three regions, with both community richness and network complexity increasing significantly toward lower latitudes. Nitrate (NO₃⁻), ferric iron (Fe³⁺), and dissolved oxygen (DO) were identified as key environmental factors governing archaeal community structure. Notably, archaeal community assembly processes exhibited a clear latitudinal gradient: deterministic processes, particularly environmental filtering, were more obvious at lower latitudes, whereas the contributions of stochastic processes—including dispersal limitation and ecological drift—increased markedly at higher latitudes. A MEN analysis further revealed that archaeal networks at lower latitudes exhibited higher connectivity, modularity, and stability, suggesting that interspecific interactions may enhance ecosystem resistance to environmental disturbance under more stable environmental conditions. Overall, this study demonstrates that macro-environmental gradients jointly shape archaeal biogeographic patterns via multiple pathways, including modulation of environmental filtering, dispersal dynamics, and cross-regional interactions. These findings deepened our understanding of the stable mechanisms governing the diversity and biogeographical distribution of archaea in estuarine systems. Full article